NTS 104 A/4 W TRIM 104A.001 LAT. 56 06' 00” N

LONG. 130 04' 00” W

GEOLOGICAL, AND DIAMOND DRILLING REPORT on the

MC ROCK OF AGES, AZTEC, ALPINE Au-Ag-Cu (Pb-Zn) PROJECT

Mount Shorty Stevenson, Stewart, B.C.

SKEENA MINING DIVISION

for

Reliant Gold Corp., Suite 500-360 Bay Street,

Toronto, ON M5H 2S8

by

Trevor Boyd, P.Geo. 148 Lascelles Blvd.

Toronto, Ontario M5P 2E6

December 5, 2011

SUMMARY The MC1 and MC2 claims are located on Bear River Ridge about 10 km north of Stewart, B.C The MC1 and MC2 claims are registered to William E. Pfaffenberger (president, Fundamental Res Corp). By letter of agreement with Fundamental Res Corp, REC Minerals Corp has committed to a schedule of due diligence (fieldwork and technical reporting), and issuance of shares to Fundamental Resources Corp in order to obtain 100% interest in the claims. The MC1 and MC2 claims covers an area of 903.31 hectares. Intrusive activity in the Stewart area has been marked by the Lower and Middle Jurassic Texas Creek granodiorite with which the Big Missouri, Silbak Premier, SB, Scottie Gold, Red Mountain and many other mineral deposits in the district are associated. Younger intrusions include the Hyder Quartz Monzonite, Bitter Creek granodiorite and many Eocene stocks, dykes and sills which form a large part of the Coast Mountain Plutonic Complex. Mineral deposits such as Kitsault Lime Creek Molybdenum, Porter-Idaho Silver Mine, and a host of other deposits are related to the 48-52 Ma (Eocene) plutons. These intrusives also form the regionally extensive Portland Canal Dyke Swarm. A gold-silver-zinc bearing quartz-sulphide vein system hosted in volcanic-sedimentary rocks was drill tested in the Rock of Ages #3 Vein Zone and was found to defines wide down-hole sections of moderately elevated polymetallic values. Sulphides consist of near totally of disseminated pyrite ranging from 2 up to 20% with minor <2% sphalerite and trace chalcopyrite. The showing is aligned along a prospective northwesterly trend for approximately 1,200 metres which includes the Rock of Ages #2, Dalhousie, and Cairn showings. The drilling encountered hydrothermally altered sericite-chlorite-carbonate-sulphide rich volcanic and sedimentary rocks throughout most of the core and specifically in multiple sections varying in down-hole lengths ranging from 25 up to 210 metres. Multiple narrow sections consisting of feldspar-quartz porphyry intrusive were also indentified in the core associated with the altered rocks and an increase in the sulphide concentration. The zone continues south-southwest and future work should be expanded and directed towards exploring the Dalhousie and Rock of Ages No 2 and Cairn showings along the favourable trend. The close proximity to Bear River and Highway 37A and a mill facility at Premier are important factors in future development of the quartz-sulphide veins located on the MC Dalhousie claims The MC claim group has potential to host an economic gold-silver deposit. The MC claims requires further exploration in the Ice, Rock of Ages (No 2 and No 3 Vein Zones) and Cairn showings located at 800-1,550 meters (2,624-5,084 feet) elevation in the east to central portion of MC1 mineral tenure. A program of follow-up drilling is recommended to test for minable widths of high grade base and precious metal bearing mineralization. .

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TABLE OF CONTENTS Page Number Summary 2 1.0 Introduction 5 2.0 Location, Access, and Physiography 5 3.0 Property Status 5 4.0 Area History 6 5.0 MC Property History 7 6.0 General Geology 15 7.0 Fieldwork 16 7.1 Methods and Procedures 16 7.2 Property Geology 17 7.3 Property Mineralization and Alteration 19 7.4 Drill Core and Rock Chip Sample Geochemistry 19 8.0 Discussion of Results 20 9.0 Conclusion and Recommendations 21 References 22 Statement of Qualifications 23 Itemized Cost Statement 24

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LIST OF FIGURES FIG. 1 GENERAL AND CLAIM LOCATION MAP FIG. 2 MC CLAIMS GENERAL GEOLOGY (Source: BCGS, Map Place BC) FIG. 3 GOOGLE EARTH VIEW OF BEAR R RIDGE (No 1, 2 & 3 Veins marked) FIG. 4 TOPOGRAPHY, PROPERTY BOUNDARY AND MINERAL SHOWINGS MAP FIG. 5 ROCK OF AGES No 3 VEIN, DRILL HOLE PLAN MAP FIG. 6 AZTEC SHOWING, ROCK CHIP SAMPLE LOCATIONS FIG. 7 ALPINE SHOWING, ROCK CHIP SAMPLE LOCATIONS LIST OF APPENDICIES APPENDIX A- ROCK CHIP SAMPLE LOCATIONS APPENDIX B- DRILL CORE SAMPLE LOCATIONS AND ANALYSES APPENDIX C- DRILL LOGS APPENDIX D- DRILL SECTIONS APPENDIX E- DRILL CORE AND ROCK CHIP GEOCHEMICAL ANALYSIS CERTIFICATES

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1 INTRODUCTION

This report summarizes diamond drilling and rock and prospecting exploration work carried out between July 6 - 28, 2011 on MTO mineral tenure 567077. The purpose of the program was to locate metallic mineralization and interpret the relation between lithology, alteration and potentially economic concentrations of base and precious metal bearing sulphide and oxide mineralization. 2 LOCATION, ACCESS AND PHYSIOGRAPHY The MC claim is located on Bear River Ridge about 10 km north of Stewart, B.C. The claim group (MTO tenure numbers 567077, and 526194) are 2 km E of the Silbak-Premier Mine where a 2,000 tpd mill designed for the recovery of gold and silver is located adjacent to the Silbak-Premier and Big Missourri mines. The MC property is in the Skeena Mining Division NTS 104 A/4 W, latitude 56 06' N, longitude 130 04' W (Fig. 2). Elevations on the claim group range from 150-1950 meters. Slopes are moderate to gentle west of the Bear River Ridge and steep to moderate on the east side of the ridge towards Bear River. The claims are mostly above tree line and support sparse growth of mosses and lichens (i.e. alpine taiga). Recent recession of glacial ice has exposed extensive rock outcrop areas, especially in the vicinity of the arete shaped Mount Shorty Stevenson. The west portion of the claims can be accessed by trails that lead to prospects west of Mount Shorty Stevenson near the headwaters of Cooper Creek. The east portion of the claims can be accessed by crossing the Bear River by boat followed by hiking up steep and exposed bedrock ledges, ramps and cliffs. There are numerous helicopter landing areas above tree line (3,200 foot elevation above sea level), and the Stewart airport is about a nine minute flight.

3. PROPERTY STATUS The MC1 and MC2 claims are registered to William E. Pfaffenberger (president, Fundamental Res Corp). By letter of agreement with Fundamental Res Corp, REC Minerals Corp has committed to a schedule of due diligence (fieldwork and technical reporting), and issuance of shares to Fundamental Res Corp in order to obtain 100% interest in the claims. Details of the mineral claims are as listed in the following table:

Claim Name MTO tenure no.

Hectares

Record Date

Expiry Date

MC1 567077

867.18

Sept 29, 2007

Oct 15, 2014*

MC2 526194

36.13

Jan 25, 2006

Jan 25, 2015*

(*expiry date extension) The MC1 and MC2 claims covers an area of 903.31 hectares Fieldwork carried out by the author in July, 2011 has been filed (BC MEMPR Statement of Work), and credited to the claim group.

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4. AREA HISTORY The Stewart Complex contains numerous mineral deposits that cover an area over 150 km in length and 20-40 km in width extending from Alice Arm (Kitsault) to the lower Iskut River valley. This area is collectively referred to as the "Golden Triangle" or "Stikine Arch". This mineral belt has been recently active because of the discovery of precious and base metal deposits such as: Silbak-Premier, Granduc, Anyox, Porter-Idaho, Dunwell, Eskay Creek, Snip,\Brucejack Lake, Red Mountain, Doc, Big Missouri, Johnny Mountain, Silver Butte, Scottie Gold, Kerr, Rock 'n Roll, Inel, Bonanza, Red Bluff, Golden Wedge, Bear Pass, and Georgie River. All of these properties have been the subject of major exploration and/or development for precious and base metals in the past 20 years. The Stewart area has been exploited for minerals since 1900 when the Red Cliff deposit on Lydden Creek was mined. Since then, approximately 120 base and precious metal deposits within the Stewart mining district have been developed. Total recorded production from the Stewart area is 2,400,000 ounces gold, 40,000,000 ounces silver, and over 100,000,000 pounds copper-lead-zinc. Most of this production came from the Silbak-Premier, operating episodically from 1918 to 1996. The Eskay Creek deposit contains an estimated 4,000,000 ounces gold, 40,000,000 ounces silver and over 100,000,000 pounds copper-lead-zinc. This deposit does not outcrop and eluded discovery despite over 50 years of exploration history on the property. The unique high-grade stratiform 2-60 m wide massive sulphide horizon is remarkable in terms of predictability of its geology and tenor, and its relatively well defined, contact controlled assay boundary. The Red Mountain deposit is a recent discovery at the headwaters of Bitter Creek. Gold bearing sulphides (pyrite, arsenopyrite, chalcopyrite) are localized in a quartz-poor, major shear zone near a Texas Creek plutonic complex feldspar porphyry and Unuk River Fm volcanic contact. Over 2,000,000 tonnes of 0.4 opt Au and 1.0 opt Ag have been outlined by over 150 diamond drill holes. Numerous small scale workings near the MC claims include the Silver Crown, Monitor, Spider, Lois, Sebwacke, Hyder Gold, Dalhousie, Prince John, Big Casino, Independence, Dunwell and Ben Ali. Precious and base metal values occur as veins, and/or replacement, breccia, stockwork in quartz-sulphide gangue. Mineralization consists of sphalerite, galena, chalcopyrite, pyrite, tetrahedrite, arsenopyrite, native gold, and/or various sulphosalts in a gangue of quartz, carbonate, barite, and/or chlorite. Historic work on these showings include underground development, drilling, geological evaluations and prospecting.

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5.0 MC PROPERTY HISTORY From 1921 to 1924 a diamond drilling and trenching program was carried out on the northwest trending, steeply dipping quartz-carbonate veins on a ridge immediately south of Mount Shorty Stevenson. Mineralization consists 5-50% sphalerite-galena with minor pyrite-chalcopyrite, and trace sulphosalts, native silver and/or electrum. Mineralization is spatially related to en echelon west and northwest trending fault structures within or adjacent to quartz-sericite-pyrite (phyllic) alteration. "Bonus" Nick Benkovich discovered this showing in the 1970's and a small shipment of several hundred pounds was sent to Trail, B.C. for custom milling. Material from the shipment was assayed giving the following results:

% Cu % Pb

% Zn

Opt Ag

Opt Au

1.47 35.15

19.18

550.00

0.160

In 1986, Moche Resources flew an airborne VLF-EM and magnetometer geophysical survey. This survey identified 2 well defined (data profiles form bell-shaped curves) 45-64% VLF-EM field strength peaks (i.e. interpreted as conductive zones) located south and east of Mount Shorty Stevenson (DiSpirito, F., Assessment Report # 15,581, 1986). Magnetometer readings varied up to 1,000 gammas, but mag anomalies had little correlation with VLF-EM anomalies. In 1990, Navarre Resource Corp performed diamond drilling, trenching, geological mapping and soil sampling. Work was focused on a 0.5 X 0.2 km, northwest trending quartz-sericite-pyrite (phyllic) alteration zone. This QSP alteration is pervasive some 400 m south of Mount Shorty Stevenson. A trench sample of highly silicified pyritic material from the QSP altered zone returned a value of 6.0 opt Ag over a width of 80 cm. 20 soil samples from a 150 X 300 m area returned average values of over 20.0 ppm Ag and 100 ppb Au. A northwest trending, steeply dipping quartz-sulphide vein is located 100 m south of the QSP alteration. Trenching this vein gave an assay value of 1.35% Pb, 7.56% Zn, 26.14 opt Ag and 0.086 opt Au. A diamond drill was positioned to cut the QSP zone as well as the NW extension of the quartz-sulphide vein, but it was stopped well short of its target depth due to mechanical problems. The 99 meter drill hole intersected high grade sulphides in the final 0.2 m which gave the following results:

From To

Width

% Pb

% Zn

Opt Ag

Opt Au

98.8 m 99.0 m

0.2 m

0.37

9.24

10.02

0.052

In 1992, Navarre Resource Corp found 2 new NW trending, steeply dipping mineralized shear zones with the following assays:

Width % Pb

% Zn

Opt Ag

Opt Au

0.5 m 3.8

9.4

12.0

0.121

0.5 m 23.1

30.6

12.8

0.042

In 1996, Navarre Resource Corp outlined new showings 1.3 km ENE of Mount Shorty

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Stevenson. These showings are adjacent to crown granted claims, which are part of the Dalhousie showings. The Rock of Ages showings are currently within the MC claim and returned the following assay values:

Width % Cu

% Pb

% Zn

Opt Ag

Opt Au

0.3 m 0.06

3.21

6.54

6.48

0.362

0.4 m

0.05

3.50

5.74

7.15

0.364

0.3 m

0.05

2.66

5.69

8.41

0.655

The Rock of Ages showings consist of 5-15% sphalerite-galena with minor pyrite-chalcopyrite in a gangue of quartz-carbonate. The high silver and gold are accountable by the presence of trace amounts of tetrahedrite and/or sulphosalts/electrum. The mineralization occurs in NNW trending, steeply dipping shear zones hosted in andesite/dacite tuff/flow, volcaniclastic, and volcanic breccia. A post ore, 2 meter wide quartz monzonite dyke cuts the andesite/dacite along the shear zone which follows the main creek bed. The Rock of Ages showings that contain the higher precious metal are located between 1,500 to 1,575 meters elevation. The mineralized shears can be traced for 600 meters to 1,200 meters elevation, where a jasper-chalcopyrite-hematite-magnetite-pyrite bearing, high iron (sulphide and oxide) formation which forms a prominent bluff forming scarp feature. Quartz-sericite-pyrite (QSP) alteration is well developed across a 1.0 X 0.3 km. zone (elongated along a northwest trend). This alteration zone is located in the northeast portion of the MC claim between 1,100 to 1,400 meters elevation. QSP is locally abundant between in the 1,100 to 1,400 meter elevation. Adjacent to the QSP alteration, a northwest trending mineralized fault zone is located along Rock of Ages Creek, which contains minor jasper and chalcopyrite with 3-5% disseminated pyrite. Sub-parallel mineralization peripheral to this fault consists of pyrite-chalcopyrite-galena-sphalerite in a gangue of quartz, carbonate, magnetite, and/or jasper. The lower jasper zone (@ 1,200-1,300 m. elevation) contains 3-5% fracture filling pyrite and sparse chalcopyrite. The following results were obtained from stream sediment sampling on the MC claim (1999): SAMPLE # PPM Cu Pb Zn Ag PPB Au 54431 176 41 477 1.2 85 54432 40 29 306 0.4 70 54433 38 92 443 2.2 110 54434 75 101 557 0.6 15 54435 70 32 206 0.6 35 54436 105 51 351 0.4 29 54437 31 127 366 1.2 9 54438 42 206 483 3.5 20 Stream sediment results show that the 3 creeks draining the northeast portion of the claim (close to the old Rock of Ages crown grants) have higher Au values as well as the highest Cu

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value. The central and southern portion of the claim has relatively higher Pb and Ag values which corresponds to the elevated silver values obtained from previous rock and soil geochemical analysis from the Mt. Shorty Stevenson area. Prospecting, trenching, diamond drilling, and soil geochemistry from previous work programs have outlined several veins located east and northeast of Mount Shorty Stevenson. These silver and gold bearing veins occur near a major stratigraphic break between Lower Jurassic and Middle Jurassic volcanics and sediments that are proximal to Jurassic Texas Creek granodiorite intrusive rocks. This unconformity and proximity to the Texas Creek granodiorite are important ore controls of the nearby Silbak-Premier ore which occurs in similar stratigraphy. The strong northwest trending faults east of Mount Shorty Stevenson, that forms Dundee Creek and Dalhousie Creek, cuts Lower Jurassic stratigraphy and the margin of the Texas Creek granodiorite. This fault is a major air photo lineament and is related to pervasive quartz-sericite-pyrite alteration. Geological mapping of Rock of Ages mineral zone on the MC claim (1,300-1,550 m. elev.) confirms gold-silver bearing quartz-sulphide fissure veins which are characterized by weak chlorite-carbonate alteration with adjacent Q-S-P alteration. The Q-S-P alteration is widest and most intense in Dalhousie Creek @ 3,900 foot (1,188.7 m.) elevation and an area 400 meters SE of Mount Shorty Stevenson @ 5,600 feet (1,706.8 m.) elevation (Kikauka, 1993,1994). The Dalhousie Creek Q-S-P forms a highly visible limonite-rich gossan which hosts two distinct precious metal bearing mineral assemblages: 1) Pyrite-chalcopyrite-jasper in quartz-magnetite gangue. 2) pyrite-chalcopyrite-sphalerite-galena in a gangue of quartz-carbonate A Tertiary hornblende porphyry dyke system invades most of these mineral zones which are localized along NW trending shear zones. The dykes appear to be post-mineral and quite often split larger veins in two, e.g. 400 meters SE of Mt. Shorty Stevenson. There are two main zones on the MC claim that were defined by fieldwork carried out in 1996 and 1997: 1) Rock of Ages Creek at 1,300-1,550 m. elevation and 2) High-grade quartz sulphide veins that resemble Silbak-Premier ore which have returned assays up to 0.16 oz/t Au, 505 to 550 oz/t Ag, 1.47% Cu, 35.15% Pb, 19.18% Zn located 200-600 meters southeast of Mount Shorty Stevenson. 2000- Geological mapping was carried out by Fundamental Resources Corp at a scale of 1:5,000 over an area of 1 X 1.5 km in the western portion of the MC claim. This area is steep and ranges from 800' to 3,500' feet in elevation. Geochemical stream sediment sampling was carried out in the east edge of the claim group. Modified contour grids within a 0.1 X 0.75 km area were established in the east portion of MC 2 and the southeast portion of MC to take magnetometer readings. Geological mapping identified Unuk River Formation andesitic and dacitic tuffs and flows in the west portion of the claim. Numerous quartz-sericite alteration zones occur within the Unuk River volcanics. These 50-200 m wide altered zones are bleached white-grey colored

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and occur along northwest trending fault structures. Quartz-sericite-pyrite-clay (QSP) phyllic alteration is well developed across a 1.0 X 0.3 km. zone, located in the northeast portion of the MC claim. QSP is locally abundant between the1,300 to 1,400 meter elevation. Adjacent to the QSP alteration, a northwest trending mineralized fault zone is located along Rock of Ages Creek, which contains minor jasper and chalcopyrite with 3-5% disseminated pyrite. Sub-parallel mineralization peripheral to this fault consists of pyrite-chalcopyrite-galena-sphalerite in a gangue of quartz, carbonate, magnetite, and/or jasper. The lower jasper zone (@ 1,200-1,300 m. elevation) contains 3-5% fracture filling pyrite and sparse chalcopyrite. The southeast extension of the NW trending mineralized fault system outcrops in series of cliffs at a lower elevation (200-800 meters a.s.l.) On the cliffs above the Bear River situated in the east portion of MC 2. A northwest trending quartz-sulphide fissure vein that was located about 500 m west of the Bear River on the southeast edge of MC which gave the following results:

Claim

Width

% Cu

% Pb

% Zn

g/t Ag

g/t Au

MC

1.0 m

0.63

1.79

9.99

293.8

58.9

This high grade Zn-Ag-Au showing has a 7 meter long and 1.5 meter wide adit which has been driven at a bearing of 310 degrees into the hillside to trace the quartz-sulphide vein. A total of 4 stream sediments were taken in the southeast corner of the MC claim group. Average values of the 4 samples are listed as follows: Sample #’s ppm Cu ppm Pb ppm Zn ppm Ag ppb Au MC 21-24 85 57 298 1.1 53 These samples demonstrate relatively average values of base and precious metals. There does not appear to be any specific follow up targets developed from this survey. A total of 82 readings were taken along two 500 meter long, 020 trending grid lines. The grid is located at 600-650 meter elevation (1,968-2,132 feet) near the north end of the claims about 850 meters west of Bear River. Magnetometer readings range from 56,346 to 58,377 gammas (a range of 2,031 gammas) total field. There were several sharp increase and decrease in readings at the north end of both L 1W and L 2W. There is also an increase in steepness of terrain near the north end of both lines suggesting the anomalies may be enhanced by topography. There is also a NW trend of Tertiary (Portland Canal/Bitter Creek Pluton related) dykes that cut the north end of the magnetometer survey, suggesting that the intrusive, tabular shape, magnetite-enriched bedrock feature would produce bell-shaped or inverted bell-shaped anomalies . The sharp 1,100 gamma increase on the north end of L 1W occurs on the crest of a cliff, suggesting the presence of magnetite in a relatively restricted area (e.g. tabular shaped body of magnetite enriched bedrock). Dacitic tuff/flow and breccia hosted silicification (quartz, minor jasper) and ubiquitous pyrite,

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i.e. phyllic altered outcrops which occur in the northeast portion of the MC claim. This gossan cliff area is clearly visible from highway 37A. This gossan zone is the where the Dalhousie and Rock of Ages mineral showings occur. Quartz fissure veins consisting of polymetallic (Cu-Pb-Zn-Ag-Au bearing sulphides in a gangue of quartz are emplaced along steeply dipping NW trending fault/fracture zones. Quartz-sulphide veins occur above and below treeline at elevations ranging from 610-1,373 meters (2,000-4,500 feet). In the area of the gossan cliffs in the northeast portion of the MC claim, the treeline dips to its lowest elevation 915 meters (3,000 feet) relative to the Bear River Ridge treeline which varies from 3,000 to 5,000 feet in elevation. The east portion of the MC 2 claim follows the southeast extension of the Dalhousie/Rock of Ages mineral zone. 2002- Fundamental Resources carried out a program of geological mapping, rock chip & stream sediment sampling accompanied by geochemical analysis. Geological mapping traced a well developed quartz-sericite-pyrite-clay (QSP) phyllic alteration across a 0.5 X 0.3 km. zone, located in the northeast portion of the MC claim. QSP is locally abundant between 900 to 1,400 meter elevation. Adjacent to the QSP alteration, a northwest trending mineralized fault zone is located along Rock of Ages Creek, which contains minor jasper chert and chalcopyrite with 3-5% disseminated pyrite. Sub-parallel mineralization peripheral to this fault consists of pyrite-chalcopyrite-galena-sphalerite in a gangue of quartz, carbonate, magnetite, and/or jasper. The Rock of Ages adit is characterized by jasper chert-pyrite-chalcopyrite mineralization zone located (@ 1,200-1,300 m. elevation). The Rock of Ages adit features a northwest trending steeply southwest dipping quartz fissure vein network with 3-5% fracture filling pyrite and sparse chalcopyrite. The upper portion of the Rock of Ages mineral zone contains lenses and bands of sphalerite and galena with minor chalcopyrite. The southeast extension of the NW trending mineralized fault system outcrops in series of cliffs at a lower elevation (approximately 800 meters a.s.l.) on the cliffs above the Bear River situated in the northeast portion of the MC claim. This area (referred to as the Dalhousie showings) contains the following significant mineralized rock chip samples as follows: Sample # Width ppm Cu ppm Pb ppm Zn ppm Ag ppb Au 23653 1.0 m 2079 71 195 15.6 31,800 23654 0.8 m 1575 126 946 7.3 50,400 23657 1.0 m 6201 17 211 5.5 4,580 This showing is located near the north edge of the Dalhousie fraction claim (record # 300895) and features several localized magnetometer survey anomalies and trench cuts. The high grade gold-bearing mineral zone is located at the 800 meter elevation occurs along the axis of a cross-structure and appears to be the southeast extension of the northwest trending Rock of Ages mineralization located at 1,200-1,300 meters elevation. Parallel northwest trending mineral zones are well exposed as massive cliffs above the Dalhousie showings and this area corresponds to buff and green schists with phyllonite which contain quartz-sericite-pyrite phyllic alteration. The southeast extension of this extensive Q-S-P alteration zone carries through to the Bear River valley and onto the Dundee claim further southeast. A total of 6 stream sediments were taken in the east portion of the MC claim. A table listing

