The Shaw 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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17° on Nov. 13, 2019, the coldest reading for this week of the year since 1903. Next is 20° in 1940.
Shaw’s center stands about 140 ft above sea level. Within three miles the land runs from 120 ft to 140 ft, a difference of 20 ft: nearly flat ground.
Under the town center the state geologic map shows Alluvium (fine-detrital, coarse-detrital), 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.
Fine-detrital, coarse-detrital. 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.
A raindrop that lands in Shaw reaches the Gulf of America by way of Porter Bayou, the Big Sunflower, the Yazoo and the Mississippi: about 620 river miles.
450 miles of the trip are on the Mississippi.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Shaw; river miles along the main stem, rounded.
Shaw has a humid subtropical climate. Summer afternoons average 93° in July; winter nights fall to about 35° in January. About 49 inches of rain fall in a normal year.
On November 14 Shaw normally reaches 65° and falls to 42°. The record high is 87°, in 1955; the record low 24°, in 2013. The most rain on this date, 3.22 in, fell in 1957.
Normals 1991–2020 and records since 1903 from the Greenville Area threaded record (Greenville Asos, 14 miles west-southwest). NOAA, through RCC-ACIS.
