Search results
Results from the WOW.Com Content Network
Pisgah Crater, or Pisgah Volcano, is a young volcanic cinder cone rising above a lava plain in the Mojave Desert, between Barstow and Needles, California in San Bernardino County, California. The volcanic peak is around 2.5 miles (4.0 km) south of historic U.S. Route 66 - National Old Trails Highway and of Interstate 40 , and west of the town ...
in Category:Volcanoes of California by county. It should hold all the pages in the county-level categories, and may hold other pages such as lists. It should hold all the pages in the county-level categories, and may hold other pages such as lists.
Map all coordinates using OpenStreetMap. ... California. Name Elevation Location ... Porcupine Mountains Central-Volcano: 595: 1,958
Conejo Mountain is a 1,814-foot-high mountain (553 m) in Ventura County, California, near Camarillo on the eastern boundary of the Oxnard Plain. [ 1 ] [ 2 ] [ 3 ] At the western edge of the Conejo Valley , it is adjacent to the Santa Monica Mountains .
Clear Lake Volcanic Field; Highest point; Elevation: 4,724 ft (1,440 m) [1] Coordinates: 2]: Geography; Location: Lake County, California, United States: Parent range: North Coast Ranges: Topo map: USGS Kelseyville: Geology; Rock age: less than 2.1 million years [3]: Mountain type(s): lava domes, cinder cones, maars within volcanic field [2]: Last eruption: Holocene [2]: Geologic map of the ...
Davidson Seamount is a seamount (underwater volcano) located off the coast of Central California, 80 mi (129 km) southwest of Monterey and 75 mi (121 km) west of San Simeon. At 26 mi (42 km) long and 8 mi (13 km) wide, it is one of the largest known seamounts in the world. [ 4 ]
Mount Konocti / k oʊ ˈ n ɒ k t aɪ / is a volcano in Lake County, California on the south shore of Clear Lake.At 4,305 feet (1,312 m), it is the second highest peak in the Clear Lake Volcanic Field, which consists of numerous volcanic domes and cones ranging from 10,000 to 2.1 million years old.
Round Top, north aspect. Round Top is the remnant of a volcano that formed in the Miocene epoch, which lasted from c. 23 million years ago to c. 5 million years ago. Most of the mountain's vertical height consists of an intrusive [5] volcanic plug [6]: 3 formed of basaltic andesite. [5]