Palm Spring Formation Stratigraphic range: Lower Pleistocene | |
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Type | Geologic formation |
Underlies | Vallecito Badlands |
Overlies | Imperial Formation, Ocotillo Formation |
Location | |
Region | Colorado Desert, California |
Country | United States |
The Palm Spring Formation is a Pleistocene Epoch geologic formation in the eastern Colorado Desert of Imperial County and San Diego County County, Southern California .
The Palm Spring Formation is an extensively-exposed delta-plain deposit debouched by the ancestral Colorado River across the subsiding Salton Trough.[1] It records the development of the prehistoric Colorado River delta cone into a barrier excluding marine waters from the Salton Trough.[2]
It preserves fossils from the Pleistocene Epoch, during the Quaternary Period of the Cenozoic Era.[3]
Lower Pliocene sub−period petrified wood is found in Anza-Borrego Desert State Park.[4] The Lauraceae is represented by petrified Umbellularia, the Salicaceae with petrified Populus and Salix, and the Juglandaceae with petrified Juglans.[4]
Original source: https://en.wikipedia.org/wiki/Palm Spring Formation.
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