The Clear Spring 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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1° on Nov. 16, 1908, the coldest reading for this week of the year since 1899. Next is 9° in 1933.
Clear Spring’s center stands about 560 ft above sea level. Within three miles the land runs from 410 ft to 1,400 ft, a difference of 990 ft: steep hill country. The highest named summit within 15 miles is Cross Mountain, about 2,070 ft, 6 miles north-northwest.
Under the town center the state geologic map shows Conococheague Limestone, from the Cambrian to Early Ordovician, 471 to 497 million years old.
The section below crosses 17 rock units mapped at the surface.
Heights every 0.1 mile from the Copernicus GLO-90 surface model; vertical exaggeration about 12×. 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: Ordovician, 445 to 487 million years old. About 3 mi of the line.
Limestone. Age: Cambrian to Early Ordovician, 471 to 497 million years old. About 3 mi of the line.
Graywacke, shale. Age: Ordovician, 445 to 487 million years old. About 3 mi of the line.
Shale. Age: Ordovician, 445 to 487 million years old. About 3 mi of the line.
Limestone. Age: Cambrian, 487 to 542 million years old. About 2 mi of the line.
Limestone. Age: Ordovician, 445 to 487 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. 11 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 Clear Spring reaches Chesapeake Bay and the Atlantic Ocean by way of Toms Run and the Potomac: about 230 river miles.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Clear Spring; river miles along the main stem, rounded.
Clear Spring has a humid subtropical climate. Summer afternoons average 87° in July; winter nights fall to about 25° in January. About 36 inches of rain fall in a normal year.
On November 14 Clear Spring normally reaches 55° and falls to 38°. The record high is 75°, in 1989; the record low 10°, in 1920. The most rain on this date, 1.91 in, fell in 1995.
Normals 1991–2020 and records since 1899 from the Hagerstown Area threaded record (Hagerstown Regional Airport, 11 miles east-northeast, 130 ft higher). NOAA, through RCC-ACIS.
