Seismic monitoring at Lavic Lake Volcanic Field. Map of Mojave Trails National Monument - click to enlarge. Pisgah crater is the main feature, a prominent 100 m high cinder cone north of Lavic Lake surrounded by an 80 km2 basalt lava flow field. Of the three volcanoes discussed on this page, it is located the nearest to Southern California's city areas, being about 23 miles (37 km) from Barstow, and 50 miles (80 km) from San Bernardino. USGS Volcano Science Center Lavic Lake Volcanic Field monitoring: Monitoring. Lava flows extend 11 mi to the west and 5 to southeast of the cone. Mojave Trails contains a host of fascinating features, both geological and historical. These receivers are part of the 46 instruments that make up the network monitoring Long Valley Caldera. This lava flow is part of the Lavic Lake Volcanic Field in California's Mojave Desert. The lava field, at 1,495 m (4,905 ft) elevation, and its cones can be seen from historic Route 66 and from Interstate 40, between Barstow to the west and Needles to the east, and is located southeast of Ludlow, California. As of 2008, seismic monitoring is the most used technique for volcano surveillance. Mono Lake Volcanic Field The Mono Lake volcanic field east of Yosemite National Park and north of the Mono Craters consists of vents within Mono Lake and on its north shore. There are currently five GPS receivers that make up the continuous deformation monitoring network at Lavic Lake volcanic field. Pisgah Crater, a 100-m-high cinder cone, is the most prominent feature of the basaltic lava field. USGS Volcano Science Center Eagle Lake volcanic field monitoring: Monitoring. The Eagle Lake volcanic field occupies the junction of the Cascades, Sierra Nevada, and Basin and Range geologic provinces, and consists of 15 cinder cones and basaltic lava flow vents within a larger Quaternary basaltic field. "The Lavic Lake volcanic field was considered to contain four Holocene cinder cones, three in the Lavic Lake area and a fourth in the Rodman Mountains 20 km to the west (Miller 1989). The Lavic Lake basaltic volcanic field was considered to contain four Holocene cinder cones, three in the Lavic Lake area and a fourth in the Rodman Mountains 20 km to the west (Miller, 1989), but later work by USGS scientists revised that evaluation to late-Pleistocene. [1] This movement causes earthquakes that can be recorded with seismometers at the surface of the earth. It covers an area of about 400 km2 in Lake County and has been intensively studied since the early 1970’s. Pisgah Crater, a 100-m-high cinder cone, is the most prominent feature of the field. There may have been activity at this site as recent as 2,000 years ago; however others believe the last eruption occurred as early as 20,000 to 50,000 years ago. Lavic Lake The Lavic Lake volcanic field was considered to contain four Holocene cinder cones, three in the Lavic Lake area and a fourth in the Rodman Mountains 20 km to the west (Miller 1989). The Clear Lake volcanic field has been active for the last 2 million years. Pisgah Crater is located on the western side of the monument, just south of I 40 and west of the town of Ludlow.
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