Geology of Kansas

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The Geology of Kansas encompasses the geologic history of the US state of Kansas and the present-day rock and soil that is exposed there. Rock that crops out in Kansas was formed during the Phanerozoic eon, which consists of three geologic eras: the Paleozoic, Mesozoic and Cenozoic. Paleozoic rocks at the surface in Kansas are primarily from the Mississippian, Pennsylvanian and Permian periods.

Paleozoic Era[edit]

The oldest rocks at the surface in Kansas are Mississippian rocks that consist of limestones, shale, dolomite, chert, sandstones and siltstones. The Mississippian consisted of an environment similar to what we see today. Fast moving streams and rivers cutting into the limestone bedrock and in places creating caverns and sinkholes.[2] Pennsylvanian rocks consist predominantly of alternating marine and non-marine shales and limestones with some sandstone, coal, chert and conglomerate. The Pennsylvanian was a time that the region that is now eastern Kansas stayed nearly at sea level. Between the transgression and regression of the seas, swamps and bogs formed, depositing dead vegetation and later, after burial under younger sediments, this dead vegetation formed into coal.[2] Permian rocks predominantly consist of limestones, shales and evaporites. The Permian in Kansas began as an environment consisting of warm, shallow seas. As the Permian progressed, the climate became very dry and the seas began to subside, creating bodies of water shut off from the open seas, in turn creating areas for the generation of dark shales and evaporite minerals such as halite and gypsum as the waters evaporated.[2] The end of the Permian marks the largest extinction period in Earth's history; over 90% of all life disappeared.

Mesozoic Era[edit]

Mesozoic rocks at the surface in Kansas consist predominantly of rocks from the Cretaceous. A relatively small outcrop of Jurassic sediments are exposed in the southwest corner of the state. Cretaceous age rocks consist of limestone, chalk, shale and sandstone. The Cretaceous in Kansas was an open ocean or sea environment dominated by microscopic marine plants and animals that floated or swam near the surface of this ancient water body.[2] As these microscopic creatures died they sank to the bottom, formed a soft, limy ooze and would preserve any larger creatures that would die and sink into it.

Cenozoic Era[edit]

Cenozoic rocks at the surface were formed during the Paleogene, Neogene and Quaternary periods. Paleogene to Neogene rocks in Kansas consist of river silt, sand, freshwater limestones and some volcanic ash derived from eruptions in the western United States. Near the beginning of the Paleogene, the Rocky Mountains were born, as were the streams and rivers heading eastward out from the mountains into Kansas. Over 60 million years of erosion, the Rocky Mountains created a wedge of material extending to the Flint Hills of eastern Kansas.[2] Quaternary rocks in Kansas consist of glacial drift; river silt, sand and gravel; dune sand and wind blown silt. The Quaternary Period in western Kansas was very similar to the Neogene, continual erosion of the Rocky Mountains deposited additional sediments.[2]

Physiographic regions[edit]

Map showing physiographic regions of Kansas [3]

Kansas has been divided into eleven different physiographic regions.[4]

Ozark plateau[edit]

Main article: Ozarks

Mississippean limestones and cherts of the Ozark Plateau are exposed in extreme southeastern Kansas in Cherokee County.[5] This area was part of the Tri-state district of the nineteenth and twentieth centuries. Galena was a center of lead and zinc mining in the area.[6]

Cherokee lowlands[edit]

The Cherokee lowlands is a region of southeast Kansas immediately north and west of the Ozark plateau in Cherokee, Labette, Crawford and Bourbon Counties. The lowlands are developed on areas of gently rolling hils developed on the shale and sandstone of the Cherokee Group of Pennsylvanian age. The Cherokee Group is noted for rich deposits of coal in Kansas and across the midwestern United States.[7]

Osage Cuestas[edit]

The Osage cuesta region underlies twenty counties in southeastern Kansas. The cuestas are a region of east to southeast facing escarpments (50 to 200 feet high) formed on resistant limestone units which dip gently to the west and northwest. Areas between escarpments are underlain by shales. The cuesta region contains coal, black shale and some oil shales. Lamproite sills occur within the cuesta units of Woodson and Wilson counties. These unusual igneous rocks were intruded in the Cretaceous Period.[8][9]

Chautauqua Hills[edit]

The Chautauqua Hills represent a narrow region in southeast Kansas of sandstone capped ridges and rolling hills. The Pennsylvanian age sandstones were depositied in a large river valley. The sandstones are the Tonganoxie Sandstone Member of the Stranger Formation and Ireland Sandstone Member of the Lawrence Formation. The hills occur in the western portions of Montgomery, Wilson and Woodson counties and the eastern edges of Chautauqua, Elk and Greenwood counties. The sandstones continue into northern Oklahoma.[10]

