https://ir.uiowa.edu/igs_ofm/1038/thumbnail.jp

Bettis, E Arthur, III

Giglierano, James D

Quade, Deborah J

English

Iowa Research Online

Hudson Episode  Qo - Depressions (DeForest Formation-Woden Mbr.)  Generally 2.5 to 6 meters of black to very dark gray, calcareous, muck, peat and silty clay loam colluvium and organic sediments in drained and undrained closed and semi-closed depressions.  Overlies gray, calcareous, massive, dense loam diamicton (Dows Fm.-Alden Mbr.) or Noah Creek Fm. sand and gravel. Associated with low relief features that occupy depressions and low sags on the landscape. Supports wetland vegetation and can be permanently covered by water.   High water table.     Qal - Alluvium (DeForest Formation-Undifferentiated) Variable thickness (<1 to 5 meters) of very dark gray to brown, noncalcareous to calcareous, stratified silty clay loam, clay loam, loam to sandy loam alluvium and colluvium in stream valleys, on hill slopes and in closed depressions. May overlie Dows Formation (Morgan or Alden Mbrs.), or Noah Creek Formation. Off the Des Moines Lobe this unit overlies Sheldon Creek Formation diamicton. Associated with low-relief modern floodplain, closed depressions, modern drainageways or toeslope positions on the landscape.  Seasonal high water table and potential for frequent flooding.    Wisconsin Episode  Qe - Sand Dunes and Sand Sheets (Peoria Formation-sand facies) Generally less than 3 meters of yellowish brown, massive, calcareous loamy sand to fine sand.  It may overlie yellowish -brown coarse-grained sand and gravel (Noah Creek Fm.), or it may overlie yellowish to grayish brown, usually calcareous, stratified loam to silt loam to sandy loam diamicton (Dows Fm.-Morgan Mbr.).  Usually restricted to a narrow belt along major river valley bottoms or adjacent uplands on the Des Moines Lobe.   Off the Des Moines Lobe this unit is not restricted to dunes along valley areas and may occur as sand stringers overlying unnamed erosion surface loamy sediments.   Qtp - Till plain  (Dows Formation-Morgan Mbr.)  Less than 8 meters of yellowish brown, often calcareous and fractured, stratified loam to silt loam to sandy loam diamicton; textures can be quite variable. Overlies gray, calcareous, massive, dense loam diamicton (Dows Fm.-Alden Mbr.).  Low to moderate relief  (3 to 8 meters), undulating plains with irregular surface patterns.  Seasonal high water table.    Qtr_bm - Till ridge (Dows Formation-Morgan Mbr.)  Generally 3 to 5 meters of yellowish to grayish brown, usually calcareous and fractured, stratified loam to silt loam; stratified sands and gravels to sandy loam diamicton; textures can be quite variable.  Overlies gray, calcareous, massive, dense loam diamicton (Dows Fm.-Alden Mbr.). The Alden Mbr. in this mapping unit rarely extends to depths greater than 12 to 15 meters; and overlies the Sheldon Creek Formation diamicton. At the DML margin, this landform may be mantled with a thin layer of Peoria Formation silt.  Low to moderate relief hummocky landform features exceed 3 to 5 meters of local relief. This landform is associated with the Bemis Moraine.  The surface pattern is irregularly shaped patterns.  Seasonal high water table.    Qtr_bamc - Till ridge (Dows Formation-Morgan Mbr.)  Generally 7 to 10 meters of yellowish to grayish brown, usually calcareous and fractured, stratified loam to silt loam; stratified sands and gravels to sandy loam diamicton; textures can be quite variable.  Overlies gray, calcareous, massive, dense loam diamicton (Dows Fm.-Alden Mbr.). The Alden Mbr. in this mapping unit can extend to depths in excess of 15 meters; and overlies the Sheldon Creek Formation diamicton. Low to high relief hummocky landfor m features exceed 3 to 10 meters of local relief. In places, esker and kame features and ice-walled lakes may be present. This landform is associated with the Bemis Altamont Moraine Complex.  The surface pattern is irregularly shaped and some rounded irregularly shaped patterns.  Seasonal high water table.   
