The Scotts Corners 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
Mostly sunny; warmer
Partly cloudy
Sunny
Mostly sunny
Mostly sunny
Mostly sunny
17° on Nov. 15, 1996, the coldest reading for this week of the year since 1946. Next is 18° in 1967.
Scotts Corners’s center stands about 480 ft above sea level. Within three miles the land runs from 270 ft to 680 ft, a difference of 410 ft: hilly country. The highest named summit within 15 miles is Pine Mountain, about 1,010 ft, 12 miles north-northeast.
Under the town center the state geologic map shows Hartland Formation (amphibolite, pelitic-schist), from the Cambrian to Early Ordovician, 471 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 20×. The colored band under the surface is the rock the state geologic map shows at the surface, not a picture of what lies beneath.
Gneiss. Age: Middle Ordovician, 459 to 471 million years old. About 5 mi of the line.
Gneiss. Age: Precambrian to Mesoproterozoic. About 5 mi of the line.
Schist, gneiss. Age: Early Ordovician to Middle Ordovician, 459 to 487 million years old. About 4 mi of the line.
Marble. Age: Early Cambrian to Early Ordovician, 471 to 542 million years old. About 3 mi of the line.
Gneiss. Age: Precambrian to Mesoproterozoic. About 2 mi of the line.
Amphibolite, pelitic-schist. Age: Cambrian to Early Ordovician, 471 to 542 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. 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.
A raindrop that lands in Scotts Corners reaches Long Island Sound and the Atlantic Ocean by way of the Mill and the Rippowam: about 14 river miles.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Scotts Corners; river miles along the main stem, rounded.
Scotts Corners has a hot-summer humid continental climate. Summer afternoons average 83° in July; winter nights fall to about 23° in January. About 48 inches of rain fall in a normal year.
On November 14 Scotts Corners normally reaches 53° and falls to 37°. The record high is 71°, in 1993; the record low 20°, in 1986. The most rain on this date, 1.92 in, fell in 1972.
Normals 1991–2020 and records since 1946 at Westchester Co Airport, 12 miles southwest, 110 ft lower. NOAA, through RCC-ACIS.