Flint Hills[edit]

Main article: Flint Hills

The Flint Hills developed on the north-south exposure of Permian cherty limestones. The region extends from Marshall County in the north, to Cowley County and on into northern Oklahoma where they are known as the Osage Hills. The Permian limestones contain abundant weathering resistant chert (or flint) and the residuum and soils of the hilltops and the streambeds of the region contain abundant cherty gravels. Surface exposures of the rare igneous kimberlites occur in Riley and Marshall counties. The kimberlite diatremes are of Cretaceous age. No diamonds have been found in the Kansas kimberlite occurrences. Garnet crystals from the kimberlites have been reported in local stream gravels.[11][12][13]

Red Hills[edit]

Main article: Red Hills (Kansas)

The Red Hills cover a section of southern Kansas in Clark, Comanche, and Barber counties along the Oklahoma border. The Red Hills are named for their color derived from the Permian red beds which outcrop and underlie the region. The red color is produced by abundant iron oxides in the weathering sediments. The region is underlain by red shales, siltstones, and sandstones along with interbedded dolomites and gypsum evaporite layers. Massive gypsum deposits are mined near Sun City in northwestern Barber County. The Gyp Hills near Medicine Lodge were named for the gypsum of the Blaine Formation. The soluble gypsum, anhydrite and dolomite produce many caves in the area.[14][15] The Big Basin of Clark County is a 2 km diameter, 35 m deep, dissolution collapse feature that formed by the dissolution of salt beds in the subsurface.

Smoky Hills[edit]

Main article: Smoky Hills

The Smoky Hills constitute a large area of north central Kansas. The area is underlain by Cretaceous sediments. Rocks outcroping in the area include the sandstones of the Dakota Formation, the Greenhorn Limestone, and the thick Niobrara Chalk. Stratigraphically the Dakota is overlain by the Greenhorn and that by the Niobrara. The Dakota outcrops in the eastern portion of the region as gently westward dipping resistant ridges. Although the sandstones are the most resistant and therefor most prominent the Dakota includes shales and clays. The formation contains abundant brown iron oxides and many concretions are found in the area. In the western portions of the ares the bedrock is fossiliferous chalk of the Niobrara Formation which includes the Smoky Hill Chalk member noted for abundant fish and marine reptile fossils.[16][17]

High Plains[edit]

The western third of Kansas is in the High Plains area. The highest point in Kansas, Mount Sunflower (4,039 feet (1,231 m)), is located in the High Plains physiographic region. The uplift of the Rocky Mountains during the Cenozoic resulted in erosion and deposition of vast quantities of non-marine sediments eastward across the High Plains. The Ogallala Formation consists of a large wedge of unconsolidated sands and silts that is a significant aquifer under the plains. The Ogallala contains a sandstone layer cemented with opal. In the southwest corner of the state in Morton County rocks of Jurassic age outcrop along the Cimarron River. Loess deposits cover much of the High Plains in north and northwest Kansas.[18][19]

Glaciated Region[edit]

The northeast corner of the state, north of the Kansas River and east of the Big Blue River,is covered by glacial debris deposited during the Pre-Illinoian glaciations which occurred 600,000 years ago in the Pleistocene. The Pennsylvanian and Permian bedrock is buried under thick deposits of glacial debris, largely loess. A variety of glacial erratics were left by the melting glaciers. Many of these are of Sioux Quartzite carried south from the Sioux Falls, South Dakota area.[20]

Wellington-McPherson Lowlands[edit]

The Wellington-McPherson Lowlands of south central Kansas in Sumner, Sedgwick, Harvey and McPherson counties is underlain by fluvial sediments deposited in the ancestral Arkansas River valley during the Pleistocene Epoch one to two million years ago. The sediments consist largely of sands, silts and gravels. These include the "Equus beds" aquifer sediments, named for Pleistocene fossils it contains. Also under this area is the Permian Hutchinson salt bed which reaches a thickness of 400 feet. The area also contains inactive sand dunes.[21]

Arkansas River Lowlands[edit]

The Arkansas River Lowlands follows the course of the Arkansas River through southwest and south-central Kansas. The broad floodplain contains large quantities of sand and silt carried from the Rocky Mountains by the river. A significant area of sand dunes occur on the south side of the plain formed by the prevailing winds from the glaciers to the north during the Pleistocene.[21]

Subsurface geology[edit]

Subsurface structures of Kansas

The subsurface geology of Kansas consists of several sequences of sedimentary strata deposited on the Pre-Cambrian basement of the North American Craton.

