Berg, Richard C.

McKay III, E. Donald

Stiff, Barbara J.

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McKay, E. Donald, III

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12ROMEMARKVARNALACONHENRYPUTNAMTOLUCAMCNABBWASHBURNMAGNOLIAHOPEWELLHENNEPINTISKILWASTANDARDCEDARPOINTSPARLANDGRANVILLECHILLICOTHESPRING VALLEY PERUBUREAUJUNCTION4 32 61475 3 251855726356754545864 17718316931636122566215823158887979486716289942229859725 471334459734885497489983862526849736511846887178939535163417273322655 149263 569527139131311130301911311111111718111111111118111120192911112032321113291317241514311230301210201718161714311724181619363116262035132123 23362022221814323034302821292924212319103212171819181434351329351933243216231530332735351231332023132512141335253610123636193422 24101917331636 1724173326231529241335252820281315202524171628131414211426242835122226202836363122302522312742734171823271716 35301224212522 211918152133151223353215203335261727272929101024291718271628343618212232343320212330313433363132361522342533 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31041181121022411242116141114614211dgdgdgdg11266612723333 36674376410 410 446772 2666 66101132101116 47666115442210412410 16111112222116 124dg7122664210121126117624114224311 114dgdg 231121644 22331244444444104dg1222642123211661123 2 4104613121162612322376111235664 1106312 72133102222211262111dgdg4 106222 31223311312453331010 126132 61010103634237 112111234116466277342117210342226333623 426 10232121212121234341113642222342111 10103121212107 221212 2102 3333777711172113610664113710 26 621112126623622 612dg43 21071121111112121212731312 6 1223112310147427424212231141222 21dgdg4221221612211112411117721 6 6331110101210312243763616211104321011114110 3312211026 4212636101011114121233322212314222310311222231222101223324 2103212221237224222 2 111362424211044264212121212610 10123376637 13342210 11 211 410242222336213643222143361247102322410223324104343242233627 743427111127314 37102272662210624224 212272213 24266773dg622212 210711147124 142631012122 26621011116163 1341321 2410112136112311144721322331076111132466121 1042dg32112111231112111310346442161134124331126 101631166210241022102331112 21110741021664210101110 47610dg1010 4410106241110107776107 dg7331011743107124767711623101010 47672101010102711 14dg43310103671031167107314333dg7 dg1041010677310 6247212766631212121221010127226212227222122 1322 4211422dg4411222 44104310424324 221113722221047214223443 4211441624 424237443 2 41212422 424210711262231110114 221424264dg 24141212312 41212610112224174 224226114412102210422410414414212124143322112 22232633432281122133331138243 23212321234242234233221110112222111033144108882121210102142242226323221242231224212434224121212121232 1222dg11212121111221333323322143121122 32 1222223 6411134 21023224126222244 42126132312261334342622 4 462233222124141234336 6227222263631223 2324661 777616342726321271062113111414826131367311722 663712172236622101114142 21126142116143333310222126221021266121111211671411711221121411321166663121227101011233 122dg3223171107102310114211022262 27314267 3dg142 31272222210102763267 14 2361222 711dg 1211212333333336 dg 127927777 477411672dg10612 72666421212242211332113222611dg724111123333 31077742244117412 422227666 677 1144127622722422244443347222212927 776 77776 627716733222122722773127222323231 22 2271 393221 2 61 13 1211111111121012126dg1211255dg1211108912125104333126126641110612366661111126101212Rivers and water bodiesMunicipal boundary lineCounty lineSwampy lowland areasInterstate routeState routeU.S. routeDigital cartography by Barbara J. Stiff, Brittany M. Walbright, Jennifer E. Carrell, and Deette Lund, Illinois State Geological Survey.The Illinois State Geological Survey and the University of Illinois make no guarantee, expressed or implied, regarding the correctness of the interpretations presented in this document and accept no liability for the consequences 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 the accuracy of the geographic location, the type and quantity of data available at each location, and the scientific and technical qualifi-cations of the data sources. Maps in this document are not meant to be enlarged. 