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America's Volcanic Past
Tennessee

"Though few people in the United States may actually experience an erupting volcano, the evidence for earlier volcanism is preserved in many rocks of North America. Features seen in volcanic rocks only hours old are also present in ancient volcanic rocks, both at the surface and buried beneath younger deposits." -- Excerpt from: Brantley, 1994

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MORE America's Volcanic Past - Appalachian Mountains


Map, Location of Tennessee

Volcanic Highlights and Features:
[NOTE: This list is just a sample of various Tennessee features or events and is by no means inclusive. All information presented here was gathered from other online websites and each excerpt is attributed back to the original source. Please use those sources in referencing any information on this webpage, and please visit those websites for more information on the Geology of Tennessee.]

  • Tennessee
  • Tennessee Regions
  • Tennessee - Brief Geologic History
  • Tennessee's Igneous and Metamorphic Rocks
  • Appalachian Mountains
  • Blue Ridge Mountains
  • Blue Ridge National Parkway
  • Copper Basin
  • Great Smoky Mountains
  • Great Smoky Mountains National Park
  • Nashville

Tennessee



Excerpt from:
   
Tennessee Regions

The Appalachians:5
The Appalachians are old. A look at rocks exposed in today's Appalachian mountains reveals elongate belts of folded and thrust faulted marine sedimentary rocks, volcanic rocks and slivers of ancient ocean floor. Strong evidence that these rocks were deformed during plate collision. The birth of the Appalachian ranges, some 480 million years ago, marks the first of several mountain building plate collisions that culminated in the construction of the supercontinent Pangea with the Appalachians near the center.




The Interior Plains:5
The Interior Plains is a vast region that spreads across the stable core (craton) of North America. This area had formed when several small continents collided and welded together well over a billion years ago, during the Precambrian. Precambrian metamorphic and igneous rocks now form the basement of the Interior Plains and make up the stable nucleus of North America. With the exception of the Black Hills of South Dakota, the entire region has low relief, reflecting more than 500 million years of relative tectonic stability.




The Atlantic Plain:5
The Atlantic Plain is the flattest of the provinces. It stretches over 2,200 miles in length from Cape Cod to the Mexican border and southward another 1000 miles to the Yucatan Peninsula. The Atlantic plain slopes gently seaward from the inland highlands in a series of terraces. This gentle slope continues far into the Atlantic and Gulf of Mexico, forming the continental shelf. This region was born during the breakup of the supercontinent Pangea in the early Mesozoic Era.


   
Tennessee - Brief Geologic History

Precambrian Igneous and Metamorphic Rocks:6
Metamorphosed lavas and tuffs, metagabbro, rhyolites, diorite, granite, granitic gneisses, monzonite, quartz latites, anorthosite and diabase.

Precambrian Sedimentary and Metamorphic Rocks:6
Sandstone, conglomerate, siltstone, arkose, graywacke, quartzite, phyllite, slate and schist.

Cambrian:6
Shale, dolomite, limestone, sandstone, conglomerate, quartzite, arkose, graywacke and siltstone.

Ordovician-Cambrian:6
Dolomite, limestone, shale, chert, siltstone and sandstone.

Ordovician:6
Limestone, shale, dolomite, siltstone, sandstone and claystone.

Devonian-Silurian:6
Limestone, chert, shale, and sandstone.

Mississippian:6
Limestone, chert, shale, siltstone, sandstone and dolomite.

Pennsylvanian:6
Sandstone, shale, conglomerate, siltstone and coal.

Cretaceous:6
Sand, clay, silt and gravel.

Tertiary:6
Sand, silt, clay and gravel.

Quaternary:6
Sand, silt, clay, gravel and loess.

   

Tennessee's Igneous and Metamorphic Rocks

Tennessee's Igneous and Metamorphic Rocks:6
Extreme eastern Tennessee (Johnson, Carter, and Unicoi Counties): Metamorphosed lavas and tuffs, metagabbro, rhyolites, diorite, granite, granitic gneisses, monsonite, quartz latites, anorthosite and diabase.




Appalachian Mountains

Appalachian Mountains:1
Geologists tell us that sections of huge plates forming the crust of the earth have collided violently on numerous occasions in the past. The results are folded-up slabs of crust piled up like a deck of cards or a wrinkled throw rug. This mass of mostly igneous (cooled, molten material) and metamorphic (formed under heat and pressure) rock is the geological foundation of the Appalachians that we see today.




Blue Ridge Mountains -
Blue Ridge National Parkway

Blue Ridge Mountains:3
Most of the rocks that form the Blue Ridge are ancient granitic and metamorphosed volcanic formations, some exceeding one billion years in age. By comparison, humans have been associated with this land only about 9,000 years.

Blue Ridge National Parkway:1
The Blue Ridge National Parkway extends 469 miles along the crests of the Southern Appalachians and links two eastern national parks: Shenandoah and Great Smoky Mountains.


Copper Basin

Copper Basin:4
(During the Late Proterozoic Era - 750 to 570 million years ago) ... Large copper deposits formed in the area we now know as Copper Basin, near Ducktown, Tennessee. Geologists think that these ore deposits probably formed from hot fluids escaping from deep within the Earth through vents in this ancient sea floor. Metal-rich "black smokers" discovered recently in the Pacific Ocean off the coast of Washington and Oregon may represent a modern analogy.


Great Smoky Mountains -
Great Smoky Mountains National Park

Great Smoky Mountains:2
The Great Smoky Mountains, the majestic climax of the Appalachian Highlands.




Nashville

Lebanon Pike across from Mount Olivet Cemetery, Nashville:6
In the yard of the building supply company you can see the residue of ash falls from two of the huge volcanic eruptions that occurred about 455 million years ago. Look for two horizontal bars. Fossil hunting is better a few doors further west on Lebanon Pike. Look for lots of coral along the road going into the quarry.




Excerpts from:
1) U.S. National Park Service Website, Blue Ridge Parkway: Appalachian Geology, 2000
2) U.S. National Park Service Website, Great Smoky Mountains National Park, North Carolina and Tennessee, 2000
3) U.S. National Park Service Website, Shenandoah National Park, 2000
4) The Geologic Story of the Ocoee River: USGS General Interest Publication, July 1996
5) USGS/NPS Geology in the Parks Website, 2001
6) Tennessee Department of Environment and Conservation Website, 2002

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01/28/03, Lyn Topinka