The Castle Pines 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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Sunny; warmer
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Mostly sunny
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Chance of showers
75° on Nov. 12, 1999, the hottest reading for this week of the year since 1996. Next is 75° in 2025.
Castle Pines’s center stands about 6,560 ft above sea level. Within three miles the land runs from 5,900 ft to 6,620 ft, a difference of 720 ft: hilly country. The highest named summit within 15 miles is Bennett Mountain, about 8,030 ft, 13 miles west-southwest.
Under the town center the state geologic map shows Upper part of Dawson Arkose (arkose, conglomerate, shale), from the Paleocene to Eocene, 34 to 66 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 9×. The colored band under the surface is the rock the state geologic map shows at the surface, not a picture of what lies beneath.
Arkose, conglomerate, shale. Age: Paleocene to Eocene, 34 to 66 million years old. About 17 mi of the line.
Biotite-gneiss, schist, migmatite. Age: Paleoproterozoic, 1.6 to 2.5 billion years old. About 3 mi of the line.
Gravel, unconsolidated. Age: Pleistocene, less than 0.5 million years old. About 2 mi of the line.
Arkose, shale, mudstone. Age: Late Cretaceous to Paleocene, 56 to 100 million years old. About 1 mi of the line.
Siltstone, sandstone, conglomerate. Age: Carboniferous to Early Triassic, 247 to 324 million years old. About 0.8 mi of the line.
Unconsolidated. Age: Quaternary, less than 2.6 million years old. About 0.6 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 Castle Pines reaches the Gulf of America by way of Cherry Creek, the South Platte, the Platte, the Missouri and the Mississippi: about 2,430 river miles.
1,170 miles of the trip are on the Mississippi.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Castle Pines; river miles along the main stem, rounded.
Castle Pines has a warm-summer humid continental climate. Summer afternoons average 85° in July; winter nights fall to about 17° in December. A normal year brings about 75 inches of snow; with the rain, that comes to about 19 inches of water.
Normals 1991–2020 and records since 1996 at Elizabeth 2 NW, 15 miles east-southeast. NOAA, through RCC-ACIS.
