Geoscience Resources of Newfoundland and Labrador · bisects the Bullwinkle alteration zone and...

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001M/0932

THIRTEENTH YEAR ASSESSMENT REPORT

OF

PROSPECTING

ON

LICENSE 20917M

TEN MILE PONE AREA, BURIN PENINSULA, NL

NTS 01M/09 & 01M/10

BY

NATHANIEL NOEL MSc.

FOR

E. MICHELE NOEL MINERAL LICENCES: 20917M (10) WORK CONDUCTED: LATE NOVEMBER AND EARLY DECEMBER TOTAL EXPENDITURES: 8728.00 20917M TOTAL CLAIMS: 10

Table of Contents Page Summary 1

Introduction 1

Location and Access 2 Physiography 2 Property Summary and License Status 3 Previous Work 4

Geology 4

Regional Geology 4 Local Geology 5

Current Program 7

Work Done 8

Results 8

Drilling Unit 8 Strange Showing 12 Strange Showing Drill Results 13 Bullwinkle Showing 16 Bullwinkle Showing Drill Results 20 Assaying 23

Conclusions and Recommendations 23

List of Expenditures 26

References 26 List of Figures

Figure 1 Project Location Map 1 Figure 2 Claims Location Map 2 Figure 3 Topography looking north-eastward from the Strange Showing towards the Bullwinkle 3 Figure 4 Regional Geology 5 Figure 5 Pink weathering crystal tuff 6 Figure 6 Grey weathering intermediate tuff 6 Figure 7 Project area map showing locations of Bullwinkle and Strange Showings 7 Figure 8 Hand held coring drill 8 Figure 9 Hand held drill rig with heavy extender and bit 9 Figure 10 Drill unit with drill steel extender and bit 10 Figure 11 Peat being flused from hole during drilling. 11 Figure 12 Cuttings being flushed from bedrock 11 Cont’d…/2

Table of Contents Cont’d. Page Figure 13 Location map for drill holes at the Strange Showing 12 Figure 14 6 inch core from S-6 15 Figure 15 Core from Silica-Alunite-Hematite boulder drilled at S-15 containing what is believed to be tourmaline 16 Figure 16 Soil survey results by Cornerstone Resources Inc. covering the Bullwinkle Showing 17 Figure 17 Map showing drill hole locations at Bullwinkle 18 Figure 18 Interpreted cross section of Bullwinkle from previous work completed 19 Figure 19 Distinct orange colored cuttings when coring limonitic alteration 20 Figure 20 Core from B-12 consisting of limonitic rich quartz- sericite schist 21 Figure 21 Core from B-13 consisting of more massive and silicic unit 22 Figure 22 Cuttings or deep overburden material flushed up by return and dumped on the surface 24 List of Tables Table 1 Strange Showing Drill Results 13 Table 2 Bullwinkle Drill Results 20

1

SUMMARY

Work in 2014 utilized a portable gas powered coring drill with extender attachments to drill

through 6 feet of peat bog for the purpose of sampling the bedrock underneath. Using this

device it was shown that a linear bog adjacent to the Strange showing is actually underlain by

intensely sheared quartz‐sericite‐alunite alteration providing addition proof that the Strange

showing and Bullwinkle showing are connected and therefore part of a single large alteration

system.

Drilling also provided information about the nature of the alteration in the linear valley which

bisects the Bullwinkle alteration zone and supports the hypothesis that the two parallel silica

zones are actually the limbs of a fold structure with the central valley being the core of the

system.

INTRODUCTION

This report covers work completed on mineral license 20917m (10 claims) located on the Burin

Peninsula. (Figure 1 and 2) This license was staked to cover prospective ground on the

Paradise Trend as defined by Huard (1989) and Geovector (2002) which contained the

Bullwinkle and Strange showings. This trend marks the location of a long (7km) system which

exhibits the characteristics of high sulphidation alteration including silica‐alunite‐hematite‐

pyrophyllite rich rocks.

Figure 1 Project Location Map

2

LOCATION AND ACCESS

The property consists of 10 contiguous located approximately three kilometres south of the

Monkstown Road and approximately 1.5 km west of Ten Mile Pond on the Burin Peninsula.

