The Tick Canyon Formation (Tt) or Tick Canyon strata, is an
Early Miocene
The Early Miocene (also known as Lower Miocene) is a sub-epoch of the Miocene Epoch made up of two stages: the Aquitanian and Burdigalian stages.
The sub-epoch lasted from 23.03 ± 0.05 Ma to 15.97 ± 0.05 Ma (million years ago). It was p ...
geologic formation
A geological formation, or simply formation, is a body of rock having a consistent set of physical characteristics ( lithology) that distinguishes it from adjacent bodies of rock, and which occupies a particular position in the layers of rock exp ...
in the
Sierra Pelona Ridge
The Sierra Pelona, also known as the Sierra Pelona Ridge or the Sierra Pelona Mountains, is a mountain ridge in the Transverse Ranges in Southern California. Located in northwest Los Angeles County, the ridge is bordered on the north by the San ...
of the
San Gabriel Mountains
The San Gabriel Mountains ( es, Sierra de San Gabriel) are a mountain range located in northern Los Angeles County and western San Bernardino County, California, United States. The mountain range is part of the Transverse Ranges and lies between ...
in
Los Angeles County, California
Los Angeles County, officially the County of Los Angeles, and sometimes abbreviated as L.A. County, is the most populous county in the United States and in the U.S. state of California, with 9,861,224 residents estimated as of 2022. It is th ...
.
[ Elsmerecanyon.com: "Tick Canyon Geology"]
/ref>
The Tick Canyon Basin drains into the Santa Clara River.
Geology
The formation overlies the Oligocene
The Oligocene ( ) is a geologic epoch of the Paleogene Period and extends from about 33.9 million to 23 million years before the present ( to ). As with other older geologic periods, the rock beds that define the epoch are well identified but ...
to Lower Miocene
The Early Miocene (also known as Lower Miocene) is a sub-epoch of the Miocene Epoch made up of two stages: the Aquitanian and Burdigalian stages.
The sub-epoch lasted from 23.03 ± 0.05 Ma to 15.97 ± 0.05 Ma (million years ago). It was prec ...
Vasquez Formation
The Vasquez Formation (Tvz) is a geologic formation cropping out at the eponymous Vasquez Rocks in southern California. The formation dates to the Late Oligocene to Early Miocene ( Arikareean in the NALMA classification).
Description
The V ...
, and underlies the Upper Miocene
The Late Miocene (also known as Upper Miocene) is a sub-epoch of the Miocene Epoch made up of two stages. The Tortonian and Messinian stages comprise the Late Miocene sub-epoch, which lasted from 11.63 Ma (million years ago) to 5.333 Ma.
The ...
Mint Canyon Formation
The Mint Canyon Formation (Tm) is a Miocene geologic formation in the Sierra Pelona Mountains of Los Angeles County, southern California. The formation preserves fossils dating back to the Middle to Late Miocene ( Barstovian and Clarendonian ...
.[
The Tick Canyon strata was deposited on land mostly by streams and consists of green ]sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks.
Most sandstone is composed of quartz or feldspar (both silicates ...
s, coarse-grained conglomerates, and red claystone
Mudrocks are a class of fine-grained siliciclastic sedimentary rocks. The varying types of mudrocks include siltstone, claystone, mudstone, slate, and shale. Most of the particles of which the stone is composed are less than and are too sm ...
s.[ Caltech.edu: THESIS - "Geology of the Upper Tick Canyon area, California"]
Birman, Joseph Harold; 1950.Caltech.edu: THESIS - "Geology of the Mint Canyon area, Los Angeles County, California"
Holser, William T.; 1946 The Tick Canyon strata also contain abundant volcanic clasts, most of which resemble volcanic rocks of the Vasquez Formation.[Coffey et al., 2019, p.481] It has an average thickness of .[
North of the Tick Canyon Fault, the beds are almost vertical.][
]
Fossil content
It preserves vertebrate fossils
A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved ...
of the Lower Miocene
The Early Miocene (also known as Lower Miocene) is a sub-epoch of the Miocene Epoch made up of two stages: the Aquitanian and Burdigalian stages.
