The Bemiss 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.
Sunny
Mostly sunny; warmer
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Partly cloudy
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87° on Nov. 12, 1986, the hottest reading for this week of the year since 1948. Next is 87° in 2011.
Bemiss’s center stands about 250 ft above sea level. Within three miles the land runs from 150 ft to 260 ft, a difference of 110 ft: gently rolling country.
Under the town center the state geologic map shows Miccosukee Formation (clay, sand, gravel), from the Tertiary Neogene, 2.6 to 23 million years old.
The section below crosses 3 rock units mapped at the surface.
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.
Clay, sand, gravel. Age: Tertiary Neogene, 2.6 to 23 million years old. About 10 mi of the line.
Sand, gravel. Age: Pliocene to Pleistocene, less than 5.3 million years old. About 7 mi of the line.
Dolostone, sand, clay. Age: Miocene, 5.3 to 23 million years old. About 5 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.
Bemiss has a humid subtropical climate. Summer afternoons average 92° in July; winter nights fall to about 39° in January. About 48 inches of rain fall in a normal year.
On November 14 Bemiss normally reaches 72° and falls to 47°. The record high is 85°, in 1993; the record low 27°, in 1963. The most rain on this date, 1.17 in, fell in 2018.
Normals 1991–2020 and records since 1948 at Valdosta Regional Airport, 11 miles south. NOAA, through RCC-ACIS.
