The Crandall 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.
20° on Nov. 12, 2019, the coldest reading for this week of the year since 1940. Next is 22° in 2014.
Crandall’s center stands about 430 ft above sea level. Within three miles the land runs from 350 ft to 450 ft, a difference of 100 ft: gently rolling country.
Under the town center the state geologic map shows Neylandville and Marlbrook Marls, undivided (claystone), from the Late Cretaceous, 66 to 72 million years old.
The section below crosses 6 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.
Claystone. Age: Late Cretaceous, 66 to 72 million years old. About 11 mi of the line.
Fine-detrital, coarse-detrital. Age: Holocene, less than 12,000 years old. About 7 mi of the line.
Sandstone-mudstone. Age: Late Cretaceous, 66 to 72 million years old. About 4 mi of the line.
Sand. Age: Pleistocene to Holocene, less than 2.6 million years old. About 2 mi of the line.
Sandstone. Age: Late Cretaceous, 66 to 72 million years old. About 0.9 mi of the line.
Claystone. Age: Late Cretaceous, 66 to 72 million years old. About 0.4 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 Crandall reaches Galveston Bay and the Gulf of America by way of Buffalo Creek and the Trinity: about 420 river miles.
Lake on the way: Woodlands Golf Course Lake.
230 miles of the trip are on the Trinity.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Crandall; river miles along the main stem, rounded.
Crandall has a humid subtropical climate. Summer afternoons average 97° in August; winter nights fall to about 36° in January. About 41 inches of rain fall in a normal year.
On November 14 Crandall normally reaches 68° and falls to 45°. The record high is 89°, in 1989; the record low 25°, in 2018. The most rain on this date, 1.32 in, fell in 1994.
Normals 1991–2020 and records since 1940 at Ferris, 14 miles west-southwest. NOAA, through RCC-ACIS.