Shoreline Erosion Assessment and Atlas of the San Diego Region: The San Diego shoreline PDF Download
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Author: Reinhard E Flick
Publisher:
ISBN:
Category : Beach erosion
Languages : en
Pages : 156
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Book Description
Author:
Publisher:
ISBN:
Category : Flood damage prevention
Languages : en
Pages : 1120
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Book Description
Author: Reinhard E Flick
Publisher:
ISBN:
Category : Beach erosion
Languages : en
Pages : 156
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Book Description
Author: Reinhard E Flick
Publisher:
ISBN:
Category : Beach erosion
Languages : en
Pages : 112
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Book Description
Author:
Publisher: FEMA
ISBN:
Category :
Languages : en
Pages : 286
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Book Description
Author:
Publisher:
ISBN:
Category :
Languages : en
Pages : 366
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Book Description
Author:
Publisher:
ISBN:
Category :
Languages : en
Pages : 302
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Book Description
Author: Glenn Roquemore
Publisher: DIANE Publishing
ISBN: 0788142623
Category :
Languages : en
Pages : 215
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Book Description
The San Diego region had enjoyed a long period of seismic quiescence since the last damaging earthquake in 1862. This quiescence was broken in 1984 with several earthquake swarms in San Diego Bay. Because of the lack of consensus among geoscientists about future earthquake threats, a workshop was conducted that: brought together all interested geoscientists; brought together all available data for debate and discussion; evaluated the data; and identified data gaps and recommended a collective approach. Includes charts, graphs, and drawings. Extensive references.
Author:
Publisher:
ISBN:
Category : Natural disasters
Languages : en
Pages : 426
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Book Description
Author:
Publisher:
ISBN:
Category :
Languages : en
Pages : 326
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Book Description
Author: National Research Council
Publisher: National Academies Press
ISBN: 0309255945
Category : Science
Languages : en
Pages : 274
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Book Description
Tide gauges show that global sea level has risen about 7 inches during the 20th century, and recent satellite data show that the rate of sea-level rise is accelerating. As Earth warms, sea levels are rising mainly because ocean water expands as it warms; and water from melting glaciers and ice sheets is flowing into the ocean. Sea-level rise poses enormous risks to the valuable infrastructure, development, and wetlands that line much of the 1,600 mile shoreline of California, Oregon, and Washington. As those states seek to incorporate projections of sea-level rise into coastal planning, they asked the National Research Council to make independent projections of sea-level rise along their coasts for the years 2030, 2050, and 2100, taking into account regional factors that affect sea level. Sea-Level Rise for the Coasts of California, Oregon, and Washington: Past, Present, and Future explains that sea level along the U.S. west coast is affected by a number of factors. These include: climate patterns such as the El Niño, effects from the melting of modern and ancient ice sheets, and geologic processes, such as plate tectonics. Regional projections for California, Oregon, and Washington show a sharp distinction at Cape Mendocino in northern California. South of that point, sea-level rise is expected to be very close to global projections. However, projections are lower north of Cape Mendocino because the land is being pushed upward as the ocean plate moves under the continental plate along the Cascadia Subduction Zone. However, an earthquake magnitude 8 or larger, which occurs in the region every few hundred to 1,000 years, would cause the land to drop and sea level to suddenly rise.
