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APPROXIMATE MEANDECLINATION, 2004
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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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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
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
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
8368A
280C2
131A
801B
8073A
279B2
3406L
87B
87B
567B2
3092L
3092L
24D
131B
19D3
86B
131B
440A
3092
L
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
3304A
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
A
257A
131A
935F
257A
3239A
3304A
224F
330A
280C2
279B2
379A
24D
279B
68A
7070A
131D
125A
567B2
68A
257A
280C2
3028A
68A
7070A
440B
689B
131B
54C
19E3
279B
257A
618C2
280C2
19D3
24D
279B
279B
290A
87B
279B
24D
618C2
17A
17A
818D
24D
570A
86B
68A
17A
87B
330A
630C
24C2
19C3
68A
279C2
19C3
567B2
131B
257A
257A
87B
689D
672B
935G
87B
145C2
131B
17A
618C2
257A
280D2
379A
280C2
802B
148B
131B
233D2
233C2
125A
8073
A
440A
131F
630C
24D
19C3
589B
125A
280C2
24D
87B
570C2
801B
618D2
224D3
379A
935G
43A
279B2
3304A
7070A
257A
570B
440A
54B
54B
7070
A
131B
3451A
233D2
17A
689B
131F
379A
68A
618C2
570C2
567B2
689B
68A
280D2
280D2
279B
570A
279C2
7070A
24D
224F
689B
17A
131A
125A
68A
935F
689D
87B210A
131B
131A
134C2
567B2
279B
818D
280F
24D
570A
818D
131B
801B
17A
37B
54B
3360A
280C2
818D
440B
17A
935G
131D
689B
672B
440A
689B
224F
440 A
279C2
131B
570A
131D
87B
224F
827B
134C2
327C2
87B
440A
570A
8077A
440A
131C
43A
3092A
630C
7070A
570C2
24D
3092L
279B
24D
570A
689D
17A
54B
19C3
672B
17A
131D
279B
243A
17A
87B
440A
440B
68A
330A
17A
8073A
7070
A
19C3
672B
87B
3070L
224F
935F
16A
199A
330A
210A
689D
440A
54C
68A
87B
17A
54C
233C2
814A
330A
43A
379A
8077A
68A
87B
8077A
16A
330A
17A
43A
379A
86C2
801B
567C2
290A
43A
43A
935G
257A
618D2
440A
131D
125A
440A
131A
24C2
68A
43A
17A
224F
567B2
257A
54C
567C2
17A
233D2
86B
224F
87B
3092L
689B
7070A
125A
145C2
8368A
279B
801B
131A
689B
618D2
257A
857G
330A
125A
125A
279B
818D
935F
131F
17A
17A
233C2
233C2
19C3
567B2
935G
279B2
224F
279C2
68A
233D2
279C2
567B2
68A
618C2
570E2
567B2
279B2
8073A
689B
87B
43A
279B
801B
131D379A
818D
224F
818D
618C2
24C2
224F
935G
935F
8107A
618C2
279B2
567C2
54B
233C2
24C2
672B
935G
8073A
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
857G857G
857G
857G
857G
857G
818D
24C2
279B
279B
857G
857G
857G
857G
857G
857G
857G
857G
857G
857G857G
857G
857G
857G
857G
857G
279B
279B
86B
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