The Quanah 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.
Quanah’s center stands about 1,570 ft above sea level. Within three miles the land runs from 1,490 ft to 1,600 ft, a difference of 110 ft: gently rolling country.
Under the town center the state geologic map shows Blaine Formation (shale), from the Permian, 252 to 299 million years old.
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 64×. 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. Age: Permian, 252 to 299 million years old. About 13 mi of the line.
Coarse-detrital, fine-detrital. Age: Pleistocene, less than 2.6 million years old. About 3 mi of the line.
Sand. Age: Holocene, less than 12,000 years old. About 2 mi of the line.
Sandstone-mudstone. Age: Permian, 252 to 299 million years old. About 2 mi of the line.
Fine-detrital, coarse-detrital. Age: Holocene, less than 12,000 years old. About 1 mi of the line.
Gypsum, dolostone. Age: Permian, 252 to 299 million years old. About 0.9 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 Quanah reaches the Gulf of America by way of Groesbeck Creek, the Red River, the Atchafalaya and the Lower Atchafalaya: about 1,160 river miles.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Quanah; river miles along the main stem, rounded.