Lomita Marl

Last updated
Lomita Marl
Stratigraphic range: Pleistocene
Type Geologic formation
Lithology
Primary Marl
Location
Region Los Angeles County,
Southern California
Country United States
Type section
Named for Lomita, California

The Lomita Marl is a geologic formation in Los Angeles County, southern California.

Los Angeles County, California County in California, United States

Los Angeles County, officially the County of Los Angeles, in the Los Angeles metropolitan area of the U.S. state of California, is the most populous county in the United States, with more than 10 million inhabitants as of 2017. As such, it is the largest non–state level government entity in the United States. Its population is larger than that of 41 individual U.S. states. It is the third-largest metropolitan economy in the world, with a Nominal GDP of over $700 billion—larger than the GDPs of Belgium, Norway, and Taiwan. It has 88 incorporated cities and many unincorporated areas and, at 4,083 square miles (10,570 km2), it is larger than the combined areas of Delaware and Rhode Island. The county is home to more than one-quarter of California residents and is one of the most ethnically diverse counties in the U.S. Its county seat, Los Angeles, is also California's most populous city and the nation's second largest city with about 4 million people.

California State of the United States of America

California is a state in the Pacific Region of the United States. With 39.6 million residents, California is the most populous U.S. state and the third-largest by area. The state capital is Sacramento. The Greater Los Angeles Area and the San Francisco Bay Area are the nation's second and fifth most populous urban regions, with 18.7 million and 9.7 million residents respectively. Los Angeles is California's most populous city, and the country's second most populous, after New York City. California also has the nation's most populous county, Los Angeles County, and its largest county by area, San Bernardino County. The City and County of San Francisco is both the country's second-most densely populated major city after New York City and the fifth-most densely populated county, behind only four of the five New York City boroughs.

It preserves Pleistocene fossils.

See also

Paleontology in California

Paleontology in California refers to paleontologist research occurring within or conducted by people from the U.S. state of California. California contains rocks of almost every age from the Precambrian to the Recent. Precambrian fossils are present but rare in California.


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Paleobiology Database

The Paleobiology Database is an online resource for information on the distribution and classification of fossil animals, plants, and microorganisms.

Annona Chalk geologic formation, Arkansas

The Annona Chalk is a geologic formation in Arkansas, Texas, Louisiana, and Oklahoma. It preserves fossils dating back to the Cretaceous period. The formation is a hard, thick-bedded to massive, slightly fossiliferous chalk. It weathers white, but is blue-gray when freshly exposed. The unit is commercially mined for cement. Fossils in the Annona Chalk include coelenterates, echinoderms, annelids, bivalves, gastropods, cephalopods, and some vertebrate traces. The beds range in thickness, up to over 100 feet in depth in some areas. There is a gradual transition between the Annona chalk and the underlying Brownstown formation, where chalk and marl are interbedded.

The Arkadelphia Marl is a geologic formation in Arkansas in Clark, Nevada, and Hempstead counties. It preserves fossils dating back to the Cretaceous period.

The White Bluff Formation is a marl, sand, and clay geologic formation in Arkansas that is part of the Jackson Group. It preserves fossils dating back to the Paleogene period, specifically the Eocene.

The Sharps Formation is a geologic formation in South Dakota. It preserves fossils dating back to the Paleogene period.

The Chatsworth Formation is a Cretaceous period sandstone geologic formation in the Simi Hills and western Santa Susana Mountains of southern California.

Punchbowl Formation

The Punchbowl Formation is a sedimentary sandstone geologic formation in the northern San Gabriel Mountains, above the Antelope Valley in Los Angeles County, southern California.

The Hungry Valley Formation is a geologic formation in the San Emigdio Mountains — near Gorman in northeastern Los Angeles County, California.

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.

The Mint Canyon Formation is a Miocene geologic formation in the Sierra Pelona Mountains of Los Angeles County, southern California.

The Towsley Formation is a geologic formation in the Santa Susana Mountains, in Los Angeles County, California.

The Topanga Canyon Formation is a Miocene epoch geologic formation in the Santa Monica Mountains, Simi Hills, Santa Ana Mountains and San Joaquin Hills, in Los Angeles County, Ventura County, and Orange County, southern California. It is primarily composed of hard sandstone with some inter-bedded siltstone.

The Santa Margarita Formation is a Neogene Period geologic formation in the San Joaquin Valley of central California.

The Llajas Formation is a non-marine to marine conglomerate geologic formation in Southern California.

The Martinez Formation is an Eocene Epoch geologic formation in California.

The Tecopa Lake Beds is a Blancan Pleistocene geologic formation in the Mojave Desert in eastern California. It is in the Tecopa area, east of Death Valley, in southeastern Inyo and northeastern San Bernardino County.

The Tick Canyon Formation is a Miocene epoch geologic formation in the Sierra Pelona Mountains of Los Angeles County, California.

References