San Andreas Fault - Wikipedia
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. [1] It forms part of the tectonic boundary between the Pacific plate and the North American plate .
San Andreas Fault Homepage: Information, photos, maps, fault …
Comprehensive source of information about the San Andreas Fault, how to see it, earthquakes, tsunamis, etc.
圣安德烈亚斯断层 - 维基百科，自由的百科全书
圣安德列斯断层 （英語： San Andreas Fault，又譯 聖安地列斯斷層 、 聖安德烈亞斯斷層 、 聖安德魯斯斷層），是北美洲一處頻繁活動的斷層。 此斷層约1300公里長，位于 太平洋板块 和 北美洲板块 交界处的錯動性板塊，横跨 美国 加利福尼亚州 西部和南部以及 墨西哥 下加利福尼亚州 北部和东部的 断层。 這是地球上地層活動最頻繁的區域之一，最近一次的重大地震紀錄是1906年，强度达 里氏震级 7.8的 舊金山大地震。 1895年，加州柏克萊大學的教授 安德魯·勞森 首先發現 …
San Andreas Fault Line - Fault Zone Map and Photos - Geology.com
What is the San Andreas Fault? The San Andreas Fault is the sliding boundary between the Pacific Plate and the North American Plate. It slices California in two from Cape Mendocino to the Mexican border. San Diego, Los Angeles and Big Sur are on the Pacific Plate.
圣安地列斯断层 - 百度百科
贯穿美国加利福尼亚西南部的圣安地列斯断层 (SanAndreas Fault)，是地球表面最长和最活跃的断层之一。 地壳并非铁板一块，而是由若干被称为“构造板块”的巨大固态岩石块组成的。 圣安地列斯断层的终端已经有250年没有发生大的地震了，现在它聚集的压力已经临近暴发。 科学家表示，在过去300多年的时间里，圣安地列斯地壳 断层带 南端所承受的压力一直在不断地累积——所积蓄的能量足够造成一次强度在里氏7级或以上的大地震在 洛杉矶 和 圣地亚哥 附近发生。 导致3000 …
San Andreas Fault | California, Earthquakes, Plate Tectonics
2024年12月31日 · San Andreas Fault, major fracture of the Earth’s crust in extreme western North America. The fault trends northwestward for more than 800 miles (1,300 km) from the northern end of the Gulf of California through western California, U.S., passing seaward into the Pacific Ocean in the vicinity of San
San Andreas Fault Field Guide
Information about the San Andreas Fault and how to see it, with GPS coordinates, accurate fault locations, all in full color. Available as book or CD.
San Andreas Fault - WorldAtlas
2021年11月22日 · San Andreas Fault is a major continental transform boundary that is situated in the extreme western part of the continent of North America and forms the border between two principal tectonic plates: the North American Plate on …
Information and resources about the San Andreas Fault
The San Andreas Fault is a place where two tectonic plates touch, the North American and Pacific Plates. The plates are rigid (or almost rigid) slabs of rock that comprise the crust and upper mantle of the Earth.
region. The entire San Andreas fault system is more than 800 miles long and extends to depths of at least 10 miles within the Earth. In detail, the fault is a complex zone of crushed and broken rock from a few hundred feet to a mile wide. Many smaller faults branch from and join the San Andreas fault zone. Almost any road cut in the