The Paige 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.
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Paige’s center stands about 540 ft above sea level. Within three miles the land runs from 460 ft to 590 ft, a difference of 130 ft: gently rolling country. The highest named summit within 15 miles is Yegua Knobbs, about 740 ft, 10 miles north-northwest.
Under the town center the state geologic map shows Cook Mountain Formation (claystone, sandstone), from the Eocene, 34 to 56 million years old.
The section below crosses 8 rock units mapped at the surface.
Heights every 0.1 mile from the Copernicus GLO-90 surface model; vertical exaggeration about 59×. The colored band under the surface is the rock the state geologic map shows at the surface, not a picture of what lies beneath.
Claystone, sandstone. Age: Eocene, 34 to 56 million years old. About 11 mi of the line.
Sandstone. Age: Eocene, 34 to 56 million years old. About 3 mi of the line.
Siltstone, sandstone. Age: Middle Eocene, 38 to 48 million years old. About 2 mi of the line.
Sandstone. Age: Eocene, 34 to 56 million years old. About 2 mi of the line.
Sandstone. Age: Eocene, 34 to 56 million years old. About 2 mi of the line.
Claystone. Age: Late Paleocene to Early Eocene, 48 to 59 million years old. 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. 2 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 Paige reaches the Gulf of America by way of Turner Creek, Pin Oak Creek and the Colorado: about 220 river miles.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Paige; river miles along the main stem, rounded.