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geochemical analysis of the 6 stream sediment samples is as follows: Sample # ppm Cu ppm Pb ppm Zn ppm Ag ppb Au KS-1 83 360 641 1.8 115 KS-2 22 37 211 0.4 35 KS-3 121 41 380 1.0 110 KS-4 1214 62 94 6.8 10,490 KS-5 321 81 599 1.2 180 KS-6 140 218 3130 2.4 240 These samples demonstrate relatively elevated values of base and precious metals. Stream sediment sample KS-4 contains 10.49 grams per tonne gold and 0.12% copper. These anomalous values are likely due to the presence of an adit and trenches located on the Dalhousie fraction claim situated directed above the small creek from where sample KS-4 was taken. Stream sediment samples KS-1 and KS-6 were both taken from large creeks and both samples contain relatively elevated lead and zinc values. It is possible that these anomalous lead and zinc values are derived from the higher elevation areas of the claim where sphalerite and galena mineralization occurs in quartz-sulphide vein networks. In addition to the presence of lead and zinc bearing mineralization occurring in higher elevation zones of quartz-sulphide, there is a 1.2 meter quartz sulphide vein located at 600 meters elevation in Dundee Creek which returned a value of 322 ppm Pb and 3,045 ppm Zn. 2003- Fundamental Res Corp takes rock chip samples from the southeast extension of the NW trending Rock of Ages Creek mineralized fault system outcrops in series of cliffs at a lower elevation (approximately 800 meters a.s.l.) on the cliffs above the Bear River situated in the SE portion of the MC1 claim. This area (referred to as the Dalhousie showings) contains the following significant mineralized rock chip samples as follows: Sample # Width ppm Cu ppm Pb ppm Zn ppm Ag ppb Au Dalhousie 20572 0.5 m 3,309 27 314 48.6 1,580 20573 0.6 m 31,397 158 1,712 254.0 1,980 20574 0.3 m 5,525 30 76 73.3 48,580 Glacier Zone 20579 0.9 m 202 315 193 5.1 4,120 20580 0.9 m 5,555 456 1,052 27.3 1,580 Southeast Zone 20582 1.0 m 254 350 50 126.4 810 2010- Geophysical and geochemical fieldwork was carried out on mineral tenure ID # 567077 (Skeena Mining Division) between July 16-22, and Sept 4-10, 2010 by Fundamental Resources for REC Minerals Corp (name changed to Reliant Gold Inc.). Fieldwork included geochemical analysis (95 soil, 22 rock samples, 30 ICP & Au geochemistry), as well as total field magnetometer along 1.9 km (total = 152 readings at 12.5 m spacing) of north-south oriented grid lines surveyed with a GPS. The 1.9 km of grid lines were surveyed using GPS and marked with

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flagging at soil sample stations. Geological mapping, geophysical magnetometer surveys and geochemical rock and soil sampling was carried out over a 1.6 X 1.2 km area in the east-central portion of the MC1 claim. This area is steep and ranges from 750-1,500 meters (2,460-4,920 ft) in elevation. The upper portion of the fieldwork area is above tree line which is roughly 1,067 m (3,500') elevation. Rock chip sampling (22 samples total), was carried out in 6 areas: 1) Dalhousie (No 1 vein zone, rock sample MC10AR-1) elev 758 m 2) Rock of Ages (No 3 vein zone, rock samples MC10AR-51 to 60) elev 1102-1295 m 3) Aztec (rock samples MC10AR-101, 102) elev 1140-1149 m 4) Ice 3B (rock sample MC10AR-103) elev 1495 m 5) Cairn (AKA Carrin, rock sample MC10AR-151) elev 1505 m 6) Rock of Ages (No 2 vein zone, rock samples MC10AR-201 to 207) elev 822-946 m Quartz-sericite-pyrite-clay (QSP) phyllic alteration is well developed across a 0.5 X 0.3 km. zone, located in the east-central portion of the MC1 claim. QSP is locally abundant between 900 to 1,400 meter elevation. Adjacent to the QSP alteration, a northwest trending mineralized fault zone is located along Rock of Ages Creek, which contains minor jasper chert and chalcopyrite with 3-5% disseminated pyrite. Sub-parallel mineralization peripheral to this fault consists of pyrite-chalcopyrite-galena-sphalerite-tetrahedrite in a gangue of quartz, carbonate, magnetite, specularite, barite and/or jasper. The mineralization and alteration appear to be localized near the contact of rhyolite flows, overlain by andesitic tuffs and the classification of deposit type includes (concordant, and stratiform) Noranda/Kuroko massive sulphide type (Cu-Pb-Zn-Ag-Au), polymetallic veins and breccia (Ag-Au-Pb-Zn-Cu), and polymetallic manto (Ag-Au-Pb-Zn). The following tables show Cu-Pb-Zn-Ag-Au geochemical analysis results from Eco-tech Labs: Dalhousie L4924 No 1 Vein Zone sample no width Cu ppm Pb ppm Zn ppm Ag ppm Au ppb MC10AR-1 18 cm 20030 3 20 26.5 235 Rock of Ages L4940 No 2 Vein Zone sample no width Cu ppm Pb ppm Zn ppm Ag ppm Au ppb MC10AR-201 sub-crop 30 27 138 0.7 45 MC10AR-202 85 cm 10800 432 738 12.8 570 MC10AR-203 55 cm 24 9 34 0.2 40 MC10AR-204 38 cm 13100 3 42 82.3 19560 MC10AR-205 sub-crop 438 183 30 15.4 860 MC10AR-206 85 cm 18600 12 122 36.7 1540 MC10AR-207 20 cm 326 54 34 20.1 1200 Rock of Ages L4940, L4938 No 3 Vein Zone sample no width Cu ppm Pb ppm Zn ppm Ag ppm Au ppb MC10AR-51 sub-crop 50 36 244 1 15 MC10AR-52 22 cm 464 33900 151000 66.5 85 MC10AR-53 55 cm 410 936 4696 6.2 40

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MC10AR-54 20 cm 268 4776 6888 4.7 10 MC10AR-55 15 cm 14 150 248 3.1 80 MC10AR-56 55 cm 114 2695 7188 9 65 MC10AR-57 sub-crop 74 75 5300 2.1 15 MC10AR-58 sub-crop 110 11700 8276 24 30 MC10AR-59 32 cm 990 30 5362 3.3 55 MC10AR-60 sub-crop 160 36 460 2.6 20 Cairn (AKA Carrin) sample no width Cu ppm Pb ppm Zn ppm Ag ppm Au ppb MC10AR-151 20 cm 68 208000 94700 228 10800 Aztec (SE Zone) sample no width Cu ppm Pb ppm Zn ppm Ag ppm Au ppb MC10AR-101 20 cm 28900 3 226 39.4 120 MC10AR-102 38 cm 12800 3 192 36.8 130 Ice 3B (AKA Mt Shorty Ag gossan) sample no width Cu ppm Pb ppm Zn ppm Ag ppm Au ppb MC10AR-103 sub-crop 10 27 262 1.9 150 The best gold values were obtained from the Rock of Ages No 2 Vein Zone (sample MC10AR-204). There was also a strong magnetometer and coincident Au-Cu soil anomaly that coincides with this zone and represents a high order follow-up exploration drill target. Silver values in rock chip samples are highest with elevated Pb-Zn (e.g. MC10AR-151, 52 & 58) or elevated Cu values (e.g. MC10AR-204, 206, 101 & 102). A gold-copper bearing quartz-sulphide vein system was located in the Rock of Ages No 2 Vein Zone defined by rock chip sample MC10AR-204, and supported by Au-Cu in soil geochemical anomalies and total field magnetic anomalies located 100-200 m east of the Cu-Au bearing rock sample. These showings occur at an elevation of 775-950 meters and appear to line up with the northwest trending faults and lineaments of Rock of Ages Creek that exposes the No 3 Vein Zone at 1,180 meters elevation (No 3 tunnel) where a prominent 30-80 m wide gossan with quartz-sericite-pyrite-clay (phyllic alteration) cuts the northwest trend roughly north-northeast, following the contour lines. The Dalhousie zone continues south-southwest and future work should be directed towards exploring the combined 500 meters of strike length of the Dalhousie and Rock of Ages No 2 and No 3 Vein Zones gold-enriched copper & iron bearing mineralized zones, located at 700-1300 m elevation. Based upon these results a diamond drilling program was recommended to test the Rock of Ages #2 and #3 and Cairn showings.

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6.0 GENERAL GEOLOGY The Stewart Complex includes a thick sequence of Late Triassic to Middle Jurassic volcanics, sediments, and metamorphic rocks. These have been intruded and cut by mainly calc-alkaline and lesser alkaline Lower Jurassic and Eocene plutons which form part of the Coast Plutonic Complex. Deformation, in part related to intrusive activity, has produced complex fold structures along the main intrusive contacts with simple open folds and warps dominant along the east side of the complex. Cataclasis, marked by strong N-S structures, are prominent features that cut this sequence. Country rocks in the Stewart area comprise mainly Hazelton Group strata which includes the Lower Jurassic Unuk River Fm and the Middle Jurassic Betty Creek Fm/Mount Dillworth Fm. This sequence is unconformably overlain by Middle Jurassic Salmon River Fm/Nass River Fm (Grove, 1971, 1986). Unuk River strata includes mainly fragmental andesite-dacite, epicalstics and minor sediments. Widespread Aalenian uplift and erosion was followed by deposition of the partly marine volcaniclastic Betty Creek Fm, the mixed Salmon River Fm, and the dominantly shallow marine Nass River Fm. Intrusive activity in the Stewart area has been marked by the Lower and Middle Jurassic Texas Creek granodiorite with which the Big Missouri, Silbak Premier, SB, Scottie Gold, Red Mountain and many other mineral deposits in the district are associated. Younger intrusions include the Hyder Quartz Monzonite, Bitter Creek granodiorite and many Eocene stocks, dykes and sills which form a large part of the Coast Mountain Plutonic Complex. Mineral deposits such as Kitsault Lime Creek Molybdenum, Porter-Idaho Silver Mine, and a host of other deposits are related to the 48-52 Ma (Eocene) plutons. These intrusives also form the regionally extensive Portland Canal Dyke Swarm. More than 700 mineral deposits and showings have been discovered in the Stewart Complex. The Silbak-Premier represents a telescoped (transitional) epithermal gold-silver base metal deposit localized along complex, steep fracture systems in Lower Jurassic volcaniclastics unconformably overlain by shallow dipping Middle Jurassic sediments/volcanics. These overlying units form a barrier or dam to migrating hydrothermal fluids, trapping bonanza type gold-silver mineralization at a relatively shallow depth. Metallogeny of the Silbak-Premier, Big Missouri, SB, Red Mountain and most of the major deposits in the Stewart District is related to early Middle Jurassic plutonic-volcanic activity. Overall, at least 4 major episodes of mineralization involving gold-silver, base metals (including Mo-W), dating from Lower Jurassic to Eocene, have been recorded throughout the Stewart Complex.

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7.0 FIELDWORK 2011 See Methods and Procedures 7.1 METHODS AND PROCEDURES Diamond drilling and rock and prospecting exploration work was carried out on mineral tenure ID # 567077 (Skeena Mining Division) between July 6 - 28, 2011 supervised by Trevor Boyd for Reliant Gold Corp. (formally REC Minerals Corp.). The drilling contractor was More Core Diamond Drilling Limited and the pad builders were Rugged Edge Holdings Ltd. Diamond drilling, which comprised of 710 metres, focused on the testing of surface geochemical rock and soil Au-Ag-Zn-Pb-Cu anomalies supported by favorable magnetic signatures from a surface exploration program completed in 2010. The drilling consisted of three holes from two pad set-ups which tested the Rock of Ages No.3 Showing which had been identified from previous work to host precious and base metal bearing veins and breccia bodies. The hole locations are shown in Fig. 5 and the sample locations are in Appendix B. Drill logs, sections and analytical certificates are available in the ceappendis C, D and E. Drill Hole Collars NAD 83 UTM cords Elevation (m) Orientation (deg. AZ / deg. dip)

MC-11-01

9 V 441455 6213817 1251 050 / -44 MC-11-02

9 V 441764 6213765 1144 025 / -35

MC-11-03

9 V 441764 6213765 1144 045 / -45 Analysis of obtained 461 core samples returned multiple sections of anomalous gold, silver and zinc values of up to 0.9 metres of 1.03 g/t gold (Au) in Hole MC-11-02, and 1.8 metres of 1.2% zinc (Zn) and 2.4 metres of 7.3 g/t silver (Ag) in Hole MC-11-01. Wider sections of anomalous metal contents The deepest hole tested the target area to a maximum depth of approximately 140 metres. The results were encouraging because they indicate the presence of a large hydrothermal mineralizing system to be followed up with additional exploration starting with the completion of borehole geophysical surveys in the three holes. The BTW core samples from the diamond drilling were split in half using a diamond saw, sealed in secure packages and submitted directly by the author to Eco Tech Laboratories in Stewart and Kamloops, British Columbia, where they were analyzed using method Au2-30 gold by fire assay and multi-element ICP-AES following aqua regia digestion. High analyses (greater than 10,000 ppm, 1%) for copper, zinc, lead and (greater than 30 ppm) silver underwent ore grade AA analysis. Polymetallic standards and blanks, unknown to the laboratories, were included with each submission of samples. Eco Tech is an international accredited ISO 9001 compliant laboratory which fulfills standard QA/QC protocols. Surface fieldwork included the examination and rock sampling of known metal occurrences and gossanous quartz-pyrite-sericite altered areas in general focusing on the Aztec and Alpine showings. In total, 30 samples were taken from rock outcrop with a hammer, and approximately 1-2 kilograms of chips were collected into marked poly ore bags. Rock chip samples were secured with tamper-proof straps, and submitted directly by the author to Eco Tech Laboratories

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in Stewart and Kamloops, British Columbia where they were analyzed by the same methods as the core samples. The samples with their GPS locations are shown in Appendix A and Figs 6 and 7. Analytical certificates are available in Appendix E. 7.2 PROPERTY GEOLOGY The majority of the property is underlain by Lower Jurassic Unuk River Formation green, red, and purple volcanic breccia, conglomerate, crystal and lithic tuffs, sandstone, and siltstone. Early Jurassic Texas Creek granodiorite cuts the Unuk River Formation on the southeast portion of the claim group. The Middle Jurassic Betty Creek Formation green, red, purple, and black volcanic breccia, hematitic volcaniclastics, andesitic to dacitic tuffs and flows, Mount Dillworth Formation rhyolite, and Salmon River Formation siltstone-sandstone sequence unconformably overlies the Unuk River Formation near the summit of Mount Shorty Stevenson. Well preserved primary volcanic textures such as devitrified glass, pumice conglomerates, crystals of feldspar, and broken quartz-jasper fragments with feathery and wispy edges occur within dacitic volcanics located on Bear River Ridge north of Mount Shorty Stevenson. This sequence is cut by several northwest trending Tertiary andesite-dacite dykes 1-10 meters in width. Bedrock mapped on the MC consists mainly of Unuk River Fm. volcaniclastics cut by northwest trending mineralized and silicified shear zones. Geological mapping identified Lower Jurassic Unuk River Formation andesitic tuffs and flows in the east portion of the claim in the 600-1,300 meter elevation range. Abundant hematite occurs as 1-20 meter wide bands and lenses intercalated in the volcanic sequence. This hematite occurs with disseminated pyrite and minor chalcopyrite adjacent to northwest trending and southwest dipping quartz-sericite-pyrite (phyllic) alteration. Numerous quartz-sericite alteration zones occurs as bands and lenses within the Unuk River volcanics. These 50-200 m wide altered zones are bleached white-grey colored and occur along northwest trending fault structure

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Detailed lithology of the mapped areas is summarized as follows; TERTIARY INTRUSIVE ROCKS 7 ANDESITE-DACITE DYKE- Aphanitic to medium-grained, greyish-green colour, 1-10 meters wide. EARLY-MIDDLE JURASSIC INTRUSIVE ROCKS 6 Texas Creek granodiorite MIDDLE JURASSIC VOLCANICS AND SEDIMENTS SALMON RIVER FORMATION 4 Siltstone (carbonaceous), sandstone, minor limestone MOUNT DILLWORTH FORMATION 3A Rhyolite sequence (dust, lapilli, and welded tuffs) BETTY CREEK FORMATION 2A CONGLOMERATE, SANDSTONE, SILTSTONE- Grey, green, purple, hematitic volcaniclastic sediments, minor andesitic-dacitic ash, crystal, and lapilli tuffs and tuff breccia. LOWER JURASSIC- UNUK RIVER FORMATION 1 VOLCANIC BRECCIA, CONGLOMERATE- Green, red, and purple coloured matrix supported sub-rounded clasts to 30 cm., fine grained green-grey matrix, minor andesite ash, crystal, and lapilli tuffs, and tuff breccia. Bedrock mapped on the MC1 and MC2 claims (Figure 3) consists mainly of Unuk R Fm. volcaniclastics cut by northwest trending dykes/sills of the Early Jurassic Texas Creek plutonic complex (granodiorite, qtz diorite) and/or Portland Canal Eocene dykes/sills. Both Early Jurassic and Eocene intrusive mineralized and silicified shear zones carry base and precious metal mineralization. Eocene deposits have relatively highAg:Au ratios and dominant galena-sphalerite mineralization, whereas Early Jurassic deposits have relatively low Ag:Au ratios and dominant pyrite-pyrrhotite-chalcopyrite mineralization.

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7.3 PROPERTY MINERALIZATION AND ALTERATION Quartz-sericite-pyrite-clay (QSP) phyllic alteration is well developed across a 0.5 X 0.3 km. zone, located in the east-central portion of the MC1 claim. QSP is locally abundant between 900 to 1,400 meter elevation. Adjacent to the QSP alteration, a northwest trending mineralized fault zone is located along Rock of Ages Creek, which contains minor jasper chert and chalcopyrite with 3-5% disseminated pyrite. Sub-parallel mineralization peripheral to this fault consists of pyrite-chalcopyrite-galena-sphalerite-tetrahedrite in a gangue of quartz, carbonate, magnetite, specularite, barite and/or jasper. The mineralization and alteration appear to be localized near the contact of rhyolite flows, overlain by andesitic tuffs and the classification of deposit type includes (concordant, and stratiform) Noranda/Kuroko massive sulphide type (Cu-Pb-Zn-Ag-Au), polymetallic veins and breccia (Ag-Au-Pb-Zn-Cu), and polymetallic manto (Ag-Au-Pb-Zn). All three deposit types (massive sulphide, manto and vein/breccia) occur within Jurassic aged mineralization. Whereas, only vein/breccia type mineralization occurs in Eocene age deposits. The geochemical data collected from rock sampling suggests that Pb-Zn rich, and high Ag:Au ratio mineralization at Cairn & Ice 3B are related to intrusive rocks of Eocene age, whereas Rock of Ages No 2 & 3 Vein and Dalhousie No 1 Vein are Pb-Zn poor, have low Ag:Au ratios, have elevated Cu values, and are probably Jurassic age. The No 3 Vein may be a massive sulphide and/or manto based on the host rock consisting of banded chert horizons that contain 0.1-3 cm wide layers of alternating jasper-magnetite-hematite with rusty, altered limestone above the banded chert. The No 3 Vein Zone altered dacite host rock is cut by two late-stage, NNW trending andesite porphyry dykes (1-5 m wide) that twin the fault zone that follows the creek. 7.4 DRILL CORE AND ROCK CHIP SAMPLE GEOCHEMISTRY The following table lists the significant Cu-Pb-Zn-Ag-Au drilling intersections for the three drill holes testing the #3 Rock of Ages Showing: All of the analyses and their certificates are available in the appendices B and E. DDH MC11-01 From-To(ft) Width (ft) Cu ppm Pb ppm Zn ppm Ag ppm Au ppb 199 – 207 322 – 328 340 – 355 587 – 590 605 – 608 680 – 683 717 – 720 788 – 789 918 – 928

8 6

15 3 3 3 3 1 10

46 81 8 52 96

2750 766 146 470

580 47 48

1120 729 24 45 39 24

3530 12050

2480 1720 2590 148 454

17100 267

7.7 2.0 0.8 7.6 2.2 10.2 6.0 3.6 2.4

34 70 25 10 5 70 530 135 120

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DDH MC11-02 From-To(ft) Width (ft) Cu ppm Pb ppm Zn ppm Ag ppm Au ppb 129 – 132 196 – 221 266 – 269 452 – 455 452 – 473 531 – 534 918 – 932

3 15 3 3 21 3 14

60 70

102 8140 1820

90 410

543 210 159 <3 35 30 22

2070 990

2140 760 381 140 377

3.4 4.9 1.2

14.8 4.2 0.6 2.1

20 15 25

565 145

1000 91

DDH MC11-03 From-To(ft)

Width (ft)

Cu ppm

Pb ppm

Zn ppm

Ag ppm

Au ppb

241 – 247 6 35 167 1770 2.3 82 511 – 514 3 68 1990 3580 1.2 85 532 – 543.5 11.5 1210 21 174 4.6 101 The following table lists the significant analytical results from samples obtained from the surface investigation of the occurrences. All of the analyses and their certificates are available in the appendices A and E. Surface Rock Samples Sample no width showing Cu ppm Pb ppm Zn ppm Ag ppm Au ppb MC11-TB-02 grab Rock of Ages #3 64 390 3902 3.0 25 MC11-TB-11 30 cm chip Aztec 38 21 8 22.6 25 MC11-TB-22 grab talus Rock of Ages#3 32 1047 12000 1.2 15 MC11-TB-26 grab Alpine 1278 27 13900 3.6 395 8.0 DISCUSSION OF RESULTS A gold-silver-zinc bearing quartz-sulphide vein system hosted in volcanic-sedimentary rocks was drill tested in the Rock of Ages #3 Vein Zone and was found to defines wide down-hole sections of elevated polymetallic values. Sulphides consist of near totally of disseminated pyrite ranging from 2 up to 20% with minor <2% sphalerite and trace chalcopyrite. The showing is aligned along a prospective northwesterly trend for approximately 1,200 metres which includes the Rock of Ages #2, Dalhousie, and Cairn showings. The drilling encountered hydrothermally altered sericite-chlorite-carbonate-sulphide rich volcanic and sedimentary rocks throughout most of the core and specifically in multiple sections varying in down-hole lengths ranging from 25 up to 210 metres. Multiple narrow sections consisting of feldspar-quartz porphyry intrusive were also indentified in the core associated with the altered rocks and an increase in the sulphide concentration. The zone continues south-southwest and future work should be expanded and directed towards exploring the Dalhousie and Rock of Ages No 2 and Cairn showings along the favourable trend. The close proximity to Bear River and Highway 37A and a mill facility at Premier are important factors in future development of the quartz-sulphide veins located on the MC Dalhousie claims.

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9.0 CONCLUSION AND RECOMMENDATIONS The MC claim group has potential to host an economic gold-silver deposit based on the following facts; 1) Favourable geological structure and stratigraphy to host a mineral deposit.

2) Previous and current work programs have outlined significant gold, silver and base metal values from trench, soil, stream sediment and diamond drilling samples thoughout the property especially in the vicinity of the Rock of Ages #2 and Ice showings which were not drill tested during this program

3) Diamond drilling of the Rock of Ages #3 Showing has indentified the

presence of extensive iron sulphide mineralization and related quartz-pyrite-sericite alteration in NW trending faults associated with Jurassic age rocks intruded by porphyritic Texas Creek type bodies similar to those described on the adjacent Silback Preimer property bounding on the west side of the MC Dalhousie claims. .

