The Temescal Valley 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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22° on Nov. 17, 1958, the coldest reading for this week of the year since 1897. Next is 25° in 1964.
Temescal Valley’s center stands about 1,150 ft above sea level. Within three miles the land runs from 930 ft to 3,280 ft, a difference of 2,350 ft: mountain country. The highest named summit within 15 miles is Santiago Peak, about 5,660 ft, 5 miles southwest.
Under the town center the state geologic map shows Older Quaternary alluvium and marine deposits (coarse-detrital), from the Pleistocene, less than 2.6 million years old.
The section below crosses 7 rock units mapped at the surface.
Heights every 0.1 mile from the Copernicus GLO-90 surface model; vertical exaggeration about 5×. The colored band under the surface is the rock the state geologic map shows at the surface, not a picture of what lies beneath.
Tonalite. Age: Middle Jurassic to Late Cretaceous, 66 to 175 million years old. About 10 mi of the line.
Felsic-volcanic, mafic-volcanic. Age: Late Jurassic to Early Cretaceous, 100 to 164 million years old. About 4 mi of the line.
Argillite. Age: Paleozoic to Late Jurassic, 145 to 542 million years old. About 4 mi of the line.
Coarse-detrital. Age: Pleistocene, less than 2.6 million years old. About 3 mi of the line.
Coarse-detrital. Age: Pleistocene to Holocene, less than 2.6 million years old. About 2 mi of the line.
Mudstone, sandstone. Age: Paleocene to Oligocene, 23 to 66 million years old. About 0.5 mi of the line.
From the USGS State Geologic Map Compilation (Horton and others, 2017), the states’ geologic maps joined at a common scale. 1 smaller unit along the line are not listed.
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 Temescal Valley reaches the Pacific Ocean by way of Temescal Wash and the Santa Ana: about 50 river miles.
Often dry. About 70% of the way is mapped as streams that run only after rain or snowmelt; the water makes the whole trip in floods.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Temescal Valley; river miles along the main stem, rounded.
Temescal Valley has a hot semi-arid climate. Summer afternoons average 98° in August; winter nights fall to about 40° in December. About 12 inches of rain fall in a normal year.
On November 14 Temescal Valley normally reaches 74° and falls to 46°. The record high is 94°, in 1906; the record low 25°, in 1964. The most rain on this date, 0.97 in, fell in 1944.
Normals 1991–2020 and records since 1897 at Elsinore, 9 miles southeast, 120 ft higher. NOAA, through RCC-ACIS.
