The Spring 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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3.00 inches of rain fell in two days, the most for this week of the year since records began in 1899. The next wettest, 2.34 inches, fell in 1944.
Spring Valley’s center stands about 390 ft above sea level. Within three miles the land runs from 240 ft to 980 ft, a difference of 740 ft: hilly country. The highest named summit within 15 miles is Lyons Peak, about 3,690 ft, 14 miles east-southeast.
Under the town center the state geologic map shows Eocene nonmarine rocks, unit 2 (Southern California) (conglomerate, sandstone), from the Middle Eocene to Late Eocene, 34 to 48 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 17×. 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 6 mi of the line.
Conglomerate, sandstone. Age: Middle Eocene to Late Eocene, 34 to 48 million years old. About 5 mi of the line.
Coarse-detrital. Age: Pleistocene to Holocene, less than 2.6 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.
Schist, gneiss. Age: Paleoproterozoic to Cretaceous, 66 to 2,500 million years old. About 2 mi of the line.
Sandstone, mudstone. Age: Miocene to Pleistocene, less than 23 million years old. About 2 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 Spring Valley reaches the Pacific Ocean by way of the Sweetwater: about 12 river miles.
Often dry. About 60% 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 Spring Valley; river miles along the main stem, rounded.
Spring Valley has a hot semi-arid climate. Summer afternoons average 89° in August; winter nights fall to about 42° in December. About 12 inches of rain fall in a normal year.
On November 14 Spring Valley normally reaches 76° and falls to 48°. The record high is 98°, in 1906; the record low 25°, in 1916. The most rain on this date, 1.07 in, fell in 1950.
Normals 1991–2020 and records since 1899 from the El Cajon Area threaded record (El Cajon, 6 miles northeast, 100 ft higher). NOAA, through RCC-ACIS.