(Figure 2). It can be accessed from the Burin Highway via a major power line access trail which

almost reaches the western portion of the properties and then by ATV by traveling trails either

to the north or south of Ten Mile Pond. The northern portion of the property can be easily

accessed from Monkstown Road when the water level in the Paradise River is low however

access requires fording the river.

Figure 2 Claims location map.

PHYSIOGRAPHY

The area is relatively barren and consists of low rolling hills rising to the east to form a higher

plateau. There are numerous small ponds. Outcrop is sporadic and glacial overburden forms a

thin cover over most of the area. The silica alteration zones are local topographic highs

however the main alteration zone lies within a relatively low area.

3

Figure 3 Topography looking north‐eastward from the Strange Showing towards Bullwinkle. The alteration zone is interpreted to pass through on the left side of the photo.

PROPERTY SUMMARY AND LICENSE STATUS

Mineral license 20917m (10 claims) is a reduced license from an older claim block. The claims

were staked by E. Michele Noel. Since that time some of the claims (in particular those

included in the older license 19914m have been optioned to Western Keltic Minerals,

Comaplex Minerals Corp of Calgary Alberta, and Cornerstone Capital. In the spring of 2010 the

claims were returned to Michele Noel, the original claim holder. In the late fall of 2010 and

early winter of 2011 work on the claims was conducted under a grubstake agreement with

61716 Newfoundland and Labrador Limited who expressed an interest in the Burin Peninsula.

This grubstake work did not produce an option agreement. All claims are currently in good

standing.

4

PREVIOUS WORK

The region encompassing the claim block was mapped at 1:50,000 scale in 1984 by the

Newfoundland Geological Survey. With the discovery of the Paradise Trend alteration zones ie

Monkstown Road, Ridge, Paradise River showings along strike of the project area, the

immediate area was again mapped in 1989 by Allan Huard as part of his masters thesis. This led

to the discovery of the Bullwinkle and Strange showings. The Strange showing was found to

contain up to 800ppb gold when sampled by Huard. The area was staked by Stewart in 1985

and several anomalous gold values were obtained within the confines of the Bullwinkle

Alteration Zone in the vicinity of the small pond at the southwest end of the showing. In 1989

the area was staked by Corona Corporation who completed a program of mapping, lake

sediment, soil and rock sampling primarily to the east and north of the project area. The area

encompassing the Strange Showing was staked by Noel N. and the area around the Bullwinkle

Showing was staked by Noel E.M. in 2002. The property was then optioned to Western Keltic

Mines Ltd. and work was performed in 2002 by Geovector Management Inc. for Western Keltic

Mines. They conducted a limited mapping and prospecting program on the two properties and

confirmed that the Bullwinkle Showing was part of a larger, aurifferous high sulphidation

alteration system and obtained a grab sample assaying 1600 ppb gold from the Strange

Showing, doubling any previous results. In 2008 Cornerstone Capital Corp. optioned the

property and conducted soil and rock sampling. Sampling by Cornerstone at the Strange

showing produced and assay of 3.2 gm/ton Au. Work by the author includes prospecting on

and around the claim block.

While the area in the immediate vicinity of the Bullwinkle and Strange Showings inclusive has

had some exploration work completed on it, the project area is largely unexplored.

GEOLOGY

REGIONAL GEOLOGY

The area lies within the Avalon Terrain and is underlain by a suite of calc‐alkaline, volcanic

rocks with associated clastic and volcanoclastic sediments. The rocks formed some 550‐600

mya (O”Brien et al. 1998) and are considered to be part of the Marystown/Love Cove Group.

In this region the units define a broad anticlinorium which is cored by granitic rocks of the Swift

Current Granite. (Figure 4) The project area is at the southern end of this major structure.

5

Figure 4 Regional Geology (Modified from O'Brien et al. 1998)

LOCAL GEOLOGY

The claim block is underlain primarily by intermediate‐felsic volcanic and volcanoclastic rocks.

The felsic units consist of pinkish weathering crystalithic tuffaceous rocks (figure 5) while

intermediate units are green‐grey. (Figure 6) No sediments were observed on the claim block..

6

The claim block is bisected by a NE‐SW trending alteration zone known as the Bullwinkle Zone

containing advanced argillic alteration including zones of intense silicification.

Figure 5 Pink weathering crystal tuff.

Figure 6 Grey weathering intermediate tuff.

