Figure 1. Status of county-wide investigations in South Dakota.
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1 Harding Corson Campbell McPherson Marshall Roberts Perkins Walworth Edmunds Brown Day Dewey Grant Potter Faulk Butte Codington Ziebach Sully Spink Clark Hamlin Deuel Meade Hyde Hand Lawrence Haakon Stanley Hughes Beadle Kingsbury Brookings Pennington Jones Lyman Buffalo Jerauld Sanborn Miner Lake Moody Custer Jackson Brule Aurora Davison Hanson McCook Minnehaha Mellette Fall River Shannon Bennett Todd Tripp Gregory Charles Mix Douglas Hutchinson Turner LICOL Bon Homme Yankton Clay UIO This report Investigation in progress Report completed Figure. Status of county-wide investigations in South Dakota Miles Kilometers
2 04 o 9 o 45 o 43 o Miles Kilometers Lincoln and Union Counties (study area) Base map modified from Rothrock, 3, and Flint, 5 divisions and location of the study area.
3 R. 5 W. R. W. R. 49 W. MIEHAHA CO., SD 2 2 Sioux Falls 2 Tea Harrisburg Lennox Worthing TURER CO., SD TURER CO., SD 8 Canton Fairview Hudson 4 UIO CO., SD R. 5 W. R. W. R. 49 W. R. W. R. 4 W MILES KILOMETERS PRECAMBRIA SIOUX QUARTZITE IGEOUS AD METAMORPHIC ROCKS, UDIFFERETIATED Data point; number is elevation of Precambrian surface in feet above mean sea level. A less than symbol (<) indicates elevation is less than the number shown. A question mark (?) indicates elevation is uncertain. Data point where two test holes were drilled; numbers are elevation of Precambrian surface in feet above mean sea level. Contour on Precambrian surface. umber is elevation above mean sea level. Dashed where approximate. Contour interval = feet. Approximate boundary of geologic formations. Figure 3. Precambrian geologic map of Lincoln County, South Dakota.
4 LICOL CO., SD R. W. R. 49 W. R. W Alcester PLYMOUTH CO., IA MILES KILOMETERS 9 9 Elk Point R. 5 E. R. E. PRECAMBRIA SIOUX QUARTZITE IGEOUS AD METAMORPHIC ROCKS, UDIFFERETIATED Data point; number is elevation of Precambrian surface in feet above mean sea level. A less than symbol (<) indicates elevation is less than the number shown Contour on Precambrian surface. umber is elevation above mean sea level. Dashed where approximate. Contour interval = feet. Approximate boundary of geologic formations. WOODBURY CO., IA PLYMOUTH CO., IA DIXO CO., E 05 orth Sioux City Figure 4. Precambrian geologic map of Union County, South Dakota. DAKOTA CO., E R. E. R. E. R. 8 E.
5 GREELAD ALASKA CAADA CAADA UITED SD STATES MEXICO Miles Land surface above sea level Kilometers (modified from Gill and Cobban, ) Figure 5. Map showing probable extent of the Western Interior Seaway during a portion of the late Cretaceous Period.
6 R. 5 W. R. W. R. 49 W. MIEHAHA CO., SD 2 2 Sioux Falls 2 4 TURER CO., SD TURER CO., SD Tea Harrisburg 2 0(?) 04 9(?) < Lennox (?) Worthing < <03 Canton < <080 8 Fairview <3 < < <02 Hudson 4 < UIO CO., SD R. 5 W. R. W. R. 49 W. R. W. R. 4 W MILES KILOMETERS DAKOTA FORMATIO DAKOTA FORMATIO ABSET <02 Data point; number is elevation of the Dakota Formation top in feet above mean sea level. A less than symbol (<) indicates elevation is less than the number shown. A question mark (?) indicates elevation is uncertain. Contour of elevation of the Dakota Formation top. umber is elevation above mean sea level. Dashed where approximate. Contour interval = feet. Boundary of the Dakota Formation. Dashed where approximately located. Figure. Contour map of the top of the Dakota Formation in Lincoln County, South Dakota.