2 / °1 2APPROXIMATE MEANDECLINATION, 2015MAGNETIC  NORTHTRUE  NORTHQUADRANGLES1 Princeton South2 DePue3 Spring Valley4 Putnam5 Florid6 McNabb7 Lacon8 Henry9  Varna10 Rome11 Chillicothe12 Washburn1 2 34 657 8 910 11 12© 2015 University of Illinois Board of Trustees. All rights reserved.For permission information, contact the Illinois State Geological Survey.For more information contact:  Prairie Research Institute Illinois State Geological Survey  615 East Peabody Drive Champaign, Illinois 61820-6918 (217) 244-2414 http://www.isgs.illinois.eduBase map compiled by the Illinois State Geological Survey from digital and paper data provided by the United States Geological Survey.North American Datum of 1983 (NAD 83)Projection: Transverse MercatorRecommended citation:Berg, R.C., B.J. Stiff, and E.D. McKay III, 2015, Soil parent materials of the middle Illinois River valley, Bureau, LaSalle, Marshall, Peoria, Putnam, and Woodford Counties, Illinois: Illinois State Geological Survey, Illinois Map 21, 1:62,500.SOIL PARENT MATERIALS OF THE MIDDLE ILLINOIS RIVER VALLEYBUREAU, LASALLE, MARSHALL, PEORIA, PUTNAM, and WOODFORD COUNTIES, ILLINOISRichard C. Berg, Barbara J. Stiff, and E. Donald McKay III 2015Illinois Map 212015ILLINOIS STATE GEOLOGICAL SURVEYPrairie Research InstituteUniversity of Illinois at Urbana-Champaign1 7  KILOMETERS0 1 2 43 5 6SCALE 1:62,5001 5 MILES10 2 3 4DiscussionThe Soil Parent Materials map for the area of the middle Illinois River valley (from south of Chillicothe to just south of the big bend of the Il-linois River) was developed for the Illinois Route 29 project under a contract with the Illinois Department of Transportation. The map shows geological materials that compose the uppermost five feet beneath the land surface as interpreted from U.S. Department of Agriculture (USDA) soil maps for Peoria (Walker 1992), Bureau (Zwicker 1992a), Putnam (Zwick-er 1992b), Woodford (Teater 1999), Marshall (USDA-Natural Resources and Conservation Service 2000), and LaSalle (Deniger 2008) Counties. The Soil Parent Materials map provides a detailed depiction of the vari-ous geologic materials that constitute the parent materials from which developed the profile of the modern soil. It differs from the original soil maps by emphasizing parent material but does not retain other components of soil series map unit classification, such as slope, horizon thickness, or drainage class. The uppermost geological materials were determined by grouping 122 soil series in the mapping area into 14 soil parent material groups (see map legend). The groups, summarized below, are differentiated on the basis of soil series compositions and on their positions on the landscape.• Thick loess (wind-deposited silt) soil series, including Tama, Musca-tine, and Downs, are all developed in loess more than 60 inches (152 centimeters) thick and mostly occur on uplands overlying diamicton (glacially deposited mixture of sand, silt, clay, and gravel that is com-monly called “till”). • Soils developed in 40 to 60 inches (102 to 152 centimeters) of loess occur over diamicton or sand and gravel. Five soil series, including Flanagan and Catlin, are characterized by loess overlying diamicton that occurs mostly on uplands and on the upper portions of slopes. Seven soil series, including Virgil and Batavia, have loess overlying sand and gravel that occurs mainly along the sides of streams tributary to the Illinois River and also in the main Illinois River valley. • Seventeen soil series, including Blount, Miami, and Senachwine, usually are characterized by less than 20 inches (51 centimeters) of loess overlying diamicton and occur on slopes of streams tributary to the Illinois River as well as on slopes adjacent to the main Illinois River valley. Thirteen soils, including Camden and Brenton, have less than 40 inches (102 centimeters) of loess (or silty alluvium) overlying sand and gravel. These soils occur along the sides of streams tributary to the Illinois River and also in the main Illinois River valley. Mar-seilles, which is characterized as loess overlying shale bedrock, occurs in lower slope positions in northeastern Peoria County and extends northward into Marshall County.