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Mississippi embayment

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530: 542: 33: 518: 1690: 329: 107: 483:. The uplifted land quickly eroded and, as North America moved away from the hot spot and as the hotspot's activity declined, the crust beneath the embayment region cooled, contracted and subsided to a depth of 2.6 km, forming a 76:
by the filling with sediment of a pre-existing basin. An explanation for the embayment's formation was put forward by Van Arsdale and Cox in 2007: movement of the Earth's crust brought this region over a volcanic
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Imlay, R.W., 1949. Lower Cretaceous and Jurassic formations of southern Arkansas and the oil and gas possibilities. Arkansas Resource and Development Commission, Division of Geology, Information Circular 12,
1159: 529: 1119: 517: 258:. The current sedimentary basin results from the filling of a Cretaceous tectonic basin and existed as a large bay in the Cretaceous through early Cenozoic shoreline. 869: 1707: 843: 1761: 1182: 541: 1114: 853: 917: 794: 1187: 1086: 491:. As sea levels dropped, the Mississippi and other rivers extended their courses into the embayment, which gradually became filled with sediment. 1104: 346: 128: 1109: 1023: 912: 789: 678: 266: 479:
from the hotspot forced the further uplift to a height of perhaps 2–3 km of part of the Appalachian-Ouachita range, forming an
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The Mississippi embayment represents a break in what was once a single, continuous mountain range comprising the modern
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Evidence for this explanation is found in the presence of the seismic zones centered on New Madrid, Missouri, and
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which formed the Appalachian-Ouachita range. Subsequent erosion caused a deep trough that was flooded by the
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range, which runs roughly on a north–south axis along the Atlantic coast of the United States, and the
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As Pangaea began to break up about 200 million years ago, North America passed over a volcanic "
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Significant shorelines along the U.S. Gulf and Atlantic Coasts since the Cretaceous Period
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The Mississippi embayment stretches from central Louisiana into southern Missouri.
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Jason Morgan, W. (1983). "Hotspot tracks and the early rifting of the Atlantic".
328: 282: 239: 106: 53: 687: 499: 231:. The northern end of the embayment appears as an anomalous break in regional 224: 216: 69: 61: 1722: 1709: 691: 480: 304: 278: 247: 236: 212: 503: 308: 255: 251: 243: 228: 73: 576: â€“ Geological formation in the U.S. states of Arkansas and Missouri 265:
lies at the northern end of the embayment. It was the site of the large
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no doubt affected and may have partially re-activated the old rift.
476: 437:. The ancestral Appalachian-Ouachita range was thrust up when the 86: 31: 269:
of 1811-12. The area is underlain by some anomalous geology. The
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and eventually filled with sediment from the Mississippi River.
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Low-lying basin filled with Cretaceous to recent sediments
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range, which runs on a rough east–west axis west of the
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Van Arsdale, Roy B.; Cox, Randel T. (January 2007).
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Pages displaying wikidata descriptions as a fallback
52:. It is essentially a northward continuation of the 1196: 1168: 1148: 1085: 1022: 956: 928: 862: 710: 68:. The current sedimentary area was formed in the 535:Mississippi Embayment Top Cretaceous Contour Map 44:is a physiographic feature in the south-central 672: 8: 453:when all three became joined in the ancient 445:came into contact with the plates carrying 135:. Unsourced material may be challenged and 679: 665: 657: 413:Learn how and when to remove this message 199:Learn how and when to remove this message 592: 513: 7: 547:Mississippi Embayment Structural Map 351:adding citations to reliable sources 133:adding citations to reliable sources 602:"The Mississippi's Curious Origins" 506:, which are products of volcanism. 1762:River valleys of the United States 561: â€“ Natural region of Arkansas 25: 295:. The more recent opening of the 273:is an ancient failed continental 1688: 540: 528: 516: 327: 105: 338:needs additional citations for 1: 1004:Ridge-and-Valley Appalachians 460:about 300 million years ago. 1160:Chattanooga–Cleveland–Dalton 650:10.1016/0040-1951(83)90013-6 60:to its confluence with the 1783: 989:Mississippi Alluvial Plain 496:Charleston, South Carolina 319:Formation of the embayment 281:, which dates back to the 242:rocks both to the east in 50:Mississippi Alluvial Plain 1684: 1120:Kingsport–Bristol–Bristol 870:Colleges and universities 698: 979:Great Appalachian Valley 839:Tennessee National Guard 487:that was flooded by the 18:Mississippi River Valley 362:"Mississippi embayment" 263:New Madrid Seismic Zone 148:"Mississippi embayment" 85:causing an upthrust of 58:Mississippi River Delta 267:New Madrid earthquakes 37: 1747:Mississippi embayment 994:Mississippi embayment 42:Mississippi embayment 35: 1695:Tennessee portal 1183:Tullahoma–Manchester 969:Cumberland Mountains 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Index

Mississippi River Valley

United States
Mississippi Alluvial Plain
fluvial sediments
Mississippi River Delta
Ohio River
Cairo, Illinois
Cretaceous
Cenozoic
hotspot
mantle
magma
Gulf of Mexico

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