 Qoch - Valley train outwash (Noah Creek Formation) Generally 8 to 15 meters of dark gray, dark grayish brown, dark brown to dark yellowish brown medium to coarse sand, gravelly sand to pebbly gravel.   Overlies gray, calcareous, massive, dense loam diamicton (Dows Fm.-Alden Mbr.).  In valley positions, it is at the land surface of older terraces.  On the modern floodplain it is buried by DeForest Fm. alluvium.  Low-relief landforms expressed as broad terraces; long, narrow longitudinal terraces or cuspate-shaped point terraces. Terraces associated with the major valleys are benched on a gray, calcareous, massive, dense loam diamicton (Dows Fm.-Alden Mbr.).  Qnw- In areas of the county, beyond the extent of the Des Moines Lobe landform this unit is benched on Wisconsin -age Sheldon Creek Fm diamicton.  This unit encompasses deposits that accumulated in stream valleys during the Wisconsin Episode.  No flooding potential.  Qglp(ls)- Lake plain  (Dows Formation-Lake Mills Mbr.)  Generally less than 10 m of dark grayish brown, massive, calcareous silty clay loam, or silt loam and fine sand (rhythmites common); often overlying a thin basal increment of sand and gravel (<1 m).  Overlies yellowish to grayish brown  usually calcareous, stratified loam to silt loam to sandy loam diamicton; textures can be quite variable (Sheldon Creek Fm. diamicton). This feature is recognized as Glacial Lake Spencer and has a significantly thicker sequence of lake sediments than other former glacial lakes found on or adjacent to the Des Moines Lobe (DML).  It is theorized this lake formed as advancing DML ice dammed the flow from the Ocheyedan River.  Low relief broad plain with less than 3 m of local relief.  Seasonal high water table.   Qglp(ss) - Lake Sediment small-scale landform features (Dows Formation-Lake Mills Mbr.)  Generally less than 3 meters of dark grayish brown, massive, calcareous silty clay loam, silt loam overlying a thin (<1 meter) basal increment of sand and gravel.   Unit overlies yellowish to grayish brown calcareous, stratified loam to silt loam to sandy loam diamicton; textures can be quite variable (Dows Fm.-Morgan Mbr.) or it may overlie a gray, calcareous, massive, dense loam diamicton (Dows Fm.-Alden Mbr.).  Small glacial lake beds associated with very low relief till plain with reticulate linked-depression systems. High water table.    Qsc2 -- Loamy Sediments Shallow to Glacial Till (Unnamed erosion surface sediment )  One to three meters of yellowish brown to gray, massive to weakly stratified, well to poorly sorted loamy, sandy and silty erosion surface sediment. Hatched pattern indicates areas high on the landscape that are mantled with less than one meter of Peoria Formation (silt or sand facies). Overlies massive, fractured, slightly firm glacial till of the Sheldon Creek Formation  Qsc -- Glacial Till (Sheldon Creek Formation-undiff.)  Generally 30 to 40 meters of a yellowish brown to gray, calcareous fractured to massive clay loam; at depth this unit can be variably textured and contain significant sand and gravel bodies.  It is not uncommon to see Pierre Shale clasts in core samples.  