• Sandy soils are divided as fololws: (1) The Metea series, characterized by less than 20 inches (51 centimeters) of sand overlying diamicton, occurs only east of the Illinois River, where it was probably derived from sand in the Illinois valley that was blown by wind onto the adja-cent uplands. (2) Other dune soils (eight series), including Bloomfield, Sparta, and Oakville, are all characterized by more than 60 inches (152 centimeters) of sandy windblown sediments that occur on terraces in the Illinois River valley or on the uplands east of the valley. (3) Twelve sand and gravel soil series, including Rodman, Warsaw, and Dakota, occur mainly on terraces in the Illinois River valley and in some of the larger streams tributary to the Illinois River. • Alluvial and colluvial soils are composed of fine and coarse sediments that often overlie silty materials or sand and gravel. Peotone, Slacwa-ter, and Raveenwash are colluvial soils that occur along lower slopes as slopewash and gravity deposits, and in depressions on uplands. Sawmill, Lawson, and Huntsville, for example, are soils that formed in alluvial valleys of modern streams and rivers. Some alluvial soils, such as Worthen and Terril, occur as alluvial fans that emanated from tribu-tary streams and were deposited on terraces along the Illinois River. • Peat (Lena series) occurs in restricted areas of the Illinois River flood plain.• Soils on urban land, dumps, fill, and pits are characterized as disturbed ground.The Soil Parent Materials map was used to help define geological bound-aries for the Surficial Geology of the Middle Illinois River Valley map (McKay et al. 2010), particularly between (a) thick (>60 inches) and thin (<60 inches) loess overlying diamicton, (b) alluvium and colluvium in val-leys, and (c) diamicton and bedrock on valley sides. The Soil Parent Materials map complements the Surficial Geology of the Middle Illinois River Valley map (McKay et al. 2010), which delineates geologic materials classified by both their lithology (sediment type or rock type) and stratigraphy (relative position and age).ReferencesDeniger, J., 2008, Soil survey of LaSalle County, Illinois: U.S. Department of Agriculture, Natural Resource Conservation Service, in cooperation with the Illinois Agricultural Experiment Station, 913 p. McKay, E.D., III, R.C. Berg, A.J. Stumpf, and C.P. Weibel, 2010, Surficial geology of the middle Illinois River valley, Bureau, Marshall, Peoria, Putnam, and Woodford Counties, Illinois: Illinois State Geological Survey, Illinois Map 16, 1:48,000; report, 7 p.Teater, W.M., 1999, Soil survey of Woodford County, Illinois: U.S. De-partment of Agriculture, Natural Resources Conservation Service, in cooperation with the Illinois Agricultural Experimental Station, 326 p.U.S. Department of Agriculture, Natural Resources Conservation Ser-vice, 2000, Soil Survey Geographic (SSURGO) database for Marshall County, Illinois: U.S. Department of Agriculture, Natural Resources Conservation Service, IL123, http://websoilsurvey.nrcs.usda.gov/ (ac-cessed December 16, 2015). (Data originally accessed in 2000 from http://www.ftw.nrcs.usda.gov/ssur_data.html)Walker, M.B., 1992, Soil survey of Peoria County, Illinois: U.S. Depart-ment of Agriculture, Soil Conservation Service, in cooperation with the Illinois Agricultural Experiment Station, 225 p.Zwicker, S.E., 1992a, Soil survey of Bureau County, Illinois: U.S. Depart-ment of Agriculture, Soil Conservation Service, in cooperation with the Illinois Agricultural Experiment Station, 302 p.Zwicker, S.E., 1992b, Soil survey of Putnam County, Illinois: U.S. Depart-ment of Agriculture, Soil Conservation Service, in cooperation with the Illinois Agricultural Experiment Station, 168 p. Disturbed groundLoess >60 inchesLoess 40–60 inches over diamictonLoess <40 inches over diamictonLoess <20 inches over loamy diamictonLoess <20 inches over clayey diamictonLoess 40–60 inches over outwashLoess over limestone bedrockLoess over bedrock (sandstone, siltstone, shale)PeatSand and gravelDune sandAlluvium and colluviumOther (mine spoil or earth fill)Other (gravel pits)Soil Parent Materials1413121110987654321dg

Soil parent materials of the middle Illinois River Valley : Bureau, LaSalle, Marshall, Peoria, Putnam, and Woodford counties, Illinois

https://www.ideals.illinois.edu/bitstream/2142/89863/2/imap21.pdf

Soil parent materials of the middle Illinois River Valley : Bureau, LaSalle, Marshall, Peoria, Putnam, and Woodford counties, Illinois

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