4) The MC Dalhousie Property is in close proximity to mill and mining

infrastructure. The MC claims requires further exploration in the Ice, Rock of Ages (No 2 and No 3 Vein Zones) and Cairn showings located at 800-1,550 meters (2,624-5,084 feet) elevation in the east to central portion of MC1 mineral tenure. A program of follow-up drilling is recommended to test for below surface base and precious metal bearing mineralization It is recommended that diamond drilling and further geological mapping and sampling be carried out on the Rock of Ages No 2 Cairn and Ice targets from previous work. A helicopter assisted drill program could be carried out between June and October. An approximate budget for this program would be $500,000 (including field crew and field costs).

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REFERENCES Alldrick, D.J., (1983) Geological Setting of the Precious Metal Deposits Stewart, B.C. Min. of E.M.&P.Res. Geological Fieldwork. DeLeen, J., 1991, Description of Bear Pass Mining Properties, Stewart, B.C. private report for Tournigan Mining Explorations Ltd., Vancouver, B.C. DiSpirito, F., 1986, Moche Resources, Assessment report of an airborne geophysical survey on the Ice claims, Mount Shorty Stevenson, Stewart, B.C. A.R. # 15,581. Grove, E.W., (1971) Geology and Mineral Deposits of the Stewart Area, B.C. Min.of E.M.& P.Res., Bull. 58. Grove, E.W., (1986) Geology of the Unuk River-Salmon River-Anyox Map Area, B.C.Min. of E.M.& P.Res., Bull. 63. Harris, C.R., 1984, Rufus Claim Group, Bear River, Stewart, B.C. Kikauka, A.,(1990, 1992, 1993, 2010) Geological, Geochemical, and Geophysical Report(s) on the Ice 1,2,3,4 and MC 1-4 Claims, Navarre Resources Corp. and Fundamental Resources Ltd. Assessment Reports, B.C. Govt. file. Yacoub F., (1990) Geology, Geochemistry, and Geophysics of the Rich 1-4 Claims, White Channel Resources Inc. Assessment Report

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CERTIFICATE OF AUTHOR

I, TREVOR BOYD, of 148 Lascelles Blvd., Toronto, Ontario, do hereby certify that:

The report to which this certificate relates is entitled “GEOLOGICAL, AND DIAMOND DRILLING REPORT on the MC ROCK OF AGES, AZTEC, ALPINE Au-Ag-Cu (Pb-Zn) PROJECT, Mount Shorty Stevenson, Stewart, B.C.” I am responsible for preparation of all of the Sections of this report. I am an officer and the qualified person for Reliant Gold Corp. of Suite 500, 360 Bay Street, Toronto, Ontario, M5H 2V6 I hold a M.Sc.(A) Minex. (1988) from McGill University, Montreal, Quebec, (Canada); and a Ph.D. (1996) from the University of Toronto, Ontario, (Canada). I am a Professional Geoscientist and a member in good standing of the Association of Professional Geologists of Ontario since 2003 (#1023). I have practiced my profession continuously since 1988 and have worked on metallic, exploration and mining development stage projects including those containing Au, Ag, Ni-Cu-PGE, Cu-Pb-Zn, W-Mo-Sn-In, and U-Th elements. Iam registered as a professional geologist (Association of Professional Geologists of Ontario, #1023). The information, opinions and recommendations in this report are based upon fieldwork carried out in my presence on the subject property and on published and unpubished literature and maps. I have a direct interest in Reliant Gold and the subject property.

Signed this the 7th of December, 2011, at Toronto, Ontario. “Trevor Boyd” __________________________ Trevor Boyd, PhD., P.Geo.

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ITEMIZED COST STATEMENT Field Crew Trevor Boyd 22 days 12,100 Dillan Marshall 18 days 4,900 Field Costs Helicopter charters 45,200 Assays 15,100 Diamond Drilling 125,800 Pad Building 26,500 Food, accommodations and supplies 21,400 Total costs 251,000

ITEMIZED COST STATEMENT Field Crew Trevor Boyd P.Geo., Reliant Gold Inc. (Supervising Geologist, $550/day) 22 days 12,100 Dillan Marshall, Skll km Lax Ha Nation Tsetsaut Ventures Ltd. (Core Cutter, $275/day) 18 days 4,900 Field Costs Helicopter charters for pad building and drilling program, approx. 44 hours Prism Helicopters Ltd., (Hughes 500D $950/hr+fuel, A-Star B $1,650/hr+fuel) 45,200 Geochemical Analyses and Assays, Eco Tech Laboratories Ltd. 490 drill core and hand rock samples, (Gold plus multi-element ICP analyses and assays, approx. $31/sample) 15,100 Diamond Drilling, More Core Diamond Drilling Ltd., $92–112/m plus drilling costs, mob and demob etc., 2,370 feet(710 m) (Three holes, including coring, field costs, consumables and rentals) 125,800 Pad Building, Rugged Edge Holdings Ltd., three drill pads 26,500 Food, accommodations and supplies, local Stewart suppliers, (King Edward Hotel, restaurants, grocery stores, service station, ISL supplies Ltd., Home Hardware etc.) 21,400 Total costs 251,000

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26

27

28

29

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Lab Sample# sample no width easting northing elevation lithology alteration mineralization strike dip comments zone name

sample ID apparent GPS CORDS NAD 83 9V meters rock type minerals sulphides, oxides apparent apparent landmarks source: Minfile

88151 MC-11-TB-01 50 cm chip 441782 6213844 1176 m felsic-Int (dacite?) vol. ser, qtz, hem py cliff face gossan, flinty Rock of ages # 388152 MC-11-TB-02 grab 441703 6213835 1235 m felsic-Int (dacite?) vol. ser, qtz,carb, hem py,sph cliff face gossan Rock of ages # 388153 MC-11-TB-03 grab 441106 6213892 1358 m felsic-Int (dacite?) vol. ser, qtz,hem py 320 subvertical rusty anistimosing shears next to snowfield Aztec88154 MC-11-TB-04 75 cm 441090 6213897 1372 m felsic-Int (dacite?) vol. ser, qtz,hem py 75 subvertical rusty anistimosing shears next to snowfield Aztec88155 MC-11-TB-05 50 chip 441134 6213763 1356 m felsic-Int (dacite?) vol. ser, qtz,hem py 75 subvertical green purple gossan cliff face Aztec88156 MC-11-TB-06 grab 441139 6213769 1357 m qtz vein qtz, ser py qtz vein with sulphidic selveges Aztec88157 MC-11-TB-07 50 cm 441135 6213767 1353 m felsic-Int (dacite?) vol. chl, ser, hem py gossanous highly sulphidic wallrock to qtz vein Aztec88158 MC-11-TB-08 50 cm 441193 6213740 1312 m felsic-Int (dacite?) vol. chl, ser, hem py gossanous cliff face Aztec88159 MC-11-TB-09 grab 441197 6213785 1306 m felsic-Int (dacite?) vol. chl, ser, hem py 70 subvertical chloritic sulphidic seam Aztec88160 MC-11-TB-10 40 cm 441182 6213710 1246 m felsic-Int (dacite?) vol. chl, ser, hem py,sph 315 subvertical clay altered sulphidic gossan Aztec88161 MC-11-TB-11 30 cm 441204 6213681 1278 m felsic-Int (dacite?) vol. chl, ser, hem py,sph sulphidic gossan Aztec88162 MC-11-TB-12 40 cm same felsic-Int (dacite?) vol. chl, ser, hem py,sph clay altered sulphidic gossan Aztec88163 MC-11-TB-13 20 cm 441221 6213567 1267 m felsic-Int (dacite?) vol. chl, ser, hem py, sph, cpy 320 subvertical clay altered sulphidic gossan Aztec88164 MC-11-TB-14 60 cm 441197 6213554 1296 m felsic-Int (dacite?) vol. chl, ser, hem py, sph, cpy 330 & 085 subvertical sulphidic gossan assoc. with intersecting shears Aztec88165 MC-11-TB-15 grab 441205 6213521 1291 m felsic-Int (dacite?) vol. chl, ser, hem py, sph, cpy same same Aztec88166 MC-11-TB-16 50 cm 441191 6213455 1281 m felsic-Int (dacite?) vol. chl, ser, hem py, sph, cpy 310 subvertical same Aztec88167 MC-11-TB-17 grab 441210 6213453 1275 m qtz vein/felsic-Int (dacite?) vol.qtz, ser,hem py 330 subvertical rusty sulphidic qtz vein Aztec88168 MC-11-TB-18 1 m 441234 6213536 1264 m felsic-Int (dacite?) vol. ser, qtz,hem py 330 highly fractured and sheared gossan Aztec88169 MC-11-TB-19 grab boulder same volcanic breccia chl, ser, hem py breccia rock with chloritic sulphide matrix Aztec88170 MC-11-TB-20 grab 441558 6213654 1225 m felsic-Int (dacite?) vol. ser, qtz,hem py gossan, flinty Alpine88171 MC-11-TB-21 40 cm 441887 6213886 1103 m felsic-Int (dacite?) vol. ser, qtz,hem py, aspy 35 subvertical cliff face gossan flinty North of Rock of Ages #388172 MC-11-TB-22 grab boulder 441865 6213834 1106 m iron formation-sedimentcarb, chl, hem (ank?)py, mag, sph, gal narrow bands of iron fm and carbonate Rock of Ages #388173 MC-11-TB-23 grab boulder 441834 6213797 1116 m volcanic plus qtz veins. qtz, ser, hem py, cpy, sph manganese encrusted Rock of ages #388174 MC-11-TB-24 40 cm 441790 6213738 1117 m felsic-Int (dacite?) vol. ser, qtz,hem py cliff face gossan Rock of ages #388175 MC-11-TB-25 30 cm 441743 6213649 1107 m volcaniclastic sed ser, qtz,hem py, cpy, gal roughly layered gossanous sediment Alpine88176 MC-11-TB-26 grab 441730 6213662 1110 m volcaniclastic sed ser, qtz,hem py, sph, gal 35 70 NW roughly layered gossanous sediment Alpine88177 MC-11-TB-27 40 cm 441715 6213657 1114 m volcaniclastic sed ser, qtz,hem py 30 50NW roughly layered gossanous sediment Alpine88178 MC-11-TB-28 30 cm 441680 6213664 1123 m volcaniclastic sed ser, qtz,hem py, sph, gal 20 65 NW roughly layered gossanous sediment Alpine88179 MC-11-TB-29 20 cm 441725 6213627 1122 m volcaniclastic sed ser, qtz,hem py gossanous highly friable cliff face Alpine88180 MC-11-TB-30 comp. grab 50 cm 441721 6213627 1116 m volcaniclastic sed chl, ser, hem py gossanous highly friable cliff face Alpine

APPENDIX B MC Drill Core Sample List

Drill Hole collars UTM NAD 83 Cords ElevationMC-11-01 9 V 441455 6213817 1251 mMC-11-02 9 V 441764 6213765 1144 mMC-11-03 9 V 441764 6213765 1144 m

Hole Sample no from (ft) to width (ft) Au ppb Au g/t Zn ppm Zn% Ag ppm Al% As Ba Be Bi Ca% Cd Co Cr Cu Fe% Hg K% La Li Mg% Mn Mo Na% Ni P Pb Pb % S% Sb Sc Se Sn Sr Ti% U V W Y

MC-11-01 87301 196 199 3 15 810 1.4 1.23 20 52 <1 <5 2.77 7 7 54 42 2.87 <5 0.32 8 12 0.64 2660 11 0.03 4 480 81 0.41 <5 2 <10 <5 42 0.04 <5 40 <5 587302 199 202 3 20 2310 9.0 0.54 70 16 <1 <5 >10 25 6 14 26 2.80 <5 0.05 4 10 0.40 >10000 35 0.02 4 210 1149 2.88 10 <1 <10 <5 416 0.02 <5 40 <5 487303 202 204.5 2.5 15 2156 10.2 1.13 185 28 <1 <5 >10 18 6 14 40 5.58 <5 0.06 4 6 0.40 >10000 54 0.04 6 270 444 4.89 15 <1 <10 <5 322 0.03 <5 52 <5 487304 204.5 207 2.5 70 6152 3.8 1.25 90 10 <1 <5 8.48 42 12 30 78 7.81 <5 0.08 4 10 0.58 8010 28 0.07 4 340 105 4.52 10 1 <10 <5 108 0.05 <5 44 <5 587305 207 209 2 10 538 1.8 2.65 35 172 <1 <5 1.40 3 23 38 42 6.69 <5 0.69 6 26 1.11 5005 5 0.07 6 1040 75 1.23 5 11 <10 <5 38 0.26 <5 204 <5 587306 322 325 3 90 >10000 1.51% 1.8 0.29 25 148 <1 <5 0.25 103 7 78 66 1.22 <5 0.24 8 <2 0.06 345 7 0.02 3 420 57 1.65 <5 1 <10 <5 10 0.03 <5 16 <5 387307 325 328 3 50 9006 2.2 0.50 35 150 <1 <5 0.25 71 6 70 96 1.74 <5 0.27 8 4 0.15 560 5 0.02 2 480 36 1.44 <5 2 <10 <5 8 0.04 <5 30 <5 387308 328 331 3 15 580 1.0 0.71 30 134 <1 <5 0.39 4 8 40 26 1.96 <5 0.49 10 6 0.23 590 3 0.02 2 640 39 1.24 <5 2 <10 <5 10 0.06 <5 40 <5 487309 331 334 3 20 100 1.0 0.82 25 128 <1 <5 0.85 <1 12 60 8 2.80 <5 0.56 8 8 0.46 1150 1 0.03 2 590 39 1.46 <5 4 <10 <5 20 0.12 <5 64 <5 487310 334 337 3 30 88 1.4 0.76 35 108 <1 <5 1.19 <1 11 70 10 3.05 <5 0.54 8 8 0.52 1390 3 0.02 4 440 36 1.51 <5 3 <10 <5 22 0.08 <5 54 <5 487311 337 340 3 10 140 0.8 0.97 20 82 <1 <5 0.46 <1 6 66 6 2.73 <5 0.37 16 8 0.43 1645 2 0.02 2 430 93 0.66 <5 2 <10 <5 14 0.07 <5 36 <5 487312 340 343 3 30 1852 1.0 1.20 20 72 <1 <5 0.41 11 9 38 8 3.52 <5 0.31 20 6 0.49 2285 2 0.02 3 480 42 0.79 <5 2 <10 <5 12 0.06 <5 38 <5 487313 343 346 3 50 4890 1.0 1.39 25 70 <1 <5 0.51 27 9 32 10 3.83 <5 0.38 18 8 0.55 2685 2 0.02 2 540 66 0.81 <5 2 <10 <5 12 0.07 <5 38 <5 487314 346 349 3 15 1582 0.8 0.91 20 96 <1 <5 0.26 9 6 62 8 2.89 <5 0.28 12 6 0.40 1790 2 0.02 3 450 54 1.08 <5 2 <10 <5 12 0.08 <5 36 <5 487315 349 352 3 15 2716 0.6 0.81 30 112 <1 <5 0.24 17 6 74 6 2.67 <5 0.23 10 4 0.36 1855 2 0.02 2 410 66 0.90 <5 2 <10 <5 10 0.09 <5 40 <5 387316 352 355 3 5 1382 0.6 0.88 15 102 <1 <5 0.19 9 6 68 6 2.41 <5 0.29 10 6 0.39 1770 2 0.02 3 440 42 0.50 <5 2 <10 <5 10 0.09 <5 32 <5 387317 355 358 3 5 858 0.4 0.88 10 100 <1 <5 0.24 6 6 92 8 2.45 <5 0.34 14 6 0.38 1840 1 0.02 2 420 21 0.43 <5 2 <10 <5 12 0.11 <5 32 <5 387318 358 361 3 5 126 0.4 1.48 5 86 <1 <5 0.43 <1 6 56 6 2.42 <5 0.69 10 12 0.53 1945 2 0.09 3 440 18 0.18 <5 2 <10 <5 24 0.11 <5 38 <5 387319 361 364 3 5 140 0.2 1.69 5 72 <1 <5 0.79 <1 5 60 4 2.23 <5 0.74 10 14 0.65 1810 1 0.12 2 480 12 0.13 <5 2 <10 <5 32 0.12 <5 42 <5 487320 364 367 3 <5 180 0.8 0.93 20 76 <1 <5 1.67 1 6 62 8 1.63 <5 0.42 10 6 0.32 2350 2 0.05 2 420 42 0.34 <5 1 <10 <5 32 0.07 <5 22 <5 487321 367 370 3 <5 150 0.4 1.26 10 78 <1 <5 1.15 <1 6 50 4 1.81 <5 0.54 14 10 0.39 2080 1 0.07 1 470 30 0.20 <5 1 <10 <5 26 0.08 <5 22 <5 487322 370 373 3 5 580 0.4 1.23 10 86 <1 <5 1.82 6 6 62 10 1.64 <5 0.47 10 10 0.39 2115 2 0.10 3 440 15 0.19 <5 2 <10 <5 32 0.09 <5 34 <5 687323 373 376 3 25 162 1.6 0.28 45 124 <1 <5 4.41 1 8 36 16 1.73 <5 0.17 10 4 0.11 3275 14 0.02 1 490 30 1.53 <5 2 <10 <5 64 0.02 <5 12 <5 987324 376 377.5 1.5 15 144 1.2 0.54 30 132 <1 <5 3.37 1 10 38 6 2.08 <5 0.31 6 4 0.17 1945 7 0.02 3 600 21 1.87 <5 2 <10 <5 34 0.05 <5 20 <5 587325 377.5 381 3.5 35 110 0.8 0.70 10 156 1 <5 0.27 <1 8 36 6 1.68 <5 0.47 10 2 0.09 310 5 0.02 2 970 15 1.51 <5 2 <10 <5 8 0.03 <5 18 <5 487326 381 384 3 25 378 1.2 1.03 10 102 <1 <5 0.32 4 14 32 12 3.06 <5 0.66 6 6 0.26 605 7 0.04 4 1040 24 2.53 <5 2 <10 <5 12 0.09 <5 28 <5 587327 384 387 3 10 184 2.2 1.20 20 90 <1 <5 0.73 <1 19 26 12 4.20 <5 0.63 10 8 0.44 1300 5 0.05 5 1220 45 3.69 <5 2 <10 <5 26 0.10 <5 30 <5 587328 387 390 3 10 136 1.6 0.99 30 92 <1 <5 1.00 <1 19 26 10 4.04 <5 0.48 6 8 0.40 1465 6 0.03 5 1140 60 3.67 <5 2 <10 <5 30 0.07 <5 26 <5 587329 390 393 3 5 164 0.8 0.97 15 102 <1 <5 0.87 <1 17 22 6 3.94 <5 0.49 10 8 0.36 1355 4 0.02 4 1010 39 3.48 <5 2 <10 <5 34 0.07 <5 24 <5 587330 393 396 3 15 70 1.0 1.06 20 100 <1 <5 0.68 <1 17 24 6 3.33 <5 0.56 8 8 0.40 1125 4 0.02 4 1000 42 2.80 <5 2 <10 <5 24 0.07 <5 28 <5 587331 396 399 3 15 204 1.2 1.46 25 94 <1 <5 0.76 <1 17 20 8 4.25 <5 0.65 10 10 0.68 1720 4 0.03 4 1230 51 2.86 <5 3 <10 <5 24 0.10 <5 36 <5 687332 399 402 3 20 388 1.2 1.16 15 78 <1 <5 0.45 5 17 32 14 4.02 <5 0.67 8 10 0.39 1165 4 0.04 5 1060 30 3.31 <5 3 <10 <5 16 0.11 <5 36 <5 687333 402 405 3 45 368 1.6 1.08 15 92 <1 <5 0.34 3 16 20 14 3.89 <5 0.51 12 14 0.43 925 3 0.03 4 1130 27 2.91 <5 2 <10 <5 12 0.05 <5 32 <5 787334 405 408 3 45 696 1.8 0.83 10 26 <1 5 1.36 6 17 24 24 3.74 <5 0.47 8 8 0.24 1385 4 0.02 5 1260 30 3.75 <5 2 <10 <5 54 0.02 <5 22 <5 887335 408 411 3 35 874 2.0 1.18 5 70 <1 <5 0.73 7 13 14 22 4.64 <5 0.49 12 16 0.62 1740 3 0.02 3 780 96 4.03 <5 2 <10 <5 22 0.07 <5 22 <5 687336 411 414 3 50 412 2.6 0.95 10 22 <1 <5 0.47 4 14 14 28 4.59 <5 0.48 8 8 0.42 940 3 0.02 3 680 120 4.37 <5 2 <10 <5 14 0.04 <5 18 <5 587337 522 525 3 5 370 0.8 1.90 20 150 <1 <5 3.19 1 19 18 26 3.90 <5 0.33 4 22 1.40 2705 4 0.07 4 1070 18 2.40 <5 3 <10 <5 64 0.07 <5 38 <5 487338 525 528 3 5 538 1.0 1.69 20 74 <1 <5 2.37 3 21 16 44 4.45 <5 0.37 4 18 1.16 2040 3 0.06 4 1100 33 3.41 <5 3 <10 <5 52 0.06 <5 36 <5 587339 528 531 3 5 124 1.2 1.07 20 28 <1 <5 1.38 <1 20 22 28 4.97 <5 0.40 4 10 0.56 1030 3 0.04 5 1040 39 4.92 <5 2 <10 <5 30 0.03 <5 28 <5 587340 531 534 3 <5 216 0.8 2.33 10 48 <1 <5 2.20 <1 21 18 28 4.66 <5 0.33 4 22 1.53 1985 3 0.09 4 1040 27 2.81 <5 3 <10 <5 56 0.06 <5 46 <5 587341 534 537 3 <5 152 0.8 1.64 15 56 <1 <5 1.51 <1 21 16 18 4.70 <5 0.38 2 16 1.10 1425 4 0.04 5 1140 21 3.37 <5 3 <10 <5 34 0.06 <5 36 <5 487342 537 540 3 5 158 2.0 1.34 20 46 <1 <5 0.90 <1 38 18 100 6.79 <5 0.42 <2 12 0.65 795 2 0.06 17 1220 51 6.10 <5 4 <10 <5 28 0.12 <5 42 <5 587343 540 542 2 25 286 1.8 1.38 35 24 <1 <5 0.59 2 38 36 34 7.66 <5 0.48 <2 10 0.61 625 6 0.10 19 1140 84 6.89 <5 5 <10 <5 28 0.13 <5 48 <5 487344 542 545 3 <5 108 0.2 1.73 10 72 <1 <5 0.96 <1 14 74 12 2.73 <5 0.41 6 20 1.53 1050 2 0.13 10 1320 12 0.16 <5 3 <10 <5 80 0.24 <5 74 <5 387345 545 548 3 15 710 1.0 3.58 10 64 <1 <5 1.83 5 33 62 18 7.44 <5 0.75 2 16 1.15 920 4 0.42 17 1200 96 7.23 <5 8 <10 <5 80 0.22 <5 130 <5 687346 548 551 3 15 304 1.0 4.91 15 92 1 <5 2.49 1 37 76 22 7.29 <5 1.08 2 20 1.55 1430 5 0.38 20 1000 78 6.61 <5 9 <10 <5 82 0.23 <5 176 <5 587347 551 554 3 10 326 1.6 4.65 20 48 1 <5 1.99 1 43 50 44 7.71 <5 1.56 2 24 1.83 1625 8 0.25 21 1420 42 5.79 <5 11 <10 <5 70 0.27 <5 160 <5 587348 554 557 3 5 232 1.4 2.87 15 78 <1 <5 1.30 <1 25 28 40 5.11 <5 1.16 2 12 0.92 1065 4 0.14 5 1100 33 4.14 <5 5 <10 <5 44 0.16 <5 80 <5 387349 557 560 3 <5 112 1.4 2.78 20 44 <1 <5 1.93 <1 24 20 32 4.46 <5 0.95 2 14 0.86 1180 5 0.14 5 1130 27 3.51 <5 4 <10 <5 58 0.14 <5 72 <5 487350 560 563 3 5 102 1.2 1.58 10 98 <1 <5 2.19 <1 22 16 26 4.03 <5 0.50 4 12 0.73 1315 7 0.08 4 1120 27 3.29 <5 3 <10 <5 50 0.10 <5 38 <5 587351 563 566 3 <5 136 1.2 1.90 10 116 <1 <5 1.96 <1 20 14 26 4.18 <5 0.46 4 18 1.01 1300 10 0.10 5 1060 33 2.81 <5 3 <10 <5 50 0.11 <5 44 <5 587352 566 569 3 <5 92 1.4 1.55 10 130 <1 <5 2.76 <1 22 14 24 3.93 <5 0.40 4 14 0.80 1430 3 0.08 5 1040 36 3.14 <5 3 <10 <5 58 0.11 <5 36 <5 587353 569 572 3 <5 156 1.2 2.59 10 122 <1 <5 2.66 <1 22 18 22 4.67 <5 0.52 4 20 1.26 1860 3 0.13 5 1070 54 3.15 <5 4 <10 <5 64 0.15 <5 54 <5 687354 572 575 3 5 236 1.8 2.69 15 170 <1 <5 2.80 <1 23 14 30 4.56 <5 0.51 4 24 1.50 2745 3 0.09 5 1130 51 2.35 <5 4 <10 <5 54 0.16 <5 58 <5 687355 575 578 3 10 134 2.6 1.69 15 122 <1 <5 2.69 <1 22 18 34 4.13 <5 0.50 4 14 0.81 2285 4 0.07 4 1050 51 3.32 <5 3 <10 <5 50 0.16 <5 42 <5 687356 578 581 3 10 730 4.4 1.07 25 68 <1 <5 2.08 10 22 26 42 3.02 <5 0.46 4 8 0.44 1780 12 0.03 5 1060 573 2.82 5 3 <10 <5 34 0.14 <5 32 <5 587357 581 584 3 5 648 1.8 1.82 30 210 <1 <5 2.65 5 21 14 32 3.37 <5 0.40 4 18 1.16 3670 5 0.04 4 1280 150 1.36 <5 4 <10 <5 52 0.14 <5 40 <5 687358 584 587 3 10 522 1.4 2.19 20 266 <1 <5 3.06 2 19 16 22 3.54 <5 0.37 4 20 1.34 3940 7 0.04 4 1130 222 1.04 <5 4 <10 <5 60 0.14 <5 44 <5 687359 587 590 3 10 1722 7.6 1.07 35 40 <1 <5 3.76 12 20 22 52 3.05 <5 0.37 4 10 0.63 3480 5 0.02 3 1410 1119 2.89 10 3 <10 <5 76 0.12 <5 30 <5 787360 590 593 3 0 182 2.8 1.36 10 88 <1 <5 2.27 <1 23 20 26 4.59 <5 0.38 4 14 0.89 1735 3 0.06 4 960 270 4.11 <5 3 <10 <5 50 0.21 <5 36 <5 787361 593 596 3 <5 174 1.6 1.77 10 126 <1 <5 2.94 <1 24 22 16 4.21 <5 0.37 4 18 1.18 2155 2 0.10 4 850 69 3.08 <5 3 <10 <5 66 0.20 <5 42 <5 887362 596 599 3 <5 110 1.2 4.06 10 90 <1 <5 2.87 <1 25 40 18 4.58 <5 0.89 2 18 1.39 2040 4 0.36 5 930 39 3.22 <5 7 <10 <5 74 0.20 <5 114 <5 687363 599 602 3 5 234 1.2 4.16 10 82 1 <5 2.95 <1 25 48 32 5.12 <5 0.99 4 16 1.43 1800 5 0.45 5 920 57 4.20 <5 7 <10 <5 80 0.22 <5 132 <5 787364 602 605 3 5 246 1.0 2.93 10 196 <1 <5 3.28 <1 21 16 18 4.12 <5 0.63 6 22 1.77 3065 2 0.13 4 1010 51 1.68 <5 4 <10 <5 62 0.18 <5 64 <5 887365 605 608 3 5 2592 2.2 3.42 15 138 <1 <5 2.76 22 21 46 96 4.31 <5 1.17 6 16 1.68 2025 4 0.32 4 970 729 2.25 <5 6 <10 <5 82 0.19 <5 118 <5 887366 608 611 3 <5 258 0.6 3.28 5 252 <1 <5 1.27 1 26 40 34 3.94 <5 1.45 8 16 2.01 1525 3 0.29 5 1080 21 0.75 <5 8 <10 <5 72 0.26 <5 158 <5 987367 611 614 3 <5 102 0.4 2.49 10 136 <1 <5 1.31 <1 17 58 12 3.46 <5 0.86 8 16 1.65 1290 2 0.13 5 1090 15 0.07 <5 7 <10 <5 102 0.26 <5 140 <5 987368 NS87369 NS87370 646.5 648 1.5 25 90 1.4 2.22 5 60 <1 <5 0.97 <1 28 60 234 3.79 <5 0.56 6 18 1.89 1260 4 0.06 5 1160 18 0.51 <5 4 <10 <5 64 0.20 <5 118 <5 6

