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Cima volcanic field is a volcanic field in San Bernardino County, California, close to the border with Nevada. The volcanic field covers a surface area of within the Mojave National Preserve west of the Cima Dome and consists of about 40 with about 60 lava flows. The volcanic cones range from simple cones over multi-cratered mountains to eroded hills, and lava flows are up to long. At least one lava tube exists in the field and can be visited.
Volcanic activity in the field commenced in the Late Miocene and after a pause between 3 and 1 million years ago continued into the latest Pleistocene. The youngest cone is known as the Black Tank cone and formed about 15,000 years before present, although it is possible that it was formed through two separate eruption events; formerly it was considered to be of historical age.
Interstate 15 passes north of the field and just south of older volcanic units, while California State Route 127 runs west and southwest of the field, The city of Las Vegas is northeast of the area. The Cima volcanoes are part of the Mojave National Preserve and since 1973 they make up the Cinder Cones National Natural Landmark.
During the Holocene and until recent times, humans engraved into the lava flows. One cinder cone was quarry to obtain materials for road construction. The volcanic field has been the subject of and landscape development research.
Generally, volcanic activity was widespread in the dry regions of the western United States during the Tertiary period and Quaternary, forming several volcanic fields. An earlier phase of felsic volcanism during the Tertiary was followed during the Quaternary by more basaltic volcanism, often in the form of short-lived volcanic vents. Examples of this kind of volcanism are the Cima volcanic field, the San Francisco volcanic field (Arizona), the Southwest Nevada volcanic field (Nevada) and the Zuni-Bandera volcanic field (New Mexico).
The Cima volcanic field is part of the Mojave Desert, which in turn belongs to the Basin and Range Province and features both mountains exceeding height which trend in southeast–northwest direction, with broad valleys between the mountains. Other volcanoes there include Dish Hill, Amboy Crater and Pisgah Crater.
The youngest cone () in the southwestern part of the field is called Black Tank cone. The Black Tank cone is the source of a long lava flow, which at first forms a levee-bound channel and then narrows out into a lobate shape. It also shows traces of a lava tube and has a volume of . This flow may have been preceded by a previous lava flow which was later buried by the main flow. An older vent lies just south-southwest of the Black Tank Cone.
The field presents black and red volcanic rocks in the form of Scoria, exposed feeder dikes and , as well as Agglutination which are exposed in gullies and eroded vents. Bombs and cinders cover the less eroded cones, which are also sometimes surrounded by base surge deposits. At some vents, formed through phreatomagmatic activity. Erosion has dug gullies and larger valleys in the older cones, including one deep gorge.
Volcanic material covers a surface area of about within an area of . The volcanic field was emplaced on a basement of Tertiary age, which comprises both crystalline bedrock and thick gravel deposits. Other rock formations in the area are of ProterozoicPaleozoic to Mesozoic (Teutonia batholith) age, and the region is considered to be part of the Ivanpah uplift.
Younger flows often show crisp lava flow features while older flows are almost always mantled with younger material and have lost their original surface features. The oldest flows have flat or gentle surfaces and their source vents are heavily degraded. Lava flows are also in part covered by wind-transported or erosional material and desert varnish.
The magma erupted in the field ultimately appears to originate from the lithospheric or Asthenosphere mantle with little contribution of crustal components, unlike earlier felsic volcanism. Upwelling of asthenosphere material appears to be responsible for the volcanism at the end, possibly associated with the change in the tectonics of the region from subduction-dominated to tectonics of a transform boundary. Fractional crystallization, magma ponding in the crust, differences in the mantle sources and partial melting processes have been invoked to explain certain compositional differences in the erupted rocks. Xenoliths indicate that magma ascent to the surface is rapid, with no stalling, and processes of magma formation to surface eruption take only a few days.
Vegetation in the area is classified as shrubland, with plants including brittle bush, creosote bush, Mormon tea and white bursage. grow at higher elevations. Some of these species arrived during the Holocene, while others became established during the Pleistocene or appeared and disappeared repeatedly. Vegetation grows in clusters separated by soil covered by desert pavement. The youngest cone is unvegetated and little vegetation has developed on other recent volcanic vents and lava flows.
According to potassium-argon dating, volcanic activity started in the Miocene and continued to the end of the Pleistocene. Activity has been subdivided into five phases, the first between 7.6 and 6.5 million years ago, the second between 5.1 and 3.6 million years ago, the third between 1.1 and 0.6 million years ago, the fourth between 750,000 and 200,000 years ago and the fifth and last between 200,000 and 10,000 years ago. The radiometric ages have been corroborated by morphological and paleomagnetic information. Volcanic activity paused between 3 and 1 million years ago.
The oldest volcanic phase left a heavily dissected volcano in the southeastern part of the field, while the subsequent phase involved lava flows in the northern part of the field that take the form of eroded . The final three phases formed lava flows and the volcanoes in the southern part of the field. Eruptions commenced as maar-forming eruptions and continued with the growth of and lava flows. Unlike regular cinder cones which usually erupt only once, some cones at Cima experienced more than one eruption and were active over hundreds of thousands of years.
The Black Tank cone, the youngest cone in the field, has been dated to 15,000 ± 5,000 years before present by several methods. Some evidence suggested a historical age for one of the southern lava flows, with earlier radiocarbon dating yielding an age of 330–480 years. Several chronological data imply that the lava flow was formed during two separate eruptive episodes, one 20,000 years ago and the other 11,500 - 13,000 years ago. The lava flow was probably laid down in less than a week of time, and the growth of the cone was influenced by wind, which transported tephra east-southeastwards where it fell out and formed a tephra blanket.
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