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Sequatchie River Earthcache EarthCache

This cache has been archived.

geoawareUSA9: This CO has not been active since 2010 and has not logged into the site since 2021, so while I was hopeful I'd hear something back, I was not betting the farm. I am archiving due to lack of owner response.

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Hidden : 8/6/2007
Difficulty:
1.5 out of 5
Terrain:
5 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

Welcome to Dunlap, TN. You are about to venture on a tour of the Sequatchie River. You will need a non-motorized form of aqua transportation to get this earthcache.


"The mountains of the Sequatchie country are part of one of the large physiographic provinces of the eastern United States known as the Appalachian Plateau, which extends from southern New York into central Alabama. This province is known, south of West Virginia as the Cumberland Plateau. The Cumberland Plateau is a broad, relatively flat-topped tableland capped with hard resistant rock which has protected the softer underlying strata from erosion.

The most striking geological feature of the plateau is the Sequatchie anticline, an elongated upfold of rock into which nature has eroded an impressive valley. ... Only the portion of the trough within Tennessee is known as the Sequatchie Valley, the valley drained by the river of the same name. Within this long depression, extending halfway across Tennessee from the river's mouth near the Alabama line, the valley floor averages some five miles in width and lies about one thousand feet below the height of the plateau, which is marked by sheer slopes".

Despite the rumors, Sequatchie Valley is not a rift valley.

In fact, it more closely relates to a compressional geologic structure, the Sequatchie Valley anticline.

At the crest of the Sequatchie Valley anticline (an upward fold), Pennsylvanian sandstone was breached by erosion. (This sandstone serves as a resistant cap rock for the plateaus in the Chattanooga area.) The valley was formed by extensive weathering of the underlying Ordovician, Silurian, and Mississippian limestone, which occupies a structurally higher than normal position at the core of the anticline.


These blocks show steps in the formation of the Sequatchie Valley. Unfolded rocks (A) were subsequently warped and displaced by a thrust fault (B). A stream first eroded through the sandstone "cap" (C) and later into underlying limestone (D). Presently, a wide stream valley containing numerous sinkholes has developed on the limestone exposed along the axis of the folded rocks (E)


Earthcache Requirements are as follows.


You will need a canoe or non-motorized flotation to get this earthcache.
Email me the elevation and the approximate width of the Sequatchie River at the point of coordinates.
Email me a description of the Sequatchie Valley in your own words. What is unique about it?
Upload a picture of you in the area.

Additional Hints (No hints available.)