87371 648 651 3 15 186 0.6 2.54 5 154 <1 <5 0.89 <1 28 50 42 4.40 <5 1.20 10 18 2.04 1180 3 0.10 4 1270 33 1.09 <5 5 <10 <5 88 0.25 <5 148 <5 887372 651 654 3 5 126 0.6 2.47 <5 108 <1 <5 1.12 <1 20 58 16 3.32 <5 1.07 8 18 2.17 1085 4 0.07 5 1160 18 0.22 <5 4 <10 <5 144 0.25 <5 126 <5 787373 654 657 3 10 98 0.4 2.50 5 86 <1 <5 1.08 <1 24 52 32 3.40 <5 0.54 8 20 2.36 1185 4 0.06 5 1240 12 0.24 <5 4 <10 <5 152 0.22 <5 124 <5 787374 657 658.5 1.5 10 178 0.4 2.31 <5 170 <1 <5 0.86 <1 20 54 16 3.64 <5 1.18 10 18 2.02 990 4 0.07 5 1200 24 0.98 <5 4 <10 <5 124 0.20 <5 122 <5 887375 658.5 661.5 3 20 1000 1.0 2.20 10 92 <1 <5 0.41 9 25 26 64 6.75 <5 0.42 10 40 1.55 1210 5 0.05 4 1270 75 2.45 <5 4 <10 <5 18 0.03 <5 110 <5 987376 661.5 664.5 3 25 618 1.2 2.70 5 148 <1 <5 0.90 2 24 30 168 5.12 <5 1.15 8 32 1.80 1410 3 0.09 4 1150 54 1.00 <5 7 <10 <5 36 0.12 <5 154 <5 987377 664.5 668 3.5 25 1070 1.2 2.36 10 112 <1 <5 0.63 5 22 32 122 5.64 <5 0.87 10 26 1.51 1400 4 0.08 4 1140 90 1.77 <5 6 <10 <5 26 0.10 <5 122 <5 987378 668 671 3 25 496 1.0 2.13 10 92 <1 <5 0.94 2 22 32 44 6.41 <5 0.66 8 30 1.45 1405 4 0.06 4 1120 48 2.61 <5 5 <10 <5 28 0.08 <5 124 <5 987379 671 674 3 35 354 1.2 3.08 10 120 <1 <5 1.10 1 23 48 108 5.20 <5 1.69 6 18 1.74 1240 4 0.19 4 1100 111 1.91 <5 7 <10 <5 46 0.19 <5 154 <5 787380 674 677 3 20 528 1.0 1.70 <5 68 <1 <5 1.06 3 17 56 20 4.06 <5 0.54 6 16 1.29 1115 4 0.06 4 1100 24 1.70 <5 5 <10 <5 80 0.19 <5 118 <5 787381 677 680 3 35 332 2.0 2.09 15 104 <1 <5 1.08 2 24 46 320 4.65 <5 0.51 10 30 1.47 1455 4 0.05 4 1110 24 1.38 10 6 <10 <5 50 0.16 <5 122 <5 887382 680 683 3 70 148 10.2 2.16 10 116 <1 <5 0.97 <1 34 56 2748 3.77 <5 0.71 8 18 1.65 1250 4 0.07 4 1150 24 0.89 <5 5 <10 <5 104 0.22 <5 126 <5 787383 683 686 3 10 118 2.8 1.82 5 96 <1 <5 1.17 <1 21 58 484 3.35 <5 0.60 8 16 1.38 1185 4 0.05 4 1150 18 0.52 <5 5 <10 <5 88 0.22 <5 130 <5 787384 686 689 3 <5 116 0.4 2.29 <5 94 <1 <5 1.33 <1 17 58 18 3.17 <5 0.70 8 16 1.71 1275 3 0.07 4 1190 15 <0.01 <5 4 <10 <5 132 0.24 <5 134 <5 887385 689 692 3 5 108 0.4 2.17 <5 78 <1 <5 1.31 <1 17 56 16 3.23 <5 0.46 8 16 1.58 1330 3 0.05 4 1120 15 0.06 <5 5 <10 <5 138 0.23 <5 132 <5 787386 692 695 3 20 122 0.6 3.43 10 168 <1 <5 1.04 <1 24 42 62 4.92 <5 1.89 8 18 2.19 1515 3 0.19 4 1200 15 0.63 <5 7 <10 <5 68 0.23 <5 184 <5 787387 695 699 4 100 372 4.8 2.26 30 100 <1 <5 1.03 3 33 60 482 5.15 <5 0.92 6 16 1.35 1295 6 0.10 4 950 174 2.42 <5 6 <10 <5 44 0.15 <5 118 <5 687388 699 702 3 5 102 <0.2 1.37 <5 36 <1 <5 1.50 <1 15 70 22 3.23 <5 0.09 16 18 1.21 715 3 0.05 8 1640 12 0.13 <5 2 <10 <5 82 0.17 <5 68 <5 387389 702 708 6 <5 72 <0.2 1.37 <5 34 <1 <5 1.72 <1 13 76 14 3.18 <5 0.12 26 20 1.22 720 3 0.05 7 1730 6 0.11 <5 2 <10 <5 104 0.06 <5 64 <5 487390 708 711 3 15 148 0.8 2.71 5 146 <1 <5 1.33 <1 25 40 112 4.70 <5 0.99 10 22 1.88 1830 3 0.09 4 1130 15 0.38 <5 6 <10 <5 84 0.19 <5 158 <5 887391 711 714 3 25 334 2.4 2.44 10 80 <1 <5 1.54 2 23 36 478 6.11 <5 0.41 12 42 1.75 1695 4 0.05 4 1160 180 1.81 <5 5 <10 <5 84 0.04 <5 126 <5 987392 714 717 3 50 122 0.8 2.29 <5 80 <1 <5 3.38 <1 7 28 120 4.93 <5 0.32 14 38 1.60 2745 3 0.03 4 1160 18 0.64 <5 5 <10 <5 156 0.04 <5 126 <5 1387393 717 720 3 530 454 6.0 1.87 15 68 <1 <5 2.28 2 29 54 766 6.70 <5 0.31 10 30 1.33 2165 5 0.03 4 890 45 3.53 <5 4 <10 <5 112 0.04 <5 90 <5 1287394 720 723 3 140 570 1.4 2.41 10 100 <1 <5 0.95 3 23 40 194 5.41 <5 1.01 8 18 1.61 1590 4 0.07 4 1100 21 2.17 <5 6 <10 <5 46 0.15 <5 122 <5 887395 723 726 3 15 104 0.4 2.49 5 148 <1 <5 1.26 <1 19 38 28 4.22 <5 1.00 12 22 1.63 1400 4 0.09 4 1230 18 1.07 <5 7 <10 <5 62 0.12 <5 132 <5 1087396 726 729 3 15 210 0.4 2.37 15 96 <1 <5 1.40 <1 22 26 38 5.60 <5 0.60 12 32 1.55 1985 3 0.04 4 1170 18 2.16 <5 5 <10 <5 72 0.06 <5 106 <5 1087397 729 732 3 35 144 0.6 2.11 10 70 <1 <5 1.84 <1 22 34 18 6.88 <5 0.41 10 34 1.57 1960 3 0.04 4 1060 36 3.72 <5 5 <10 <5 94 0.05 <5 108 <5 1187398 732 735 3 20 258 1.0 2.07 10 74 <1 <5 2.04 1 25 32 52 6.76 <5 0.31 10 38 1.51 1860 3 0.03 4 1080 24 3.58 <5 4 <10 <5 100 <0.01 <5 94 <5 1187399 735 738 3 15 124 0.6 2.64 5 164 <1 <5 2.19 <1 21 38 42 4.44 <5 0.62 12 26 1.86 1525 3 0.10 5 1250 27 0.67 <5 6 <10 <5 76 0.13 <5 142 <5 1087400 738 742.5 4.5 20 108 0.2 1.87 <5 80 <1 <5 2.24 <1 20 68 22 4.34 <5 0.05 18 24 1.75 955 3 0.05 8 2780 9 0.05 <5 3 <10 <5 100 0.20 <5 94 <5 588101 742.5 745.5 3 15 130 0.4 3.04 10 154 <1 <5 0.90 <1 24 40 32 4.36 <5 1.16 8 24 2.00 1340 3 0.15 4 1190 21 0.73 <5 7 <10 <5 40 0.19 <5 154 <5 888102 745.5 747.5 2 35 144 2.8 3.18 10 138 <1 <5 0.97 <1 26 44 928 5.22 <5 1.46 8 26 1.89 1410 3 0.16 4 1230 48 1.52 <5 9 <10 <5 42 0.21 <5 168 <5 788103 747.5 750.5 3 <5 110 0.4 1.83 <5 26 <1 <5 1.94 <1 24 68 20 4.55 <5 0.05 16 26 1.83 960 2 0.05 12 2670 9 0.04 <5 4 <10 <5 66 0.24 <5 98 <5 688104 750.5 753 2.5 10 124 0.6 2.16 5 36 <1 <5 1.88 <1 23 62 40 4.58 <5 0.08 16 28 1.84 1040 3 0.06 11 2460 102 0.16 <5 5 <10 <5 62 0.24 <5 108 <5 688105 753 756 3 35 146 1.2 3.23 10 114 <1 <5 1.07 <1 25 46 186 5.94 <5 1.45 8 26 1.98 1240 4 0.20 4 1120 75 2.27 <5 8 <10 <5 58 0.19 <5 182 <5 888106 756 759 3 65 130 3.6 3.23 15 96 <1 <5 1.02 <1 26 46 596 5.50 <5 1.71 6 18 1.70 1185 4 0.23 4 1120 21 2.63 <5 7 <10 <5 46 0.19 <5 158 <5 888107 759 762 3 70 186 1.2 2.75 15 104 <1 <5 0.77 <1 22 46 42 5.37 <5 1.20 8 22 1.65 1395 5 0.13 4 1120 21 2.09 <5 7 <10 <5 30 0.17 <5 134 <5 788108 762 765 3 15 156 0.6 3.09 10 154 1 <5 0.97 <1 26 46 34 4.05 <5 1.56 8 20 1.60 1215 3 0.19 4 1200 18 0.98 <5 7 <10 <5 42 0.16 <5 138 <5 888109 765 768 3 15 102 0.4 3.05 5 170 <1 <5 1.32 <1 21 54 12 3.79 <5 1.37 8 16 1.61 1160 4 0.23 4 1140 18 1.04 <5 6 <10 <5 76 0.22 <5 150 <5 888110 768 771 3 20 320 1.0 2.46 5 166 <1 <5 1.13 1 16 54 124 3.51 <5 1.11 8 12 1.33 1170 3 0.14 4 1110 15 0.96 <5 6 <10 <5 56 0.20 <5 126 <5 788111 771 774 3 15 86 0.6 1.77 10 138 <1 <5 1.03 <1 16 56 24 3.34 <5 0.67 8 12 1.17 1190 4 0.08 4 1070 15 0.92 <5 4 <10 <5 52 0.19 <5 110 <5 788112 774 777 3 10 108 0.4 2.42 <5 152 <1 <5 1.16 <1 13 52 38 3.38 <5 0.93 8 14 1.40 1275 3 0.14 4 1120 18 0.20 <5 5 <10 <5 68 0.22 <5 140 <5 788113 777 780 3 10 92 0.8 2.17 <5 148 <1 <5 1.18 <1 12 50 38 3.18 <5 0.62 8 14 1.34 1305 3 0.11 4 1150 15 0.22 <5 6 <10 <5 64 0.23 <5 132 <5 888114 780 783 3 25 240 0.8 2.52 10 94 <1 <5 0.68 <1 28 36 38 6.08 <5 0.83 8 24 1.52 1760 4 0.09 4 1060 24 2.62 <5 6 <10 <5 32 0.17 <5 100 <5 788115 783 786 3 30 850 1.0 2.62 10 100 <1 <5 0.59 5 24 28 56 6.50 <5 0.51 8 32 1.70 2215 4 0.07 4 1230 21 2.42 <5 5 <10 <5 22 0.17 <5 94 <5 788116 786 788 2 40 362 0.6 2.48 15 44 <1 <5 0.44 <1 24 34 20 7.64 <5 0.75 6 22 1.38 2070 4 0.07 4 1060 27 3.83 <5 4 <10 <5 18 0.16 <5 80 <5 688117 788 789 1 135 >10000 1.71 3.6 2.14 20 34 <1 <5 0.63 103 18 88 146 6.15 <5 0.80 4 14 0.94 1410 15 0.12 4 640 39 4.37 <5 4 <10 <5 34 0.12 <5 74 <5 488118 789 792 3 15 246 0.6 5.21 10 80 1 <5 2.92 <1 30 50 48 5.84 <5 1.41 2 16 1.67 1345 6 0.42 8 1430 24 5.02 <5 5 <10 <5 104 0.17 <5 162 <5 588119 792 795 3 10 194 1.0 6.23 10 96 <1 <5 3.42 <1 34 48 68 5.77 <5 1.90 2 18 2.03 1875 4 0.66 8 1470 24 3.80 <5 4 <10 <5 142 0.16 <5 182 <5 588120 795 798 3 10 334 1.0 6.48 10 100 <1 <5 3.11 1 30 42 58 5.90 <5 2.04 2 18 2.38 1830 4 0.69 8 1570 24 3.90 <5 5 <10 <5 126 0.16 <5 194 <5 588121 798 801 3 10 100 0.6 5.63 15 96 <1 <5 2.69 <1 34 52 38 5.09 <5 1.70 2 16 2.03 1365 4 0.55 9 1480 21 3.50 <5 4 <10 <5 108 0.16 <5 150 <5 488122 801 804 3 10 64 0.6 4.36 20 66 1 <5 2.39 <1 33 46 28 5.64 <5 0.75 2 22 1.43 755 4 0.40 8 1610 24 5.21 <5 4 <10 <5 86 0.18 <5 124 <5 588123 804 807 3 10 56 0.8 5.22 15 70 1 <5 3.15 <1 32 64 64 6.40 <5 0.80 2 12 1.13 685 5 0.51 9 1520 30 6.42 <5 4 <10 <5 94 0.15 <5 134 <5 588124 807 810 3 10 76 0.4 5.23 10 64 <1 <5 3.28 <1 32 54 24 6.31 <5 0.91 2 14 1.43 865 3 0.63 8 1470 27 6.06 <5 3 <10 <5 106 0.13 <5 142 <5 588125 810 813 3 5 110 0.6 5.71 20 92 <1 <5 2.93 <1 31 48 60 5.83 <5 1.36 2 20 2.16 1140 4 0.64 8 1600 39 4.68 <5 5 <10 <5 106 0.15 <5 168 <5 588126 813 816 3 5 134 0.6 4.18 10 90 <1 <5 2.28 <1 26 46 52 4.46 <5 1.02 2 24 1.90 1335 3 0.49 8 1610 30 2.57 <5 5 <10 <5 88 0.17 <5 144 <5 688127 816 819 3 5 292 0.6 4.19 10 76 <1 <5 2.20 1 31 50 50 4.96 <5 0.87 2 20 1.53 955 3 0.52 8 1410 27 3.93 <5 4 <10 <5 90 0.16 <5 122 <5 588128 819 822 3 10 256 0.6 5.20 20 120 <1 <5 2.57 <1 29 42 50 5.27 <5 1.26 4 34 2.47 1285 4 0.53 8 1670 48 2.72 <5 7 <10 <5 96 0.19 <5 176 <5 688129 822 825 3 10 110 0.4 5.32 15 116 <1 <5 3.25 <1 31 46 44 5.28 <5 1.36 2 20 1.88 1210 4 0.61 8 1540 27 3.60 <5 4 <10 <5 110 0.16 <5 160 <5 488130 825 828 3 5 174 0.4 6.26 15 138 <1 <5 3.43 <1 30 38 68 5.46 <5 1.88 2 20 2.39 1485 5 0.65 8 1600 30 3.06 <5 5 <10 <5 114 0.17 <5 180 <5 488131 828 831 3 5 122 0.6 6.05 10 110 1 <5 3.76 <1 30 38 44 5.48 <5 1.58 2 24 2.31 1370 4 0.63 8 1590 27 4.10 <5 4 <10 <5 120 0.15 <5 172 <5 588132 831 834 3 10 106 0.6 5.48 10 92 <1 <5 2.85 <1 29 48 40 5.04 <5 1.34 2 22 1.92 1050 5 0.62 7 1700 24 3.92 <5 4 <10 <5 100 0.15 <5 150 <5 588133 834 837 3 5 390 0.8 5.20 10 78 <1 <5 3.24 3 29 50 38 5.18 <5 1.10 2 20 1.61 1060 4 0.61 8 1530 36 4.48 <5 5 <10 <5 100 0.13 <5 152 <5 588134 837 840 3 5 134 0.8 6.25 20 80 1 <5 3.40 <1 30 40 52 5.74 <5 1.75 4 30 2.52 1125 5 0.63 8 1600 30 4.68 <5 6 10 <5 100 0.15 <5 188 <5 688135 840 843 3 10 156 1.0 5.95 20 78 1 <5 3.30 <1 30 44 52 6.10 <5 1.60 4 30 2.24 1210 4 0.63 8 1690 36 4.99 <5 7 10 <5 98 0.14 <5 200 <5 688136 843 846 3 5 260 0.8 6.67 25 98 1 <5 3.69 <1 36 62 54 6.50 <5 1.94 4 28 2.41 1435 6 0.58 10 1610 39 4.25 <5 7 10 <5 102 0.18 <5 216 <5 688137 846 848 2 10 146 0.8 4.97 25 64 1 <5 2.64 <1 35 52 38 7.34 <5 1.55 4 26 1.87 1035 5 0.44 9 1560 27 5.67 <5 8 <10 <5 80 0.18 <5 182 <5 688138 848 851 3 25 290 0.8 6.23 15 88 1 <5 3.57 <1 36 62 38 7.23 <5 1.50 4 28 2.08 1235 5 0.57 9 1460 30 5.85 <5 8 10 <5 96 0.21 <5 220 <5 688139 851 854 3 20 220 1.0 5.78 15 84 1 <5 5.06 <1 33 56 38 7.28 <5 1.36 4 20 1.79 1550 4 0.59 9 1500 30 6.22 <5 6 10 <5 110 0.16 <5 204 <5 888140 854 857 3 10 188 0.6 7.59 25 140 1 <5 3.81 <1 37 42 34 6.52 <5 2.94 4 30 3.63 2095 6 0.63 10 1610 30 3.23 <5 10 <10 <5 114 0.20 <5 258 <5 788141 857 860 3 25 278 0.8 6.32 15 106 <1 <5 4.35 <1 36 50 52 6.95 <5 1.60 4 28 2.70 1720 5 0.61 11 1620 30 5.36 <5 6 <10 <5 128 0.20 <5 220 <5 788142 860 863 3 30 464 0.6 6.10 25 64 <1 <5 2.91 2 43 54 20 8.02 <5 2.15 2 32 2.85 1485 5 0.59 11 1490 30 5.12 <5 10 <10 <5 116 0.21 <5 216 <5 588143 863 866 3 15 1520 1.4 5.39 5 136 <1 <5 2.54 12 46 62 246 6.42 <5 2.09 2 20 2.37 1460 5 0.42 12 1400 24 2.08 <5 6 <10 <5 102 0.25 <5 170 <5 588144 866 869 3 10 214 0.8 3.30 10 184 <1 <5 1.89 <1 24 64 128 4.95 <5 0.84 10 22 1.93 1125 6 0.22 10 1940 24 0.68 <5 6 <10 <5 74 0.26 <5 146 <5 688145 869 872 3 20 168 3.2 5.80 5 298 1 <5 2.61 <1 22 50 736 5.57 <5 2.42 4 24 2.65 1410 6 0.49 11 1410 21 0.81 <5 9 <10 <5 108 0.26 <5 206 <5 788146 872 875 3 20 170 0.8 6.03 5 170 1 <5 2.66 <1 32 48 168 6.06 <5 2.36 4 24 2.60 1370 4 0.56 8 1630 24 1.82 <5 12 <10 <5 98 0.25 <5 238 <5 688147 875 878 3 25 134 0.6 6.12 <5 310 <1 <5 2.79 <1 23 46 98 5.61 <5 1.98 4 28 2.68 1455 4 0.55 7 1610 21 0.69 <5 10 <10 <5 104 0.25 <5 240 <5 588148 878 881 3 15 148 0.4 6.72 5 216 1 <5 2.96 <1 28 44 52 6.12 <5 2.68 4 22 2.72 1415 4 0.56 9 1650 24 1.17 <5 12 <10 <5 100 0.23 <5 252 <5 5