This unit overlies Pre-Illinois diamicton.  In Clay county, this unit outcrops along steep slopes adjacent to the Little Sioux River valley and steep slopes along other major tributaries flowing into the Little Sioux River off the Des Moines Lobe landform.  Qf - Fill  Areas of major land filling.  Fill associated with railroad grades, highway grades and land leveling.  Variable in texture ranging from loamy to sandy to concrete rubble.  Extent mapped as shown in county soil surveys.    Qpq - Pits and Quarries   Sand and gravel pits and rock quarries. Extent mapped as shown in county soil surveys.     Water Features      Drill Sites     
Surficial Geologic Materials of Clay County, Iowa
 SURFICIAL GEOLOGIC MATERIALS OF THE DES MOINES LOBE OF IOWA  Phase 7:  Clay County  Iowa Geological Survey Open File Map 05 -02, July 2005  Prepared by Deborah J. Quade 1, James D. Giglierano1, and E. Arthur Bettis III2  Iowa Geological Survey, Robert D. Lib ra, State Geologist Iowa Department of Natural Resources , Jeffrey R. Vonk, Director   Supported by the U.S. Geological Survey , Cooperative Agreement Number 04HQAG0067 National Cooperative Geologic Mapping Program (STATEMAP)   ACKNOLEDGEMENTS:   Recognized for contributions to map’s production:  Andrew B.Asell, Pete Kollasch, Heather Buresh, Katie, Foreman, Mary Pat Heitman, and Lois Bair.   Drilling was provided  under contract with Aquadrill of Iowa City, Iowa; a special thanks to Diane Edberg, Jay Joslyn an d drilling crew members who worked at times in challenging drilling conditions.  Assistance in describing solum cores was provided by the Nat ural Resources Conservation Service, Storm Lake Office soil scientists, Mark Minger and Julie McLaughlin.  A special thanks to the following individuals who graciously allowed access to their land for drilling,  Dick Beving, Merlin Beving, Allan Bredinger, David Dudycha, Robert Gould, Dean Hartmann, Bob McClain, Denny Nielsen, Don Nielsen, Dennis Peterson, Ron Petersen, Glen Recher, Merle Roberts, Ted Schutte, Walt Sievert, Shirley Swenson, Kent Theisen, Alvin VanWyck, Sievert Wasmund, Don Wilson and Don Zevenbergen.  We would like to thank the Iowa Department of Natural Resources for allowing access on public lands for drilling.    1Iowa Department of Natural Resources, Iowa Geological Survey  109 Trowbridge Hall, Iowa City, IA  52242 -1319  2 Department of Geoscience, The University of Iowa, 121 Trowbridge Hall, Iowa City, IA  52242   
LEGENDDescription of Map Units
!5
Location Diagram
Mapped Area
Des MoinesLobeRegion
Willow Creek
Littl
e Sioux
 River
Ocheyedan Ri
ver
Prai rie Cre
ek
Stony Creek
Elk Cre
ek
Big 
Mud
dy C
reek
Sp rin
g Cre
ek Pickerel Run Lost Island Outlet
Little Muddy Creek
Drainage D itch 60
Montgomery Creek
Lexin
gton
 Cre
ek
Drainage D itch 61
Sewer C reek
Little Meadow Creek
Hen
ry Cre
ek
North Bra
nch Li
zard C
reek
Little Sioux River
Spencer
Everly
Dickens
Webb
Fostoria
Royal
Peterson
Rossie Greenville
GillettGrove
T95N
T95N
T96N
T97N
T94N
T96N
T95N
T95N
T96N
T97N
T94N
T96N
R35WR37W R36WR37W R36WR38W
R38W R37W R36WR37W R36W R35W
0118
0171
0171
QR10
QR240
95°22'30"W
95°22'30"W
95°15'0"W
95°15'0"W
95°7'30"W
95°7'30"W
95°0'0"W
95°0'0"W
43°0'0"N 43°0'0"N
43°7'30"N 43°7'30"N
43°15'0"N 43°15'0"N
±
0 205 10 15 Miles
0 205 10 15 Kilometers
1:100,000


Surficial geologic materials of the Des Moines Lobe of Iowa, Phase 7: Clay County, Iowa

https://ir.uiowa.edu/cgi/viewcontent.cgi?article=1038&amp;context=igs_ofm

Surficial geologic materials of the Des Moines Lobe of Iowa, Phase 7: Clay County, Iowa

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