7 R. W. R. 49 W. R. W. 4 4 LICOL CO., SD 4 < Alcester <3 <2 < <32 <3 < < <08 <2 0 <8 <084 <08 <0 <09 04 < < <0 < <085 PLYMOUTH CO., IA 4 4 < <0 05 <00 < MILES KILOMETERS 0(?) < <025 <05 90 <043 <08 <0 <08 <088 <00 <028 < < <0 <053 <05 <02 DAKOTA FORMATIO Data point; number is elevation of the Dakota Formation top in feet above mean sea level. A less than symbol (<) indicates elevation is less than the number shown. A question mark (?) indicates elevation is uncertain. Contour of elevation of the Dakota Formation top. umber is elevation above mean sea level. Dashed where approximate. Contour interval = feet. Figure. Contour map of the top of the Dakota Formation in Union County, South Dakota. 020 R. 5 E. R. E. <0 DIXO CO., E DAKOTA CO., E Elk Point 2 < 9 <04 <5 R. E. <08 <02 <8 0 R. E. <9 < <082 2 Jefferson 2 < < 3 <00 <9 8 0(?) <02 9 <9 <3 9 R. 8 E. 9 9 (?) 05 0 orth Sioux City 0 0 < 8 9 < 0 < WOODBURY CO., IA PLYMOUTH CO., IA
8 TURER CO., SD TURER CO., SD > > >4 35 >2 243 >9 8 >8 Lennox 2 >4 >5 >3 03 >05 > > > > 4 >5 R. 5 W. R. W. R. 49 W. 8 > > > > (?) (?) > Tea 39 82? 4 20 >259 > 3 >35 4 > > (?) >55 2 > (?) 235 >53 0 2(?) 9 203(?) > Worthing > >0 5 > UIO CO., SD Sioux Falls > (?) Harrisburg 4 42 > >43 > >49 > >40 4 >0 >83 >200 >55 2 2(?) 9 59 >0 5 >5 >45 5 > > > >4 >200 5(?) > >0 > (?) > 9 35 > >85 0 > > MIEHAHA CO., SD Canton > 2 > > >9 5 > > > > R. 5 W. R. W. R. 49 W. R. W. R. 4 W > 85 (?) > >82 >08 80 > 0 32 >23 >24 05 > > > > (?) >53 83 > > > >52 >84 > 5 > 55 >39 32 > > >90 > > > 42 Fairview (?) Hudson (?) >54 > MILES KILOMETERS > Data point; number is thickness of Quaternary sediments in feet. A greater than symbol (>) indicates thickness is greater than the number shown. A greater than or equal to symbol (>) indicates thickness is greater than or equal to the number shown. A question mark (?) indicates thickness is uncertain. Data point where two test holes were drilled; numbers are thickness of Quaternary sediments. Contour of thickness of Quaternary sediments. Dashed where approximate. Contour interval = feet. Figure 8. Thickness of Quaternary sediments in Lincoln County, South Dakota.
9 > >90 > >240 2 > >2 232 R. W. R. 49 W. R. W > > >8 34 9(?) >22 22 >38 >3 8 4 > > > >53 > > Alcester > >45 > >200 > > >3 > > > > >0 >0 53 > >38 2 >0 4 >25 >40 8 LICOL CO., SD > 43 > > >55 58 > 32 > 4 >4 >0 >20 >34 >38 > 9 >2 > > >25 >4 PLYMOUTH CO., IA MILES KILOMETERS >09 >9 > 254 >85 > >0 >90 >40 >9 > >05 > > > 54 >0 Elk Point 8 > >08 9 R. 5 E. R. E. >20 > >9 >90 > >9 >40 >55 4 Data point; number is thickness of Quaternary sediments in feet. A greater than symbol (>) indicates thickness is greater than the number shown. A greater than or equal to symbol (>) indicates thickness is greater than or equal to the number shown. A question mark (?) indicates thickness is uncertain. Data point where two test holes were drilled; numbers are thickness of Quaternary sediments. Contour of thickness of Quaternary sediments. Dashed where approximate. Contour interval = feet. Figure 9. Thickness of Quaternary sediments in Union County, South Dakota. >02 >0 8 DIXO CO., E DAKOTA CO., E >0 >0 R. E. > >0 43 > 59 > > 03 >8 83 R. E. >25 9 >90 55 Jefferson > > > 5 >8 >34 >0 0 R. 8 E. >0 > > > >45 orth Sioux City >20 >35 > WOODBURY CO., IA PLYMOUTH CO., IA 90
10 R. 5 W. R. W. R. 49 W. MIEHAHA CO., SD 2 2 Sioux Falls 2 Tea Harrisburg 8 9 Lennox Channel A Channel B 24 Worthing 4 TURER CO., SD TURER CO.,SD 8 Canton Fairview UIO CO., SD 9 Channel D 24 R. 5 W. R. W. R. 49 W. R. W. R. 4 W. 4 Channel C 4 03 Hudson 9 9 Data point; number is thickness of preglacial(?) quartz sand MILES KILOMETERS Approximate location of channel boundaries. Approximate extent of ewton Hills sand. Arrow showing direction of drainage. Figure 0. Location of preglacial bedrock channels and preglacial(?) quartz sand in Lincoln County, South Dakota.
11 R. W. R. 49 W. R. W LICOL CO., SD Channel C 4 >45 Channel D 2 0 Channel C Alcester (?) 5(?) PLYMOUTH CO., IA MILES KILOMETERS 9 >85 9 Elk Point R. 5 E. R. E. >85 Data point; number is thickness of preglacial(?) quartz sand. A greater than symbol (>) indicates thickness is greater than the number shown. A question mark (?) indicates thickness is uncertain. Approximate location of channel boundaries. Arrow showing direction of drainage. Jefferson WOODBURY CO., IA PLYMOUTH CO., IA Figure. Location of preglacial bedrock channels and preglacial(?) quartz sand in Union County, South Dakota. DIXO CO., E DAKOTA CO., E 05 orth Sioux City R. E. R. E. R. 8 E.
12 04 o 9 o 45 o 43 o Miles Kilometers Lincoln and Union Counties (study area). Approximate extent of late Wisconsin ice. Arrows indicate flow direction. Base map modified from Rothrock, 3, and Flint, 5. Figure 2. Generalized relationship of James lobe and Des Moines lobe ice to eastern South Dakota.
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