The Rutledge 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.
Rutledge’s center stands about 720 ft above sea level. Within three miles the land runs from 550 ft to 810 ft, a difference of 260 ft: rolling country. The highest named summit within 15 miles is Alcovy Mountain, about 1,100 ft, 11 miles northwest.
Under the town center the state geologic map shows Biotite Gneiss/ Feldspathic Biotite Gneiss, from the Precambrian to Paleozoic.
The section below crosses 9 rock units mapped at the surface.
Heights every 0.1 mile from the Copernicus GLO-90 surface model; vertical exaggeration about 51×. The colored band under the surface is the rock the state geologic map shows at the surface, not a picture of what lies beneath.
Gneiss. Age: Precambrian to Paleozoic. About 7 mi of the line.
Biotite-gneiss. Age: Precambrian to Paleozoic. About 5 mi of the line.
Amphibolite, biotite-gneiss, mica-schist. Age: Precambrian to Paleozoic. About 4 mi of the line.
Gneiss. Age: Precambrian to Paleozoic. About 4 mi of the line.
Gneiss. Age: Precambrian to Paleozoic. About 1 mi of the line.
Schist, gneiss, amphibolite. 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. 3 smaller units 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 Rutledge reaches the Atlantic Ocean by way of Hard Labor Creek, Big Sandy Creek, the Apalachee, the Oconee and the Altamaha: about 340 river miles.
190 miles of the trip are on the Oconee.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Rutledge; river miles along the main stem, rounded.