So i l S a n d P Ma t e r i a l S o f SP r i n g Ba y Qu a...
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1 2 3 4 5 6 7 8 1° APPROXIMATE MEAN DECLINATION, 2004 MAGNETIC NORT H TRUE NORTH The Illinois State Geological Survey, the Illinois Department of Natural Resources, and the State of Illinois make no guarantee, expressed or implied, regarding the correctness of the interpretations presented in this document and accept no liability for the conse- quences of decisions made by others on the basis of the information presented here. The geologic interpretations are based on data that may vary with respect to accuracy of geographic location, the type and quantity of data available at each location, and the scientific/technical qualifications of the data sources. Maps or cross sections in this document are not meant to be enlarged. For more information contact: Illinois State Geological Survey 615 East Peabody Drive Champaign, Illinois 61820-6964 (217) 244-2414 http://www.isgs.uiuc.edu Base map compiled by Illinois State Geological Survey from digital data provided by the United States Geological Survey. Topography compiled by the United States Geological Survey from imagery dated 1946. Revised and updated from imagery dated 1995. Field checked 1996. North American Datum of 1983 (NAD 83) Projection: Transverse Mercator 10,000-foot ticks: Illinois State Plane Coordinate system, west zone (Transverse Merca- tor) 1,000-meter ticks: Universal Transverse Mercator grid system, zone 16 Recommended citation: Stumpf, A.J., and C.P. Weibel, 2004, Soils and Parent Materials of Spring Bay Quadran- gle, Peoria and Woodford Counties, Illinois: Illinois State Geological Survey, Illinois Geologic Quadrangle Map, IGQ Spring Bay-SPM, 1:24,000. BASE MAP CONTOUR INTERVAL 10 FEET SUPPLEMENTARY CONTOUR INTERVAL 5 FEET NATIONAL GEODETIC VERTICAL DATUM OF 1929 Released by the authority of the State of Illinois: 2004 Transfer of soil map units by Soil Survey staff, Natural Resources Conservation Service, Rock Falls, Illinois. Raster to vector conversion completed by C. Abert. Map review provided by Soil Survey staff, Natural Resources Conservation Service, Champaign, Illinois. Digital cartography by M. Barrett, Illinois State Geological Survey. Department of Natural Resources ILLINOIS STATE GEOLOGICAL SURVEY William W. Shilts, Chief SOILS AND P ARENT MATERIALS OF SPRING B AY QUADRANGLE PEORIA AND W OODFORD COUNTIES, ILLINOIS Andrew J. Stumpf and C. Pius Weibel 2004 Illinois Geologic Quadrangle Map IGQ Spring Bay-SPM IGQ Spring Bay-SPM ADJOINING QUADRANGLES 1 Edelstein 2 Rome 3 Chillicothe 4 Dunlap 5 Germantown Hills 6 Peoria West 7 Peoria East 8 Washington .5 1 KILOMETER 1 0 SCALE 1:24000 1/2 1 MILE 0 1 6000 5000 4000 7000 FEET 3000 1000 1000 0 2000 ROAD CLASSIFICATION Primary highway, hard surface Secondary highway, hard surface Light-duty road, hard or improved surface Unimproved road State Route Sarpy* (3092A, 3092L) Joy (275)P Osco (86)P Ipava (43)P Sable (68)P Elkhart (567)P Clarksdale (257)TR Fayette (280)(827)T Rozetta (279)(827)T Keomah (17)(814)T Rushville (16)(814)T Navlys (630)T Sylvan (19)T Catlin (171)P Birkbeck (233)T Saybrook (145)P Dodge (24)T Senachwine (618)T Hennepin (935)(818)(87)T Hickory (818)T Strawn (224)(818)(857)T Plano (199)P Elburn (198)P St. Charles (243)T Proctor (148)P Starks (132)T Camden (134)T Jasper (440)P Selma (125)P Ockley (387)T Martinsville (570)T Cresent (672)P Warsaw (290)(828)P Dakota (379)(828)P Fox (327)T Plainfield (54)T* Coloma (689)T* Dickinson (87)P Alvin (131)T Worthen (37)P Peotone (330)P Lena (210A) Palms (100A) Landes (3304A, 7304B) Ross (8073A) Raveenwash (8368A) Slacwater (3360A) Jules (3028A) Paxico (3406A, 3406L) Dorchester (3239A) Huntsville (8077A) Lawson (3451A, 8451A) Radford (8074A) Beaucoup (3070L, 7070A) Sawmill (8107A) Bowdre (589B) ORTHENTS (801, 802) MAN-MADE MATERIALS (865, 533) Loess (0–20 inches thick) over glacial till Loess (40–60 inches thick) over glacial outwash Loess (20–40 inches thick) over glacial outwash Loess (0–20 inches thick) over glacial outwash Loamy materials (40–60 inches thick) over glacial outwash Loamy materials (20–40 inches thick) over glacial outwash Loess (>60 inches thick) Loess (40–60 inches thick) over glacial till Loess (20–40 inches thick) over glacial till Aeolian sand (>60 inches thick) Loamy materials (20–40 inches thick) over aeolian sand Silty and clayey materials Silty and loamy materials (>40 inches