7

Structurally, the rocks are tightly folded and contain a strong penetrative foliation which strikes

NE‐SW at approximately 20‐30 degrees and generally dips steeply to the NW. F1 folds are tight

and isoclinal and are occasionally seen on outcrop scale. F2 folding is more open and can be

seen on a variety of scales. For a more detailed description of the local geology please see the

first year (2002) assessment report on these properties completed by Geovector Management

Inc.

CURRENT PROGRAM

The current program consisted of prospecting the Strange and Bullwinkle showings (Figure 7)

using a small gas powered portable drill unit. The purpose of using the drill was to attempt to

sample the bedrock adjacent to and along strike of the Strange Showing, and to determine the

nature of the alteration beneath the bog in the unexposed valley portion of the Bullwinkle

Showing.

Figure 7 Project area map showing locations of Bullwinkle and Strange showings

8

WORK DONE

The work was conducted in late November of 2014 (5 days) and Early December of 2014 (5

days) for a total of ten days which included travel to and from the project area. Work was

conducted from a small gravel pit adjacent to the Burin Highway near Dunns River. Access to

and from the project area was by ATV on a daily basis. Due to the time of year the days were

short. Accounting for travel time in and out from the camp to the project area which was about

1.25 hours each way and to ensure that the trip back to camp was conducted in daylight, the

actual prospecting day was about 5 hours long.

With the ATV loaded with gear, the initial trip in to the site, and the last trip out, took more

than 2 hours each way.

RESULTS

Drilling Unit

The drilling unit used was a Kor‐it hand held gas powered coring drill. (Figure 8) This particular

model (525) is geared for higher rpm’s than other models with a top speed of 1700 RPM.

Figure 8 Hand Held Coring Drill.

9

In figure 8 the drill is coring directly into bedrock. A 36 inch extender (figure 9) is available to

allow deeper drilling however such an extender is unnecessarily robust and extremely heavy.

The mass of the extender combined with its diameter ends up using a considerable amount of

torque just to turn the drill and can lead to overheating of the engine during drilling.

Figure 9 Hand held drill rig with heavy extender and bit.

To allow deeper drilling without stressing the drill a 1.5 meter length of drill steel, used for

percussion drilling was machined so that it could adapt to both the drill and the bit. (Figure 10)

The air hole down the center of the drill steel allows water to pass through for cooling the bit.

The narrowness of the drill steel allows for easy turning by the drill thereby transferring most

of the torque of the drill to turning the bit. The extender and bit combined allowed for drilling

to a depth of over 2 meters.

10

Figure 10 Drill unit with drill steel extender and bit.

For drilling through bog, pipe, normally used for chain link fencing was cut in 1.3 meter lengths

and using a grinder, one end was sharpened. A 2” metal pipe cap could then be placed on top

of the casing to protect it and then struck with a sledge hammer driving the casing into the

bog. The casing could then be pulled and in most cases the peat “plug” in the casing could

simply be blown out by placing ones mouth against the other end and blowing hard. In this

manner the casing could be easily driven approximately 90 cm into the bog. This provided

stability for the drill. A half horse power jet pump powered by a 2000 watt camp generator

provided enough water pressure to flush the hole of any additional peat and drill cuttings.

(Figures 11 and 12)

11

Figure 11 Peat being flushed from hole during drilling. Notice the metal pipe cap which was used to drive the casing into the bog.

Figure 12 Cuttings being flushed from bedrock.

300 feet of garden hose was brought in to insure that a nearby water source could be reached.

12

A hammer drill with a 2 inch masonry bit, which could also run off the generator, was brought

in with the expectations that it would be required to penetrate cobbly glacial till however none

was encountered.

While the drill was used previously on another project it was only used for drilling exposed

bedrock. This prospecting project was the first to test the extensions and their suitability for

drilling through peat bogs and while it required a considerable amount of time to drill each hole

much was learned while doing this. It is for this reason the claim holder has only been charged

for consumables.

STRANGE SHOWING

A total of 15 holes were drilled to test for extensions along strike of the main Strange showing

and also to determine if the alteration zone hosting the Strange showing was limited to the

exposure or if it extended further across strike and under the adjacent bog. Figure 13 shows

the location of the holes relative to the main showing.

