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Nashville Basin

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downward away from Nashville. The uplifting of the Nashville Dome fractured overlying strata, making it more easily eroded, and thus the "dome" resulted in a "basin". Uplifted strata in the center of a geological dome have higher potential erosive energy than the surrounding strata, because they are
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physically higher. Erosion thus acts on the uplifted area at a greater rate than on the surrounding flat-lying area, creating a low area, i.e., a basin. This area is more correctly referred to as the "Central Dome" of Tennessee.
271:. Here also are seen the horse farms somewhat reminiscent of the Kentucky Bluegrass region. Supposedly the underlying rock weathers to a soil particularly suited to the growing of the sorts of grasses most favored by horses. 181:
Nashville is located in the northwestern portion of the Central Basin. The basin extends for approximately forty-five to sixty miles to the east of Nashville and about eighty miles to the south, near the
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Counties, are open areas where the flat limestone rock is denuded of overlying soil or nearly so, provide an environment for flora unlike any other in the world.
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state line. Travelers leaving Nashville in a northerly or easterly direction will soon begin the climb up the
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is located to the south and east of Nashville, primarily in the counties of
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Center for Cedar Glades Studies at Middle Tennessee State University
24: 1204: 709: 383: 237: 1218: 873: 742: 686: 670: 603: 232:. The Nashville Basin and a similar but smaller area surrounding 183: 170: 303: 244:" area, are the two primary areas of this sort in the world. 145:, is a term often used to describe the area surrounding 169:. The Nashville Dome is evidenced by the underlying 251:of the flattest terrain and most limestone-derived 49:. Unsourced material may be challenged and removed. 279:), located to the east of Nashville, primarily in 2455: 334:. Nashville Geology Homepage. 24 September 2007 157:is located. The Central Basin was caused by an 2438: 1332: 1134: 994:Geographic data and information organizations 399: 221:The Central Basin is underlain primarily by 328:"Field Guide to the Limestone Cedar Glades" 2445: 2431: 1339: 1325: 1141: 1127: 406: 392: 1045:National Council for Geographic Education 109:Learn how and when to remove this message 128: 120: 16:Area surrounding Murfreesboro, Tennessee 2456: 1346: 1148: 1320: 1122: 387: 2397: 1299: 1089: 413: 47:adding citations to reliable sources 18: 1101: 13: 14: 2485: 2401: 2348: 1298: 1286: 1275: 1274: 1261: 1100: 1088: 1076: 1065: 1064: 1040:International Geography Olympiad 23: 2413:geography–related article is a 305:United States Geological Survey 34:needs additional citations for 753:Geographic information science 346: 320: 297: 1: 1664:Ridge-and-Valley Appalachians 859:Geographic information system 290: 210:as it flows northwest toward 2417:. 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Murfreesboro
Tennessee
Nashville
uplifting
dome
rock strata
dip
Alabama
escarpment
geographic
geologic province
Highland Rim
Cumberland Plateau
Cumberland River
Ashland City
Clarksville, Tennessee
limestone

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