The Bear Lake 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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−10° on Nov. 17, 1989, the coldest reading for this week of the year since 1931. Next is −9° in 1986.
Bear Lake’s center stands about 1,280 ft above sea level. Within three miles the land runs from 1,190 ft to 1,390 ft, a difference of 200 ft: rolling country.
Under the town center the state geologic map shows Cambrian, undivided (sandstone), from the Cambrian, 487 to 542 million years old.
Heights every 0.1 mile from the Copernicus GLO-90 surface model; vertical exaggeration about 49×. 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. Age: Cambrian, 487 to 542 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 Bear Lake reaches the Gulf of America by way of Little Bear Creek, Bear Creek, the Red Cedar, the Chippewa and the Mississippi: about 1,870 river miles.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Bear Lake; river miles along the main stem, rounded.
Bear Lake has a warm-summer humid continental climate. Summer afternoons average 79° in July; winter nights fall to about 0° in January. A normal year brings about 56 inches of snow; with the rain, that comes to about 34 inches of water.
On November 14 Bear Lake normally reaches 39° and falls to 23°. The record high is 67°, in 1999; the record low −2°, in 1940. The most rain on this date, 0.57 in, fell in 1951.
Normals 1991–2020 and records since 1931 at Cumberland, 9 miles west-southwest. NOAA, through RCC-ACIS.
