California landslides

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Landslides in California occur mainly due to intense rainfall but occasionally are triggered by earthquakes. Landslides are common in Southern California, the San Francisco Bay Area and other parts of Northern California, and the Sierra Nevada. Although they most often are reported when they impact residential developments, landslides also damage roads, railroads, pipelines, electrical lines, and other infrastructure throughout the state, and occur in unoccupied parts of the state.

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California Geological Survey

CGS is California's primary source of geologic and seismologic products and services for decision making by California's government agencies, its businesses and the public. [1] Since the 1960s, when it was known as the California Division of Mines and Geology, CGS has produced many maps that depict landslide features and potential slope-failure areas. CGS products have included geologic maps and reports for land-use planning, landslide hazard identification maps, watershed maps, and earthquake-triggered landslide-zone maps. Many of these maps were advisory in nature: cities and counties could choose to use or ignore them. [2] However, watershed maps are routinely used in the review of timber harvest plans outside federally owned lands. [3] CGS has a legislatively mandated Seismic Hazards Zonation Program that produces regulatory maps areas where the probability of liquefaction and earthquake-triggered landslides are significant enough to require site evaluation prior to most developments. [2]

Landslide maps in California and laws and regulations

The State of California Department of Conservation produces regulatory maps showing locations where the hazard from earthquake-triggered landslides must be evaluated prior to specific types of land-use development in accordance with provisions of Public Resources Code, Section 2690 et seq. (Seismic Hazards Mapping Act). These maps and related products incorporate evaluations of probabilistic ground shaking and existing geologic conditions. Recently released landslide inventory and related hazard zone maps are available free from the CGS website. [4] Watershed maps, used in the review of timber harvest plans (regulated by the California Department of Forestry) are available for downloading in PDF and GIS data formats. [5]

From 1983 through 1994, CGS was directed to produce Landslide Hezard Identification Maps under the State's Landslide Hazard Identification Act. Though of high quality and designed for land-use planning purposes, the Act did not require local governments to use the maps. The Act was repealed January 1, 1995 per a sunset provision in the Act. [2] Those maps, and many older non-regulatory landslide-related products are available for purchase from CGS offices and/or available for download from the CGS website.

List of historic California landslides

See also

Related Research Articles

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An earthquake – also called a quake, tremor, or temblor – is the shaking of the Earth's surface resulting from a sudden release of energy in the lithosphere that creates seismic waves. Earthquakes can range in intensity, from those so weak they cannot be felt, to those violent enough to propel objects and people into the air, damage critical infrastructure, and wreak destruction across entire cities. The seismic activity of an area is the frequency, type, and size of earthquakes experienced over a particular time. The seismicity at a particular location in the Earth is the average rate of seismic energy release per unit volume.

<span class="mw-page-title-main">San Andreas Fault</span> Geologic feature in California

The San Andreas Fault is a continental right-lateral strike-slip transform fault that extends roughly 1,200 kilometers (750 mi) through the U.S. state of California. It forms part of the tectonic boundary between the Pacific plate and the North American plate. Traditionally, for scientific purposes, the fault has been classified into three main segments, each with different characteristics and a different degree of earthquake risk. The average slip rate along the entire fault ranges from 20 to 35 mm per year.

<span class="mw-page-title-main">1971 San Fernando earthquake</span> Earthquake in California

The 1971 San Fernando earthquake occurred in the early morning of February 9 in the foothills of the San Gabriel Mountains in southern California. The unanticipated thrust earthquake had a magnitude of 6.5 on the Ms scale and 6.6 on the Mw scale, and a maximum Mercalli intensity of XI (Extreme). The event was one in a series that affected Los Angeles County during the late 20th century. Damage was locally severe in the northern San Fernando Valley and surface faulting was extensive to the south of the epicenter in the mountains, as well as urban settings along city streets and neighborhoods. Uplift and other effects affected private homes and businesses.

The Alquist-Priolo Earthquake Fault Zoning Act was signed into California law on December 22, 1972, to mitigate the hazard of surface faulting to structures for human occupancy.

<span class="mw-page-title-main">Hayward Fault Zone</span> Geological fault in the San Francisco Bay Area

The Hayward Fault Zone is a right-lateral strike-slip geologic fault zone capable of generating destructive earthquakes. The fault was first named in the Lawson Report of the 1906 San Francisco Earthquake in recognition of its involvement in the earthquake of 1868. This fault is about 119 km (74 mi) long, situated mainly along the western base of the hills on the east side of San Francisco Bay. It runs through densely populated areas, including Richmond, El Cerrito, Berkeley, Oakland, San Leandro, Castro Valley, Hayward, Union City, Fremont, and San Jose.

