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Geology of South Dakota

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beyond the Missouri River, with an uncertain age, often thought to be the Wisconsin glaciation. The Brookings till plain is a belt of heavily weathered ground moraine, running through Brookings. Dating to the Illinoisan, it escaped burial by the Wisconsin ice sheet. A narrow strip in the central Prairie Hills holds the Toronto till plain, the oldest definitively Wisconsin drift, while the Bemis stage on the eastern edge of the hills formed a belt of moraines. Although the ice did not advance east of the Prairie Hills, it left a remaining moraine ridge, known as the Altamont stage, which encroaches the western side of the hills. Late in the Wisconsin, the ice sheet divided at the Prairie Hills, extending the Des Moines lobe to the east and a western lobe along the James River valley. A final advance of the glacier, known as the Big Stone stage, traced the Minnesota River lowland in the northeast.
1704: 19: 344:, the Black Hills eroded, shedding debris into the east, during a period with sub-tropical temperatures. Iron pyrite in shales oxidized, becoming bright red and yellow iron oxides. Sediments did not accumulate in the region until the end of the Eocene, as large streams carried material away to the ocean. Volcanic rocks from the Eocene preserve petrified trees. 389:, but the period came with a return to warm and wet conditions. Revitalized streams carried away large amounts of sediments, wiping out much of the White River Formation. Hundreds of feet of younger sediment cover the White River group in southwest South Dakota. Miocene sandstones, which often form cliffs, often overlay the White River Formation. 378:
jagged pinnacles of the Badlands. By the late 1990s, paleontologists had discovered 150 genera of mammals, ranging between rodents and rhinoceroses, as well as horses and camels. At the end of its five million year deposition, the formation was capped with the brilliantly white Rocky Ford ash, the windfall from powerful
356:, while some erosion occurred in the east. Gravel deposits containing crocodile bones and land snails, tortoises and hackberry seeds are also common in the fossil record. Bird bones and even fossil duck eggs have been found in association with clams, snails and the remains of algal mats in temporary ponds. 167:
formed during this period, exposed as a 400-foot thick unit in the walls of the Spearfish Canyon, ranging to 50 feet thick by Wind Cave. Cambrian rocks are only exposed in the Black Hills and disappear in boreholes drilled to the south of Wind Cave, beyond the ancient shoreline. However, the Deadwood
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ice ages, South Dakota experienced multiple sequences of glaciation. The oldest glacial drift deposits are in the southeast, at Sioux Falls and Newton Hills, overlain by deeply weathered Illinoisan, or potentially pre-Illinoisan age material. A large expanse of till fills the James River lowland and
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encompasses clay laid down by water, windblown sand, silt and volcanic ash, with a maximum thickness of up to 450 feet. Desert caliche soils are sometimes preserved as lime nodules and small clay buttes are often capped by well-cemented channel sands and gravels. The Brule Formation erodes into the
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until its closure in 2002, merged the Deadwood, Golden Terra, Father DeSmet and Caledonia gold mines around 1900. Its employees used emerging pneumatic drill technology and cyanide processing, creating the Ross Shaft and Yates Shaft—both 5000 feet deep—by 1941. Mine activity was suspended during
246:, depositing thick sequences of black Pierre shale—the thickest and most widespread sedimentary unit in the state. Originally, the shale ranged between 2500 feet thick at the Wyoming line and only tens of feet thick in the east, although erosion stripped it away in the Black Hills. The 456:
in the northwest, although it produces only one percent of the US total, primarily from traditional vertical wells. One hundred wells produce 1.6 million gallons of oil annually. Almost all production is centered in a 400 square mile area within Harding County, relying on the
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began to recede, 15 million years after the Pierre shale first started to form. Low permeability shale yielded a poorly drained landscape, cut streams and rivers, which brought in large amounts of sediment—clay, silt and sand up to 500 feet thick—which deposited as the
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brought a shift in the climate to arid conditions, transforming the region into a vast alluvial desert plain. Up to 600 feet of sands and clays, buried the Black Hills within 2000 feet of their crests in western South Dakota, forming the
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is the lower unit, covering over the oxidizing Eocene erosion surface and reaching up to 180 feet thick. The thickness of the formation varies widely, where it fills into pre-existing valleys or blankets hills. It contains light-green
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is up to 350 feet thick and in the northwest contains no obvious break in continental deposition at the time of the mass extinction, except for being sandier and less well-cemented. Further east, the formation contains the subsidiary
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fossils and other large mammals have been found in the formation. Due to the high concentration of clay and the ease with which it erodes, the Chadron Formation tends to form gentle sloping hills and buttes. The overlying
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The Deadwood Formation is beach sand and gravel at its base, but as the ancient shoreline moved eastward, thin layers of mudstone and limestone formed in the west, in deeper waters. The formation contains
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bones. Tepee buttes form as small, conical hills in the Pierre shale landscape, from lenses of more erosion resistant limestone. Beach sand coal sequences left behind as the up to 200 feet thick
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World War II and resumed. By the mine's centennial in 1976, it was 8000 feet deep and had produced 31 million ounces of gold, seven million ounces of silver and 115 million tons of milled ore.
