The Deering 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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86° on Nov. 13, 1955, the hottest reading for this week of the year since 1893. Next is 83° in 1964.
Deering’s center stands about 260 ft above sea level. Within three miles the land runs from 250 ft to 260 ft, a difference of 10 ft: nearly flat ground.
Under the town center the state geologic map shows Holocene series (clay, silt, sand), from the Holocene, less than 12,000 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.
Clay, silt, sand. Age: Holocene, less than 12,000 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.
Deering has a humid subtropical climate. Summer afternoons average 90° in July; winter nights fall to about 30° in January. About 55 inches of rain fall in a normal year.
On November 14 Deering normally reaches 60° and falls to 40°. The record high is 82°, in 1955; the record low 17°, in 1940. The most rain on this date, 3.00 in, fell in 1957.
Normals 1991–2020 and records since 1893 at Caruthersville, 13 miles east. NOAA, through RCC-ACIS.