88149 881 884 3 15 176 1.0 5.88 10 128 1 <5 2.13 <1 61 40 118 7.45 <5 2.97 4 26 3.01 1395 8 0.40 9 1540 24 2.18 <5 14 <10 <5 88 0.25 <5 258 <5 788150 884 885 1 10 140 0.6 1.75 <5 70 <1 <5 2.17 <1 23 78 46 4.68 <5 0.13 16 20 1.46 970 3 0.12 12 2600 48 0.62 <5 5 <10 <5 62 0.28 <5 98 <5 688351 885 887 2 20 226 0.6 4.77 15 108 <1 <5 1.11 <1 32 24 66 8.96 <5 2.15 6 34 2.86 2090 4 0.17 9 1700 21 2.19 <5 11 <10 <5 46 0.25 <5 204 <5 888352 887 890 3 25 140 0.8 5.93 5 334 1 <5 2.26 <1 34 34 130 5.83 <5 2.79 6 20 2.81 1390 5 0.48 9 1760 21 0.76 <5 15 <10 <5 110 0.27 <5 258 <5 888353 890 893 3 35 156 1.4 5.77 5 340 <1 <5 1.91 <1 28 32 314 6.54 <5 2.94 6 22 3.14 1525 4 0.42 9 1620 21 0.74 <5 14 <10 <5 98 0.28 <5 254 <5 888354 893 896 3 25 196 0.4 5.59 10 378 <1 <5 1.75 <1 38 20 68 6.26 <5 2.40 6 36 3.01 1430 4 0.36 9 1680 18 0.64 <5 15 <10 <5 100 0.31 <5 252 <5 888355 896 899 3 65 106 1.0 5.45 10 202 <1 <5 2.06 <1 42 40 188 6.81 <5 2.25 4 24 2.30 1220 7 0.41 11 1600 21 1.80 <5 10 <10 <5 102 0.28 <5 232 <5 588356 899 902 3 20 104 1.6 5.17 10 216 <1 <5 2.22 <1 29 40 306 5.94 <5 2.16 4 20 1.99 1075 4 0.41 10 1690 21 1.10 <5 9 <10 <5 108 0.25 <5 216 <5 688357 902 905 3 70 180 1.2 4.73 15 156 <1 <5 1.29 <1 33 26 200 9.12 <5 2.28 6 30 2.43 1525 5 0.25 10 1650 21 1.98 <5 15 <10 <5 60 0.27 <5 258 <5 988358 905 907 2 15 98 0.6 4.70 5 232 <1 <5 1.79 <1 20 50 70 4.86 <5 2.18 6 22 2.07 995 4 0.37 8 1400 18 0.82 <5 11 <10 <5 94 0.24 <5 208 <5 788359 907 911 4 10 66 0.2 1.71 <5 108 <1 <5 0.86 <1 12 96 6 2.27 <5 0.80 6 12 1.06 600 3 0.19 11 940 12 0.06 <5 2 <10 <5 82 0.16 <5 68 <5 288360 911 914 3 35 268 0.6 4.91 10 128 <1 <5 1.63 <1 53 36 68 7.04 <5 1.97 4 20 2.10 1195 5 0.29 10 1740 21 1.98 <5 11 <10 <5 90 0.23 <5 208 <5 688361 914 917 3 60 170 1.0 6.05 10 156 <1 <5 1.43 <1 51 26 142 8.65 <5 3.40 4 24 3.27 1675 4 0.25 10 1680 24 1.65 <5 16 <10 <5 76 0.32 <5 264 <5 888362 917 918 1 30 68 0.4 3.95 15 36 <1 <5 1.64 <1 108 64 36 7.84 <5 1.65 4 12 1.58 910 3 0.31 9 1280 21 5.12 <5 11 <10 <5 92 0.21 <5 174 <5 488363 918 922 4 80 218 1.4 4.54 15 126 <1 <5 0.86 <1 38 26 202 >10 <5 1.65 4 26 2.16 2585 5 0.17 11 1510 21 2.07 <5 12 <10 <5 48 0.24 <5 206 <5 488364 922 925 3 160 316 4.2 5.04 20 118 <1 <5 0.78 <1 33 24 840 >10 <5 1.86 4 40 2.84 2630 6 0.12 10 1510 27 2.07 <5 12 <10 <5 32 0.27 <5 208 <5 488365 925 928 3 125 282 2.4 3.62 20 92 <1 <5 0.90 <1 34 32 436 8.85 <5 0.86 8 54 2.21 2020 5 0.09 9 1340 27 2.66 <5 10 <10 <5 32 0.23 <5 168 <5 688366 928 932 4 10 692 0.2 2.09 5 134 <1 <5 1.07 2 22 70 58 4.25 <5 0.08 16 20 1.43 815 2 0.10 14 2450 12 0.02 <5 4 <10 <5 76 0.21 <5 82 <5 688367 oreas 67a std. >1000 2.18 72 32.2 0.90 320 126 <1 20 0.32 <1 13 148 320 4.28 <5 0.04 4 4 0.48 160 5 0.14 37 300 168 1.32 80 1 10 5 54 0.07 <5 28 <5 388368 oreas 131b std. <5 >10000 3.01 31.8 0.84 70 50 1 <5 4.24 91 21 14 226 5.49 <5 0.68 18 18 2.89 1600 3 0.03 24 600 >10000 1.84 5.15 35 2 <10 <5 20 0.02 <5 12 <5 988369 blank <5 2 <0.2 0.01 <5 6 <1 <5 <0.01 <1 <1 <2 <2 0.02 <5 <0.01 <2 <2 <0.01 <5 <1 <0.01 <1 <10 3 0.02 <5 <1 <10 <5 <2 <0.01 <5 <2 <5 <188370 dup37389 <5 70 <0.2 1.34 <5 32 <1 <5 1.57 <1 13 74 6 3.01 <5 0.11 22 18 1.17 675 3 0.05 7 1680 6 0.08 <5 2 <10 <5 98 0.08 <5 60 <5 488371 dup37389 5 72 <0.2 1.36 <5 30 <1 <5 1.40 <1 13 66 2 2.77 <5 0.11 18 18 1.19 630 2 0.05 6 1700 6 0.02 <5 2 <10 <5 108 0.13 <5 54 <5 3

Hole Sample no from (ft) to width (ft)Au ppb Au g/tZn ppm Zn% Ag ppm Al% As Ba Be Bi Ca% Cd Co Cr Cu Fe% Hg K% La Li Mg% Mn Mo Na% Ni P Pb Pb % S% Sb Sc Se Sn Sr Ti% U V W Y

MC-11-02 88372 NS88373 126 129 3 15 748 3.0 1.85 10 24 <1 <5 1.81 6 36 36 68 6.80 <5 0.38 4 26 1.62 1575 2 0.11 8 1720 249 6.48 <5 7 10 <5 40 0.33 <5 84 <5 1188374 129 132 3 20 2074 3.4 2.48 10 20 <1 <5 2.73 19 34 30 60 6.37 <5 0.35 4 34 2.13 2185 2 0.13 8 1730 543 6.23 <5 7 10 <5 62 0.29 <5 94 <5 988375 132 135.5 3.5 65 920 4.6 1.80 15 16 <1 5 1.43 7 38 40 60 7.86 <5 0.39 4 24 1.40 1375 2 0.10 9 1780 300 6.98 <5 6 20 <5 34 0.28 <5 78 <5 988376 NS88377 NS88378 NS88379 NS88380 NS88381 NS88382 NS88383 NS88384 NS88385 NS88386 166 169 3 15 156 2.6 1.01 15 14 <1 5 1.00 <1 34 44 54 7.06 <5 0.38 4 8 0.38 675 2 0.05 10 1760 75 6.44 <5 3 10 <5 16 0.15 <5 42 <5 888387 169 172 3 5 160 2.2 1.63 20 22 <1 5 0.75 <1 38 38 64 7.51 <5 0.44 4 18 1.20 900 1 0.05 11 1870 51 6.57 <5 4 10 <5 14 0.16 <5 58 <5 888388 172 175 3 5 68 3.2 0.72 15 16 <1 5 0.89 <1 36 46 60 7.66 <5 0.43 4 2 0.07 195 2 0.05 11 1950 117 7.10 <5 3 10 <5 14 0.16 <5 32 <5 788389 175 178 3 5 62 2.6 0.78 15 18 <1 5 0.68 <1 36 50 66 7.87 <5 0.46 4 4 0.11 135 1 0.05 10 1730 93 7.11 <5 4 10 <5 10 0.20 <5 36 <5 788390 178 181 3 10 196 1.2 2.69 15 40 <1 <5 1.63 <1 38 34 58 6.58 <5 0.38 6 32 2.03 1910 2 0.07 10 1900 42 4.65 <5 7 <10 <5 20 0.27 <5 98 <5 1188391 181 184 3 5 254 0.4 4.18 25 68 <1 <5 3.40 <1 35 20 36 5.74 <5 0.19 6 54 3.32 3490 2 0.05 9 1760 21 0.83 <5 10 <10 <5 34 0.28 <5 138 <5 1288392 184 187 3 5 192 0.2 3.81 10 100 <1 <5 4.85 <1 33 18 22 5.21 <5 0.24 8 42 2.66 3575 2 0.05 9 1810 18 0.61 <5 9 <10 <5 54 0.28 <5 132 <5 1288393 187 190 3 5 208 1.0 3.67 10 88 <1 <5 2.61 <1 35 22 60 6.11 <5 0.32 6 44 2.77 2785 2 0.09 9 1870 30 2.60 <5 8 <10 <5 40 0.26 <5 126 <5 1188394 190 193 3 5 348 0.4 4.22 5 94 <1 <5 2.52 <1 35 20 54 5.74 <5 0.44 8 52 3.20 3255 2 0.15 9 1890 30 2.47 <5 10 <10 <5 42 0.28 <5 142 <5 1388395 193 196 3 20 146 2.0 1.78 10 26 <1 5 1.31 <1 39 36 74 7.25 <5 0.61 6 18 0.88 1010 1 0.09 10 1830 51 6.56 <5 6 20 <5 20 0.22 <5 70 <5 1088396 196 199 3 15 1112 5.6 0.90 10 18 <1 15 0.75 9 36 40 56 7.91 <5 0.52 4 6 0.13 165 2 0.06 11 1940 168 7.26 <5 4 20 <5 12 0.20 <5 42 <5 888397 199 203 4 30 478 5.6 0.87 10 18 <1 15 0.80 4 37 42 58 8.08 <5 0.52 4 4 0.11 185 2 0.05 12 2030 237 7.39 <5 4 30 <5 16 0.14 <5 40 <5 988398 203 206 3 15 736 5.6 0.94 10 12 <1 10 0.76 5 36 44 62 7.91 <5 0.55 4 6 0.14 170 2 0.06 11 1920 204 7.26 <5 4 30 <5 16 0.16 <5 42 <5 888399 206 212 6 10 1348 4.4 1.81 10 16 <1 10 1.16 9 37 38 52 7.45 <5 0.90 4 18 0.72 615 1 0.11 11 1910 216 7.18 <5 6 20 <5 24 0.19 <5 68 <5 988400 NS85651 212 215 3 10 726 4.0 2.26 10 22 <1 5 1.13 4 36 42 42 7.41 <5 1.02 4 20 0.83 625 2 0.18 10 1940 309 7.18 <5 7 20 <5 30 0.21 <5 78 <5 1085652 215 218 3 10 880 4.6 1.30 10 16 <1 <5 0.92 6 36 42 98 8.00 <5 0.73 4 10 0.31 295 2 0.08 10 1940 231 7.51 <5 5 20 <5 18 0.20 <5 54 <5 985653 218 221 3 25 1370 5.2 1.47 10 18 <1 <5 0.78 11 38 44 148 8.24 <5 0.67 6 14 0.59 570 3 0.08 11 1970 108 7.35 <5 6 20 <5 18 0.20 <5 64 <5 985654 221 224 3 10 348 0.8 5.81 15 96 <1 <5 1.81 <1 35 36 72 6.66 <5 1.25 6 52 3.62 3385 3 0.36 10 1810 27 2.45 <5 12 <10 <5 62 0.27 <5 212 <5 1085655 224 227 3 10 202 0.6 5.20 5 228 <1 <5 1.77 <1 33 44 80 5.90 <5 1.42 8 46 3.46 2955 3 0.27 9 1850 21 0.93 <5 13 <10 <5 72 0.32 <5 222 <5 1185656 261 263 2 20 122 4.8 3.56 5 92 <1 <5 2.11 <1 60 54 794 5.52 <5 1.11 8 22 1.80 1505 1 0.21 11 1690 60 2.47 <5 7 10 <5 80 0.30 <5 172 <5 1185657 263 266 3 30 438 1.0 2.56 10 38 <1 <5 1.77 3 31 72 26 6.31 <5 0.98 6 16 1.36 1170 5 0.12 9 1510 27 4.26 5 7 <10 <5 60 0.23 <5 134 <5 785658 266 269 3 25 2144 1.2 3.01 5 34 <1 <5 2.31 17 34 52 102 6.94 <5 0.78 4 24 1.49 1075 2 0.37 9 1770 159 6.30 5 10 10 <5 68 0.18 <5 198 <5 785659 269 272 3 15 156 0.8 3.51 10 44 <1 <5 3.05 <1 34 38 64 6.50 <5 0.90 6 32 2.01 1430 3 0.39 9 1800 45 5.76 <5 11 10 <5 82 0.21 <5 194 <5 985660 272 276 4 15 92 0.4 1.91 5 38 <1 <5 4.04 <1 23 46 34 4.78 <5 0.29 16 36 1.45 1545 3 0.05 11 1520 18 2.71 <5 4 <10 <5 82 0.01 <5 78 <5 1185661 276 279 3 5 72 <0.2 1.44 <5 32 <1 <5 2.67 <1 10 74 22 2.45 <5 0.25 18 20 1.01 930 2 0.05 12 1150 12 0.26 <5 2 <10 <5 64 <0.01 <5 40 <5 685662 311 313 2 10 136 0.8 3.35 15 122 <1 <5 2.38 <1 36 60 70 4.73 <5 0.68 8 24 1.72 1430 3 0.20 10 1870 42 1.12 5 9 <10 <5 108 0.33 <5 176 <5 885663 313 316 3 30 236 2.2 3.64 15 126 <1 <5 2.37 <1 65 52 410 5.47 <5 0.88 8 26 2.00 1325 7 0.25 10 1870 123 2.06 5 9 10 <5 126 0.37 <5 186 <5 985664 316 319 3 25 232 0.6 2.44 10 36 <1 <5 2.17 <1 28 66 26 4.87 <5 0.12 12 28 1.64 1260 2 0.08 7 2440 66 0.32 5 9 <10 <5 82 0.40 <5 142 <5 885665 319 322 3 20 166 0.6 2.81 25 30 <1 <5 2.95 <1 19 58 16 3.47 <5 0.11 8 20 1.68 1465 4 0.07 9 1680 171 0.39 5 9 <10 <5 190 0.39 <5 154 <5 985666 322 325 3 10 148 1.2 2.57 10 34 <1 <5 2.79 <1 19 68 420 3.67 <5 0.14 10 18 1.52 1255 8 0.08 7 2090 90 0.36 10 8 <10 <5 170 0.44 <5 132 <5 8