Figure 13 Location map for drill holes at the Strange Showing

13

Table 1 lists the locations of the holes and a brief description of what was encountered.

STRANGE SHOWING DRILL RESULTS

Table 1 Strange Showing Drill Results

*All holes which did not make it to bedrock were drilled to depth of 2 meters.

S‐1 was drilled directly into the main showing, which consists an intense silicic alteration. Due

to the nature of the material the drill bit could barely penetrate the rock. A 2 inch diameter

coring bit shattered and lost its segments after a prolonged attempt to core the unit. For this

reason it was decided to step out from the showing.

S‐2 was drilled to test for an extension to the main showing. It encountered bedrock at

approximately 1 meter consisting of strongly foliated quartz, sericite, pyrite schist. A piece of 6

inch core was collected.

Hole # Easting Northing Description

S‐1 686449 5284690 Center of Strange showing on bedrock. So silicic drill would not penetrate to any depth. Shattered 2” drill bit.

S‐2 686459 5284692 Bedrock at 1 meter depth. Quartz‐sericite‐pyrite schist.

S‐3 686453 5284696 ? Boulder at 1.2 m. Mafic volcanic with slight alteration

S‐4 686442 5284684 Bedrock at 20 cm. Quartz sericite alunite hematite schist

S‐5 686434 5284678 Bedrock at 1.2 meters. Quartz alunite hematite schist

S‐6 686426 5284682 Bedrock at 1.5 meters. Quartz sericite alunite hematite schist

S‐7 686421 5284687 ? bedrock. Cuttings in return very sericitic but sandy

S‐8 686484 5284729 No Bedrock

S‐9 686479 5284733 No bedrock

S‐10 686477 5284739 No bedrock

S‐11 686476 5284749 No bedrock

S‐12 686476 5284760 No bedrock

S‐13 686475 5284769 No bedrock

S‐14 686442 5284699 Bedrock at 1.6 meters. Quartz sericite alunite hematite schist

S‐15 686603 5284846 Flat boulder. Quartz alunite hematite ? tourmaline. Only weakly foliated.

14

S‐3 cored a slightly altered mafic volcanic unit, believed to be an erratic, at approximately 1.2

meters.

S‐4 located immediately to the southwest of the main showing encountered bedrock at

approximately 20 cm. A 6 inch core of strongly foliated quartz‐sericite‐?alunite‐hematite was

collected.

S‐5 located further to the south west encountered the same unit as S‐4 at approximately 1.2

meters. Six inches of core was collected.

S‐6 stepped out across strike to the northwest, downslope from S‐5 and on to the bog. After

passing through approximately 1 meter of peat, it then continued to bore down while flushing

out what appeared to be sand. Bedrock was encountered at approximately 1.5 meters and

consisted of very strongly foliated Quartz‐sericite‐alunite‐hematite alteration. (figure 14) The

foliation was down the core axis which matched the bedrock located up slope immediately to

the east.

15

Figure 14 6 inch core from S‐6

S‐7 located northwest of S‐6 passed through a similar peat layer and bottomed in what

appeared to be sericite rich sand. It is possible that it was actually coring sericite rich bedrock

but that much of the core was being ground up due to the softness of the rock.

S‐8 – S‐13 attempted to encounter bedrock while following a small stream that had incised its

way through the peat layer and transected the linear occupied by the bog. Probing with a piece

of casing showed that there was indeed rock in the bed of the stream however these turned

out to be boulders/erratics. No bedrock was encountered in any of the holes and in some

cases the casing was almost lost down the hole.

S‐14 was drilled just north of the main showing as another step out hole into the bog. Bedrock

consisting of intensely foliated/sheared quartz‐sericite‐?alunite‐hematite schist similar to that

encountered in S‐6 was sampled.

16

S‐15 was a flat boulder of slightly foliated intensely altered quartz‐alunite‐hematite +

?Tourmaline schist. (Figure 15) It was drilled because it represents the closest erratic found to

date along strike of the Strange showing. It could not be sampled with a sledge hammer due to

its flat and smooth nature.

Figure 15 Core from Silica‐Alunite‐Hematite boulder drilled at S‐15 containing what is believed to be tourmaline.

