Moccasin Gap is the more dramatic of only two true, natural gaps in the Clinch Mountain ridge. It is located in the present day state of Virginia, in
Scott County. It lies between two cities;
Weber City is built into the south side of the gap and Gate City is to the northwest. The area surrounding Moccasin Gap is
sedimentary which is formed by the compaction of particles of gravel, sand, silt, mud, and carbonate minerals from the repetitive rise and fall of shallow seas, dating to the
Cambrian or
Pennsylvanian period. Moccasin Gap is a
water gap that is currently traversed by a channel of water,
Big Moccasin Creek which is a tributary to the
North Fork Holston River. The climate in Scott County is classified as
continental or warm-to-temperate consisting of four seasons. Average temperatures reach in the summer months and drop to in the wintertime. The greatest mean of rainfall is also during these times while the least precipitation occurs in the fall. ==History==