The Fairview 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.
Mostly cloudy
Partly cloudy
Mostly cloudy
Showers likely
Chance of showers; cooler
Showers likely
Showers likely
Fairview’s center stands about 6,210 ft above sea level. Within three miles the land runs from 6,110 ft to 7,150 ft, a difference of 1,040 ft: steep hill country. The highest named summit within 15 miles is Mount Fitzpatrick, about 10,840 ft, 11 miles east-northeast.
Under the town center the state geologic map shows Alluvium and Colluvium (clay, silt, sand), from the Pleistocene to Holocene, less than 2.6 million years old.
The section below crosses 14 rock units mapped at the surface.
Heights every 0.1 mile from the Copernicus GLO-90 surface model; vertical exaggeration about 4×. The colored band under the surface is the rock the state geologic map shows at the surface, not a picture of what lies beneath.
Clay, silt, sand. Age: Pleistocene to Holocene, less than 2.6 million years old. About 4 mi of the line.
Mudstone, sandstone, limestone. Age: Triassic, 202 to 252 million years old. About 4 mi of the line.
Siltstone, sandstone, limestone. Age: Middle Jurassic to Late Jurassic, 145 to 175 million years old. About 3 mi of the line.
Age: Carboniferous to Permian, 252 to 324 million years old. About 3 mi of the line.
Shale, limestone, siltstone. Age: Early Triassic to Late Triassic, 202 to 252 million years old. About 2 mi of the line.
Limestone. Age: Carboniferous to Permian, 252 to 359 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. 8 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.
