The Ovid 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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4° on Nov. 12, 2019, the coldest reading for this week of the year since 1897. Next is 5° in 1933.
Ovid’s center stands about 1,000 ft above sea level. Within three miles the land runs from 960 ft to 1,060 ft, a difference of 100 ft: gently rolling country.
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 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 Ovid reaches Lake Michigan by way of the Coldwater and the Saint Joseph: about 180 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 Ovid; river miles along the main stem, rounded.
Ovid has a warm-summer humid continental climate. Summer afternoons average 82° in July; winter nights fall to about 16° in January. A normal year brings about 43 inches of snow; with the rain, that comes to about 39 inches of water.
On November 14 Ovid normally reaches 47° and falls to 31°. The record high is 69°, in 1902; the record low 8°, in 2019. The most rain on this date, 0.96 in, fell in 1957.
Normals 1991–2020 and records since 1897 at Coldwater St School, 7 miles north. NOAA, through RCC-ACIS.
