Blackshare Formation | |
---|---|
Stratigraphic range: Miocene, | |
Type | Formation |
Unit of | Santa Fe Group |
Underlies | Tuerto Formation |
Overlies | Tanos Formation |
Thickness | Over 1,260 m (4,130 ft) |
Lithology | |
Primary | Sandstone, conglomerate |
Other | Mudstone |
Location | |
Coordinates | 35°25′05″N106°18′25″W / 35.418°N 106.307°W |
Region | New Mexico |
Country | United States |
Type section | |
Named for | Blackshare Ranch |
Named by | S.D. Connell and S.M. Cather |
Year defined | 2002 |
The Blackshare Formation is a geologic formation exposed in the Hagan Basin west of the Ortiz Mountains of New Mexico. It is estimated be to of Miocene age. [1] [2] [3]
The Blackshare Formation consists primarily of sandstone and conglomerate with minor mudstone. The conglomerate forms lenticular bodies, with clasts consisting mostly of Ortiz porphyry with small amounts of hornfels and chert. The sandstone layers tends to be more coarse at their base. The dip of the beds (which is to the northeast) decreases from 16 degrees to 1 degree from the base to the top of the formation. Paleocurrents confirm deposition by stream flow from the Ortiz Mountains to the east. The total thickness is over 1,260 meters (4,130 ft).
The formation is divided into four informal members, described as a sandstone facies, a conglomeratic sandstone facies, a conglomerate facies, and a muddy sandstone facies. The formation interfingers with the underlying Tanos Formation and is overlain with angular unconformity by the Tuerto Formation. [1]
An ash bed about 200 meters (660 ft) below the top of the formation has a radiometric age of 11.65 ± 0.38 million years (Ma). [1]
The formation is interpreted as deposition by streams flowing from the east into a closed basin. [1] The progressive tilting of the beds, with the lower beds showing significant dip while the uppermost are nearly horizontal, may be connected to the uplift of the Sandia Mountains to the south while the sediments making up the formation were being deposited. [4]
The beds making up this formation were first assigned to the Santa Fe Formation by Stearns in 1953. [5] They were designated as the Blackshare Formation of the Santa Fe Group by Connell et al. in 2002. [1]
The Caballo Mountains, are a mountain range located in Sierra and Doña Ana Counties, New Mexico, United States. The range is located east of the Rio Grande and Caballo Lake, and west of the Jornada del Muerto; the south of the range extends into northwest Doña Ana County. The nearest towns are Truth or Consequences and Hatch.
The Camp Rice Formation is a geologic formation in west Texas and southern New Mexico. It preserves fossils of the Pliocene-Pleistocene. These include the distinctive Tonuco Mountain Local Fauna.
The Palomas Formation is a geologic formation exposed in the southern Rio Grande rift of New Mexico. It preserves fossils dating back to the Pliocene to Quaternary.
The Abiquiu Formation is a geologic formation found in northern New Mexico. Radiometric dating constrains its age to between 18 million and 27 million years, corresponding to the late Oligocene to Miocene epochs.
The Popotosa Formation is a geologic formation in New Mexico. It preserves fossils dating back to the Neogene period. These include the Socorro flora, notable for its fine preservation of plant reproductive structures.
The Rincon Valley Formation is a geologic formation found in the Rincon Valley of New Mexico. It preserves fossils dating back to the Miocene epoch and records a time when the valley was a closed basin, just before being integrated into the ancestral Rio Grande River.
The Tesuque Formation is a geologic formation in north-central New Mexico, United States. The formation provides an unusually complete record of the evolution of mammals during the Miocene epoch.
The Zia Formation is a geologic formation in the southwestern Jemez Mountains and northwestern Santo Domingo basin. It contains vertebrate fossils that date it to early to middle Miocene in age.
The Galisteo Formation is a geologic formation in New Mexico. It contains fossils characteristic of the Bartonian stage of the Eocene epoch, Duchesnean in the NALMA classification.
The geology of New Mexico includes bedrock exposures of four physiographic provinces, with ages ranging from almost 1800 million years (Ma) to nearly the present day. Here the Great Plains, southern Rocky Mountains, Colorado Plateau, and Basin and Range Provinces meet, giving the state great geologic diversity.
The Espinaso Formation is a geologic formation in New Mexico. It has a radiometric age of 34.6 to 26.9 million years, corresponding to the late Eocene through Oligocene epochs.
The Santa Fe Group is a group of geologic formations in New Mexico and Colorado. It contains fossils characteristic of the Oligocene through Pleistocene epochs. The group consists of basin-filling sedimentary and volcanic rocks of the Rio Grande rift, and contains important regional aquifers.
The El Rito Formation is a geologic formation in New Mexico dating to the Eocene epoch. It records a time when sediments were trapped in deep basins in western North America rather than being carried downstream to the Gulf of Mexico, so that sediments of this age in the western Gulf are mostly from the Appalachian Mountains.
The Tanos Formation is a geologic formation in central New Mexico. It is estimated to be about 25 million years in age, corresponding to the Oligocene epoch.
The Arroyo Ojito Formation is a late Miocene geologic formation exposed near Albuquerque, New Mexico. It records deposition of sediments in the Albuquerque Basin of the Rio Grande Rift after full integration of the Rio Grande through the basin.
The Tuerto Formation is a geologic formation exposed around the Ortiz Mountains of New Mexico. It is estimated to be of Pliocene to Pleistocene age, and forms the gravel cap of the Ortiz surface, one of the first pediment surfaces recognized by geologists.
The Cerro Conejo Formation is a middle to late Miocene geologic formation exposed near Albuquerque, New Mexico.
The Ceja Formation is a Pliocene to Pleistocene geologic formation exposed near Albuquerque, New Mexico.
The Hayner Ranch Formation is a geologic formation found near the San Diego Mountains of New Mexico. It is estimated to have been deposited during the Miocene epoch.
The Picuris Formation is a geologic formation exposed in the eastern flank of the Rio Grande rift in northern New Mexico. It was deposited from the late Eocene to Miocene epochs.