<span class="mw-page-title-main">California Geological Survey</span> California state geologic agency

The California Geological Survey, previously known as the California Division of Mines and Geology, is the California state geologic agency.

<span class="mw-page-title-main">Coyote Creek (Santa Clara County)</span> Creek in California, United States

Coyote Creek is a river that flows through the Santa Clara Valley in Northern California. Its source is on Mount Sizer, in the mountains east of Morgan Hill. It eventually flows into Anderson Lake in Morgan Hill and then northwards through Coyote Valley to San Jose, where it empties into San Francisco Bay.

<span class="mw-page-title-main">Bruce Bolt</span> Seismologist and academic

Bruce Bolt was an Australian-born American seismologist and a professor of earth and planetary science at the University of California, Berkeley. Professor Bolt was known as a pioneer of seismic engineering. He served for 15 years on the California Seismic Safety Commission leading public debate on earthquake safety in that state, and acted as a consultant on major projects throughout the world. As well, Bolt published a number of popular and technical books on seismology.

<span class="mw-page-title-main">Berkeley Hills</span> Region of the Pacific Coast Ranges

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The California Department of Conservation is a department within the government of California, belonging to the California Natural Resources Agency. With a team of scientists, engineers, environmental experts, and other specialists, the Department of Conservation administers a variety of programs vital to California's public safety, environment and economy. The department's mission is to manage California's working lands. It regulates oil, natural gas and geothermal wells; studies and maps earthquakes and other geologic phenomena; maps and classifies areas containing mineral deposits; ensures reclamation of land used for mining; and administers agricultural and open-space land conservation programs. A division within the department dedicated to encouraging beverage container recycling has been moved into the newly created Department of Resources Recovery and Recycling (CalRecycle). Despite the similar name, the Department of Conservation should not be confused with the California Conservation Corps, another department within the Natural Resources Agency, which provides work experience for young adults. The Department of Conservation often collaborates with its federal equivalents, such as the U.S. Geological Survey.

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The United States Geological Survey (USGS), founded as the Geological Survey, is an agency of the U.S. Department of the Interior whose work spans the disciplines of biology, geography, geology, and hydrology. The agency was founded on March 3, 1879, to study the landscape of the United States, its natural resources, and the natural hazards that threaten it. The agency also makes maps of extraterrestrial planets and moons based on data from U.S. space probes.

The 1992 Cape Mendocino earthquakes occurred along the Lost Coast of Northern California on April 25 and 26. The three largest events were the M7.2 thrust mainshock that struck near the unincorporated community of Petrolia midday on April 25 and two primary strike-slip aftershocks measuring 6.5 and 6.6 that followed early the next morning. The sequence encompassed both interplate and intraplate activity that was associated with the Mendocino triple junction, a complex system of three major faults that converge near Cape Mendocino. The total number of aftershocks that followed the events exceeded 2,000.

<span class="mw-page-title-main">Hazard map</span> Visualization of vulnerable areas

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Kate E. Allstadt is a geologist and seismologist employed by the U.S. Geological Survey (USGS) who works out of Golden, Colorado. She is a self-described "present-day geologist" for her interest in connections between geology of the Pacific Northwest and the people in its local communities. She is a published expert on the 2014 Oso landslide.

References

  1. "Welcome to the California Geological Survey". California Geological Survey. Retrieved 3 March 2012.
  2. 1 2 3 Smith, Theodore C.; McKamey, Bea (2000). "Summary of outreach activities for California's Seismic Hazards Mapping Program, 1996–1998". California Division of Mines and Geology Special Publication 121.
  3. "Forest and Watershed Geology Program". California Geological Survey. Archived from the original on 28 September 2012. Retrieved 3 March 2012.
  4. "Landslides". California Geological Survey. Archived from the original on 27 February 2012. Retrieved 3 March 2012.
  5. "Forest and Watershed Geology Program". California Geological Survey. Archived from the original on 2012-03-14. Retrieved 2012-03-03.
  6. Beuter, Thomas. "A brief history of the Ocean Shore Railroad". San Francisco Trains. Retrieved 3 March 2012.
  7. Ellen, S.D.; Wieczorek, G.F. (1988). "Landslides, floods, and marine effects of the storm of January 3–5, 1982, in the San Francisco Bay region, California" (PDF). U.S. Geological Survey Professional Paper (1434).
  8. Smith, T.C.; Hart, E.W. (July 1982). "Landslides and related storm damage, January 1982, San Francisco Bay region". California Geology. 35 (7): 139–152.
  9. Jones, Donna (January 6, 2012). "Devastating disaster: Storm of 1982 left 22 dead, many more homeless". Santa Cruz Sentinel .
  10. Jibson, Randall W. (2005). "Landslide Hazards at La Conchita, California". U.S. Geological Survey Open File Report 05-1067. Retrieved 3 March 2012.