The Caseville 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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5° on Nov. 16, 1933, the coldest reading for this week of the year since 1887. Next is 9° in 1959.
Caseville’s center stands about 600 ft above sea level. Within three miles the land runs from 570 ft to 650 ft, a difference of 80 ft: gently rolling country.
Under the town center the state geologic map shows Michigan Formation (shale), from the Carboniferous, 324 to 359 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.
Shale. Age: Carboniferous, 324 to 359 million years old. About 12 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 Caseville reaches Lake Huron by way of the Pigeon: about 1 river miles. From there it moves on through the Great Lakes, over Niagara Falls and down the St. Lawrence to the Atlantic.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Caseville; river miles along the main stem, rounded.
Caseville has a warm-summer humid continental climate. Summer afternoons average 80° in July; winter nights fall to about 16° in January. About 33 inches of rain fall in a normal year.
On November 14 Caseville normally reaches 46° and falls to 32°. The record high is 65°, in 1989; the record low 12°, in 1986. The most rain on this date, 1.01 in, fell in 1957.
Normals 1991–2020 and records since 1887 at Bad Axe, 17 miles east-southeast, 120 ft higher. NOAA, through RCC-ACIS.