thick) Alluvium (sandy) (20–40 inches thick) over alluvium (loamy) Alluvium (loamy) Alluvium (silty) Alluvium (clayey) Sapric materials (muck) (>51 inches thick) Sapric materials (muck) (16–51 inches thick) over glacial drift Loess: Windblown silt and fine-grained sand; dark yellowish gray to yellowish brown in color; texturally ranges from a silt to silt loam; blankets upland areas along the Illinois River valley; absent from geomorphic surfaces that postdate its deposition (e.g., floodplains). Glacial till: Sediment composed of a mixture of clay, silt, sand, and rocks deposited by glaciers; reddish brown to dark grayish brown in color; loamy textured; hard to firm; forms many of the uplands in the area; absent in the Illinois River valley where it has been removed by postglacial erosion. Glacial outwash: Stratified deposits of sand, gravel, cobbles, and boulders; yellowish brown to grayish brown in color; mostly clean with very little silt; very well to moderately sorted proglacial fluvial sediments deposited by meltwater flowing in front of melting glaciers; forms a series of terraces, bars, and channel deposits in the Illinois River valley. Aeolian sand: Very fine- to medium- grained sand; loose; non-calcareous in upper part; postglacial windblown sand composing dunes and undulating sandy deposits on terraces and uplands. Colluvium: Stratified or massive, silty or clayey deposits infilling depressions on the uplands and on foot slopes of valley walls; remobilized till, outwash, and loess. Organic soil material: Peat, organic silt, and muck; dark gray to black; usually water saturated; accumulates in abandoned channels, shallow lakes, and low-lying depressions on the modern floodplain. Alluvium: Stratified sand and gravel with some beds of silt and clay or diamicton; yellowish brown to gray; may be either calcareous or non-calcareous; seasonally wet and often gleyed; subject to flooding and overland flow; the finer-grained sediments often contain humus, dispersed wood fragments and shells, or man-made waste; upper part weathered; postglacial (modern) lake or stream sediments deposited over the past 12,000 years on floodplains, along channels, and in seasonally ponded lakes; also includes sediments forming fan-shaped landforms in areas where streams or ravines emerge from uplands onto lower-gradient floodplains. Orthents (silty to loamy): Materials generally in cut- and-fill areas. In the cut areas, the topsoil has been removed and the subsoil or underlying material has been exposed. In fill areas, additional loamy material has been placed on the original surface and in many cases has been mixed with the original soil. Man-made land (human-disturbed deposits): The map unit consists of areas from which gravel, sand, or both have been removed (including the surrounding area in which the mining by-products have been placed) and urban land (areas covered by buildings, roads, and parking lots). 1 Map symbols consist of numbers or of a combination of numbers and a letter. The initial numbers represent the kind of soil. An uppercase letter following these numbers indicates the class of slope, A = 0–2%, B = 2–5%, C = 5–10%, D = 10–15%, E = 15–25%, F = 25–35%, G = 35–60%, except for the letter "L," which indicates flooding of long duration. Symbols without a slope letter are for miscellaneous areas. A final number of 2 following the slope letter indicates that the soil is moderately eroded, and a final number of 3 indicates that the soil is severely eroded. 2 Asterisk denotes soils that are excessively to somewhat excessively drained. 3 The type of vegetation cover associated with each soil series is denoted by symbols: P = prairie; TR = transitional cover; T = timber (forested). Poorly drained Somewhat poorly drained Moderately well drained Excessively to well drained Parent material class Natural soil drainage 2,3 Table 1 Soil series (map unit) by parent materials and drainage class. 