| Mehrten Formation | |
|---|---|
| Stratigraphic range: Neogene | |
| Type | Formation |
| Location | |
| Region | California |
| Country | United States |
The Mehrten Formation is a geologic formation in California that is a type of inverted relief. It consists primarily of andesitic clastic and pyroclastic materials, deposited by volcanic activity that filled ancient rivers and valleys. Over time, the rock from these deposits proved more resistant to erosion than the surrounding land, leaving behind ridges that follow the paths of the former river channels, resembling inverted river meanders.
It was originally described in 1939 in Geology and Ground-Water Hydrology of the Mokelumne Area, California, Piper et. al.
Naturalist John Muir described the formation as "dead rivers" in his writings.
It preserves fossils dating back to the Neogene period.
See also
References
- Various Contributors to the Paleobiology Database. "Fossilworks: Gateway to the Paleobiology Database". Retrieved 17 December 2021.
- Geology and Ground-Water Hydrology of the Mokelumne Area, California. Retrieved 16 June, 2024.
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