85667 325 328 3 40 140 3.0 3.50 15 82 <1 <5 2.42 <1 48 50 702 5.30 <5 0.47 8 26 1.85 1325 3 0.26 9 1820 36 2.00 5 8 <10 <5 112 0.34 <5 186 <5 985668 328 331 3 20 100 1.2 3.39 10 76 <1 <5 2.98 <1 47 42 78 5.86 <5 0.58 10 28 1.77 1345 2 0.22 9 1860 27 2.81 <5 9 <10 <5 126 0.25 <5 168 <5 1185669 351.5 356 4.5 25 114 0.4 5.33 10 78 <1 <5 2.21 <1 38 32 18 6.07 <5 1.78 6 32 3.25 1090 3 0.45 9 1980 36 3.60 5 12 10 <5 86 0.32 <5 226 <5 1185670 356 359 3 20 134 0.8 6.22 10 138 <1 <5 2.44 <1 33 36 148 5.43 <5 2.39 4 30 3.41 1255 2 0.43 8 1890 27 2.32 <5 12 <10 <5 74 0.32 <5 226 <5 1085671 359 362 3 20 172 0.4 4.64 5 124 <1 <5 1.66 <1 34 32 24 6.30 <5 2.20 4 32 3.62 1355 2 0.36 9 1650 24 2.83 <5 11 <10 <5 62 0.19 <5 194 <5 385672 362 365 3 15 110 0.2 4.09 10 84 <1 <5 1.95 <1 27 50 90 5.41 <5 1.85 4 18 2.28 1015 3 0.38 7 1370 30 2.93 <5 8 <10 <5 82 0.17 <5 162 <5 285673 365 368 3 65 94 <0.2 4.10 10 58 1 <5 1.64 <1 36 44 24 5.77 <5 2.08 4 20 2.25 855 2 0.39 9 1630 45 3.62 <5 10 <10 <5 64 0.18 <5 174 <5 385674 368 371 3 10 98 <0.2 3.35 10 156 <1 <5 2.08 <1 36 60 18 4.08 <5 0.85 10 20 1.99 1040 3 0.28 9 1680 18 1.62 5 7 <10 <5 84 0.19 <5 144 <5 485675 371 374 3 25 116 <0.2 4.13 5 154 <1 <5 1.98 <1 36 50 88 4.71 <5 1.89 8 20 2.43 1125 2 0.39 8 1630 21 1.81 5 9 <10 <5 72 0.18 <5 174 <5 385676 374 377 3 15 126 <0.2 4.90 5 100 <1 <5 1.91 <1 33 42 36 5.49 <5 2.76 6 20 3.09 1110 3 0.50 9 1670 24 2.35 5 11 <10 <5 68 0.19 <5 204 <5 385677 377 380 3 20 82 <0.2 3.73 5 52 <1 <5 1.67 <1 41 54 60 6.28 <5 1.99 4 14 1.97 770 2 0.46 9 1600 27 4.18 5 9 <10 <5 76 0.19 <5 168 <5 385678 380 383 3 30 94 <0.2 3.29 10 36 <1 <5 1.27 <1 37 48 38 8.28 <5 1.87 4 18 2.16 865 2 0.35 9 1550 30 5.43 <5 10 <10 <5 58 0.18 <5 178 <5 385679 383 386 3 15 80 0.2 2.49 5 86 <1 <5 1.64 <1 30 64 20 5.57 <5 0.65 8 20 1.85 830 2 0.30 7 1660 18 3.08 <5 8 <10 <5 74 0.20 <5 158 <5 385680 386 389 3 20 116 0.4 2.84 10 50 <1 <5 2.93 <1 28 32 68 5.76 <5 0.63 6 44 2.97 1480 2 0.13 5 1160 18 2.26 <5 12 <10 <5 84 0.19 <5 182 <5 285681 389 392 3 15 90 <0.2 2.50 5 96 <1 <5 2.42 <1 31 42 22 5.39 <5 0.78 6 32 2.48 1140 2 0.14 7 1320 18 3.00 <5 10 <10 <5 78 0.21 <5 180 <5 385682 392 395 3 20 68 <0.2 1.63 5 52 <1 <5 1.19 <1 38 50 38 6.38 <5 0.66 6 20 1.78 755 2 0.12 8 1430 24 4.65 5 10 <10 <5 56 0.20 <5 174 <5 385683 395 398 3 10 102 <0.2 2.56 10 166 <1 <5 1.39 <1 28 46 16 4.48 <5 1.04 6 28 2.80 1135 2 0.12 6 1350 15 1.22 5 9 <10 <5 80 0.22 <5 186 <5 285684 398 401 3 10 100 <0.2 2.72 5 206 <1 <5 1.42 <1 33 46 16 4.55 <5 1.52 6 28 2.87 1135 2 0.15 6 1330 18 1.24 5 9 <10 <5 106 0.23 <5 200 <5 285685 401 404 3 90 122 <0.2 3.69 15 246 <1 <5 1.19 <1 29 48 70 5.88 <5 2.53 6 24 3.32 1260 2 0.27 7 1350 21 1.16 5 13 <10 <5 64 0.20 <5 228 <5 385686 404 407 3 15 116 <0.2 3.82 10 294 <1 <5 1.32 <1 23 44 30 4.91 <5 2.43 6 26 3.12 1260 2 0.31 7 1290 18 0.85 5 12 <10 <5 68 0.19 <5 200 <5 385687 407 410 3 20 102 <0.2 4.18 10 126 <1 <5 1.85 <1 32 46 22 5.66 <5 2.36 4 24 2.86 1235 2 0.42 7 1380 24 2.31 5 11 <10 <5 82 0.19 <5 196 <5 385688 410 413 3 20 90 <0.2 3.96 10 66 <1 <5 1.94 <1 36 36 18 7.04 <5 1.99 6 32 2.69 1200 2 0.34 8 1580 24 4.15 5 12 <10 <5 66 0.20 <5 196 <5 385689 413 416 3 20 64 <0.2 2.60 5 66 <1 <5 2.79 <1 34 26 16 6.33 <5 0.91 8 42 2.18 1180 2 0.16 7 1440 21 4.73 <5 11 <10 <5 52 0.20 <5 168 <5 385690 416 419 3 35 108 <0.2 3.35 10 58 <1 <5 2.23 <1 33 24 34 8.10 <5 1.65 8 54 3.07 1405 2 0.17 8 1570 27 5.41 <5 12 <10 <5 46 0.16 <5 174 <5 385691 419 422 3 50 172 0.4 3.42 10 54 <1 <5 2.50 <1 33 22 44 7.94 <5 0.44 10 54 3.04 2035 2 0.06 8 1710 21 4.17 <5 8 <10 <5 30 0.32 <5 130 <5 1185692 422 425 3 30 100 <0.2 3.80 5 58 <1 <5 3.31 <1 31 18 32 6.47 <5 0.60 6 66 3.49 1715 2 0.07 7 1550 18 3.48 <5 10 <10 <5 50 0.31 <5 162 <5 1185693 425 428 3 70 42 0.8 1.28 15 26 <1 <5 2.15 <1 34 30 64 7.88 <5 0.53 14 20 0.61 730 3 0.06 8 1650 21 6.93 5 6 10 <5 28 0.23 <5 72 <5 1185694 428 431 3 50 50 0.6 2.16 15 24 <1 <5 1.48 <1 38 48 32 8.83 <5 0.74 10 18 0.82 605 3 0.20 10 1590 21 7.30 5 8 10 <5 40 0.26 <5 122 <5 985695 431 434 3 40 116 0.2 4.60 10 52 1 <5 2.43 <1 39 38 24 9.04 <5 0.88 6 54 3.08 1725 3 0.23 9 1670 24 4.54 5 12 <10 <5 68 0.29 <5 198 <5 1185696 434 437 3 75 104 0.6 2.96 10 36 <1 <5 1.88 <1 37 40 40 9.84 <5 0.43 12 42 2.32 1615 2 0.07 8 1600 24 5.93 <5 9 <10 <5 26 0.28 <5 122 <5 1385697 437 439.5 2.5 55 186 0.6 3.46 15 36 <1 <5 0.89 <1 36 34 28 >10 <5 0.59 8 54 2.67 1750 5 0.10 8 1670 36 5.15 <5 10 <10 <5 26 0.31 <5 152 <5 1085698 439.5 442 2.5 10 260 <0.2 2.22 10 58 <1 <5 1.16 <1 25 70 24 5.57 <5 0.21 22 30 1.58 845 1 0.08 6 2650 18 1.00 <5 8 <10 <5 60 0.38 <5 112 <5 685699 442 446 4 20 136 0.4 4.56 10 60 <1 <5 1.79 <1 36 32 32 9.06 <5 1.48 6 56 3.09 1615 4 0.18 8 1580 30 4.38 5 12 <10 <5 60 0.28 <5 200 <5 985700 446 449 3 20 116 0.4 2.94 10 48 <1 <5 2.57 <1 36 36 42 8.23 <5 0.62 8 52 2.19 1560 3 0.09 8 1680 24 4.87 <5 10 <10 <5 32 0.32 <5 146 <5 1185701 449 452 3 60 212 0.6 3.94 15 40 <1 <5 1.46 <1 31 38 96 >10 <5 0.70 6 38 2.51 2895 4 0.13 8 1600 27 5.17 5 9 <10 <5 34 0.28 <5 138 <5 785702 452 455 3 565 760 14.8 3.48 15 28 <1 10 0.75 6 26 52 8136 >10 <5 0.68 4 18 1.66 2360 5 0.14 5 1040 <3 5.55 5 7 <10 <5 36 0.18 <5 118 <5 485703 455 458 3 75 344 3.6 3.95 15 28 <1 10 0.70 <1 31 40 2212 >10 <5 0.41 2 18 1.75 2970 3 0.14 5 1360 30 4.65 <5 7 <10 <5 36 0.21 <5 110 <5 585704 458 461 3 85 324 1.4 4.25 10 60 <1 <5 0.87 <1 21 46 402 >10 <5 0.56 4 24 1.90 2665 3 0.15 5 1160 42 2.98 5 8 <10 <5 26 0.24 <5 132 <5 785705 461 464 3 40 438 1.0 5.05 10 148 <1 <5 0.69 <1 25 22 244 >10 <5 0.70 4 26 2.43 3365 2 0.13 6 1450 36 1.75 5 9 <10 <5 26 0.23 <5 146 <5 985706 464 467 3 105 322 1.8 4.31 10 32 <1 <5 0.85 <1 28 38 372 >10 <5 1.06 4 20 1.93 2575 2 0.15 7 1350 36 3.17 5 8 <10 <5 34 0.24 <5 132 <5 885707 467 470 3 55 208 1.2 4.86 10 66 <1 <5 1.26 <1 31 36 192 >10 <5 1.85 4 34 2.41 1975 3 0.16 6 1550 33 2.97 5 11 <10 <5 50 0.28 <5 174 <5 585708 470 473 3 100 274 5.4 5.09 10 44 <1 <5 1.28 <1 31 38 1166 >10 <5 2.12 2 30 2.37 1805 3 0.19 6 1450 30 3.81 5 10 <10 <5 46 0.26 <5 172 <5 785709 473 476 3 60 148 1.6 3.50 15 98 <1 <5 1.34 <1 30 54 370 7.29 <5 1.12 8 34 1.82 1240 2 0.15 7 1920 24 2.62 <5 8 <10 <5 56 0.32 <5 124 <5 785710 476 479 3 65 92 0.6 3.62 10 68 <1 <5 1.45 <1 38 36 308 6.71 <5 1.40 4 34 1.89 1050 2 0.16 6 1690 18 3.36 <5 9 <10 <5 38 0.27 <5 152 <5 1085711 479 481.5 2.5 50 94 0.4 4.93 10 76 1 <5 1.65 <1 35 38 76 7.06 <5 2.39 4 34 2.35 1055 3 0.21 6 1630 24 2.96 <5 11 <10 <5 54 0.31 <5 174 <5 985712 481.5 484 2.5 10 114 <0.2 1.83 <5 44 <1 <5 1.83 <1 22 84 44 4.21 <5 0.10 20 18 1.34 670 2 0.12 7 2740 18 0.49 <5 5 <10 <5 74 0.33 <5 82 <5 585713 484 487 3 45 58 0.6 3.66 10 42 1 <5 1.73 <1 31 76 64 8.07 <5 1.24 4 20 1.37 680 5 0.29 6 1210 36 5.68 5 8 <10 <5 60 0.24 <5 150 <5 785714 487 490 3 45 70 0.4 4.90 15 52 1 <5 2.07 <1 34 48 28 7.46 <5 2.01 4 20 1.91 775 3 0.35 6 1620 27 4.73 5 10 <10 <5 60 0.27 <5 188 <5 985715 490 493 3 30 70 0.2 4.42 5 60 <1 <5 1.63 <1 35 42 32 6.82 <5 2.12 4 22 1.96 800 3 0.31 6 1550 24 3.76 5 10 <10 <5 62 0.27 <5 180 <5 985716 493 496 3 80 80 0.8 4.02 10 46 <1 <5 1.34 <1 33 38 64 7.73 <5 1.97 4 24 1.87 875 2 0.26 6 1550 27 4.69 <5 10 <10 <5 54 0.27 <5 158 <5 985717 496 499 3 40 64 0.6 3.67 10 46 <1 <5 1.41 <1 32 54 40 7.13 <5 1.69 4 18 1.48 655 4 0.29 6 1470 21 4.68 <5 10 <10 <5 44 0.25 <5 164 <5 885718 499 502 3 25 100 0.2 5.28 <5 158 1 <5 2.03 <1 28 40 34 5.52 <5 2.39 4 24 2.25 1100 3 0.36 6 1630 24 1.47 <5 12 <10 <5 68 0.27 <5 200 <5 885719 502 505 3 30 94 0.4 4.66 <5 122 1 <5 1.54 <1 29 34 38 5.82 <5 2.28 4 26 2.13 1030 3 0.33 6 1560 21 2.06 <5 12 <10 <5 60 0.28 <5 194 <5 985720 505 508 3 20 86 0.2 4.96 5 152 1 <5 1.82 <1 31 36 30 5.18 <5 2.20 4 24 2.01 980 3 0.39 6 1510 21 1.56 <5 11 <10 <5 78 0.28 <5 192 <5 985721 508 511 3 20 124 <0.2 4.14 5 146 1 <5 1.43 <1 31 34 36 6.24 <5 2.56 6 26 2.40 980 2 0.38 6 1480 27 2.09 <5 11 <10 <5 64 0.16 <5 190 <5 385722 511 514 3 10 88 0.4 3.72 10 164 <1 <5 1.62 <1 31 44 184 5.15 <5 2.09 6 18 1.97 1000 3 0.37 6 1420 30 1.47 5 8 <10 <5 74 0.17 <5 174 <5 385723 514 516 2 10 96 <0.2 4.07 10 170 <1 <5 1.50 <1 26 38 28 5.29 <5 2.50 6 20 2.19 945 2 0.44 6 1460 36 1.43 <5 9 <10 <5 72 0.16 <5 190 <5 385724 516 519 3 5 90 <0.2 3.55 <5 218 <1 <5 1.47 <1 17 42 68 4.84 <5 2.28 6 20 2.02 990 3 0.28 5 1430 21 0.63 5 8 <10 <5 88 0.17 <5 174 <5 385725 519 522 3 10 98 <0.2 3.34 10 166 <1 <5 1.36 <1 25 42 128 5.10 <5 2.10 6 20 1.98 1010 2 0.29 5 1450 24 1.24 5 7 <10 <5 72 0.17 <5 172 <5 385726 522 525 3 10 92 <0.2 3.25 5 160 <1 <5 1.24 <1 36 40 28 5.28 <5 2.27 6 20 2.13 955 3 0.27 6 1390 27 1.51 5 7 <10 <5 90 0.17 <5 164 <5 285727 oreas 131b std. 10 >10000 3.02 32.2 0.80 80 76 1 <5 4.51 94 21 12 228 5.30 <5 0.62 14 16 2.97 1625 3 0.03 23 580 >10000 1.87 4.78 35 2 <10 <5 24 0.01 <5 10 10 885728 blank <5 2 <0.2 0.01 <5 8 <1 <5 0.01 <1 <1 <2 <2 0.02 <5 <0.01 <2 <2 <0.01 <5 <1 <0.01 <1 <10 3 0.02 <5 <1 <10 <5 <2 <0.01 <5 <2 <5 <185729 oreas 67a std. >1000 2.2 70 33.0 0.84 355 152 <1 20 0.32 <1 13 128 324 4.33 <5 0.04 4 4 0.47 155 6 0.13 35 300 162 1.24 75 1 <10 5 56 0.06 <5 26 <5 385730 blank 10 4 <0.2 0.01 <5 8 <1 <5 <0.01 <1 <1 <2 <2 0.02 <5 <0.01 <2 <2 <0.01 <5 <1 <0.01 <1 <10 <3 0.01 <5 <1 <10 <5 <2 <0.01 <5 <2 <5 <185731 525 528 3 15 136 <0.2 3.91 <5 204 <1 <5 1.16 <1 23 32 90 6.47 <5 2.45 8 30 2.95 1355 2 0.24 2 1350 21 0.43 <5 10 <10 <5 52 0.19 <5 202 <5 385732 528 531 3 5 84 <0.2 4.32 <5 206 <1 <5 1.71 <1 27 44 14 5.23 <5 2.65 8 16 2.36 960 3 0.46 4 1430 24 1.22 5 7 <10 <5 74 0.17 <5 188 <5 385733 531 534 3 >1000 1.03 140 0.6 3.95 15 116 <1 <5 1.50 <1 39 30 90 7.75 <5 2.42 8 30 2.48 1210 2 0.32 6 1330 30 2.94 <5 11 <10 <5 70 0.16 <5 190 <5 385734 534 537 3 5 124 <0.2 3.03 10 124 <1 <5 2.96 <1 40 138 26 6.43 <5 0.46 12 20 2.84 840 2 0.33 31 1260 24 0.27 5 10 <10 <5 104 0.25 <5 140 <5 385735 537 539.5 2.5 10 90 <0.2 2.92 5 110 <1 <5 3.03 <1 39 134 32 6.54 <5 0.38 12 22 2.87 820 2 0.28 30 1240 21 0.41 5 11 <10 <5 90 0.26 <5 144 <5 385736 539.5 542.5 3 65 150 1.0 4.04 10 50 <1 <5 1.55 <1 29 32 202 9.14 <5 2.10 6 38 2.40 1460 3 0.31 5 1310 39 4.45 5 12 <10 <5 50 0.14 <5 188 <5 385737 542.5 546 3.5 55 146 0.2 3.99 10 56 1 <5 1.53 <1 30 42 58 7.36 <5 2.15 6 22 1.91 1195 3 0.34 5 1410 30 3.93 5 7 <10 <5 48 0.15 <5 152 <5 285738 546 549 3 40 336 <0.2 3.64 10 58 1 <5 1.03 3 31 30 90 8.09 <5 2.19 6 24 1.94 1365 3 0.25 6 1450 24 3.96 <5 8 <10 <5 36 0.15 <5 140 <5 385739 549 552 3 50 142 0.4 3.07 15 46 <1 <5 0.77 <1 29 34 116 9.52 <5 1.95 4 24 1.77 1435 3 0.17 6 1360 21 5.21 <5 7 <10 <5 26 0.13 <5 116 <5 285740 552 555 3 65 220 2.8 2.66 15 30 <1 <5 0.49 <1 33 30 466 >10 <5 1.40 4 24 1.82 1930 3 0.10 6 1350 24 5.82 5 5 <10 <5 14 0.14 <5 92 <5 385741 555 558 3 45 86 <0.2 4.19 10 58 <1 <5 1.49 <1 29 46 28 7.69 <5 2.25 6 20 2.04 1080 3 0.39 4 1400 27 4.51 5 9 <10 <5 54 0.17 <5 168 <5 385742 558 561 3 30 108 <0.2 4.31 5 56 <1 <5 1.42 <1 26 46 26 7.41 <5 2.13 6 24 2.40 1270 3 0.35 3 1330 30 4.02 5 10 <10 <5 46 0.16 <5 170 <5 385743 561 563 2 40 236 <0.2 3.38 5 56 <1 <5 0.55 <1 25 28 26 9.44 <5 1.18 6 34 2.74 2715 2 0.13 3 1250 24 3.78 5 7 <10 <5 22 0.14 <5 114 <5 285744 563 566 3 80 190 0.8 2.93 15 32 <1 <5 0.64 <1 25 58 68 9.50 <5 1.44 4 22 1.90 1885 4 0.17 4 1130 24 5.12 5 6 <10 <5 22 0.13 <5 104 <5 2

85745 566 567 1 65 148 1.6 2.65 20 24 1 <5 0.85 <1 30 38 104 9.64 <5 1.54 2 16 1.25 1230 5 0.20 3 1450 39 7.01 5 7 <10 <5 24 0.15 <5 90 <5 285746 567 570 3 55 160 0.8 3.17 10 28 <1 <5 0.76 <1 29 38 64 9.42 <5 1.60 4 24 2.11 1800 4 0.18 3 1310 39 5.75 5 7 <10 <5 26 0.17 <5 110 <5 285747 570 573 3 110 118 1.0 3.51 10 36 <1 <5 0.90 <1 26 46 96 9.11 <5 2.01 4 26 2.28 1560 4 0.20 2 1200 24 4.94 5 9 <10 <5 30 0.17 <5 130 <5 285748 573 576 3 120 128 0.4 3.42 15 36 <1 <5 0.92 <1 25 68 26 9.24 <5 2.00 4 20 1.93 1605 6 0.24 3 990 24 5.22 5 7 <10 <5 34 0.14 <5 106 <5 285749 576 579 3 65 124 1.0 3.59 10 38 <1 <5 1.09 <1 24 62 90 7.97 <5 1.95 4 22 2.02 1530 3 0.30 3 1060 24 4.68 <5 9 <10 <5 44 0.14 <5 130 <5 285750 579 582 3 65 158 1.4 3.45 10 38 <1 <5 0.96 <1 25 40 138 7.71 <5 1.75 4 26 2.20 1480 3 0.27 3 1230 30 4.83 5 8 <10 <5 46 0.14 <5 124 <5 235801 582 585 3 40 112 0.2 5.37 5 130 1 <5 1.97 <1 26 30 22 5.80 <5 2.14 4 20 2.18 1125 3 0.44 5 1530 42 3.74 <5 12 <10 <5 64 0.23 <5 210 <5 735802 585 588 3 35 132 0.2 5.08 5 84 <1 <5 1.59 <1 28 26 22 6.90 <5 2.21 4 30 2.37 1320 3 0.35 4 1430 30 4.10 <5 11 <10 <5 60 0.23 <5 180 <5 635803 588 591 3 25 98 <0.2 3.15 5 138 <1 <5 1.15 <1 20 48 26 5.08 <5 1.38 4 24 1.53 1105 2 0.24 5 1430 18 2.29 <5 6 <10 <5 56 0.23 <5 114 <5 435804 591 594 3 40 104 <0.2 3.60 <5 240 <1 <5 1.78 <1 31 28 36 5.21 <5 1.46 6 20 1.67 1315 3 0.30 11 1570 27 1.68 <5 8 <10 <5 70 0.27 <5 188 <5 835805 594 596.5 2.5 35 80 <0.2 4.05 <5 270 <1 <5 1.63 <1 39 28 20 4.30 <5 1.68 6 18 1.68 910 3 0.40 10 1690 27 1.36 <5 6 <10 <5 86 0.27 <5 182 <5 835806 596.5 599.5 3 20 92 <0.2 2.55 5 186 <1 <5 1.56 <1 29 42 84 4.70 <5 0.57 18 26 1.49 810 2 0.31 15 2580 27 0.50 <5 6 <10 <5 64 0.33 <5 126 <5 735807 599.5 603 3.5 35 82 0.6 4.27 <5 334 <1 <5 1.53 <1 48 26 242 5.37 <5 2.09 8 20 1.85 975 3 0.38 13 1600 27 1.40 <5 8 <10 <5 88 0.29 <5 202 <5 935808 603 606 3 25 94 <0.2 3.63 <5 314 <1 <5 1.16 <1 31 22 72 5.01 <5 2.11 6 22 2.07 1040 2 0.23 9 1550 24 0.96 <5 7 <10 <5 84 0.31 <5 180 <5 935809 606 609 3 20 86 <0.2 4.23 <5 526 <1 <5 1.55 <1 26 34 14 4.56 <5 2.31 8 18 2.12 1030 3 0.35 15 1540 33 0.95 5 8 <10 <5 90 0.33 <5 196 <5 935810 609 612 3 35 74 <0.2 4.64 10 354 <1 <5 1.73 <1 35 28 18 5.48 <5 2.12 6 18 1.88 900 5 0.55 17 1600 42 2.74 <5 9 <10 <5 82 0.27 <5 208 <5 835811 612 615 3 30 60 <0.2 3.10 5 376 <1 <5 1.13 <1 26 34 20 4.43 <5 1.60 6 16 1.51 780 2 0.30 10 1400 27 2.31 <5 7 <10 <5 48 0.23 <5 144 <5 835812 615 618 3 30 68 <0.2 4.43 10 128 <1 <5 1.68 <1 37 30 16 6.16 <5 1.75 6 20 1.84 850 3 0.50 5 1460 27 4.01 <5 8 <10 <5 62 0.25 <5 188 <5 835813 618 621 3 100 66 <0.2 3.82 10 98 <1 <5 1.29 <1 45 34 18 6.14 <5 1.88 6 18 1.85 865 3 0.36 4 1430 24 3.84 <5 10 <10 <5 46 0.24 <5 182 <5 835814 621 624 3 60 98 <0.2 5.22 5 438 1 <5 1.82 <1 35 24 50 5.32 <5 2.60 6 22 2.40 1230 3 0.49 12 1560 36 1.32 <5 11 <10 <5 74 0.31 <5 236 <5 835815 624 627 3 30 68 <0.2 3.63 5 446 <1 <5 1.40 <1 42 38 16 5.33 <5 2.04 4 16 2.04 980 2 0.37 13 1430 33 2.27 <5 7 <10 <5 88 0.31 <5 190 <5 735816 627 630 3 25 84 <0.2 4.54 5 332 1 <5 1.72 <1 28 24 24 4.80 <5 2.12 6 20 2.02 1065 3 0.44 10 1500 30 1.32 <5 10 <10 <5 70 0.31 <5 210 <5 835817 630 633 3 20 86 0.4 4.30 5 306 1 <5 1.69 <1 27 30 204 4.62 <5 1.82 4 22 1.92 1105 2 0.34 11 1490 27 1.16 <5 9 <10 <5 60 0.26 <5 184 <5 735818 633 636 3 20 92 0.4 3.87 <5 264 <1 <5 1.32 <1 37 24 176 5.11 <5 1.98 4 20 1.87 1090 2 0.32 9 1660 24 1.26 <5 8 <10 <5 70 0.29 <5 192 <5 835819 636 639 3 30 80 0.2 3.80 5 296 <1 <5 1.56 <1 34 28 106 4.39 <5 1.74 6 16 1.65 930 2 0.34 9 1810 24 1.20 <5 6 <10 <5 100 0.28 <5 184 <5 835820 639 642 3 25 96 <0.2 3.07 <5 226 <1 <5 1.36 <1 28 30 30 4.40 <5 1.24 10 18 1.67 860 2 0.24 9 1780 21 1.19 <5 7 <10 <5 100 0.32 <5 162 <5 835821 642 645 3 30 94 <0.2 3.13 <5 194 <1 <5 1.49 <1 36 30 54 4.81 <5 1.11 8 20 1.52 935 2 0.25 8 2020 21 1.73 <5 6 <10 <5 90 0.26 <5 148 <5 735822 645 648 3 20 152 <0.2 2.51 5 124 <1 <5 1.57 <1 29 36 48 4.44 <5 0.36 18 28 1.37 1000 2 0.20 10 2590 24 0.69 <5 5 <10 <5 74 0.31 <5 106 <5 735823 648 651 3 25 120 <0.2 3.25 5 234 <1 <5 1.62 <1 27 32 38 4.32 <5 0.92 6 18 1.60 1020 2 0.23 8 1620 27 1.15 <5 5 <10 <5 112 0.26 <5 146 <5 735824 651 654 3 25 98 0.2 4.74 5 362 1 <5 1.83 <1 24 30 100 4.95 <5 2.15 4 16 1.96 1270 2 0.41 11 1540 33 0.96 <5 9 <10 <5 80 0.29 <5 216 <5 735825 654 657 3 35 78 <0.2 4.82 5 186 1 <5 1.84 <1 35 32 30 5.84 <5 2.00 4 14 1.73 1070 3 0.46 9 1540 33 3.18 <5 10 <10 <5 80 0.24 <5 202 <5 735826 657 660 3 30 76 0.4 4.65 <5 262 1 <5 1.91 <1 36 30 194 5.82 <5 1.80 6 16 1.60 1085 3 0.47 14 1610 30 3.03 <5 8 <10 <5 74 0.23 <5 194 <5 735827 660 663 3 25 108 <0.2 5.60 5 178 1 <5 2.04 <1 33 28 40 6.12 <5 2.19 6 18 1.94 1420 3 0.54 9 1760 30 2.80 <5 11 <10 <5 70 0.23 <5 228 <5 735828 663 666 3 35 88 <0.2 5.37 5 308 2 <5 2.31 <1 33 30 60 5.35 <5 1.80 6 16 1.58 1320 3 0.56 14 1750 36 2.77 <5 9 <10 <5 76 0.23 <5 218 <5 735829 666 669 3 20 98 <0.2 4.02 5 222 <1 <5 1.68 <1 28 50 16 4.52 <5 1.36 6 18 1.53 1185 2 0.48 11 1460 27 1.62 <5 6 <10 <5 138 0.25 <5 140 <5 535830 669 672 3 30 86 <0.2 4.36 <5 326 1 <5 1.99 <1 27 38 28 4.34 <5 1.14 6 20 1.49 1035 4 0.45 13 1440 33 1.70 <5 8 <10 <5 110 0.25 <5 184 <5 635831 672 675 3 20 272 <0.2 2.55 5 120 <1 <5 2.00 1 20 52 44 4.45 <5 0.25 20 26 1.42 965 2 0.22 13 2960 27 0.18 <5 5 <10 <5 76 0.28 <5 96 <5 635832 675 678 3 35 226 <0.2 2.32 <5 94 <1 <5 1.83 <1 20 58 10 4.42 <5 0.17 20 28 1.44 955 2 0.18 13 3130 18 0.03 <5 4 <10 <5 88 0.30 <5 84 <5 535833 678 682.5 4.5 10 214 <0.2 2.36 <5 102 <1 <5 1.88 <1 20 56 20 4.50 <5 0.18 22 28 1.44 975 1 0.20 13 3030 21 0.13 <5 4 <10 <5 80 0.29 <5 90 <5 635834 682.5 686 3.5 60 172 0.4 4.84 10 54 1 <5 1.48 <1 35 20 60 >10 <5 1.99 4 34 2.05 1355 6 0.34 7 1520 45 5.91 <5 11 10 <5 54 0.24 <5 192 <5 635835 686 689 3 50 78 <0.2 3.22 10 52 <1 <5 1.26 <1 31 34 48 6.48 <5 1.28 4 18 1.17 870 4 0.27 7 1440 21 4.95 <5 7 <10 <5 56 0.21 <5 126 <5 735836 689 692 3 35 146 <0.2 2.72 10 94 <1 <5 1.54 <1 29 48 30 6.49 <5 0.56 10 22 1.23 885 4 0.24 6 2020 21 4.06 <5 7 <10 <5 52 0.28 <5 112 <5 635837 692 695 3 15 142 <0.2 2.12 <5 70 <1 <5 1.85 <1 18 54 18 4.39 <5 0.16 22 26 1.40 970 1 0.17 10 2990 15 0.03 <5 5 <10 <5 72 0.32 <5 80 <5 635838 695 698 3 40 146 0.2 4.72 5 94 1 <5 2.11 <1 31 32 24 6.82 <5 1.46 4 18 1.74 970 3 0.32 7 1550 36 4.92 <5 9 <10 <5 78 0.26 <5 190 <5 835839 698 701 3 35 172 0.2 3.21 10 102 <1 <5 1.84 <1 31 36 42 5.81 <5 0.36 12 24 1.51 820 2 0.21 6 2160 33 3.22 <5 7 <10 <5 68 0.30 <5 126 <5 835840 701 704 3 30 106 <0.2 2.90 10 120 <1 <5 1.28 <1 24 56 20 5.21 <5 0.96 6 14 1.21 850 3 0.31 7 1390 24 3.19 <5 5 <10 <5 110 0.26 <5 100 <5 535841 704 707 3 20 88 <0.2 2.89 <5 150 <1 <5 1.69 <1 16 72 68 3.50 <5 0.52 10 18 1.35 860 2 0.33 9 1560 18 0.44 <5 4 <10 <5 132 0.30 <5 92 <5 335842 707 710.5 3.5 15 180 <0.2 2.16 <5 88 <1 <5 1.83 <1 18 56 44 4.45 <5 0.17 24 28 1.48 1095 2 0.16 10 2960 18 0.03 <5 4 <10 <5 62 0.32 <5 86 <5 635843 710.5 713 2.5 50 80 0.4 1.60 10 60 <1 <5 1.04 <1 39 62 44 6.37 <5 0.33 4 14 0.90 680 8 0.09 5 1010 27 4.58 <5 5 <10 <5 42 0.17 <5 80 <5 435844 713 716 3 35 70 <0.2 2.89 5 78 1 <5 1.18 <1 38 28 22 6.10 <5 1.35 6 16 1.44 725 4 0.22 6 1640 21 3.74 <5 9 <10 <5 62 0.27 <5 154 <5 835845 716 719 3 40 64 <0.2 3.73 <5 116 1 <5 1.68 <1 37 38 20 5.30 <5 1.34 4 14 1.52 730 3 0.36 6 1440 24 3.35 <5 9 <10 <5 98 0.25 <5 172 <5 835846 719 722 3 35 72 <0.2 3.62 5 156 <1 <5 1.80 <1 33 32 22 4.92 <5 1.09 6 20 1.69 865 3 0.36 7 1660 18 2.61 <5 8 <10 <5 90 0.28 <5 174 <5 1035847 722 725 3 25 70 <0.2 3.14 5 116 <1 <5 1.34 <1 38 34 22 5.68 <5 1.39 6 18 1.79 865 2 0.29 6 1560 18 3.15 <5 8 <10 <5 74 0.30 <5 174 <5 1035848 725 728 3 20 84 <0.2 3.28 <5 606 <1 <5 1.45 <1 27 38 18 4.49 <5 1.75 8 20 2.56 1080 3 0.21 8 1430 24 1.13 <5 8 <10 <5 132 0.37 <5 198 <5 935849 728 731 3 20 86 <0.2 3.42 <5 428 <1 <5 1.58 <1 41 42 10 4.58 <5 1.85 8 18 2.49 1160 2 0.21 8 1440 24 0.89 5 8 <10 <5 114 0.38 <5 198 <5 935850 731 734 3 30 90 <0.2 3.45 <5 250 <1 <5 1.41 <1 33 32 16 5.20 <5 1.71 6 22 2.37 1080 2 0.27 8 1430 24 1.71 5 8 <10 <5 118 0.34 <5 194 <5 835851 734 737 3 30 72 <0.2 3.54 <5 228 <1 <5 1.55 <1 35 42 14 5.25 <5 1.77 4 16 2.18 1000 2 0.33 7 1350 24 2.06 <5 7 <10 <5 136 0.34 <5 172 <5 735852 737 740 3 40 80 <0.2 3.70 <5 194 <1 <5 1.47 <1 35 38 12 5.87 <5 1.83 6 20 2.49 1050 3 0.37 10 1380 27 2.66 <5 7 <10 <5 114 0.33 <5 194 <5 735853 740 743 3 35 112 <0.2 5.04 <5 208 <1 <5 1.71 <1 33 26 16 5.97 <5 2.50 6 20 3.00 1390 2 0.57 9 1470 30 2.09 <5 7 <10 <5 120 0.32 <5 224 <5 735854 743 746 3 35 84 <0.2 4.03 5 124 <1 <5 1.44 <1 31 28 24 6.27 <5 1.77 4 22 2.46 1055 2 0.45 7 1410 27 3.39 <5 8 <10 <5 106 0.28 <5 212 <5 835855 746 749 3 30 90 <0.2 4.62 <5 220 <1 <5 1.71 <1 31 28 18 5.54 <5 2.21 6 18 2.61 1140 2 0.51 7 1530 24 1.96 <5 8 <10 <5 102 0.31 <5 216 <5 835856 749 752 3 35 72 <0.2 4.69 5 212 <1 <5 1.88 <1 35 30 26 5.70 <5 1.87 6 16 1.92 915 3 0.57 9 1610 24 2.41 <5 8 <10 <5 96 0.27 <5 218 <5 935857 752 755 3 50 84 <0.2 5.50 5 146 <1 <5 1.94 <1 31 20 12 6.42 <5 2.41 4 18 3.09 1020 2 0.72 12 1630 36 3.45 <5 9 <10 <5 114 0.25 <5 220 <5 835858 755 758 3 35 74 <0.2 5.13 5 170 1 <5 1.84 <1 31 24 20 5.68 <5 2.20 4 18 2.43 955 3 0.52 7 1510 24 2.76 <5 11 <10 <5 106 0.28 <5 220 <5 935859 758 761 3 45 104 <0.2 6.72 5 226 1 <5 2.64 <1 31 26 26 6.52 <5 2.54 4 20 2.95 1415 3 0.67 11 1470 39 2.64 <5 6 <10 <5 128 0.32 <5 234 <5 735860 761 764 3 45 100 <0.2 6.48 <5 180 1 <5 2.71 <1 29 32 44 6.71 <5 2.23 4 20 2.71 1235 3 0.69 12 1520 42 3.47 <5 6 <10 <5 112 0.28 <5 248 <5 735861 764 767 3 35 102 <0.2 5.47 5 130 1 <5 2.18 <1 32 26 26 6.76 <5 1.83 4 26 2.43 1210 3 0.48 4 1510 27 4.13 <5 9 <10 <5 88 0.30 <5 216 <5 735862 767 770 3 25 116 <0.2 5.46 5 92 1 <5 2.09 <1 34 20 42 7.05 <5 2.02 4 22 2.20 1535 3 0.39 7 1570 27 4.63 <5 11 10 <5 68 0.26 <5 196 <5 935863 770 773 3 20 136 <0.2 3.50 5 92 1 <5 1.60 <1 30 34 30 6.71 <5 0.83 14 26 1.78 935 2 0.27 5 2070 27 3.57 <5 8 <10 <5 72 0.32 <5 140 <5 735864 773 776 3 25 150 <0.2 6.01 5 134 2 <5 2.16 <1 36 16 48 7.02 <5 2.24 4 28 2.38 2120 3 0.32 6 1520 27 2.77 <5 12 <10 <5 88 0.30 <5 218 <5 735865 776 778 2 40 80 <0.2 4.06 10 70 1 <5 1.10 <1 36 28 70 8.91 <5 1.90 6 28 2.17 1085 3 0.22 5 1300 21 4.86 5 8 <10 <5 66 0.26 <5 148 <5 735866 778 780 2 30 74 <0.2 5.31 <5 156 1 <5 2.10 <1 32 24 16 6.10 <5 2.07 6 24 2.50 955 3 0.40 6 1360 27 3.05 5 10 <10 <5 94 0.30 <5 208 <5 835867 780 784 4 25 184 <0.2 2.98 5 108 <1 <5 1.72 <1 27 52 30 5.99 <5 0.74 16 30 2.08 1125 2 0.16 7 2290 24 1.76 <5 7 <10 <5 62 0.32 <5 128 <5 635868 784 788.5 4.5 35 114 1.0 1.97 5 42 2 <5 0.81 <1 31 38 42 8.19 <5 0.91 2 12 0.73 685 3 0.19 8 1480 36 6.88 <5 4 <10 <5 34 0.10 <5 68 <5 635869 788.5 792 3.5 20 74 <0.2 1.34 <5 110 <1 <5 0.66 <1 6 106 18 1.32 <5 0.26 12 8 0.52 485 3 0.16 4 480 12 0.31 <5 2 <10 <5 32 0.10 <5 32 <5 735870 792 794 2 20 52 <0.2 1.42 <5 140 <1 <5 0.73 <1 6 102 10 1.21 <5 0.23 12 6 0.31 385 4 0.19 3 350 12 0.39 <5 2 <10 <5 52 0.09 <5 24 <5 735871 794 796 2 45 90 1.0 0.84 5 42 1 <5 0.40 <1 32 36 34 7.66 <5 0.39 4 4 0.17 185 5 0.07 8 1330 30 6.34 <5 3 <10 <5 18 0.09 <5 40 <5 6