1 Parent materials in soil profile (USDA) Thick loess (> 60 inches) Moderately thick loess (40–60 inches) on medium- to fine-textured, Wisconsinan loamy sands or sands Moderately thick to thin loess or silty material (24–60+ inches) on medium- textured, Wisconsinan outwash Thin loess (10–40 inches) on loam, Wisconsinan till Thin loamy or silty materials on gravelly Wisconsinan outwash Thin silty or loamy materials on sandy and loamy Wisconsinan outwash Thick, sandy Wisconsinan outwash and aeolian materials Sandy to clayey alluvial sediments on bottomlands Organic materials (peat and mucks) Port Byron-Joy Tama-Ipava-Sable Herrick-Virden-Piasa Catlin-Flanigan-Drummer Plano-Proctor-Worthen Saybrook-Dana-Drummer Lorenzo-Warsaw-Wea Jasper-LaHogue-Selma Sparta-Dickinson-Onarga Lawson-Sawmill-Darwin Houghton-Palms-Muskego Fayette-Rozetta-Stronghurst Clinton-Keomah-Rushville Birkbeck-Sabina-Sunbury St. Charles-Camden-Drury Dodge-Russell-Miami Casco-Fox-Ockley Martinsville-Sciotoville Oakville-Lamont-Alvin Table 2 Soil associations of Illinois in the Spring Bay Quadrangle (after Fehrenbacher et al. 1984). Soil parent materials Prairie (dark and moderately dark) Timber (light and moderately dark) Soils and Parent Materials The soils and parent materials map of the Spring Bay Quadrangle was developed from the compilation and correlation of the soil surveys for Peoria County (Walker 1992), Woodford County (Teater 1999), and Tazewell County (Teater 1996). This compilation was produced specifically for the Illinois State Geological Survey (ISGS) project as part of an agreement with the U.S. Department of Agriculture, Natural Resources Conservation Service (USDA, NRCS). The soil map unit boundaries (soil series) were transferred onto mylar overlays superimposed on 1:12,000 scale (quarter-quadrangle) prints of the 1998/1999 Digital Orthophoto Quadrangles and 1996 U.S. Geological Survey Digital Line Graph hypsography (contour lines). The mylar overlays with hand-drawn boundaries were then scanned. The resulting raster image was translated into vector data using ArcInfo ® software. This process created a digital database to which various attributes of the soil series were added. Prior to the release of NRCS soils data, correlation of Major Land Resource Areas (MLRA) in Peoria and Woodford Counties was required. The updated MLRA legends for Peoria County, Woodford, and Tazewell Counties were used to compile the map unit legend. Because this update was applied only to the soils on this map, its publication makes available the most recent interpretation of the soils and parent materials on the quadrangle. The soil series displayed on this map are organized by their parent material in the map legend using a soil key provided by the NRCS office in Champaign (table 1). Because soil properties are closely related to the characteristics of their parent materials, the individual soil series within parent material classes were categorized using information from the USDA soil associations of Illinois (table 2) and information collected during field work for the surficial geology map of the quadrangle (Stumpf and Weibel in review). Within each parent material class, the soil series were further organized based upon the thickness of a silty or loamy surface cover, the vegetation type under which the soil series formed, and the USDA drainage class. The soil series or map unit is color-coded according to the soil association in which it belongs. The colors correspond to those used in the soil associations of Illinois (table 2). Soil associations of Illinois, as defined in Fehrenbacher et al. (1984), group soils on the basis of the parent materials in which they formed, their surface-soil color, degree of development, and natural soil drainage. The soils in an association tend to form a characteristic pattern on the landscape that is often repeated. References Fehrenbacher, J.B., J.D. Alexander, I.J. Jansen, R.G. Darmody, R.A. Pope, M.A. Flock, E.E. Voss, J.W. Scott, W.F. Andrews, and L.J. Bushue, 1984, Soils of Illinois: University of Illinois at Urbana-Champaign, College of Agriculture, Agricultural Experiment Station and U.S. Department of Agriculture, Soil Conservation Service, Bulletin 778, 85 p. Teater, W.M., 1996, Soil survey of Tazewell County, Illinois: Washington DC, United States Department of Agriculture, Natural Resources Conservation Service, 210 p. Teater, W.M., 1999, Soil survey of Woodford County, Illinois: Washington DC, United States Department of Agriculture, Natural Resources Conservation Service, 326 p. Walker, M.B., 1992, Soil survey of Peoria County, Illinois: United States Department of Agriculture, Soil Conservation Service, 225 p. 572 800 800 800 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 700 700 700 700 700 700 700 700 700 700 700 700 700 700 700 700 700 700 650 650 650 650 650 650 650 650 650 650 650 650 650 650 650 650 650 650 650 650 650 600 600 600 600 600 600 600 600 600 600 600 600 600 