BULLWINKLE SHOWING

A total of 15 holes were drilled at the Bullwinkle showing to determine the nature of the

alteration underlying the gold in soil anomaly discovered during a soil sampling program by

Cornerstone in 2008 and 2009. (Figure 16)

17

Figure 16 Soil survey results by Cornerstone Resources Inc. covering the Bullwinkle Showing

A route into the showing established the year before allowed the drilling gear to be brought

into the site by ATV.

Figure 17 shows the location of the drill holes. Holes B‐1 to B‐8 were drilled in the low ground

between two bands of intense silicic alteration. This low ground is currently interpreted to

represent the core of a fold with the two siliceous bands representing the limbs. (Figure 18)

Holes 9 – 15 stepped up the slope of the east limb.

18

Figure 17 Map showing drill hole locations at Bullwinkle

19

Figure 18 Interpreted cross section of Bullwinkle from previous work completed. Looking Southwest.

Table 2 summarizes the results of the drilling and provides the locations of the holes. Initially it

was thought that the Limonitic‐sericitic cuttings encountered in the bottom of drill holes B1 –

B4 represented a talus or sandy overburden layer however it is now thought to be the ground

equivalent of bedrock cored in holes B5 and B12 indicating that was most likely derived from

bedrock.

20

BULLWINKLE DRILL RESULTS

TABLE 2 Bullwinkle drill results

B‐1 to B‐4 were drilled in an area containing some of the highest gold in soil values (up to 85

ppb) identified by Cornerstone in 2008. All holes were drilled to a depth of 2 meters. Peat

formed a layer approximately 1.0 meter thick. Coring below this produced a distinct orange

colored return believed to be the result of limonite. (figure 19)

Figure 19 Distinct orange colored cuttings when coring limonitic alteration

Hole # Easting Northing Description

B‐1 687337 5285816 ?Bedrock/gravel. Limonitic sericitic cuttings.

B‐2 687342 5285813 Drilled through small boulder of Ackley Grantite then ?Bedrock/gravel. Limonitic sericitic cuttings.



B‐5 687342 5285790 Bedrock at 1 m. Sericite‐Limonite‐silica schist

B‐6 687369 5285859 ?Bedrock. Limonitic sericitic cuttings



B‐9 687498 5285886 Lost casing down hole. No Bedrock encountered

B‐10 687493 5285876 No bedrock

B‐11 687493 5285869 Possible bedrock at 1.4 m. Sericite‐limonite cuttings

B‐12 687498 5285866 Bedrock at 1 m Quartz‐sericite‐limonite schist.

B‐13 687498 5285861 Bedrock at surface. Quartz‐alunite‐hematite boudon

B‐14 687493 5285848 Bedrock at surface. Quartz‐alunite‐hematite boudon

B‐15 687485 5285840 Bedrock at surface. Quartz‐Hematite with some vuggy silica.

21

This same color in the cuttings was noted when coring bedrock composed of limonite rich

quartz‐sericite alteration as found in B‐5 and B‐12 (Figure 20)

Figure 20 Core from B‐12 conisting of limonite rich quartz ‐sericite schist.

B‐5 encountered very strongly foliated quartz‐sericite‐limonite schist at approximately 1 meter

similar to that shown in figure 19.

B6 – B8 were drilled in an area previously reported to contain a lot of angular quartz float. No

definite bedrock was encountered but like the other holes the cuttings were a distinct orange

color and appeared to be highly sericitic. In addition, the cuttings were comprised of coarse

chips suggesting that they may have been the result of ground up core.

22

B‐9 was collared in a small stream which had incised a deeper channel at right angles to the

strike of the foliation. No bedrock was encountered and a 4 foot length of casing was lost

down the hole.

B‐10 was collared slightly up slope from B‐9 and did not appear to reach bedrock. The base of

the hole however did produce an orange colored return.

B‐11 hit possible bedrock at 1.4 meters at that point producing coarse sericite cuttings and a

bright orange return from 1.4 to 2.0 meters.

B‐12 encountered definite bedrock at approximately 1.0 meter and produced the core shown in

figure 19.

B‐13 – 15 cored outcrop consisting of what appeared to be boudons of intense silicic alteration

containing subordinate amounts of alunite and hematite. This material was notably more

massive and less foliated than the surrounding rocks. (Figure 21) B‐15 contained vuggy

textures and was immediately adjacent to an a previous sample site which produced an assay

result of 110 ppb Au.