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66 million years ago. Below the boundary clay, fossil pollen from large fields is common, but pollen is uncommon for a long period in the record afterward.
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in parallel with the rapid proliferation of multi-cellular life, terrestrial erosion continued in the region. The area was flooded during a large scale
326:, deposited during a brief resurgence of the inland sea and bearing fossil oysters, snails and clams. The 300 feet of sandstone and lignite of the 2051: 670: 434: 2071: 873: 758: 103:, active until 2002, was a major gold mine that reached up to 8000 feet underground and is now used for dark matter and neutrino research. 1614: 775: 1301: 790: 293:
Like many other locations around the world, South Dakota preserves the inch thick boundary clay, left by the asteroid impact of the
200:, widespread terrestrial erosion affected all but the north-central part of the state. Additional limestone deposits formed in the 330:
overlies the Ludlow Formation, getting thicker to the east and holding some of the major coal deposits found in northern Wyoming.
119:, over 2.5 billion years ago. The Archean crystalline basement rock formed with the intrusion of the Little Elk and Bear Mountain 2100: 2033: 1414: 1356: 770: 726: 421:, lead, zinc, uranium, lithium and sand, as well as oil, beginning in the 1870s. The Homestake Mining Company, which managed the 1809: 1619: 1524: 1474: 1321: 1604: 1584: 1549: 1429: 1384: 1379: 1206: 1041: 936: 795: 721: 716: 368:
clay, with a high shrink-swell capacity, as well as lenses of limestone containing snail, clam and algae remains from ponds.
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and storing marine and mammal fossils. Much of the state's landscape was reworked during several phases of glaciation in the
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West of the Missouri River, the Niobrara chalk formed in the inland sea during the Cretaceous, which contains
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The Black Hills were extensively explored and periodically mined for silver, gold, mica, tungsten, feldspar,
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In the northwest, the Ludlow, Cannonball and Tongue River formations are categorized as the
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Since the 1800s, geologists have debated how to subdivide the White River Formation. The
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Driscoll, Daniel G.; Carter, Janet M.; Williamson, Joyce E.; Putnam, Larry D. (1990).
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is also common, resulting from fragments of limestone broken up in waves The
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fossils and tracks left by worms, exposed at low tide. Intraformational
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and the Harney Peak granite emplaced around 1.71 billion years ago. The
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Formation reaches a thickness of 700 feet in wells in the northwest.
43:. Igneous crystalline basement rock continued to emplace through the 135:
was marked by a long period of erosion in the stratigraphic record.
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flooded the region, creating vast shale, chalk and coal beds in the
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were marked by more carbonate deposition, particularly within the
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deposition. Marine sandstones and clays and deposited during the
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Smaller volumes of light-colored sand and clay deposited in the
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began the uplift of the Rocky Mountains during the Cretaceous.