600 600 600 600 600 600 600 600 600 600 600 600 600 550 550 550 550 550 550 550 550 550 550 550 550 550 550 550 550 550 550 550 550 550 550 550 550 550 550 550 510 510 510 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 450 450 450 450 450 450 450 450 450 450 450 450 480 530 540 520 520 D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " "" " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " "" " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " "" " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " "" " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " ! ! ! ! ! ! ! ! ! ! ! ! n n æ æ æ 2 11 14 23 26 35 15 22 11 14 23 1 12 13 24 25 10 14 23 27 34 R 3 W R 4 W R 8 E T 10 N T 9 N T 10 N T 9 N 6 7 18 35 2 11 13 24 26 35 5 36 31 1 12 18 19 25 36 6 30 31 6 7 18 19 30 31 6 7 18 19 5 8 17 20 29 32 5 8 17 20 4 9 16 21 28 33 4 9 16 21 3 10 15 22 27 34 3 10 15 22 T 28 N T 27 N R 3 W R 4 W 26 R 9 E R 8 E 40 29 6 29 26 6 40 381 381 29 40 29 26 116 P E O R I A L A K E U P P E R I L L I N O I S RIVER Dickison Run Big Hollow Creek Funks Run Blue Creek 89°37'30" 40°52'30" 89°37'30" 40°45' 40°45' 40°52'30" 89°30' 89°30' 45 28 000m. N. 45 15 000m. N. 45 27 45 26 45 25 45 24 45 23 45 22 45 21 45 20 45 19 45 18 45 17 45 16 45 27 45 26 45 25 45 24 45 23 45 22 45 21 45 20 45 19 45 18 45 17 45 16 2 79 2 80 2 81 2 82 2 83 2 84 2 85 2 86 2 87 2 88 000m. E. 2 81 2 82 2 83 2 84 2 85 2 86 2 87 2 80 000m. E. 2 88 CHILLICOTHE P A R T R I D G E RICHWOODS RICHWOODS M E D I N A S P R I N G W O R T H B A Y P E O R I A C I T Y 857G 279B 7304B 7304B 7304B 7304B 87B 801B 827B 827B 827B 533 54C 54C 54C 814A 87B 87B 689B 279B 279B 440A 290A 672B 290A 440A 87B 801B 290A 827B 290A 54B 199A 224F 224F 224F 54B 43A 43A 865 828B 827B 827B 827B 24D 935G 3304A 224F 224F 224F 54B 857G 440A 827B 3406L 3406A 533 7304B 857G 857G 818D 818D 689B 689B 689D 3239A 290A 224F 689B 224F 224F 827B 8368A 87B 935F 210A 24D 279B 818D 818D 86B 672B 689D 857G 280C2 199A 802B 3070L 801B 533 8073A 567B2 17A 818D 131A 224F 935F 935F 54B 935G 801B 17A 24D 24D 379A 3239A 689D 224F 3406L 689B 689B 802 379A 3028A 533 24C2 8077A 279B 567B2 100A 935G 37B 3070L 131F 24D 379A 224F 827B 3360A 8368A 440A 131F 87B 54B 131B 279C2 280D2 37B 131D 131D 935G 570A 935F 68A 68A 54B 17A 672B 533 8077A 131D 131D 131F 3304A 689B 935G 3092L 672B 935G 3092L 54B 68A 3092A 567B2 24D 131B 290A 3070L 935F 818D 290A 224F 125A 279B 87B 24D 17A 570B 802 199A 24D 19C3 570A 387A 935F 131F 7070A 54B 3360A 87B 125A 801B 7070A 87B 54B 3360A 689B 8077A 279B 672B 54C 54C 24D 131A 17A 3092L 24D 801B 280C2 935F 86B 814A 379A 224F 567B2 257A 8073A 145B2 801B 224F 935G 131B 131A 24D 24 D 689D 935G 865 3092A 125A 54B 24D 935G 280C2 24C2 54C 87B 131B 131B 68A 379A 87B 54B 24C2 24D 131A 672B 689B 224F 379A 131F 379A 827B 280D2 224F 87B 672B 24D 125A 440A 801B 224F 24D 54B 24D 814A 131B 279B 54B 379A 3304A 210A 86B 68A 224F 131A 243A 379A 379A 131A 24D 570B 440A 131D 131A 387A 802B 801B 125A 290A 567C2 24C2 3360A 279B 440B 86B 935F 8077A 689B 818D 24C2 672B 131B 125A 8077A 379A 87B 689D 87B 17A 233D2 570B 24D 17A 54C 131B 689D 672B 857G 857G 689D 827B 131B 17A 43A 24D 257A 279C2 689 B 233C2 3360A 131B 233C2 570B 8107A 3092A 131B 68A 131C 689B 24D 567B2 131A 224F 570A 689D 233C2 280C2 145C2 131A 131A 8368A 570A 87B 54B 131B 233C2 935G 827B 54B 131D 257A 131A 672B 801B 3360A 224F 131D 865 689B 570C2 131D 818D 54C 440A 440A 131F 279B 257A 689B 280C2 87B 280C2 145B2 280C2 134C2 275A 54C 7070 A 54C 224F 131B 86B 818D 198 A 3092L 131B 68A 131A 19E3 379A 257 A 689B 935F 689B 672B 570A 43A 570B 54B 533 24D 379A 131A 19D3 689B 171B2 87B 570B 280D2 86B 43A 125A 86B 857G 8077A 818D 87B 330A 17A 3406A 43A 570 A 330A 379A 280C2 86B 224F 224E 24C2 7070A 570A 87B 125A 8368A 8077A 198A 290A 131B 570B 570B 280D2 54B 570B 131F 280 C2 19E3 17 A 19C3 131 B 233C2 224F 87B 330A 280C2 19C3 672B 280C2 280D2 7304B 210A 131A 672B 672B 24D 54C 279B2 131A 131B 570B 689D 257A 379A 567B2 24D 689D 570 C2 54 B 131A 16A 280D2 8451A 131F 131A 279B 672 B 8077A 233 C2 279B2 570C2 24 D 279C2 827B 570A 131D 689B 54B 131 B 570B 54B 24C2 935F 131B 280D2 935G 132A 131F 814A 7070A 8368A 280C2 131A 801B 8073A 279B2 3406 L 87B 87B 567B2 3092L 3092L 24D 131B 19D3 86B 131 B 440A 3092L 570 C2 280F 279 C2 19D3 131B 37B 440 A 8077A 689D 630C 233C2 68A 43A 672 B 280C2 19C3 280C2 131B 87B 279C2 570A 3092L 87B 131B 24D 689D 3360A 125 A 3304A 17 A 233 C2 43A 37B 19 D3 3092L 440 A 279B 570C2 935G 171B2 570C2 689D 689D 54B 570B 