Figure 21 Core from B‐13 consisting of more massive and silicic unit

23

ASSAYING

To date, none of the cores collected have been assayed. It is the intention of the claimholder

to engage in a grubstake arrangement with a local exploration company to cover the costs of

the assays. The results will be presented in the next assessment report.

CONCLUSIONS AND RECOMMENDATIONS

The drill rig works extremely well and may in some cases offer a cheaper and more practical

alternative to trenching with an excavator. This would be especially true in areas of bog

where trenching results only in the creation of water filled depressions or worse, sunken

excavators. To some degree this program also served to work some of the bugs out of using

the apparatus for deeper drilling and the last few deeper holes happened much quicker than

the earlier ones.

The entire apparatus can be made lighter by substituting a small gas powered water pump (13

lbs) for the combination generator and turbine pump (100 lbs) Unless the hammer drill is

required to penetrate proper till or moraine (requiring the generator to power it) the gas pump

would definitely be the way to go.

The drill had no trouble turning the extender made from the drill steel. In fact, that worked so

well it is possible that two steel lengths of 1.5 meters could be connected to allow for even

deeper drilling.

A core extractor made for extracting the core out of a deep hole did not work and in the end

was unnecessary. With a bit of wear on the bit the hole was too narrow for the core extractor.

Inevitably, during drilling, the core broke off and lodged in the bit which allowed it to be

brought to the surface. Tapping the bit with a wrench caused the stuck core to loosen and slide

out.

It is possible that the apparatus could also be used as a deep overburden sampler. A collector

could be added to the top of the casing to catch the cuttings, brought up by the return, which

currently simply spill out on the ground. (figure 22) The cuttings could be assayed or examined

with a microscope or both.

24

Figure 22 Cuttings or deep overburden material flushed up by return and dumped on the surface.

The Strange showing originally called “strange” because of what appeared to be a very small

and intense pod of alteration appearing to be surrounded by relatively unaltered units is still

very much an enigma however this phase of exploration has demonstrated that indeed a much

larger alteration zone, lying beneath an adjacent bog, forms an envelope around the Strange

thereby making it less “strange”. Furthermore, the alteration observed in the drill core brought

up from beneath the bog is similar to alteration observed at the south west end of the

Bullwinkle zone and in erratics found between the two offering further evidence to suggest that

the two showings are part of a much larger and continuous alteration system. Further drilling

should be conducted around the main showing to determine if other pods of the auriferous

silicification exist and whether or not the grades are higher.

25

In addition, the identification of intense alteration beneath the bog adjacent to the Strange

Showing suggests that other such unexposed bog filled linears in this area may also contain

substantial alterations zones

Drilling at the Bullwinkle suggests that the siliceous zones form the higher ground and the

sericite‐hematite/limonite alteration forms the lower ground. While this might seem to be an

obvious conclusion, it has been found that in some locations where the siliceous zones are

folded they have shattered or broken up and resulting glaciation has plucked out the blocks

resulting in the creation of a depression, usually filled by a pond or bog. Further drilling of the

unexposed portions of the Bullwinkle will help create a detailed map of the alteration helping

to pinpoint where an economic zone might lie and with any luck, might actually sample it.

A full chip sampling program is still intended for the Bullwinkle portion of the alteration system,

a job made easier now that an ATV route into the center of the showing has been established.

The portable drill could then be used to expand on the results of such a program by sampling

unexposed areas adjacent to anomalous areas defined by the chip sampling.

The unexposed area between the Bullwinkle and Strange showings should be tackled using the

portable drill, primarily to locate and track the alteration zone and prove beyond a doubt that

the two are connected but also to check for any auriferous alteration which may be present.

26

LIST OF EXPENDITURES

REFERENCES

Dyke, B.

