Plush_Ranch_Formation
The Plush Ranch Formation is a geologic formation in the Transverse Ranges of southern California. The formation preserves fossils dating back to the Late Oligocene to Early Miocene (Arikareean in the NALMA classification).
| Plush Ranch Formation | |
|---|---|
| Stratigraphic range: Late Oligocene-Early Miocene (Arikareean) ~27–20.4 Ma | |
| Type | Formation |
| Underlies | Caliente Formation (unconformably) |
| Overlies | Basement (unconformably) |
| Lithology | |
| Primary | Conglomerate, sandstone, siltstone, shale |
| Other | Limestone, evaporite, interbedded basalt |
| Location | |
| Coordinates | 34.8°N 119.1°W / 34.8; -119.1 |
| Approximate paleocoordinates | 33.8°N 113.6°W / 33.8; -113.6 |
| Region | California |
| Country |  United States |
| Extent | Plush Ranch Basin, Transverse Ranges |
| Type section | |
| Named for | Plush Range |
| Named by | Carman |
| Year defined | 1954 |
The formation is the oldest non-marine unit of the Tejon region where the small Plush Ranch Basin is formed by the bounding Big Pine/Lockwood Valley and San Andreas Faults. The unit is composed of alluvial and lacustrine conglomerates, sandstones, siltstones, shales, limestones, and evaporites. Interbedded basalt has been dated by whole-rock and plagioclase K-Ar methods as ca. 26–23 Ma. Northwest of Plush Ranch Basin, on the opposite side of Mount Pinos (which includes exposures of Pelona Schist), Oligocene–Miocene strata are generally mapped as Simmler Formation, but are considered equivalent to the Plush Ranch Formation. These strata coarsen upward, from mostly sandstone at the base to coarse conglomerate at the top.[1]
The lacustrine deposits represent the central and eastern parts of the Plush Ranch basin, which received little coarse siliciclastic sediment. Chironomid flies, disarticulated fish, and coprolites indicate a more or less permanent lake.[2]
Atop the Plush Ranch Formation, separated by an angular unconformity, there is the non-marine Caliente Formation, comprising fluvial and lacustrine conglomerate, sandstone, and mudstone, with minor tuffaceous and limestone beds.[1]
The following fossils have been reported from the formation:[3]
- Insects
- Coffey et al., 2019, p.480
- Snyder, 1955
Bibliography
- Coffey, Kevin T.; Ingersoll, Raymond V.; Schmitt, Axel K. (2019). "Stratigraphy, provenance, and tectonic significance of the Punchbowl block, San Gabriel Mountains, California, USA". Geosphere. 15 (2): 479–501. Bibcode:2019Geosp..15..479C. doi:10.1130/GES02025.1.
- Snyder, T. E (1955). "A new fossil termite, Parastylotermes frazieri, from California (Isoptera, Rhinotermitidae)". Proceedings of the Entomological Society of Washington. 57: 79–80.