The Websters Crossing 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.
Showers likely
Mostly cloudy
Mostly cloudy
Sunny; warmer
Mostly sunny
Partly cloudy
Partly cloudy
78° on Nov. 11, 2020, the hottest reading for this week of the year since 1898. Next is 73° in 2012.
Websters Crossing’s center stands about 1,390 ft above sea level. Within three miles the land runs from 900 ft to 2,040 ft, a difference of 1,140 ft: steep hill country. The highest named summit within 15 miles is Gannett Hill, about 2,320 ft, 12 miles east-northeast.
Under the town center the state geologic map shows West Hill and Gardeau Formations (shale, siltstone), from the Late Devonian, 359 to 384 million years old.
The section below crosses 6 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, siltstone. Age: Late Devonian, 359 to 384 million years old. About 11 mi of the line.
Shale. Age: Late Devonian, 359 to 384 million years old. About 6 mi of the line.
Sandstone. Age: Late Devonian, 359 to 384 million years old. About 4 mi of the line.
Shale. Age: Late Devonian, 359 to 384 million years old. About 3 mi of the line.
Sandstone. Age: Late Devonian, 359 to 384 million years old. About 1 mi of the line.
Shale. Age: Late Devonian, 359 to 384 million years old. About 0.3 mi of the line.
From the USGS State Geologic Map Compilation (Horton and others, 2017), the states’ geologic maps joined at a common scale.
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 Websters Crossing reaches Lake Ontario by way of McMillan Creek, Conesus Creek and the Genesee: about 60 river miles. From the lake it goes down the St. Lawrence to the Atlantic.
Lake on the way: Conesus Lake.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Websters Crossing; river miles along the main stem, rounded.
Websters Crossing has a warm-summer humid continental climate. Summer afternoons average 81° in July; winter nights fall to about 16° in January. About 37 inches of rain fall in a normal year.
On November 14 Websters Crossing normally reaches 49° and falls to 33°. The record high is 69°, in 1994; the record low 12°, in 1983. The most rain on this date, 0.67 in, fell in 1997.
Normals 1991–2020 and records since 1898 at Hemlock, 8 miles north, 490 ft lower. NOAA, through RCC-ACIS.
