The Vanceburg plate. Relief from Copernicus GLO-30; rivers and lakes from USGS NHD; watersheds from the USGS Watershed Boundary Dataset; roads and city limits from Census TIGER 2024.
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Vanceburg’s center stands about 540 ft above sea level. Within three miles the land runs from 480 ft to 1,170 ft, a difference of 690 ft: hilly country. The highest named summit within 15 miles is Blue Ridge Hill, about 1,280 ft, 11 miles south.
The section below crosses 7 rock units mapped at the surface.
Heights every 0.1 mile from the Copernicus GLO-90 surface model; vertical exaggeration about 23×. The colored band under the surface is the rock the state geologic map shows at the surface, not a picture of what lies beneath.
Shale, siltstone, sandstone. Age: Devonian to Carboniferous, 324 to 422 million years old. About 9 mi of the line.
Shale. Age: Devonian to Carboniferous, 324 to 422 million years old. About 9 mi of the line.
Black-shale. Age: Devonian to Carboniferous, 324 to 422 million years old. About 3 mi of the line.
Shale. Age: Silurian, 422 to 445 million years old. About 1 mi of the line.
Sand, silt. Age: Pleistocene to Holocene, less than 2.6 million years old. About 0.8 mi of the line.
Shale, black-shale. Age: Devonian, 359 to 422 million years old. About 0.8 mi of the line.
From the USGS State Geologic Map Compilation (Horton and others, 2017), the states’ geologic maps joined at a common scale. 1 smaller unit along the line are not listed.
Heights from Copernicus GLO-90 (a surface model: it includes buildings and tree canopy); summits from USGS GNIS; rivers from USGS NHDPlus HR; rock from the USGS State Geologic Map Compilation.
A raindrop that lands in Vanceburg reaches the Gulf of America by way of Salt Lick Creek, the Ohio and the Mississippi: about 1,570 river miles.
970 miles of the trip are on the Mississippi.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Vanceburg; river miles along the main stem, rounded.