The sub-epoch lasted from 23.03 ± 0.05 Ma to 15.97 ± 0.05 Ma (million years ago). It was prec ...
subperiod of the Miocene epoch, in the Neogene Period of the Cenozoic Era
The Cenozoic ( ; ) is Earth's current geological era, representing the last 66million years of Earth's history. It is characterised by the dominance of mammals, birds and flowering plants, a cooling and drying climate, and the current configu ...
.[Tick Canyon]
at Fossilworks
Fossilworks is a portal which provides query, download, and analysis tools to facilitate access to the Paleobiology Database, a large relational database assembled by hundreds of paleontologists from around the world.
History
Fossilworks was cre ...
.org
Mammals
* Artiodactyl
The even-toed ungulates (Artiodactyla , ) are ungulates—hoofed animals—which bear weight equally on two (an even number) of their five toes: the third and fourth. The other three toes are either present, absent, vestigial, or pointing poste ...
s
** '' Miolabis californicus''[
** '' Merychyus calaminthus''][Lander & Lindsay, 2011]
** '' M. minimus''[Whistler, 1967]
* Perissodactyl
Odd-toed ungulates, mammals which constitute the taxonomic order Perissodactyla (, ), are animals—ungulates—who have reduced the weight-bearing toes to three (rhinoceroses and tapirs, with tapirs still using four toes on the front legs) ...
s
** '' Parahippus maxsoni''[Jahns, 1940]
** '' Parahippus sp.''[Maxson, 1930]
* Rodent
Rodents (from Latin , 'to gnaw') are mammals of the Order (biology), order Rodentia (), which are characterized by a single pair of continuously growing incisors in each of the upper and lower jaws. About 40% of all mammal species are roden ...
s
** '' Archaeolagus acaricolus''[Dawson, 1958]
** '' Trogomys rupinimenthae''[Reeder, 1960]
Birds
* Falconiformes
The order Falconiformes () is represented by the extant family Falconidae (falcons and caracaras) and a handful of enigmatic Paleogene species. Traditionally, the other bird of prey families Cathartidae (New World vultures and condors), Sagit ...
** '' Miohierax stocki''[Howard, 1944]
See also
* List of fossiliferous stratigraphic units in California
This article contains a list of fossil-bearing stratigraphic units in the state of California, U.S.
Sites
See also
* Paleontology in California
References
*
{{DEFAULTSORT:Fossiliferous stratigraphic units in California
California
S ...
* 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 pres ...
* Goliad Formation
* Plush Ranch Formation
The Plush Ranch Formation is a Formation (geology), 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 North American land mammal ...
* Punchbowl Formation
* Shoal River Formation
The Shoal River Formation is a geologic formation in Florida. The sandstones and marls of the formation preserve fossils dating back to the Serravallian epoch of the Middle Miocene of the Neogene period.Pineda Salgado et al., 2016
References
Bibliography
*
*
*
*
*
*
*
* {{cite LSA , last=Maxson , first=J. H , year=1930 , title=A Tertiary mammalian fauna from the Mint Canyon Formation of Southern California , journal= Carnegie Institution of Washington Publication , volume=404 , pages=77–112
Further reading
* Geology of Tick Canyon, by Ygnacio Bonillas, 1933
* Geology of the Upper Tick Canyon Area, by Albert Hedden, 1948
* Geology of the Upper Tick Canyon Area, by Joseph Birman, 1950
* Geology of the Upper Tick Canyon Area, by Carel Otte, Jr., 1950
Geologic formations of California
Miocene California
Miocene Series of North America
Burdigalian
Barstovian
Hemingfordian
Sandstone formations of the United States
Shale formations of the United States
Conglomerate formations
Fluvial deposits
Paleontology in California
Geology of Los Angeles County, California
Sierra Pelona Ridge