37B 54B 131A 131D 24D 689D 279 C2 570A 131D 16A 131B 131A 16A 440A 224F 87B 618C2 224F 802 131A 8077A 19D3 131B 131A 818D 224D3 567C2 224F 24D 24C2 24D 54B 279B 672B 24D 243B 54B 8077A 8073A 330A 233D2 379 A 379A 19 C3 8077A 24 D 8074A 257A 131A 935F 257A 3239 A 3304A 224F 330A 280C2 279 B2 379A 24D 279B 68A 7070A 131D 125A 567B2 68A 257A 280 C2 3028A 68 A 7070A 440B 689B 131B 54C 19E3 279B 257A 618C2 280C2 19D3 24D 279B 279 B 290A 87B 279B 24D 618C2 17A 17 A 818D 24D 570A 86B 68 A 17A 87B 330A 630C 24C2 19 C3 68A 279 C2 19C3 567B2 131B 257A 257 A 87B 689D 672B 935G 87B 145C2 131B 17A 618 C2 257 A 280 D2 379 A 280C2 802 B 148B 131 B 233D2 233 C2 125A 8073A 440A 131F 630C 24D 19C3 589B 125A 280C2 24D 87B 570 C2 801B 618 D2 224 D3 379A 935G 43A 279B2 3304A 7070 A 257 A 570B 440A 54B 54B 7070A 131B 3451A 233D2 17A 689 B 131F 379A 68A 618C2 570C2 567 B2 689 B 68A 280D2 280D2 279B 570A 279C2 7070A 24D 224F 689B 17A 131 A 125 A 68A 935 F 689 D 87B 210A 131 B 131A 134C2 567B2 279B 818D 280F 24D 570A 818 D 131B 801B 17A 37B 54B 3360A 280C2 818D 440B 17A 935G 131D 689B 672 B 440A 689B 224F 440 A 279 C2 131 B 570A 131D 87B 224F 827B 134C2 327C2 87B 440A 570 A 8077A 440A 131C 43A 3092 A 630 C 7070 A 570C2 24D 3092L 279B 24D 570A 689D 17A 54B 19C3 672B 17A 131D 279B 243A 17A 87B 440A 440B 68 A 330 A 17A 8073 A 7070A 19C3 672B 87B 3070L 224F 935F 16A 199 A 330A 210A 689D 440A 54C 68 A 87B 17A 54C 233C2 814A 330A 43A 379A 8077A 68 A 87B 8077A 16A 330 A 17A 43A 379A 86C2 801B 567C2 290 A 43A 43A 935G 257A 618 D2 440A 131 D 125A 440A 131A 24C2 68A 43A 17A 224F 567 B2 257A 54C 567C2 17A 233D2 86 B 224F 87B 3092L 689B 7070 A 125A 145C2 8368A 279 B 801B 131A 689B 618 D2 257A 857G 330 A 125A 125A 279 B 818 D 935F 131F 17A 17A 233C2 233C2 19C3 567B2 935G 279B2 224F 279C2 68A 233D2 279C2 567 B2 68A 618 C2 570E2 567B2 279B2 8073A 689B 87B 43A 279B 801B 131D 379A 818D 224F 818D 618C2 24C2 224F 935G 935 F 8107A 618C2 279B2 567 C2 54B 233C2 24C2 672 B 935 G 8073 A 330A 570C2 68A 935G 24C2 233C2 279B 279B 279B 279B 279B 827B 814A 3406L 7304B 54B 290A 689B 689B 689D 689D 290A 290A 210A 857G 857G 857G 857G 857G 857G 857G 857G 857G 857G 857G 857G 857G 857G 818D 24C2 279B 279B 857G 857G 857G 857G 857G 857G 857G 857G 857G 857G 857G 857G 857G 857G 857G 857G 279B 279B 86B
Transcript of So i l S a n d P Ma t e r i a l S o f SP r i n g Ba y Qu a...
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The Illinois State Geological Survey, the Illinois Department of Natural Resources, and the State of Illinois make no guarantee, expressed or implied, regarding the correctness of the interpretations presented in this document and accept no liability for the conse-quences of decisions made by others on the basis of the information presented here. The geologic interpretations are based on data that may vary with respect to accuracy of geographic location, the type and quantity of data available at each location, and the scientific/technical qualifications of the data sources. Maps or cross sections in this document are not meant to be enlarged.
For more information contact:Illinois State Geological Survey 615 East Peabody Drive Champaign, Illinois 61820-6964 (217) 244-2414 http://www.isgs.uiuc.edu
Base map compiled by Illinois State Geological Survey from digital data provided by the United States Geological Survey. Topography compiled by the United States Geological Survey from imagery dated 1946. Revised and updated from imagery dated 1995. Field checked 1996.
North American Datum of 1983 (NAD 83)Projection: Transverse Mercator10,000-foot ticks: Illinois State Plane Coordinate system, west zone (Transverse Merca-tor)1,000-meter ticks: Universal Transverse Mercator grid system, zone 16
Recommended citation:Stumpf, A.J., and C.P. Weibel, 2004, Soils and Parent Materials of Spring Bay Quadran-
gle, Peoria and Woodford Counties, Illinois: Illinois State Geological Survey, Illinois Geologic Quadrangle Map, IGQ Spring Bay-SPM, 1:24,000.
BASE MAP CONTOUR INTERVAL 10 FEET
SUPPLEMENTARY CONTOUR INTERVAL 5 FEET
NATIONAL GEODETIC VERTICAL DATUM OF 1929
Released by the authority of the State of Illinois: 2004
Transfer of soil map units by Soil Survey staff, Natural Resources Conservation Service, Rock Falls, Illinois.
Raster to vector conversion completed by C. Abert.
Map review provided by Soil Survey staff, Natural Resources Conservation Service, Champaign, Illinois.
Digital cartography by M. Barrett, Illinois State Geological Survey.
