The Pueblo 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.
Pueblo’s center stands about 6,070 ft above sea level. Within three miles the land runs from 5,890 ft to 6,960 ft, a difference of 1,070 ft: steep hill country. The highest named summit within 15 miles is El Barro Peaks, about 8,160 ft, 13 miles north.
Under the town center the state geologic map shows Permian and Pennsylvanian rocks, undivided (sandstone, limestone, dolostone), from the Carboniferous to Permian, 252 to 324 million years old.
The section below crosses 4 rock units mapped at the surface.
Heights every 0.1 mile from the Copernicus GLO-90 surface model; vertical exaggeration about 10×. The colored band under the surface is the rock the state geologic map shows at the surface, not a picture of what lies beneath.
Sandstone. Age: Permian, 273 to 290 million years old. About 9 mi of the line.
Sandstone, limestone, dolostone. Age: Carboniferous to Permian, 252 to 324 million years old. About 8 mi of the line.
Limestone, dolostone. Age: Permian, 260 to 290 million years old. About 5 mi of the line.
Sandstone, carbonate, evaporite. Age: Permian, 273 to 290 million years old. About 3 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 Pueblo reaches the Gulf of America by way of the Pecos and the Rio Grande: about 1,480 river miles.
Lakes on the way: Paz Ramirez Lake, Amistad Reservoir, Red Bluff Reservoir and Lake McMillan.
410 miles of the trip are on the Pecos.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Pueblo; river miles along the main stem, rounded.