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A period of erosion occurred in South Dakota during the
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Following the retreat of the Cretaceous inland sea, the
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beds, along with dinosaur bones, most notably those of
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were uplifted, accompanied by igneous activity in the
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began to form more than 2.5 billion years ago in the
2070: 2032: 2018: 1757: 1355: 1285: 1040: 935: 872: 804: 702: 630:"Hydrology of the Black Hills Area, South Dakota" 433:site, although the shafts are now reused for the 452:South Dakota has oil and gas production in the 1734: 664: 429:After its closure, the location was deemed a 382:eruptions in the Western Cascades in Oregon. 111:The oldest rocks in South Dakota date to the 8: 107:Stratigraphy, tectonics and geologic history 192:, east to central South Dakota. During the 1741: 1727: 1719: 671: 657: 649: 204:. A marine environment prevailed in the 17: 470: 301:Cenozoic (66 million years ago-present) 230:formed throughout the west, during the 79:began to form the Rocky Mountains. The 2106:Geology of the United States by state 537: 525: 513: 501: 489: 477: 435:Sanford Underground Research Facility 139:Paleozoic (541–251 million years ago) 63:during terrestrial conditions in the 7: 644:. Mountain Press Publishing Company. 14: 1702: 642:Roadside geology of South Dakota 579:www.mininghistoryassociation.org 208:, as sandstones, carbonates and 223:Mesozoic (251–66 million years) 274:. The formation contains thin 1: 575:"South Dakota Mining History" 1750:Geology of the United States 1042:Smaller incorporated places 937:Larger incorporated places 83:were uplifted in the early 55:deposits formed during the 2122: 215:Sea levels receded in the 1698: 847:Colleges and universities 690: 640:Gries, John Paul (1996). 2052:Northern Mariana Islands 409:Natural resource geology 2101:Geology of South Dakota 1709:South Dakota portal 445:research. Southwest of 267:Western Interior Seaway 69:Western Interior Seaway 328:Tongue River Formation 234:, at the start of the 147:, at the start of the 25: 23:Badlands National Park 1752:by political division 902:Dissected Till Plains 727:Famous South Dakotans 354:White River Formation 21: 562:Driscoll et al. 1990 550:Driscoll et al. 1990 324:Cannonball Formation 313:at the start of the 295:K-Pg mass extinction 272:Hell Creek Formation 153:marine transgression 2062:U.S. Virgin Islands 1302:Colonial Pine Hills 892:Coteau des Prairies 781:Tourist attractions 459:Red River Formation 263:Fox Hills Formation 202:Early Mississippian 1044:pop. 1,000 - 5,000 786:Towns and villages 516:, p. 191–197. 492:, p. 205–210. 447:Lead, South Dakota 165:Deadwood Formation 26: 2088: 2087: 1716: 1715: 1322:North Eagle Butte 361:Chadron Formation 2113: 2072:Outlying islands 2026:Washington, D.C. 2020:Federal district 1743: 1736: 1729: 1720: 1707: 1706: 1705: 1207:North Sioux City 673: 666: 659: 650: 645: 636: 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Retrieved 578: 569: 564:, p. 2. 557: 545: 533: 528:, p. 3. 521: 509: 497: 485: 473: 451: 428: 412: 391: 384: 358: 346: 339: 332: 304: 292: 285: 279: 252: 226: 214: 178:conglomerate 170: 159:through the 142: 110: 32:South Dakota 29: 27: 15: 2034:Territories 1880:Mississippi 1795:Connecticut 1415:Charles Mix 1247:Springfield 1167:Hot Springs 1132:Fort Pierre 1117:Eagle Butte 1112:Dell Rapids 1077:Chamberlain 1002:Sioux Falls 887:Black Hills 859:LGBT rights 771:State Parks 742:Delegations 439:dark matter 402:Pleistocene 307:Black Hills 281:Triceratops 212:deposited. 