MC-11-03 35872 144.5 148 3.5 205 294 2.1 3.18 25 64 <1 <5 1.89 <1 30 24 140 7.81 <5 1.33 28 22 2.09 2875 3 0.19 8 1420 36 3.62 <5 6 <10 <5 40 0.19 <5 128 <5 9

35873 148 151 3 20 188 0.8 3.55 10 124 <1 <5 1.37 <1 32 28 40 6.10 <5 1.46 8 26 2.78 2315 3 0.22 7 1590 27 1.81 <5 7 <10 <5 48 0.27 <5 170 <5 935874 151 154 3 20 166 0.6 2.25 10 90 <1 <5 1.64 <1 22 34 22 3.70 <5 0.52 8 18 1.73 1825 2 0.08 8 1630 39 0.95 <5 5 <10 <5 50 0.29 <5 126 <5 935875 154 158 4 25 150 1.6 3.27 15 104 <1 <5 1.44 <1 42 32 138 5.81 <5 1.47 8 22 2.39 1895 2 0.20 9 1700 30 2.26 <5 6 <10 <5 58 0.26 <5 158 <5 835876 216 218 2 15 128 0.6 2.63 5 78 <1 <5 1.26 <1 36 32 26 4.87 <5 0.48 6 26 2.19 1305 2 0.06 12 1150 15 0.66 <5 8 <10 <5 94 0.31 <5 150 <5 835877 218 219 1 15 196 1.0 2.83 10 62 <1 <5 1.24 <1 44 36 36 6.34 <5 0.17 6 28 2.43 1725 2 0.04 12 1150 18 1.40 <5 8 <10 <5 82 0.30 <5 136 <5 835878 219 222 3 15 60 0.6 1.64 5 50 <1 <5 1.67 <1 29 56 18 3.01 <5 0.20 4 12 0.81 775 2 0.04 6 780 12 0.80 <5 5 <10 <5 138 0.21 <5 82 <5 635879 222 225.5 3.5 15 102 0.6 2.47 5 88 <1 <5 1.41 <1 28 22 26 5.13 <5 0.41 8 22 2.03 1455 2 0.05 7 1200 15 1.10 <5 7 <10 <5 92 0.30 <5 136 <5 935880 225.5 229.5 4 20 100 2.6 2.49 10 38 <1 <5 2.36 <1 55 12 524 6.11 <5 0.33 8 42 2.23 1350 2 0.05 6 1550 18 1.92 <5 7 <10 <5 88 0.23 <5 132 <5 1035881 229.5 235 5.5 10 146 0.4 1.82 5 20 <1 <5 2.70 <1 22 42 34 4.72 <5 0.14 18 40 1.78 885 2 0.06 8 2930 12 0.11 <5 5 <10 <5 52 0.28 <5 90 <5 535882 235 238 3 35 128 1.2 3.88 10 108 <1 <5 1.77 <1 28 22 100 5.86 <5 1.76 6 24 2.31 1155 3 0.33 7 1420 78 2.19 <5 9 <10 <5 60 0.25 <5 182 <5 735883 238 241 3 30 258 1.0 4.09 10 40 <1 <5 1.94 1 31 28 64 5.46 <5 1.70 4 18 1.76 1265 3 0.40 9 1130 30 2.95 <5 8 <10 <5 64 0.23 <5 178 <5 735884 241 244 3 100 2446 2.2 3.22 10 28 <1 <5 2.02 18 34 38 220 5.04 <5 0.98 4 16 1.57 1965 4 0.25 9 1140 57 3.64 <5 6 <10 <5 58 0.23 <5 144 <5 735885 244 247 3 65 1086 2.4 4.68 10 60 1 <5 2.24 6 28 36 76 6.30 <5 1.68 4 16 1.92 2350 3 0.43 5 1440 159 4.95 <5 7 <10 <5 52 0.26 <5 174 <5 835886 247 250 3 75 424 1.6 4.49 15 50 1 <5 2.71 2 34 28 54 7.18 <5 1.49 4 18 1.65 2975 4 0.38 10 1140 174 6.20 <5 11 <10 <5 48 0.25 <5 186 <5 835887 250 253 3 40 142 0.8 2.12 15 74 <1 <5 1.83 <1 19 52 16 4.01 <5 0.52 6 24 1.14 1320 2 0.17 11 1110 54 2.39 <5 5 <10 <5 44 0.20 <5 90 <5 535888 253 256 3 20 68 0.4 1.33 5 24 <1 <5 1.16 <1 12 60 40 2.60 <5 0.19 6 18 1.06 855 2 0.08 12 940 9 0.41 <5 2 <10 <5 52 0.17 <5 50 <5 335889 256 259.5 3.5 65 54 0.4 1.59 25 52 <1 <5 0.73 <1 23 64 8 3.47 <5 0.49 6 14 0.91 590 2 0.13 11 900 15 1.71 <5 2 <10 <5 44 0.14 <5 44 <5 235890 oreas 67a std. >1000 2.26 70 33.4 1.02 345 94 <1 25 0.37 <1 13 148 334 4.12 <5 0.04 4 4 0.43 160 6 0.15 35 330 165 1.27 80 1 10 5 56 0.08 <5 26 <5 335891 blank <5 <2 <0.2 0.01 <5 8 <1 <5 <0.01 <1 <1 <2 <2 0.02 <5 <0.01 <2 <2 <0.01 <5 <1 <0.01 <1 <10 <3 0.01 <5 <1 <10 <5 <2 <0.01 <5 <2 <5 <135892 blank <5 <2 <0.2 0.01 <5 6 <1 <5 <0.01 <1 <1 <2 <2 0.02 <5 <0.01 <2 <2 <0.01 <5 <1 <0.01 <1 <10 <3 0.01 <5 <1 <10 <5 <2 <0.01 <5 <2 <5 <135893 280 283 3 55 82 1.4 2.08 10 38 <1 <5 1.46 <1 47 50 56 6.67 <5 0.69 6 14 1.00 785 4 0.19 9 930 48 5.50 <5 7 <10 <5 46 0.21 <5 112 <5 735894 283 286 3 55 120 0.8 3.62 10 50 1 <5 1.91 <1 32 30 44 6.64 <5 1.33 4 24 1.78 1160 3 0.24 8 1130 39 4.61 <5 9 <10 <5 50 0.23 <5 166 <5 835895 286 288 2 95 132 1.2 3.71 15 30 <1 <5 1.47 <1 27 28 64 8.63 <5 1.47 4 30 1.93 1670 5 0.20 6 1230 36 4.97 <5 9 <10 <5 38 0.23 <5 154 <5 635896 288 290.5 2.5 60 76 0.8 1.80 10 34 <1 <5 1.37 <1 26 48 22 6.86 <5 0.45 2 20 1.04 875 4 0.11 6 950 24 5.71 <5 5 <10 <5 32 0.16 <5 86 <5 635897 290.5 291.5 1 15 104 0.4 1.71 10 30 <1 <5 2.53 <1 25 48 16 5.33 <5 0.14 20 26 1.73 945 3 0.07 8 2710 18 0.91 <5 8 <10 <5 44 0.40 <5 120 <5 735898 291.5 296 4.5 55 1184 3.0 3.86 10 32 1 <5 2.04 8 32 36 96 7.57 <5 1.08 4 16 1.34 1015 3 0.40 7 1300 393 7.37 <5 8 <10 <5 46 0.20 <5 160 <5 735899 296 298 2 25 842 4.0 3.79 10 38 1 <5 2.05 5 31 32 64 6.91 <5 0.93 4 18 1.31 1355 3 0.46 7 1290 315 7.31 <5 8 <10 <5 50 0.19 <5 162 <5 735900 298 301 3 20 428 3.0 3.31 10 34 1 <5 1.70 2 31 30 86 7.73 <5 0.93 4 18 1.41 1450 2 0.39 7 1250 135 7.69 <5 8 <10 <5 46 0.18 <5 148 <5 635901 301 304 3 25 668 4.0 3.82 10 32 1 <5 1.92 4 32 36 188 8.10 <5 1.13 4 16 1.36 1505 3 0.47 7 1280 219 7.86 <5 8 10 <5 44 0.18 <5 168 <5 635902 304 307 3 70 1318 2.2 2.84 10 20 1 <5 0.91 8 30 18 82 7.59 <5 1.32 2 20 1.47 1395 3 0.18 7 1260 66 6.95 <5 5 <10 <5 30 0.17 <5 98 <5 535903 307 310 3 35 502 3.4 2.79 10 24 <1 <5 1.10 3 31 20 56 7.59 <5 1.05 4 14 1.21 1150 3 0.30 7 1360 168 7.40 <5 6 <10 <5 38 0.18 <5 116 <5 635904 310 313 3 40 164 1.2 3.97 10 38 <1 <5 1.46 <1 32 26 64 7.38 <5 1.23 4 26 2.20 1675 4 0.39 7 1320 27 5.28 <5 7 <10 <5 46 0.21 <5 140 <5 735905 313 316 3 40 124 0.6 4.38 10 70 <1 <5 1.41 <1 40 20 52 6.25 <5 1.89 4 28 2.85 1470 3 0.28 7 1370 21 2.49 <5 7 <10 <5 46 0.27 <5 162 <5 835906 316 319 3 45 186 0.6 4.77 10 164 <1 <5 0.98 <1 30 12 100 8.18 <5 2.17 4 36 3.17 1815 3 0.20 7 1350 21 1.69 <5 7 <10 <5 50 0.26 <5 160 <5 835907 319 322 3 40 120 0.6 4.71 10 152 <1 <5 1.23 <1 35 10 88 7.36 <5 2.56 6 30 2.91 1355 3 0.23 7 1390 21 1.41 <5 8 <10 <5 46 0.26 <5 166 <5 935908 322 328 6 80 208 1.0 4.35 10 48 <1 <5 1.20 <1 33 12 212 7.74 <5 1.87 4 32 3.01 1595 3 0.23 7 1350 24 3.32 <5 7 <10 <5 42 0.24 <5 152 <5 735909 328 331 3 60 406 1.4 4.20 15 26 <1 <5 1.01 2 33 10 256 9.80 <5 1.41 2 38 3.12 2325 4 0.18 7 1340 24 5.48 <5 7 <10 <5 48 0.22 <5 140 <5 635910 331 334 3 40 208 0.6 4.64 10 28 1 <5 1.78 <1 32 26 66 7.81 <5 1.89 2 18 2.40 1100 3 0.31 8 1340 27 6.07 <5 8 <10 <5 76 0.18 <5 170 <5 535911 334 337 3 50 118 1.0 2.76 15 44 <1 <5 0.99 <1 32 22 48 7.59 <5 0.93 4 24 1.78 825 4 0.17 8 1500 93 4.63 <5 7 <10 <5 46 0.20 <5 124 <5 635912 376 379 3 10 104 0.4 3.12 5 140 <1 <5 1.60 <1 21 32 20 3.99 <5 0.73 6 24 2.24 1070 3 0.19 8 1310 24 0.53 <5 6 <10 <5 88 0.24 <5 144 <5 635913 379 382 3 25 182 0.4 3.54 10 70 <1 <5 0.87 <1 28 20 48 6.58 <5 1.47 4 28 2.77 1690 4 0.18 9 1380 21 2.68 <5 8 <10 <5 38 0.20 <5 164 <5 735914 382 385 3 15 92 0.2 4.19 10 240 <1 <5 1.81 <1 24 28 40 4.23 <5 1.65 4 18 2.23 1100 8 0.36 9 1340 18 0.71 <5 8 <10 <5 74 0.24 <5 162 <5 635915 385 388 3 20 112 0.6 4.33 10 90 <1 <5 1.53 <1 29 22 116 5.71 <5 1.99 4 20 2.47 1125 5 0.35 9 1390 21 2.06 <5 7 <10 <5 64 0.23 <5 160 <5 635916 388 391 3 70 222 1.2 4.35 20 34 <1 <5 0.88 <1 32 18 74 9.92 <5 1.47 4 30 2.82 2955 6 0.17 9 1310 27 3.73 <5 8 <10 <5 28 0.21 <5 158 5 535917 391 394 3 45 316 1.6 4.59 20 110 <1 <5 0.63 <1 30 12 132 >10 <5 1.06 2 36 2.90 4105 4 0.11 9 1200 30 2.39 <5 9 <10 <5 46 0.21 <5 156 5 535918 394 397 3 45 282 1.6 3.87 20 34 <1 <5 0.62 <1 32 14 60 >10 <5 1.00 4 32 2.38 3520 4 0.13 8 1230 33 4.55 <5 6 <10 <5 32 0.18 <5 102 5 535919 397 400 3 40 498 1.2 4.13 10 28 1 <5 1.42 2 31 20 56 7.45 <5 1.71 2 24 2.59 2075 4 0.25 9 1510 57 5.92 <5 9 <10 <5 70 0.20 <5 156 <5 635920 400 403 3 30 726 2.2 4.39 5 26 <1 <5 1.68 4 33 26 76 7.34 <5 1.73 4 24 2.67 1800 4 0.47 10 1760 357 6.86 <5 10 10 <5 86 0.21 <5 178 <5 535921 403 408 5 20 478 1.6 4.95 10 34 <1 <5 1.87 3 32 24 48 6.91 <5 1.72 2 32 3.17 1670 5 0.49 10 1730 78 6.07 <5 10 <10 <5 90 0.20 <5 204 <5 635922 408 411 3 35 134 1.8 4.56 10 30 <1 <5 2.03 <1 34 36 72 7.55 <5 1.66 2 28 2.40 1330 4 0.48 11 1800 48 7.68 <5 10 10 <5 80 0.21 <5 176 <5 635923 411 414 3 25 132 0.6 5.73 10 34 1 <5 2.37 <1 34 22 58 7.26 <5 2.27 2 30 3.68 1415 4 0.42 11 1780 36 6.95 <5 11 <10 <5 122 0.22 <5 216 <5 635924 414 417 3 20 118 1.0 4.79 10 62 <1 <5 2.30 <1 35 26 118 5.32 <5 1.55 4 26 2.86 1590 4 0.25 10 1770 24 2.75 <5 7 <10 <5 114 0.24 <5 170 <5 635925 417 420 3 15 122 1.0 4.86 10 122 <1 <5 2.44 <1 26 26 370 4.66 <5 1.84 4 26 2.82 1520 6 0.19 11 1770 21 1.54 <5 6 <10 <5 92 0.25 <5 182 <5 635926 460 463 3 150 232 1.2 5.07 15 30 <1 <5 1.52 <1 33 14 78 9.68 <5 1.67 4 38 3.09 2895 4 0.20 8 1600 30 4.97 <5 8 <10 <5 48 0.24 <5 158 <5 635927 oreas 67a std. >1000 2.18 70 31.6 0.92 350 154 <1 20 0.32 <1 13 140 318 4.12 <5 0.04 6 4 0.48 155 6 0.15 37 310 174 1.27 75 1 10 5 56 0.07 <5 26 <5 335928 blank 15 2 <0.2 0.01 <5 8 <1 <5 <0.01 <1 <1 <2 <2 0.02 <5 <0.01 <2 <2 <0.01 <5 <1 <0.01 <1 <10 <3 0.01 <5 <1 <10 <5 <2 <0.01 <5 <2 <5 <135929 463 466 3 10 110 0.4 5.50 10 172 1 <5 2.19 <1 22 18 104 5.19 <5 2.17 4 24 2.65 1485 4 0.35 7 1440 24 1.16 <5 7 <10 <5 66 0.23 <5 162 <5 635930 466 469 3 30 116 2.0 5.53 5 160 1 <5 2.03 <1 26 18 844 5.30 <5 2.47 4 22 2.57 1375 4 0.36 6 1370 24 1.11 <5 8 <10 <5 64 0.24 <5 156 <5 635931 469 472 3 45 122 0.8 4.84 15 48 1 <5 1.36 <1 27 14 168 8.09 <5 2.20 4 30 2.65 1750 4 0.24 7 1380 24 3.16 <5 7 <10 <5 42 0.23 <5 136 <5 635932 472 475 3 40 114 0.8 4.83 10 52 1 <5 1.53 <1 26 12 170 6.95 <5 2.25 4 26 2.50 1475 3 0.29 6 1430 21 2.96 <5 7 <10 <5 58 0.23 <5 134 <5 735933 475 478 3 30 108 0.6 4.63 30 50 1 <5 1.81 <1 30 20 136 7.32 <5 2.08 4 24 2.29 1095 4 0.30 6 1360 24 4.75 <5 6 <10 <5 88 0.22 <5 132 <5 635934 478 481 3 15 90 0.4 4.95 10 66 1 <5 2.14 <1 29 22 30 5.40 <5 2.02 4 20 2.28 910 3 0.45 6 1420 24 3.32 <5 7 <10 <5 74 0.24 <5 150 <5 835935 481 484 3 10 140 0.6 5.38 10 182 1 <5 2.37 <1 24 18 18 4.14 <5 2.15 4 22 2.41 1150 4 0.53 7 1410 45 0.99 <5 8 <10 <5 88 0.23 <5 158 <5 735936 484 487 3 25 116 0.8 4.14 10 112 <1 <5 1.35 <1 28 18 218 5.47 <5 1.97 4 26 2.37 1380 3 0.32 6 1460 18 1.72 <5 7 <10 <5 74 0.24 <5 132 <5 735937 487 490 3 20 80 0.4 4.06 15 88 1 <5 1.69 <1 28 36 38 5.33 <5 1.67 6 22 2.21 895 3 0.41 8 1450 21 2.67 <5 7 <10 <5 100 0.26 <5 154 <5 635938 490 493 3 15 70 0.4 3.53 10 108 <1 <5 1.55 <1 21 50 20 4.20 <5 1.64 6 16 1.71 750 3 0.38 8 1390 18 1.92 <5 5 <10 <5 120 0.25 <5 104 <5 535939 493 496 3 10 68 0.2 2.31 5 102 <1 <5 1.16 <1 15 66 8 3.30 <5 0.89 6 14 1.52 720 4 0.25 10 1310 12 0.42 <5 3 <10 <5 112 0.23 <5 88 <5 435940 496 499 3 30 254 0.4 4.29 15 24 <1 <5 1.08 <1 29 26 28 8.50 <5 1.51 4 30 2.96 2650 3 0.26 8 1450 27 5.02 <5 7 20 <5 50 0.21 <5 124 <5 635941 499 502 3 50 786 0.6 3.26 15 18 <1 <5 0.74 8 31 30 92 9.86 <5 1.04 4 24 2.22 2235 3 0.15 9 1140 36 6.40 <5 6 20 <5 42 0.20 <5 98 5 535942 502 505 3 70 224 1.0 3.31 15 24 <1 <5 0.51 <1 29 16 66 >10 <5 0.85 2 30 2.30 2385 3 0.09 9 1340 36 5.10 <5 6 <10 <5 18 0.20 <5 76 5 535943 505 508 3 25 188 0.8 4.91 15 96 <1 <5 0.91 <1 31 14 130 >10 <5 1.18 4 36 3.22 3090 4 0.21 10 1310 24 2.10 <5 9 <10 <5 42 0.22 <5 152 5 635944 508 511 3 70 156 1.0 3.49 15 28 <1 <5 0.73 <1 31 30 92 8.16 <5 1.23 4 24 2.48 1970 3 0.18 9 1280 24 4.00 <5 7 <10 <5 36 0.21 <5 114 <5 635945 511 514 3 85 3580 1.2 4.25 20 28 <1 <5 0.99 23 28 20 68 9.76 <5 1.61 4 26 2.51 2160 5 0.24 9 1250 1986 3.54 <5 8 <10 <5 64 0.22 <5 146 5 635946 514 517 3 50 464 0.8 4.06 15 38 <1 <5 0.85 2 28 18 88 8.31 <5 1.77 4 28 2.80 2200 3 0.22 9 1310 87 2.40 <5 9 <10 <5 66 0.24 <5 160 <5 735947 517 520 3 15 108 0.4 4.29 10 58 <1 <5 1.56 <1 28 28 40 5.54 <5 1.80 4 18 2.48 1335 3 0.43 8 1320 21 1.93 <5 8 <10 <5 134 0.25 <5 188 <5 735948 520 523 3 50 168 0.8 3.62 15 22 <1 <5 0.90 <1 30 26 190 8.57 <5 1.73 2 24 2.47 1620 3 0.24 9 1280 27 5.48 <5 8 <10 <5 60 0.20 <5 154 <5 635949 523 526 3 90 498 2.0 3.47 15 32 <1 <5 1.17 3 35 30 560 6.71 <5 1.73 4 18 2.16 1135 4 0.30 8 1230 78 3.88 <5 9 <10 <5 70 0.22 <5 154 <5 635950 526 529 3 40 164 1.2 4.16 10 46 <1 <5 1.28 <1 35 30 260 6.88 <5 2.00 4 22 2.70 1395 3 0.34 9 1260 36 2.92 <5 8 <10 <5 78 0.24 <5 170 <5 5