Department of Natural ResourcesILLINOIS STATE GEOLOGICAL SURVEY
William W. Shilts, Chief
SoilS and Parent MaterialS of SPring Bay Quadrangle
Peoria and Woodford CountieS, illinoiS
Andrew J. Stumpf and C. Pius Weibel2004
Illinois Geologic Quadrangle Map IGQ Spring Bay-SPM
IGQ Spring Bay-SPM
ADJOINING QUADRANGLES1 Edelstein2 Rome3 Chillicothe4 Dunlap5 Germantown Hills6 Peoria West7 Peoria East8 Washington
.5 1 KILOMETER1 0
SCALE 1:24000
1/2 1 MILE 01
600050004000 7000 FEET 30001000 10000 2000
ROAD CLASSIFICATION
Primary highway,hard surface
Secondary highway,hard surface
Light-duty road, hard orimproved surface
Unimproved road
State Route
Sarpy*(3092A, 3092L)
Joy(275)P
Osco(86)P
Ipava(43)P
Sable (68)P
Elkhart(567)P
Clarksdale(257)TR
Fayette(280)(827)T
Rozetta(279)(827)T
Keomah(17)(814)T
Rushville(16)(814)T
Navlys(630)T
Sylvan(19)T
Catlin(171)P
Birkbeck(233)T
Saybrook(145)P
Dodge(24)T
Senachwine(618)T
Hennepin(935)(818)(87)T
Hickory(818)T
Strawn(224)(818)(857)T
Plano(199)P
Elburn(198)P
St. Charles(243)T
Proctor(148)P
Starks(132)T
Camden(134)T
Jasper(440)P
Selma(125)P
Ockley(387)T
Martinsville(570)T
Cresent(672)P
Warsaw(290)(828)P
Dakota(379)(828)P
Fox(327)T
Plainfield(54)T*
Coloma(689)T*Dickinson
(87)P
Alvin(131)T
Worthen(37)P
Peotone(330)P
Lena(210A)
Palms(100A)
Landes(3304A, 7304B)
Ross(8073A)
Raveenwash(8368A)
Slacwater(3360A)
Jules(3028A)
Paxico(3406A, 3406L)
Dorchester(3239A)
Huntsville(8077A)
Lawson(3451A, 8451A)
Radford(8074A)
Beaucoup(3070L, 7070A)
Sawmill(8107A)
Bowdre(589B)
ORTHENTS (801, 802)
MAN-MADE MATERIALS (865, 533)
Loess(0–20 inches thick)
over glacial till
Loess(40–60 inches thick)over glacial outwash
Loess(20–40 inches thick)over glacial outwash
Loess(0–20 inches thick)
over glacial outwash
Loamy materials(40–60 inches thick)over glacial outwash
Loamy materials(20–40 inches thick)over glacial outwash
Loess(>60 inches thick)
Loess(40–60 inches thick)
over glacial till
Loess(20–40 inches thick)
over glacial till
Aeolian sand(>60 inches thick)
Loamy materials(20–40 inches thick)over aeolian sand
Silty and clayeymaterials
Silty and loamy materials(>40 inches thick)
Alluvium (sandy)(20–40 inches thick)over alluvium (loamy)
Alluvium (loamy)
Alluvium (silty)
Alluvium (clayey)
Sapric materials (muck)(>51 inches thick)
Sapric materials (muck)(16–51 inches thick)
over glacial drift
Loess: Windblown silt and fine-grained sand; dark yellowish gray to yellowish brown in color; texturally ranges from a silt to silt loam; blankets upland areas along the Illinois River valley; absent from geomorphic surfaces that postdate its deposition (e.g., floodplains).
Glacial till: Sediment composed of a mixture of clay, silt, sand, and rocks deposited by glaciers; reddish brown to dark grayish brown in color; loamy textured; hard to firm; forms many of the uplands in the area; absent in the Illinois River valley where it has been removed by postglacial erosion.
Glacial outwash: Stratified deposits of sand, gravel, cobbles, and boulders; yellowish brown to grayish brown in color; mostly clean with very little silt; very well to moderately sorted proglacial fluvial sediments deposited by meltwater flowing in front of melting glaciers; forms a series of terraces, bars, and channel deposits in the Illinois River valley.
Aeolian sand: Very fine- to medium-grained sand; loose; non-calcareous in upper part; postglacial windblown sand composing dunes and undulating sandy deposits on terraces and uplands.
Colluvium: Stratified or massive, silty or clayey deposits infilling depressions on the uplands and on foot slopes of valley walls; remobilized till, outwash, and loess.
Organic soil material: Peat, organic silt, and muck; dark gray to black; usually water saturated; accumulates in abandoned channels, shallow lakes, and low-lying depressions on the modern floodplain.
Alluvium: Stratified sand and gravel with some beds of silt and clay or diamicton; yellowish brown to gray; may be either calcareous or non-calcareous; seasonally wet and often gleyed; subject to flooding and overland flow; the finer-grained sediments often contain humus, dispersed wood fragments and shells, or man-made waste; upper part weathered; postglacial (modern) lake or stream sediments deposited over the past 12,000 years on floodplains, along channels, and in seasonally ponded lakes; also includes sediments forming fan-shaped landforms in areas where streams or ravines emerge from uplands onto lower-gradient floodplains.
Orthents (silty to loamy): Materials generally in cut-and-fill areas. In the cut areas, the topsoil has been removed and the subsoil or underlying material has been exposed. In fill areas, additional loamy material has been placed on the original surface and in many cases has been mixed with the original soil.Man-made land (human-disturbed deposits): The map unit consists of areas from which gravel, sand, or both have been removed (including the surrounding area in which the mining by-products have been placed) and urban land (areas covered by buildings, roads, and parking lots).
1Map symbols consist of numbers or of a combination of numbers and a letter. The initial numbers represent the kind of soil. An uppercase letter following these numbers indicates the class of slope, A = 0–2%, B = 2–5%, C = 5–10%, D = 10–15%, E = 15–25%, F = 25–35%, G = 35–60%, except for the letter "L," which indicates flooding of long duration.Symbols without a slope letter are for miscellaneous areas. A final number of 2 following the slope letter indicates that the soil is moderately eroded, and a final number of 3 indicates that the soil is severely eroded.
2Asterisk denotes soils that are excessively to somewhat excessively drained.3The type of vegetation cover associated with each soil series is denoted by symbols: P = prairie; TR = transitional cover; T = timber (forested).
