The Rushville 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.
79° on Nov. 11, 2020, the hottest reading for this week of the year since 1942. Next is 73° in 1956.
Rushville’s center stands about 880 ft above sea level. Within three miles the land runs from 760 ft to 1,300 ft, a difference of 540 ft: hilly country. The highest named summit within 15 miles is Gannett Hill, about 2,320 ft, 10 miles west-southwest.
Under the town center the state geologic map shows Genesee Group (shale), from the Late Devonian, 359 to 384 million years old.
The section below crosses 7 rock units mapped at the surface.
Heights every 0.1 mile from the Copernicus GLO-90 surface model; vertical exaggeration about 13×. 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: Late Devonian, 359 to 384 million years old. About 11 mi of the line.
Shale, siltstone. Age: Late Devonian, 359 to 384 million years old. About 3 mi of the line.
Shale, siltstone. Age: Late Devonian, 359 to 384 million years old. About 3 mi of the line.
Shale. Age: Middle Devonian, 384 to 388 million years old. About 2 mi of the line.
Shale, limestone. Age: Middle Devonian, 384 to 388 million years old. About 2 mi of the line.
Shale. Age: Late Devonian, 359 to 384 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. 1 smaller unit 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 Rushville reaches Lake Ontario by way of the West River, the Canandaigua Outlet, the Erie Canal, the Clyde, the Seneca and the Oswego: about 150 river miles. From the lake it goes down the St. Lawrence to the Atlantic.
Lake on the way: Canandaigua Lake.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Rushville; river miles along the main stem, rounded.
Rushville has a hot-summer humid continental climate. Summer afternoons average 82° in July; winter nights fall to about 18° in January. About 35 inches of rain fall in a normal year.
On November 14 Rushville normally reaches 49° and falls to 34°. The record high is 69°, in 1961; the record low 13°, in 1986. The most rain on this date, 0.59 in, fell in 1997.
Normals 1991–2020 and records since 1942 at Canandaigua 3 S, 6 miles north-northwest, 160 ft lower. NOAA, through RCC-ACIS.