88051 529 532 3 30 144 1.0 4.49 10 78 <1 <5 1.34 <1 30 22 208 5.86 <5 2.13 4 24 2.80 1485 3 0.36 9 1320 24 1.96 <5 9 <10 <5 74 0.25 <5 174 <5 688052 532 533.5 1.5 95 178 6.2 3.49 15 26 <1 <5 0.79 <1 26 42 1390 8.29 <5 1.69 2 24 2.49 1620 4 0.18 8 1040 33 4.55 <5 8 <10 <5 46 0.19 <5 124 <5 488053 533.5 537 3.5 75 156 1.0 4.93 15 44 <1 <5 1.64 <1 31 20 154 6.75 <5 1.89 4 30 3.20 1600 3 0.41 9 1380 27 3.79 <5 10 <10 <5 84 0.21 <5 172 <5 688054 537 538.5 1.5 15 196 0.4 1.89 5 36 <1 <5 1.75 <1 19 44 48 4.67 <5 0.09 24 34 1.53 1035 2 0.07 7 2920 9 0.01 <5 4 <10 <5 52 0.34 <5 84 <5 688055 538.5 541.5 3 85 166 3.2 3.31 15 36 <1 <5 1.18 <1 29 22 764 7.59 <5 1.29 4 28 2.24 1715 4 0.14 8 1250 21 4.47 <5 7 <10 <5 54 0.19 <5 124 <5 588056 541.5 543.5 2 235 104 12.4 1.96 10 16 <1 <5 0.66 <1 28 50 3686 7.34 <5 1.01 <2 12 1.00 915 10 0.12 8 970 15 5.82 <5 5 <10 <5 62 0.17 <5 68 <5 288057 543.5 549 5.5 30 246 0.4 2.07 5 52 <1 <5 1.57 <1 22 46 36 4.71 <5 0.15 18 36 1.50 920 2 0.07 9 2820 15 0.53 <5 4 <10 <5 54 0.29 <5 78 <5 588058 549 551 2 110 174 2.0 1.94 10 16 <1 <5 0.48 <1 28 52 628 7.60 <5 0.99 <2 18 1.19 990 7 0.08 8 920 36 5.58 <5 6 <10 <5 56 0.17 <5 90 <5 388059 551 554 3 40 1006 0.6 4.52 10 30 1 <5 2.37 7 30 42 150 7.39 <5 1.21 2 14 1.51 650 4 0.29 10 1390 93 7.38 <5 9 <10 <5 114 0.19 <5 156 <5 588060 554 557 3 40 306 0.8 5.79 10 64 <1 <5 2.38 <1 31 32 56 6.12 <5 2.11 2 24 3.08 1515 4 0.54 10 1390 30 5.82 <5 11 <10 <5 104 0.21 <5 176 <5 588061 557 559 2 20 90 0.4 4.14 10 34 <1 <5 1.61 <1 29 34 34 6.69 <5 1.70 2 20 2.42 815 3 0.49 9 1280 21 6.58 <5 10 <10 <5 90 0.18 <5 162 <5 588062 559 563 4 30 96 0.4 4.27 10 42 <1 <5 1.57 <1 34 26 38 5.43 <5 1.98 4 20 2.47 1000 3 0.39 8 1290 21 3.31 <5 9 <10 <5 108 0.21 <5 162 <5 588063 563 566 3 30 120 0.4 4.43 15 44 <1 <5 1.36 <1 34 26 48 6.39 <5 2.30 4 26 2.87 1390 5 0.33 9 1420 21 3.62 <5 9 <10 <5 88 0.26 <5 166 <5 688064 566 569 3 30 138 0.8 4.70 15 38 <1 <5 1.28 <1 31 18 120 7.10 <5 2.38 4 34 3.34 1745 4 0.29 8 1350 21 4.33 <5 10 <10 <5 74 0.27 <5 164 <5 688065 569 571.5 2.5 45 156 1.0 4.53 15 34 <1 <5 1.26 <1 31 18 112 7.74 <5 2.06 4 42 3.14 1855 4 0.23 9 1300 24 4.47 <5 12 <10 <5 86 0.20 <5 192 <5 688066 571.5 578 6.5 10 158 0.4 2.98 10 70 <1 <5 2.92 1 38 114 34 6.38 <5 0.19 12 26 2.94 1200 2 0.23 35 1350 24 0.19 <5 12 <10 <5 128 0.32 <5 144 <5 988067 578 580 2 20 220 1.0 3.01 15 100 1 <5 0.28 <1 29 12 28 7.51 <5 0.71 14 58 2.42 1455 3 0.04 9 1410 24 2.09 <5 7 <10 <5 8 0.04 <5 112 <5 1288068 580 583 3 60 60 0.2 0.68 <5 92 <1 <5 0.37 <1 5 72 108 2.06 <5 0.29 12 6 0.26 385 2 0.02 3 440 6 0.17 <5 1 <10 <5 10 0.08 <5 22 <5 788069 583 585.5 2.5 35 174 0.2 2.04 5 40 <1 <5 1.40 <1 18 38 6 4.98 <5 0.13 22 32 1.41 1090 2 0.06 7 3000 9 <0.01 <5 4 <10 <5 26 0.37 <5 82 <5 688070 585.5 590 4.5 45 32 0.2 0.49 5 96 <1 <5 0.08 <1 5 82 44 2.02 <5 0.28 14 4 0.12 285 3 0.02 3 290 6 0.02 <5 <1 <10 <5 8 0.03 <5 18 <5 788071 345 351 6 40 176 1.0 4.93 15 58 <1 <5 1.63 <1 34 12 154 7.03 <5 1.91 4 28 2.94 1870 3 0.27 7 1380 27 2.88 <5 7 <10 <5 54 0.25 <5 156 <5 788072 oreas 67a std. >1000 2.18 68 32.2 0.90 330 90 <1 20 0.30 <1 12 134 328 4.13 <5 0.05 4 4 0.45 155 5 0.14 34 300 162 1.30 75 1 10 5 50 0.07 <5 24 <5 388073 blank <5 2 <0.2 <0.01 <5 6 <1 <5 <0.01 <1 <1 <2 <2 0.02 <5 <0.01 <2 <2 <0.01 <5 <1 0.01 <1 <10 <3 0.01 <5 <1 <10 <5 <2 <0.01 <5 <2 <5 <188074 blank <5 <2 <0.2 0.01 <5 6 <1 <5 <0.01 <1 <1 <2 <2 0.02 <5 <0.01 <2 <2 <0.01 <5 <1 <0.01 <1 <10 <3 0.01 <5 <1 <10 <5 <2 <0.01 <5 <2 <5 <1

DIAMOND DRILL RECORD Project: Dalhousie

Reliant Gold Corp. DDH No.: MC-11-02 page: 1

Collar Location: UTM NAD 83 Zone 09 0441764E 6213765N , ele. 1144m Start Date: July 16/11

Length of Hole: 796' Completion Date: July 20/11

Dip at collar: -35 acid tests 180' 35 deg, 296' 33 deg, 536' 32 deg, 776' 30 deg. Claim Number: Rock of Ages

Azimuth at Collar: 025 deg Logged By: Trevor Boyd

Core Diameter: BTW Logging Date: July 21/11

Drill Contractor: More Core Diamond Drilling Ltd. Storage: More Core Yard, Stewart

Geological DESCRIPTION Sample Sample Assays

From To Code No. From To Length Cu, Zn, Au, Ag

0 51 0 boulders see sample list see sample list

51.00 72.00 0 sand and certificates and certificates

72.00 236.00 2c Altered Intermediate Volcanic Rock, green grey, massive, pervasively chloritized

>sericitization>silicification, 10-15% x-cutting qtz-carb veining,

sections of spotted chloritoid and <2 mm carbonate amygules, non-magnetic

variable diss fine py with sph? varies from 2% up to 10%.

126-135.5 ' diss py 5-10% with poss sph noted

166.5-180.5 ' diss py 5-10% with poss sph and cpy

193.0-227.0 ' diss py 5-10%

201-201' missing core

236.00 311.00 8 Altered Intrusive (grandodiorite) dark green grey, massive, porphyritic with dom.

qtz and lessor plag visible xstals, highly sericitized>chloritization>silicification

massive, sericite occurs throughout matrix, as bands, and replaces plag xstals

sulphides <2% as intermittant py blebs and clots with minor qtz-carb veining

non-magnetic, intermttant highly brecciated endotrophic textures

261-263' band of sericite-qtz-carbonate with 5% 1-2mm sized py blebs with

hairline sph seams trending 25-30 deg CA

272-279' highly fractured and becciated intrusive section with sericitized frags and 5% py blebs

273' 5 cm wide clorite-py-sericite-mag band trending 40 deg CA

294-307' blocky degraded clay-altered core

DEPTH (ft) DEPTH (m)

311.00 334.50 2c Altered Intermediate Volcanic Rock, mottled green dark grey, fine grained, massive, rusty (ankerite?)

strong sericitization>chloritization with intermittant pervasive intense bands of both,

minor qtz-carb veining, 2-5% fine diss py plus 1-2% clots of sph with the sericite rich bands.non-magnetic328-329.5' blocky core311-319' blocky core

334.50 351.50 8 Altered Granodiorite Intrusive, mottled green grey, medium grained, 1-2 mm qtz eyes and lesser plag xstals, massive texture, intermittantly blocky core, strong sericitized bands, silicified, qtz-carb veining <5%, intermittantly rusty (ankerite?), crumbly and vuggy, tr py.

351.50 596.50 2c Altered Intermediate Volcanic Rock, green dark grey, fine grained, massivepervasive chloritization > sericitization> silicification as x-cutting bands and patches 5% qtz-carb veining assoc. with sericitization, 2-5% diss py plus intermittan t blebs and clots of coarser py with cpy and sph? Usually with the veining and enveloped by the sericite patches and chlorite clots. non-magnetic384-385' altered granodiorite section388-396.5' fractured and blocky core405.5-407' blocky core412-423' fractured and blocky core437.5-446' fractured and blocky core439.5-442' crumbly degraded fine grained intermediate dyke455-456.5' fractured and blocky core476- 477' fine grained intermediate dyke481.5-484' altered granodiorite section533-539.5' fine grained intermediate dyke with 1-2 mm carb amygules

596.50 710.50 8 Mixed Altered Granodiorite and Intermediate Volcanic, medium to dark grey, porphyritic with 1-2 mm degraded qtz and plag eyesgradual change between two rock types difficult to define due to the alteration. strong to pervasivesericitization and chloritization made up of sericite bands and patches and seams of chlorotiteIntermittantly rusty (ankerite?)and silicified, Avg. 2-5% diss sulphides plus intermittant blebs of py +- cpy and sph assoc. with qtz-carb-sericite patches and bands. Banded qtz-carb-ser-py-cpy?-sph?mineralization most pronownced adjacent to contacts with porphyritic sections which itselfis less altered and contains less sulphides unless contaminated by volcanic.673-680.5' fine grained intermediate dyke706.5-710.5' fine grained intermediate dyke

710.50 788.50 2c Altered Intermediate Volcanic or Sediment, mottled dark grey, fine grained, massivepervasive chloritization > sericitization> silicification as x-cutting bands, seams and patches carbonatization on fracture faces, 2-5% fine diss py plus blebs and smears of py+-cpy and sph adjacent to contacts with intermittant narrow sections of intrusive 755.5-756.5' rusty blocky core785.5-786' blocky core780- 788.5' intermediate plag porphyritic (1-2mm xstals) dyke, silicified and carbonitized with sharp contacts at 45 deg CA and 1-2% diss py.

788.50 796.00 8 Granodiorite Intrusive, mottled green grey, massive, qtz and plag xstals visible, medium grained, sericitized with chill margins adjacent to volcanic , undulating sharp contact at about60 deg. CA, no sig. sulphides except at contaminated chill margins.792-793' cave? with ground-up intrusive pebbles, fault?

794-796' rusty intermediate dyke, sharp contact at 40 deg. CA. no chill margin, tr sulphides

EOH

DIAMOND DRILL RECORD Project: Dalhousie

Reliant Gold Corp. DDH No.: MC-11-03 page: 1

Collar Location: UTM NAD 83 Zone 09 0441764E 6213765N , ele. 1144m Start Date: July 21/11

Length of Hole: 598' Completion Date: July 24/11

Dip at collar: -45 acid tests: 180' 44 deg., 370' 42 deg, 600' 42 deg. Claim Number: Rock of Ages

Azimuth at Collar: 045 deg Logged By: Trevor Boyd

Core Diameter: BTW Logging Date: July 25/11

Drill Contractor: More Core Diamond Drilling Ltd. Storage: More Core Yard, Stewart

Geological DESCRIPTION Sample Sample Assays

From To Code No. From To Length Cu, Zn, Au, Ag

0 48.5 0 boulders

48.50 54.50 0 sand and boulders see sample list see sample list

54.50 126.00 2 Intermediate Volcanic (Dacite?), medium to light grey, weakly sheared at 45 deg CA, and certificates and certificates

non magnetic, carbonitized with 5-10% carb-qtz x-cutting veining and on fracture faces

tr fine diss py.

126.00 229.50 2 Altered Intermediate Volcanic, mottled grey green, same as above but defined by gradual

increase in alteration, foliated at 50 deg. To CA where alteration is weaker. Stongly sericitized

bands and patches throughout, Alteration increases in sections where chloritization increases

such as equal to sericitization, 1-2% blebs py usually with sericite, qtz-carb veining 5-10%,

carbonatized on fracture faces, non magnetic.

144.5-205' chloritization increases with sericite and sulphides increase to 2-3 fine diss plus blebs

218-229.5' highly chloritic and sericitic section and rusty (anakerite?) with 2-3% py blebs and patches

216-218' blocky core, foliation at 50 deg CA.

229.50 311.50 8 Altered Granodiorite with contaminated volcanic rocks, mottled light to medium grey,

sharp undulating contact at 20 deg CA, plaf and qtz porphyritic in places with 1-2 mm xstals of both,

strongly sericitized plus lesser chloritization bands with 5% qtz-carb -py veinlets throughout.

Py as blebs and disseminations tr-1% except in sections where increases as noted.

carbonate as veinlates and on fracture faces. Alteration and sulphide content increase at contacts

where intrusives contaminate volcanics

234.5-259.5' sericite-chlorite alteration in contaminated volcanic rocks, sulphides increase as

DEPTH (ft) DEPTH (m)

py blebs in ser-qtz-carb bands and patches with poss. sph, weak foliation at 35 deg CA.

261.5-268' blocky core with ground up sections at 263-266' (drill lost circulation)

270.5-271' blocky core280-311.5' ser-chl alteration increases with 5-8% diss and blebby py in ser-chl-qtz-carb bands, poss sph, weakly foliated in contaminated volcanics at 45 deg CA286-288' fine grained int. dyke, contacts at 50 deg CA.287-288' blocky core304.5-306' blocky core

311.50 337.00 3c Altered Volcaniclastic Sediment, mottled dark grey, massive to weakly foliated trending variably 40-55 degrees CA. strong to pervasive chloritization with spotted and banded sericite, intermittantly rusty and blocky , 5-10% diss py plus gashes and 0.5 cm sized blebs of py in sericite-qtz-carb bands and veins which make up 15-20% of unit. Poss. sph with bands, non-magnetic, carbonitized on fracture faces. 317-320' blocky core322-323' blocky core328-329' blocky core336.5-337' rusty highly fractured core

337.00 376.00 2c Intermediate Dykes with Altered Volcanic Rocks, highly variable textures, medium to dark grey, Dykes are fine grained , massive with <1mm sericitized plag grains plus chloritic spots , moderately sericitized, chloritized and carbonitized. Altered volcanic rocks are lesser interlayers similar to previous unit. Dykes are magnetic, no significant sulphides in dykes but tr-5% diss and blebby py in volcanics.342.5-344' blocky core344-353.5' rusty altered volcanic interlayer as discribed above, note: contact among volcanic flow layers?, undulating and variable from 45-65 degrees CA.358-364' altered volcanic interlayer as above.372-373.5' blocky core

376.00 459.50 2 Intermediate Volcanic (Dacite), mottled medium to dark grey, equigranular, fine grained, massive, variably altered with weak diss and sericite altering plagioclase up to pervasive banded sericite-chl-qtz-carbonate textures. Sulphide content variable from tr - 10% diss and blebby py.intermittantly rusty, poss cpy with py.392-393' rusty blocky core396.5-397.5' rusty ground-up core402.5- 406' rusty blocky core398 - 403' 5-10% qtz-carb-ser veins with 5-10% py plus cpy specks.414.5-419.5' pervasive chl-ser bands with 10-15% diss and bleb py plus tr cpy.451-456' intermediate dyke, fine grained, massive and moderately sericitzed with sharp jagged contacts at 55 degrees, magnetic

459.50 580.00 2 Altered Volcaniclastic Sediment, mottled dark grey, massive to weakly foliated, upper contact undulating 45-50 degrees CA, fine grained, consistent strong to pervasive sericite and chlorite alteration as bands, patches and disseminations. Ser-Qtz-Carb-Chl bands make up 10-15% of rock. 3-5% diss py throughout

plus another 3-5% py as blebs and patches in bands, tr cpy with py in blebs, non magnetic.537-538.5' blocky core532.5-533.5' qtz-chl-carb-ser seams with patches of py and lessor cpy 10-15%, seams trendjagged at approx 50 degrees CA.543.5-548.5' intermediate dyke, fine grained570.5-571.5' blocky core 571.5-578' intermediate dyke, fine grained, massive, carbonitized, magnetic, sharp contacts 50-60 deg. CA578-580' rusty, blocky, pervasively altered volcanic rock adjacent to dyke rock and coarser grained intrusive below with 5-10% py plus poss sph and cpy575.5-570' blocky core, lost circulation at 576'

580.00 608.00 8 Granodiorite, mottled dark green, massive, equigranular with plag and qtz euhedral xstals 2-4 mm in size. Sericitzed, rusty chloritic chill margins, 1-2 diss py, sharp contact with volcanic unit above at 40 deg. CA, 585.5-590.5' rusty and degraded rock then becomes less altered with weak sericite583-585.5' intermediate dyke, contacts with intrusive at 70-80 deg. CA, fine grainedmassive, carbonatized588-590.5' blocky core602.5-606' intermediate dyke, fine grained, massive.