The Scotch Plains 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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78° on Nov. 16, 1993, the hottest reading for this week of the year since 1931. Next is 76° in 1973.
Scotch Plains’s center stands about 180 ft above sea level. Within three miles the land runs from 110 ft to 560 ft, a difference of 450 ft: hilly country. The highest named summit within 15 miles is Trowbridge Mountain, about 1,050 ft, 15 miles north-northwest.
Under the town center the state geologic map shows Passaic Formation Mudstone facies (sandstone-mudstone, siltstone-mudstone), from the Early Jurassic to Late Jurassic, 145 to 202 million years old.
The section below crosses 12 rock units mapped at the surface.
Heights every 0.1 mile from the Copernicus GLO-90 surface model; vertical exaggeration about 26×. The colored band under the surface is the rock the state geologic map shows at the surface, not a picture of what lies beneath.
Siltstone, shale. Age: Early Jurassic to Late Jurassic, 145 to 202 million years old. About 5 mi of the line.
Sandstone-mudstone, siltstone-mudstone. Age: Early Jurassic to Late Jurassic, 145 to 202 million years old. About 4 mi of the line.
Sandstone, siltstone-mudstone. Age: Early Jurassic, 175 to 202 million years old. About 3 mi of the line.
Sandstone, siltstone, mudstone. Age: Early Jurassic, 175 to 202 million years old. About 3 mi of the line.
Clay, sand. Age: Late Cretaceous, 66 to 100 million years old. About 2 mi of the line.
Basalt. Age: Early Jurassic, 175 to 202 million years old. About 2 mi of the line.
From the USGS State Geologic Map Compilation (Horton and others, 2017), the states’ geologic maps joined at a common scale. 6 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 Scotch Plains reaches New York Harbor and the Atlantic Ocean by way of Robinsons Branch and the Rahway: about 18 river miles.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Scotch Plains; river miles along the main stem, rounded.
Scotch Plains has a hot-summer humid continental climate. Summer afternoons average 86° in July; winter nights fall to about 22° in January. A normal year brings about 24 inches of snow; with the rain, that comes to about 50 inches of water.
On November 14 Scotch Plains normally reaches 55° and falls to 35°. The record high is 71°, in 1964; the record low 11°, in 1986. The most rain on this date, 1.51 in, fell in 1937.
Normals 1991–2020 and records since 1931 at Canoe Brook, 6 miles north-northeast. NOAA, through RCC-ACIS.