129:Proterozoic 117:Precambrian 115:eon of the 93:Pleistocene 81:Black Hills 45:Proterozoic 41:Precambrian 39:eon of the 30:geology of 2095:Categories 1995:Washington 1915:New Mexico 1910:New Jersey 1785:California 1620:Pennington 1525:Hutchinson 1475:Fall River 1337:Pine Ridge 1147:Gettysburg 1087:Clear Lake 1022:Vermillion 997:Rapid City 972:Harrisburg 927:West River 917:Pine Ridge 912:East River 737:Government 538:Gries 1996 526:Gries 1996 514:Gries 1996 502:Gries 1996 490:Gries 1996 478:Gries 1996 465:References 400:. In the 265:after the 259:plesiosaur 244:Cretaceous 210:evaporites 161:Ordovician 73:Cretaceous 2005:Wisconsin 1970:Tennessee 1875:Minnesota 1850:Louisiana 1605:Minnehaha 1585:McPherson 1550:Kingsbury 1430:Codington 1385:Brookings 1380:Bon Homme 1297:Blackhawk 1252:Summerset 1142:Garretson 1127:Flandreau 1122:Elk Point 1062:Beresford 1027:Watertown 1007:Spearfish 967:Brookings 957:Box Elder 922:Siouxland 842:Education 791:Townships 747:Elections 732:Geography 697:(capital) 604:sdoil.org 431:Superfund 415:bentonite 366:bentonite 349:Oligocene 311:Paleocene 174:trilobite 149:Paleozoic 57:Paleozoic 49:limestone 1990:Virginia 1940:Oklahoma 1920:New York 1895:Nebraska 1885:Missouri 1870:Michigan 1860:Maryland 1845:Kentucky 1825:Illinois 1800:Delaware 1790:Colorado 1780:Arkansas 1680:Walworth 1595:Mellette 1575:Marshall 1560:Lawrence 1410:Campbell 1357:Counties 1242:Sisseton 1232:Redfield 1222:Piedmont 1217:Parkston 1202:Mobridge 1162:Hartford 1107:Deadwood 987:Mitchell 947:Aberdeen 882:Badlands 864:Politics 854:Gun laws 817:Cannabis 812:Abortion 764:Timeline 443:neutrino 394:Pliocene 380:rhyolite 315:Cenozoic 255:mosasaur 240:Jurassic 236:Mesozoic 232:Triassic 228:Red beds 186:Devonian 182:Silurian 145:Cambrian 121:granites 89:Badlands 85:Cenozoic 65:Triassic 61:red beds 2010:Wyoming 1985:Vermont 1890:Montana 1830:Indiana 1810:Georgia 1805:Florida 1775:Arizona 1765:Alabama 1690:Ziebach 1685:Yankton 1650:Stanley 1640:Sanborn 1635:Roberts 1625:Perkins 1565:Lincoln 1540:Jerauld 1535:Jackson 1515:Harding 1490:Gregory 1470:Edmunds 1465:Douglas 1445:Davison 1400:Buffalo 1375:Bennett 1347:Rosebud 1272:Webster 1257:Tyndall 1197:Mission 1187:Milbank 1152:Gregory 1137:Freeman 1102:De Smet 1067:Britton 1032:Yankton 1012:Sturgis 982:Madison 962:Brandon 874:Regions 837:Economy 822:Culture 805:Society 776:Symbols 754:History 712:Outline 635:. USGS. 387:Miocene 276:lignite 217:Permian 155:in the 143:In the 113:Archean 75:as the 37:Archean 1945:Oregon 1900:Nevada 1840:Kansas 1815:Hawaii 1770:Alaska 1758:States 1670:Turner 1630:Potter 1580:McCook 1520:Hughes 1510:Hanson 1500:Hamlin 1495:Haakon 1440:Custer 1435:Corson 1370:Beadle 1365:Aurora 1332:Oglala 1277:Winner 1267:Wagner 1227:Platte 1212:Parker 1192:Miller 1182:Lennox 1177:Lemmon 1157:Groton 1097:Custer 1092:Crooks 1072:Canton 1057:Baltic 1052:Aurora 992:Pierre 717:Cities 704:Topics 694:Pierre 609:7 July 584:7 July 342:Eocene 99:. The 67:. The 1975:Texas 1855:Maine 1820:Idaho 1675:Union 1665:Tripp 1655:Sully 1645:Spink 1610:Moody 1600:Miner 1590:Meade 1570:Lyman 1545:Jones 1485:Grant 1480:Faulk 1460:Dewey 1455:Deuel 1420:Clark 1405:Butte 1395:Brule 1390:Brown 1262:Volga 1237:Salem 1082:Clark 977:Huron 827:Crime 680:State 633:(PDF) 419:beryl 125:shale 53:shale 2047:Guam 1980:Utah 1935:Ohio 1835:Iowa 1660:Todd 1555:Lake 1530:Hyde 1505:Hand 1425:Clay 1172:Lead 611:2018 586:2018 441:and 347:The 284:and 257:and 184:and 51:and 28:The 1450:Day 1017:Tea 682:of 2097:: 602:. 577:. 461:. 417:, 290:. 1742:e 1735:t 1728:v 672:e 665:t 658:v 613:. 588:. 552:. 480:.

Index


Badlands National Park
South Dakota
Archean
Precambrian
Proterozoic
limestone
shale
Paleozoic
red beds
Triassic
Western Interior Seaway
Cretaceous
Laramide orogeny
Black Hills
Cenozoic
Badlands
Pleistocene
Williston Basin
Homestake Mine
Archean
Precambrian
granites
shale
Proterozoic
Neoproterozoic
Cambrian
Paleozoic
marine transgression
Late Cambrian

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