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By G. Michael Clark, Edward J. Ciolkosz, J. Steven Kite, David A. Lietzke(auth.)

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Published by means of the yankee Geophysical Union as a part of the Field journey Guidebooks Series.

The geomorphology of the principal and Southern Appalachians has been the topic of numerous earlier tours. Johnson et al. (1933) led a bunch from long island via New Jersey, Pennsylvania, Maryland, and jap such a lot West Virginia to the sixteenth foreign Geological Congress in Washington, DC. Butts et al. (1933) mentioned a few points of Appalachian geomorphology in the course of their expedition from Washington to Morristown, Tennessee and go back. extra lately, Ciolkosz et al. (1971) led a geomorphology and soils journey from Pittsburgh, Pennsylvania to Washington. Kite and Linton (1987) et al., equipped box tours for the 1st assembly of the Southeastern pals of the Pleistocene in japanese West Virginia. Bogucki et al. (1973) led a visit via nice Smoky Mountains nationwide Park; a part of this course might be re-traversed on day certainly one of this day trip. Delcourt and Delcourt (1985) additionally performed a visit from Knoxville during the nice Smoky Mountains and likewise visited the terraces of the Little Tennessee River. because the sixteenth IGC, the point of interest of Appalachian geomorphic learn has shifted from hypothesis on total drainage evolution and outline and correlation of presumed erosion surfaces to quantitative description, process-oriented reports in accordance with equilibrium ideas, and utilized examine. curiosity continues to be excessive, despite the fact that, in examine that might aid clarify the origins of topography and drainage during this vintage area.

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Enter Moccasin Gap, a water gap through Clinch Mountain Exit Moccasin Gap. Enter Gate City, situated on the North side of Clinch Mountain, is underlain by a narrow strike belt of Chickamauga Group rocks. North of Gate City there is also a broad belt of Knox Group cherty dolostones. You are now on the Wilderness Road (the Orby Cantrell Highway). Clinch Mountain is on the left and Moccasin Ridge is on the right. Begin exposure in road cut on left. End exposure. Quarry on right. 3 above the local water-table levels, and have rail access to nearby markets in the Kingsport-Bristol area (Brent, 1963).

Junction with 1-81. Enter 1-81 north at exchange 12. Route enters an area underlain by calcareous Sevier Fonnation. Leave Hamblen County, enter Greene County. The ridge ahead that we will soon cross is Bays Mountain. 3 To the left are the higher ridges of the Bays Mountains. On a clear day the Great Smoky Mountains may be seen on the right skyline. The main drainage in this county is the Nolichucky River. The present floodplain and low Holocene terraces are narrow and discontinuous. 2 km from the river.

5' quadrangle). This area is the New River terrace site (FIGURE 28). For soil research purposes, Virginia Polytechnic Institute and State University acquired about 1200 acres (ca. 486 ha) located in the community of Whitehome, Montgomery County (FIGURE 28). Most of the known New River terrace levels are probably represented on the farm. Most of the site is underlain by carbonate rocks, with the exception of a shale rock unit. The youngest terrace has been designated TO, and the highest terrace is probably either T8 or T9.

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