The Cherry Log 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.
Cherry Log’s center stands about 1,600 ft above sea level. Within three miles the land runs from 1,410 ft to 3,290 ft, a difference of 1,880 ft: steep hill country. The highest named summit within 15 miles is Cowpen Mountain, about 4,160 ft, 13 miles northwest.
Under the town center the state geologic map shows Mica Schist (mica-schist), from the Precambrian to Paleozoic.
The section below crosses 5 rock units mapped at the surface.
Heights every 0.1 mile from the Copernicus GLO-90 surface model; vertical exaggeration about 8×. The colored band under the surface is the rock the state geologic map shows at the surface, not a picture of what lies beneath.
Mica-schist, gneiss. Age: Precambrian to Paleozoic. About 9 mi of the line.
Metagraywacke, mica-schist, quartzite. Age: Precambrian to Paleozoic. About 8 mi of the line.
Mica-schist. Age: Precambrian to Paleozoic. About 3 mi of the line.
Biotite-schist. Age: Precambrian to Paleozoic. About 3 mi of the line.
Metagraywacke, mica-schist, calc-silicate-gneiss. Age: Precambrian to Paleozoic. About 1 mi of the line.
From the USGS State Geologic Map Compilation (Horton and others, 2017), the states’ geologic maps joined at a common scale.
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 Cherry Log reaches Mobile Bay and the Gulf of America by way of Rock Creek, the Ellijay, the Coosawattee, the Oostanaula, the Coosa, the Alabama and the Mobile: about 750 river miles.
Lakes on the way: Lay Lake and Carters Lake.
310 miles of the trip are on the Alabama.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Cherry Log; river miles along the main stem, rounded.