Poorlydrained
Somewhatpoorly
drained
Moderatelywell
drained
Excessivelyto
well drainedParent material class
Natural soil drainage2,3
Table 1 Soil series (map unit) by parent materials and drainage class.1
Parent materials in soil profile
(USDA)
Thick loess (> 60 inches)
Moderately thick loess (40–60 inches) on medium- to fine-textured, Wisconsinan loamy sands or sands
Moderately thick to thin loess or silty material (24–60+ inches) on medium- textured, Wisconsinan outwash
Thin loess (10–40 inches) on loam, Wisconsinan till
Thin loamy or silty materials on gravelly Wisconsinan outwash
Thin silty or loamy materials on sandy and loamy Wisconsinan outwash
Thick, sandy Wisconsinan outwash and aeolian materials
Sandy to clayey alluvial sediments on bottomlands
Organic materials (peat and mucks)
Port Byron-JoyTama-Ipava-SableHerrick-Virden-Piasa
Catlin-Flanigan-Drummer
Plano-Proctor-Worthen
Saybrook-Dana-Drummer
Lorenzo-Warsaw-Wea
Jasper-LaHogue-Selma
Sparta-Dickinson-Onarga
Lawson-Sawmill-Darwin
Houghton-Palms-Muskego
Fayette-Rozetta-StronghurstClinton-Keomah-Rushville
Birkbeck-Sabina-Sunbury
St. Charles-Camden-Drury
Dodge-Russell-Miami
Casco-Fox-Ockley
Martinsville-Sciotoville
Oakville-Lamont-Alvin
Table 2 Soil associations of Illinois in the Spring Bay Quadrangle (after Fehrenbacher et al. 1984).
Soil parent materialsPrairie
(dark and moderately dark)Timber
(light and moderately dark)
Soils and Parent Materials
The soils and parent materials map of the Spring Bay Quadrangle was developed from the compilation and correlation of the soil surveys for Peoria County (Walker 1992), Woodford County (Teater 1999), and Tazewell County (Teater 1996). This compilation was produced specifically for the Illinois State Geological Survey (ISGS) project as part of an agreement with the U.S. Department of Agriculture, Natural Resources Conservation Service (USDA, NRCS). The soil map unit boundaries (soil series) were transferred onto mylar overlays superimposed on 1:12,000 scale (quarter-quadrangle) prints of the 1998/1999 Digital Orthophoto Quadrangles and 1996 U.S. Geological Survey Digital Line Graph hypsography (contour lines). The mylar overlays with hand-drawn boundaries were then scanned. The resulting raster image was translated into vector data using ArcInfo® software. This process created a digital database to which various attributes of the soil series were added.
Prior to the release of NRCS soils data, correlation of Major Land Resource Areas (MLRA) in Peoria and Woodford Counties was required. The updated MLRA legends for Peoria County, Woodford, and Tazewell Counties were used to compile the map unit legend. Because this update was applied only to the soils on this map, its publication makes available the most recent interpretation of the soils and parent materials on the quadrangle.
The soil series displayed on this map are organized by their parent material in the map legend using a soil key provided by the NRCS office in Champaign (table 1). Because soil properties are closely related to the characteristics of their parent materials, the individual soil series within parent material classes were categorized using information from the USDA soil associations of Illinois (table 2) and information collected during field work for the surficial geology map of the quadrangle (Stumpf and Weibel in review).
Within each parent material class, the soil series were further organized based upon the thickness of a silty or loamy surface cover, the vegetation type under which the soil series formed, and the USDA drainage class. The soil series or map unit is color-coded according to the soil association in which it belongs. The colors correspond to those used in the soil associations of Illinois (table 2). Soil associations of Illinois, as defined in Fehrenbacher et al. (1984), group soils on the basis of the parent materials in which they formed, their surface-soil color, degree of development, and natural soil drainage. The soils in an association tend to form a characteristic pattern on the landscape that is often repeated.
References
Fehrenbacher, J.B., J.D. Alexander, I.J. Jansen, R.G. Darmody, R.A. Pope, M.A. Flock, E.E. Voss, J.W. Scott, W.F. Andrews, and L.J. Bushue, 1984, Soils of Illinois: University of Illinois at Urbana-Champaign, College of Agriculture, Agricultural Experiment Station and U.S. Department of Agriculture, Soil Conservation Service, Bulletin 778, 85 p.
Teater, W.M., 1996, Soil survey of Tazewell County, Illinois: Washington DC, United States Department of Agriculture, Natural Resources Conservation Service, 210 p.
Teater, W.M., 1999, Soil survey of Woodford County, Illinois: Washington DC, United States Department of Agriculture, Natural Resources Conservation Service, 326 p.
Walker, M.B., 1992, Soil survey of Peoria County, Illinois: United States Department of Agriculture, Soil Conservation Service, 225 p.
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!
!! !!!
!
!
!
!!
!
nn
æ
æ
æ
2
11
14
23
26
35
15
22
11
14
23
1
12
13
24
25
10
14
23
27
34 R 3
W
R 4
W
R 8 E
T 10 N
T 9 NT 10 N
T 9 N
6
7
18
35
2
11
13
24
26
35
5
36 31
1
12
18
19
25
36
6
30
31
6
7
18
19
30
31
6
7
18
19
5
8
17
20
29
32
5
8
17
20
4
9
16
21
28
33
4
9
16
21
3
10
15
22
27
34
3
10
15
22
T 28 N
T 27 N
R 3
W
R 4
W
26
R 9
E
R 8
E
40
29
6
29
26
6
40
381 381
29
40
29
26
116
PE
OR
IA
LA
KE
UP
PE
R
IL
LIN
OIS
RI V
ER
Dickison
Run
Big
Hollow
Creek
Funks Run
Blue
Creek
89°37'30"
40°52'30"
89°37'30"40°45' 40°45'
40°52'30"
89°30'
89°30'
4528000m.N.
4515000m.N.
4527
4526
4525
4524
4523
4522
4521
4520
4519
4518
4517
4516
4527
4526
4525
4524
4523
4522
4521
4520
4519
4518
4517
4516
279 280 281 282 283 284 285 286 287 288000m.E.
