The Reese 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.
Mostly cloudy
Mostly cloudy
Mostly sunny
Sunny
Partly cloudy
Partly cloudy
Partly cloudy
77° on Nov. 11, 2020, the hottest reading for this week of the year since 1963. Next is 69° in 2012.
Reese’s center stands about 630 ft above sea level. Within three miles the land runs from 590 ft to 650 ft, a difference of 60 ft: gently rolling country.
Under the town center the state geologic map shows Saginaw Formation (sandstone, shale), from the Carboniferous, 299 to 324 million years old.
Heights every 0.1 mile from the Copernicus GLO-90 surface model; vertical exaggeration about 64×. The colored band under the surface is the rock the state geologic map shows at the surface, not a picture of what lies beneath.
Sandstone, shale. Age: Carboniferous, 299 to 324 million years old. About 24 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 Reese reaches Lake Huron by way of the Quanicassee: about 11 river miles. From there it moves on through the Great Lakes, over Niagara Falls and down the St. Lawrence to the Atlantic.
Often dry. About 60% of the way is mapped as streams that run only after rain or snowmelt; the water makes the whole trip in floods.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Reese; river miles along the main stem, rounded.
Reese has a warm-summer humid continental climate. Summer afternoons average 82° in July; winter nights fall to about 12° in January. About 34 inches of rain fall in a normal year.
Normals 1991–2020 and records since 1963 at Vassar, 8 miles southeast. NOAA, through RCC-ACIS.
