The Wintersburg 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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Wintersburg’s center stands about 1,000 ft above sea level. Within three miles the land runs from 930 ft to 1,110 ft, a difference of 180 ft: gently rolling country. The highest named summit within 15 miles is Saddle Mountain, about 2,920 ft, 10 miles west.
Under the town center the state geologic map shows Late and middle Pleistocene surficial deposits (gravel, sand), from the Pleistocene, less than 0.8 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 19×. The colored band under the surface is the rock the state geologic map shows at the surface, not a picture of what lies beneath.
Basalt, andesite, dacite. Age: Middle Eocene to Late Miocene, 11 to 38 million years old. About 10 mi of the line.
Gravel, sand. Age: Pleistocene, less than 0.8 million years old. About 9 mi of the line.
Silt, clay. Age: Holocene, less than 10,000 years old. About 2 mi of the line.
Gravel, sand. Age: Late Miocene to Pleistocene, 0.8 to 10 million years old. About 1 mi of the line.
Gravel, sand. Age: Late Pliocene to Pleistocene, 0.8 to 3 million years old. About 0.6 mi of the line.
Sand, gravel. Age: Holocene, less than 10,000 years old. About 0.4 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 Wintersburg reaches the Gulf of California by way of Winters Wash, Centennial Wash, the Arlington Canal, the Gila and the Colorado: about 310 river miles.
170 miles of the trip are on the Gila.
Often dry. About 70% of the way is mapped as streams that run only after rain or snowmelt; the water makes the whole trip in floods.
Seldom reaches the sea. Dams and canals now take nearly all of the Colorado before its old delta in Mexico.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Wintersburg; river miles along the main stem, rounded.
