The Christiansburg 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.
Partly cloudy
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Mostly sunny; warmer
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3.93 inches of rain fell in two days, the most for this week of the year since records began in 1893. The next wettest, 3.66 inches, fell in 2009.
Christiansburg’s center stands about 2,090 ft above sea level. Within three miles the land runs from 1,780 ft to 2,330 ft, a difference of 550 ft: hilly country. The highest named summit within 15 miles is Poor Mountain, about 3,930 ft, 14 miles east-northeast.
Under the town center the state geologic map shows Lower Ordovician and Upper Cambrian Formations Undivided (limestone), from the Cambrian to Ordovician, 445 to 542 million years old.
The section below crosses 9 rock units mapped at the surface.
Heights every 0.1 mile from the Copernicus GLO-90 surface model; vertical exaggeration about 13×. The colored band under the surface is the rock the state geologic map shows at the surface, not a picture of what lies beneath.
Shale. Age: Cambrian, 487 to 542 million years old. About 7 mi of the line.
Dolostone, limestone. Age: Cambrian, 487 to 542 million years old. About 6 mi of the line.
Limestone. Age: Cambrian to Ordovician, 445 to 542 million years old. About 6 mi of the line.
Limestone. Age: Cambrian, 487 to 542 million years old. About 2 mi of the line.
Quartzite, conglomerate, sandstone. Age: Cambrian, 487 to 542 million years old. About 1 mi of the line.
Shale, black-shale. Age: Devonian, 359 to 422 million years old. About 1 mi of the line.
From the USGS State Geologic Map Compilation (Horton and others, 2017), the states’ geologic maps joined at a common scale. 3 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.
Christiansburg straddles the Eastern Continental Divide. Rain on the northeast side runs to Albemarle Sound and the Atlantic Ocean; most of the rest goes to the Gulf of America.
From the center of town, a raindrop reaches the Gulf of America by way of Walnut Branch, Crab Creek, the New River, the Kanawha, the Ohio and the Mississippi: about 1,930 river miles. One that lands on the northeast side reaches Albemarle Sound and the Atlantic Ocean by way of Wilson Creek, the North Fork Roanoke and the Roanoke: about 400 river miles.
970 miles of the trip are on the Mississippi.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Christiansburg; river miles along the main stem, rounded.
Christiansburg has a warm-summer humid continental climate. Summer afternoons average 82° in July; winter nights fall to about 22° in January. A normal year brings about 25 inches of snow; with the rain, that comes to about 43 inches of water.
On November 14 Christiansburg normally reaches 55° and falls to 31°. The record high is 73°, in 1958; the record low 9°, in 1986. The most rain on this date, 1.40 in, fell in 1972.
Normals 1991–2020 and records since 1893 from the Blacksburg Area threaded record (Blacksburg Nwso, 5 miles north). NOAA, through RCC-ACIS.
