Английская Википедия:Crowder Formation

Материал из Онлайн справочника
Версия от 14:32, 22 февраля 2024; EducationBot (обсуждение | вклад) (Новая страница: «{{Английская Википедия/Панель перехода}} {{Infobox rockunit | name = Crowder Formation | image = | caption = | type = Geologic formation | age = Pliocene | period = Pliocene | prilithology = | otherlithology = | namedfor = | namedby = | region = Mojave Desert,<br>in San Gabriel Mountains and San Bernardino Mountains,<br>Los An...»)
(разн.) ← Предыдущая версия | Текущая версия (разн.) | Следующая версия → (разн.)
Перейти к навигацииПерейти к поиску

Шаблон:Infobox rockunit

The Crowder Formation is a geologic formation in the Central and Western Mojave Desert, in northern Los Angeles County and eastern San Bernardino County, in Southern California.[1]

Areas where it is exposed include at the bases of the northern San Gabriel Mountains and northwestern San Bernardino Mountains, and in the Cajon Pass between them.[1][2][3]

Geology

The Crowder Formation was formed during the Pliocene epoch of the Neogene period.[1][2] The formation was deposited by drainages carrying distinctive volcanic and metamorphic clasts from the Victorville area southward.[3]

It overlies the crystalline San Gabriel Basement Complex in its eastern section, and the San Francisquito Formation in its western section in the Antelope Valley/San Gabriels.Шаблон:Citation needed

Fossils

The formation preserves fossils of insects, reptiles, rodents, birds, and larger mammals. The species date back to the Miocene and Pliocene epochs of the Neogene period.[4] 29 taxa were collected by the San Bernardino County Museum from the Cajon Pass area of the Crowder Formation.[2]

See also

Шаблон:Portal

References

Шаблон:Reflist

  • "The Physical and Magnetic Stratigraphy of the Miocene Crowder Formation, Cajon Pass, Southern California"; by Douglas Scott Winston, University of Southern California; Los Angeles, 1985.

Шаблон:Neogene Footer


Шаблон:California-geologic-formation-stub Шаблон:Neogene-stub