(2007): Assessment Report of Satellite Imagery, Prospecting, Rock Sampling, Lake Sediment

Sampling and Stream Sediment Sampling. Burin Project; Licences 9038M (5th yr), 10975M (2nd

EXPENDITURES COST

Days Worked (travel and prospecting, sampling) 10 days @ 400.00/day) 4000.00

Vehicle (10 days at 60.00/day) 600.00

Fuel (includes fuel for ATV) 480.00

Accommodations and meals (10 days @ 60.00/day) 600.00

Quad Use (6 days @ 50.00/day (includes and maintenance) 300.00

Administration (prep work) and report writing (2 days) 800.00

Coring Drill Bits (1.5 inch @ 140.00/ bit) x 2 280.00

Coring Drill Bits (2.00 inch @ 210.00/bit) x 2 420.00

Drill use 100.00

Casing (lost casing) 1 length 10.00

Overhead @ 15% of 7590.00 1138.50

Total 8728.00

27

yr), 11092M (2nd yr), 12650M (1st yr), 13639M (4th yr) and 13640M (2nd yr), NTS 1M/06, 1M/07,

1M/09, 1M/10 & 1M/16, Burin Peninsula, NL. Cornerstone Resources Inc. Assessment Report,

25 p.

(2008a): Assessment Report of Satellite Imagery, Property Tour, Prospecting, Rock Sampling,

Lake Sediment Sampling, Stream Sediment Sampling, Soil Sediment Sampling, Mapping,

TerraSpec and Trenching. Burin Project; Licences 8405M (5th yr & 6th yr), 8406M (5th yr & 6th yr),

8509M (5th yr & 6th yr), 9038M (6th yr), 10975M (3rd yr), 11092M (3rd yr), 12650M (2nd yr),

13189M (1st yr), 13633M (1st yr), 13637M (3rd yr), 13638M (3rd yr), 13639M (5th yr), 13640M (3rd

yr), 14825M (1st yr), 14827M (1st yr), 14833M (1st yr), NTS 1M/06, 1M/07, 1M/09, 1M/10 &

1M/16, Burin Peninsula, NL. Cornerstone Resources Inc. Assessment Report, 34p.

(2008b): Assessment Report (Supplementary Report) of Satellite Imagery, Property Tour,

Prospecting, Rock Sampling, Lake Sediment Sampling, Stream Sediment Sampling, Soil Sediment

Sampling, Mapping, TerraSpec and Trenching. Burin Project; Licences 8405M (5th yr & 6th yr),

8406M (5th yr & 6th yr), 8509M (5th yr & 6th yr), 9038M (6th yr), 10975M (3rd yr), 11092M (3rd

yr), 12650M (2nd yr), 13189M (1st yr), 13633M (1st yr), 13637M (3rd yr), 13638M (3rd yr), 13639M

(5th yr), 13640M (3rd yr), 14825M (1st yr), 14827M (1st yr), 14833M (1st yr), NTS 1M/06, 1M/07,

1M/09, 1M/10 & 1M/16, Burin Peninsula, NL. Cornerstone Resources Inc. Assessment Report,

8p.

(2009): Assessment Report of Compilation on Licences 12650M (3rd yr), 13637M (4th yr),

13640M (4th yr), 15461M (7th yr), 15462M (7th yr), 15959M (2nd yr‐ Grouped from 13633M &

14827M‐Subsequently reduced to 15963M & 15964M), 14825M (2nd Year – Reduced to

15969M & 15970M), 14833M (2nd Year – Reduced to 15971M & 15972M), Burin Gold Project

(Hickey’s Pond Claim Groups), NTS 1M/09, 1M/10, 1M/16. Cornerstone Resources Inc.

Assessment Report, 32p.

Huard, A. A.

(1989): Epithermal alteration and gold mineralization in Late Precambrian volcanic rocks on the

northern Burin Peninsula, southeastern Newfoundland, Canada, MSc, Memorial University of

Newfoundland, St John's, Newfoundland, Geofile 001M/0314, 289 pages.

28

Sexton, A., Heberlein, K. and Thompson, A. J. B.

(2003a): First and second year assessment report on geological and geochemical exploration for

licences 8102M, 8405M, 8509M, 8976M‐8977M and 9039M on claims in the Paradise River

area, on the Burin Peninsula, Newfoundland, 2 reports, GeoVector Management Incorporated

and Western Keltic Mines Incorporated, Newfoundland and Labrador Geological Survey, Geofile

1M/0468, 73 pages.

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Geoscience Resources of Newfoundland and Labrador · bisects the Bullwinkle alteration zone and...

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Transcript of Geoscience Resources of Newfoundland and Labrador · bisects the Bullwinkle alteration zone and...