The Macon 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.
Macon’s center stands about 200 ft above sea level. Within three miles the land runs from 170 ft to 260 ft, a difference of 90 ft: gently rolling country. The highest named summit within 15 miles is White House Mountain, about 600 ft, 14 miles south-southwest.
Under the town center the state geologic map shows Demopolis chalk, from the Late Cretaceous, 66 to 100 million years old.
The section below crosses 6 rock units mapped at the surface.
Heights every 0.1 mile from the Copernicus GLO-90 surface model; vertical exaggeration about 60×. The colored band under the surface is the rock the state geologic map shows at the surface, not a picture of what lies beneath.
Chalk. Age: Late Cretaceous, 66 to 100 million years old. About 12 mi of the line.
Clay. Age: Paleocene, 56 to 66 million years old. About 5 mi of the line.
Limestone. Age: Paleocene, 56 to 66 million years old. About 2 mi of the line.
Chalk, clay. Age: Late Cretaceous, 66 to 100 million years old. About 2 mi of the line.
Sand, clay, limestone. Age: Late Cretaceous, 66 to 100 million years old. About 1 mi of the line.
Chalk, clay. Age: Late Cretaceous, 66 to 100 million years old. 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 Macon reaches Mobile Bay and the Gulf of America by way of Cedar Creek, the Noxubee, the Tombigbee and the Mobile: about 340 river miles.
220 miles of the trip are on the Tombigbee.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Macon; river miles along the main stem, rounded.