The Alpharetta 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.
Alpharetta’s center stands about 1,130 ft above sea level. Within three miles the land runs from 980 ft to 1,170 ft, a difference of 190 ft: gently rolling country. The highest named summit within 15 miles is Sawnee Mountain, about 1,940 ft, 13 miles northeast.
The section below crosses 3 rock units mapped at the surface.
Heights every 0.1 mile from the Copernicus GLO-90 surface model; vertical exaggeration about 47×. The colored band under the surface is the rock the state geologic map shows at the surface, not a picture of what lies beneath.
Amphibolite, biotite-gneiss, mica-schist. Age: Precambrian to Paleozoic. About 15 mi of the line.
Gneiss, mica-schist, amphibolite. Age: Precambrian to Paleozoic. About 7 mi of the line.
Age: Precambrian to Paleozoic. About 2 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 Alpharetta reaches the Gulf of America by way of Big Creek, the Chattahoochee and the Apalachicola: about 430 river miles.
Lakes on the way: Walter F George Reservoir, West Point Lake and Bartletts Ferry Lake.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Alpharetta; river miles along the main stem, rounded.