Humboldt Fault (red) and Midcontinent Rift (green) in Kansas and Nebraska

Several regional subsurface structures including five sedimentary basins exist under Kansas. These structures are important in controlling the vast deposits of petroleum and natural gas in the state. The Central Kansas Uplift is a broad arch in the rocks of west central Kansas. The rock units within this arch have been major oil producers. The Anadarko Basin of southwest Kansas contains significant natural gas. The Sedgwick Basin, the Cherokee Basin and the Forest City Basin of south and east Kansas also produce petroleum and natural gas.[22]

Proterozoic basement[edit]

The Nemaha uplift is a deep fault zone which runs diagonally across east Kansas and extends from just south of Omaha, Nebraska to Oklahoma City. This fault zone directly overlies a granite "high" in the Precambrian basement and is structurally active as the Humboldt Fault. Some fifty miles to the west the southernmost extension of the Proterozoic Midcontinent Rift System extends into northeastern Kansas.[23]

The northern two-thirds of Kansas is underlain by a Proterozoic sequence known as the Central Plains Orogen. The igneous and metamorphic rocks of this orogenic zone are considered to be an extension of the 1.7 Ga fold belt exposed in Colorado and Wyoming.[24] The southern approximately one-third of the state is underlain by the Southern granite-rhyolite province dating to 1.35 to 1.48 Ga.[24][25]

References[edit]

  1. ^ Darton, Nelson Horatio. 1916. Guidebook of the Western United States: Part C - The Santa Fe Route, With a Side Trip to Grand Canyon of the Colorado. U.S. Geological Survey. Bulletin 613, 194 pp. (See Plate 3-A)
  2. ^ a b c d e f Buchanan, R., Kansas Geology: An Introduction to Landscapes, Rock, Minerals, and Fossils, University Press of Kansas, 1984, Ch 1, p. 10 ff ISBN 978-0700602407
  3. ^ Adams, George Irving. 1903. The physiographic divisions of Kansas. Transactions of the Kansas Academy of Science 18:109-123.
  4. ^ GeoKansas from the Kansas Geological Survey (KGS)
  5. ^ http://www.kgs.ku.edu/Extension/ozark/ozark.html Ozark Plateau, KGS
  6. ^ http://www.kgs.ku.edu/Extension/ozark/mining.html Lead and Zinc Mining, KGS
  7. ^ http://www.kgs.ku.edu/Extension/cherokee/cherokee.html Cherokee Lowlands KGS
  8. ^ http://www.kgs.ku.edu/Extension/cuestas/cuestas.html Osage Cuestas—Introduction, KGS
  9. ^ http://www.kgs.ku.edu/Extension/cuestas/rocks.html Osage Cuestas—Rocks and Minerals, KGS
  10. ^ http://www.kgs.ku.edu/Extension/chautauqua/rocks.html Chautauqua Hills—Rocks and Minerals KGS
  11. ^ http://www.kgs.ku.edu/Extension/flinthills/flinthills.html Flint Hills KGS
  12. ^ http://www.kgs.ku.edu/Extension/flinthills/rocks.html Flint Hills—Rocks and Minerals KGS
  13. ^ http://www.kgs.ku.edu/General/News/99_releases/kimberlites.html Rex Buchanan, Survey Discovers Three New Volcanic Features in Northeast Kansas, Kansas Geological Survey, Oct. 29, 1999
  14. ^ http://www.kgs.ku.edu/Extension/redhills/redhills.html Red Hills KGS
  15. ^ http://www.kgs.ku.edu/Extension/redhills/rocks.html Red Hills—Rocks and Minerals KGS
  16. ^ http://www.kgs.ku.edu/Extension/smoky/smoky.html Smoky Hills KGS
  17. ^ http://www.kgs.ku.edu/Extension/smoky/rocks.html Smoky Hills—Rocks and Minerals KGS
  18. ^ http://www.kgs.ku.edu/Extension/highplains/highplains.html High Plains KGS
  19. ^ http://www.kgs.ku.edu/Extension/highplains/rocks.html High Plains—Rocks and Minerals
  20. ^ http://www.kgs.ku.edu/Extension/glacier/glacier.html Glaciated Region KGS
  21. ^ a b http://www.kgs.ku.edu/Extension/lowlands/lowlands.html Arkansas River Lowlands and Wellington-McPherson Lowlands
  22. ^ http://www.kgs.ku.edu/Publications/Oil/primer09.html Petroleum geology of Kansas KGS
  23. ^ http://www.kgs.ku.edu/Publications/pic3/pic3_4.html Earthquakes in Kansas KGS
  24. ^ a b P. K. Sims and Z. E. Petermar, Early Proterozoic Central Plains orogen: A major buried structure in the north-central United States, Geology 1986;14;488-491
  25. ^ Ben A. Van der Pluijm, Paul A. Catacosinos, Basement and basins of eastern North America, Geological Society of America, Special Paper 308, 1996, p. 14 ISBN 978-0-8137-2308-2

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