Lavic Lake

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  • Country
  • Subregion Name
  • Primary Volcano Type
  • Last Known Eruption
  • 34.75°N
  • 116.625°W

  • 1495 m
    4904 ft

  • 323190
  • Latitude
  • Longitude

  • Summit
    Elevation

  • Volcano
    Number

There are no activity reports for Lavic Lake.



 Available Weekly Reports

There are no Weekly Reports available for Lavic Lake.

There are no Holocene eruptions known for Lavic Lake. If this volcano has had large eruptions prior to 10,000 years ago, information might be found in the LaMEVE (Large Magnitude Explosive Volcanic Eruptions) database, a part of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).

The following references are the sources used for data regarding this volcano. References are linked directly to our volcano data file. Discussion of another volcano or eruption (sometimes far from the one that is the subject of the manuscript) may produce a citation that is not at all apparent from the title. Additional discussion of data sources can be found under Volcano Data Criteria.

Bassett A M, Kupfer D H, 1964. A geologic reconnaissance in the southeastern Mojave Desert, California. Calif Div Mines Geol Spec Rpt, 83: 1-43.

Chesterman C W, 1971. Volcanism in California. Calif Geol, 24: 139-147.

Luedke R G, Smith R L, 1981. Map showing distribution, composition, and age of late Cenozoic volcanic centers in California and Nevada. U S Geol Surv Map, I-1091-C.

Miller C D, 1989. Potential hazards from future volcanic eruptions in California. U S Geol Surv Bull, 1847: 1-17.

Reid M, 2002. . (pers. comm.).

Smith R L, Shaw H R, 1975. Igneous-related geothermal systems. U S Geol Surv Circ, 726: 58-83.

Wood C A, Kienle J (eds), 1990. Volcanoes of North America. Cambridge, England: Cambridge Univ Press, 354 p.

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). Pisgah Crater, a 100-m-high cinder cone, is the most prominent feature of the basaltic lava field. Nearby vents were the source of dominantly pahoehoe lava flows that traveled 8 km SE to Lavic Lake and in a narrow lobe over that traveled over alluvial-fan and playa-lake deposits as far as 18 km west of the vent. More recent work indicates a convergence of dates for Pisgah Crater from paleomagnetic, argon-argon, and cosmogenic helium at about 25,000 years BP (Reid 2002, pers. comm.). Another very youthful looking, but undated cinder cone and lava field of the Lavic Lake volcanic field is located in the Sunshine Peak area of the Lava Beds Mountains, south of the better known Pisgah Crater.