The Delaware Water Gap 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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3.42 inches of rain fell in two days, the most for this week of the year since records began in 1910. The next wettest, 2.83 inches, fell in 1970.
Delaware Water Gap’s center stands about 530 ft above sea level. Within three miles the land runs from 290 ft to 1,480 ft, a difference of 1,190 ft: steep hill country. The highest named summit within 15 miles is Camelback Mountain, about 2,120 ft, 12 miles west-northwest.
The section below crosses 18 rock units mapped at the surface.
Heights every 0.1 mile from the Copernicus GLO-90 surface model; vertical exaggeration about 11×. The colored band under the surface is the rock the state geologic map shows at the surface, not a picture of what lies beneath.
Graywacke, siltstone. Age: Middle Ordovician to Late Ordovician, 445 to 471 million years old. About 5 mi of the line.
Sandstone, siltstone, mudstone. Age: Late Devonian, 359 to 384 million years old. About 3 mi of the line.
Dolostone. Age: Cambrian to Early Ordovician, 471 to 497 million years old. About 2 mi of the line.
Shale, siltstone. Age: Early Devonian to Middle Devonian, 384 to 422 million years old. About 2 mi of the line.
Black-shale. Age: Early Devonian to Middle Devonian, 384 to 422 million years old. About 2 mi of the line.
Slate, shale. Age: Middle Ordovician, 459 to 471 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. 12 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 Delaware Water Gap reaches Delaware Bay and the Atlantic Ocean by way of the Delaware: about 180 river miles.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Delaware Water Gap; river miles along the main stem, rounded.
Delaware Water Gap has a hot-summer humid continental climate. Summer afternoons average 84° in July; winter nights fall to about 19° in January. A normal year brings about 42 inches of snow; with the rain, that comes to about 54 inches of water.
On November 14 Delaware Water Gap normally reaches 52° and falls to 32°. The record high is 72°, in 1931; the record low 11°, in 1986. The most rain on this date, 1.83 in, fell in 1972.
Normals 1991–2020 and records since 1910 at East Stroudsburg, 4 miles northwest. NOAA, through RCC-ACIS.