281 282 283 284 285 286 287280000m.E. 288
C H I L L I C O T H E
PA
RT
RI
DG
E
R ICHWOODS
RICHWOODS
M E D I N A
SP
RI
NG
WO
RT
H
BA
Y
P E O R I A C I T Y
857G
279B
7304B
7304B7304B
7304B
87B
801B
827B
827B
827B
533
54C
54C
54C
814A
87B
87B
689B
279B
279B
440A
290A
672B
290A
440A
87B
801B
290A
827B
290A
54B
199A
224F
224F
224F
54B
43A
43A
865
828B
827B
827B
827B
24D
935G
3304A
224F
224F
224F
54B
857G
440A
827B
3406L
3406A
533
7304B
857G
857G
818D818D
689B
689B
689D
3239A
290A
224F
689B
224F
224F
827B
8368A
87B
935F
210A
24D
279B
818D
818D
86B
672B
689D
857G
280C2
199A
802B
3070L
801B
533
8073A
567B2
17A
818D
131A
224F
935F
935F
54B
935G
801B
17A
24D
24D
379A
3239A
689D
224F
3406L
689B
689B
802
379A
3028A
533
24C2
8077A
279B
567B2
100A
935G
37B
3070L
131F
24D
379A
224F
827B
3360A
8368A
440A
131F
87B
54B
131B
279C2
280D2
37B
131D
131D
935G
570A
935F
68A
68A
54B
17A
672B
533
8077A
131D
131D
131F
3304A
689B
935G
3092L
672B
935G
3092L
54B
68A
3092A
567B2
24D
131B
290A
3070L
935F
818D
290A
224F
125A
279B
87B
24D
17A
570B
802
199A
24D
19C3
570A
387A
935F
131F
7070A
54B
3360A
87B
125A
801B
7070A
87B
54B
3360A
689B
8077A
279B
672B
54C
54C
24D
131A
17A
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24D
801B
280C2
935F
86B
814A
379A
224F
567B2
257A
8073A
145B2
801B
224F
935G
131B
131A
24D
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689D
935G
865
3092A
125A
54B
24D
935G
280C2
24C2
54C
87B
131B
131B
68A
379A
87B
54B
24C2
24D
131A
672B
689B
224F
379A
131F
379A
827B
280D2
224F
87B
672B
24D
125A
440A
801B
224F
24D
54B
24D
814A
131B
279B
54B
379A
3304A
210A
86B 68A
224F
131A
243A
379A
379A
131A
24D
570B
440A
131D
131A
387A
802B
801B
125A
290A
567C2
24C2
3360A
279B
440B
86B
935F
8077A
689B
818D
24C2
672B
131B
125A
8077A
379A
87B
689D
87B
17A
233D2
570B
24D
17A
54C
131B
689D
672B
857G857G
689D827B
131B
17A
43A
24D
257A
279C2
689B
233C2
3360A
131B
233C2
570B
8107A
3092A
131B
68A
131C
689B
24D
567B2
131A
224F
570A
689D
233C2
280C2
145C2
131A
131A
8368A
570A
87B 54B
131B
233C2
935G
827B
54B
131D
257A
131A
672B
801B
3360A
224F
131D
865
689B
570C2
131D
818D
54C
440A
440A
131F
279B
257A
689B
280C2
87B
280C2
145B2
280C2
134C2
275A
54C
7070A
54C
224F
131B
86B
818D
198A
3092L
131B
68A
131A
19E3
379A
257A
689B
935F
689B
672B
570A
43A
570B
54B
533
24D
379A
131A
19D3
689B
171B2
87B
570B
280D2
86B
43A
125A
86B
857G
8077A
818D
87B
330A
17A
3406A
43A
570A
330A
379A
280C2
86B
224F
224E
24C2
7070A
570A
87B
125A
8368A
8077A
198A
290A
131B
570B
570B
280D2
54B
570B
131F
280C2
19E3
17A
19C3
131B
233C2
224F
87B
330A
280C2
19C3
672B
280C2
280D2
7304B
210A
131A
672B
672B
24D
54C
279B2
131A
131B
570B
689D
257A
379A567B2
24D
689D
570C2
54B
131A
16A
280D2
8451A
131F
131A
279B
672B
8077A
233 C2
279B2
570C2
24D
279C2
827B
570A
131D689B
54B
131B
570B
54B
24C2
935F
131B
280D2
935G
132A
131F
814A
7070A
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280C2
131A
801B
8073A
279B2
3406L
87B
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567B2
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24D
131B
19D3
86B
131B
440A
3092
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570C2
280F
279C2
19D3
131B
37B
440A
8077A
689D
630C
233C2
68A
43A 672B
280C2
19C3
280C2
131B
87B
279C2
570A
3092L
87B
131B
24D
689D
3360A
125A
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17A
233C2
43A
37B
19D3
3092L
440A
279B
570C
2
935G
171B2
570C2
689D
689D
54B
570B
37B
54B
131A
131D
24D
689D
279C2
570A
131D
16A
131B
131A
16A
440A
224F
87B
618C2
224F
802
131A
8077A
19D3
131B
131A
818D
224D3
567C2
224F
24D
24C2
24D
54B
279B
672B
24D
243B
54B
8077A
8073A
330A
233D2
379A
379A
19C3
8077A
24D
8074
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257A
131A
935F
257A
3239A
3304A
224F
330A
280C2
279B2
379A
24D
279B
68A
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131D
125A
567B2
68A
257A
280C2
3028A
68A
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440B
689B
131B
54C
19E3
279B
257A
618C2
280C2
19D3
24D
279B
279B
290A
87B
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24D
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17A
17A
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24D
570A
86B
68A
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330A
630C
24C2
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279B
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