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The April 1998 El Niño-Triggered Anzar Road landslide, San Benito County, California El Niño-driven rainfall triggered many landslides and debris flows in northern and north-central California during the winter and spring of 1997-98. The 1997-98 rainy season began normally in the fall of 1997, but turned unusually wet in late November. The 1998 Anzar Road landslide occurred as a reactivation of an old landslide in Pleistocene nonmarine claystone, sandstone and conglomerate immediately adjacent to the San Andreas rift Zone. Destructive movement began during the early morning of april 22 as a moderately deep-seated earth slide within the area of the old landslide. This slide, on an average slope of 12 degrees,...
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The Aratozawa Dam landslide in Japan, was triggered by the 7.2 magnitude Iwate-Miyagi-Nariku earthquake which occurred on 14 June 2008. The landslide at the Aratozawa Dam in Kurihara measures over 1km in length and is 0.8 km wide. The landslide body mass is around 6700 million cubic meters and the amount of displacement was around 300 meters in the main section. The landslide was translational in nature and the geology comprises hard volcanic rocks overlying soft Tertiary sediments.
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The Aratozawa Dam landslide in Japan, was triggered by the 7.2 magnitude Iwate-Miyagi-Nariku earthquake which occurred on 14 June 2008. The landslide at the Aratozawa Dam in Kurihara measures over 1km in length and is 0.8 km wide. The landslide body mass is around 6700 million cubic meters and the amount of displacement was around 300 meters in the main section. The landslide was translational in nature and the geology comprises hard volcanic rocks overlying soft Tertiary sediments.
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The April 1998 El Niño-Triggered Anzar Road landslide, San Benito County, California El Niño-driven rainfall triggered many landslides and debris flows in northern and north-central California during the winter and spring of 1997-98. The 1997-98 rainy season began normally in the fall of 1997, but turned unusually wet in late November. The 1998 Anzar Road landslide occurred as a reactivation of an old landslide in Pleistocene nonmarine claystone, sandstone and conglomerate immediately adjacent to the San Andreas rift Zone. Destructive movement began during the early morning of april 22 as a moderately deep-seated earth slide within the area of the old landslide. This slide, on an average slope of 12 degrees,...
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The Aratozawa Dam landslide in Japan, was triggered by the 7.2 magnitude Iwate-Miyagi-Nariku earthquake which occurred on 14 June 2008. The landslide at the Aratozawa Dam in Kurihara measures over 1km in length and is 0.8 km wide. The landslide body mass is around 6700 million cubic meters and the amount of displacement was around 300 meters in the main section. The landslide was translational in nature and the geology comprises hard volcanic rocks overlying soft Tertiary sediments.
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The Aratozawa Dam landslide in Japan, was triggered by the 7.2 magnitude Iwate-Miyagi-Nariku earthquake which occurred on 14 June 2008. The landslide at the Aratozawa Dam in Kurihara measures over 1km in length and is 0.8 km wide. The landslide body mass is around 6700 million cubic meters and the amount of displacement was around 300 meters in the main section. The landslide was translational in nature and the geology comprises hard volcanic rocks overlying soft Tertiary sediments.
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The Aratozawa Dam landslide in Japan, was triggered by the 7.2 magnitude Iwate-Miyagi-Nariku earthquake which occurred on 14 June 2008. The landslide at the Aratozawa Dam in Kurihara measures over 1km in length and is 0.8 km wide. The landslide body mass is around 6700 million cubic meters and the amount of displacement was around 300 meters in the main section. The landslide was translational in nature and the geology comprises hard volcanic rocks overlying soft Tertiary sediments.
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The Aratozawa Dam landslide in Japan, was triggered by the 7.2 magnitude Iwate-Miyagi-Nariku earthquake which occurred on 14 June 2008. The landslide at the Aratozawa Dam in Kurihara measures over 1km in length and is 0.8 km wide. The landslide body mass is around 6700 million cubic meters and the amount of displacement was around 300 meters in the main section. The landslide was translational in nature and the geology comprises hard volcanic rocks overlying soft Tertiary sediments.
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The Aratozawa Dam landslide in Japan, was triggered by the 7.2 magnitude Iwate-Miyagi-Nariku earthquake which occurred on 14 June 2008. The landslide at the Aratozawa Dam in Kurihara measures over 1km in length and is 0.8 km wide. The landslide body mass is around 6700 million cubic meters and the amount of displacement was around 300 meters in the main section. The landslide was translational in nature and the geology comprises hard volcanic rocks overlying soft Tertiary sediments.
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The Aratozawa Dam landslide in Japan, was triggered by the 7.2 magnitude Iwate-Miyagi-Nariku earthquake which occurred on 14 June 2008. The landslide at the Aratozawa Dam in Kurihara measures over 1km in length and is 0.8 km wide. The landslide body mass is around 6700 million cubic meters and the amount of displacement was around 300 meters in the main section. The landslide was translational in nature and the geology comprises hard volcanic rocks overlying soft Tertiary sediments.
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The Aratozawa Dam landslide in Japan, was triggered by the 7.2 magnitude Iwate-Miyagi-Nariku earthquake which occurred on 14 June 2008. The landslide at the Aratozawa Dam in Kurihara measures over 1km in length and is 0.8 km wide. The landslide body mass is around 6700 million cubic meters and the amount of displacement was around 300 meters in the main section. The landslide was translational in nature and the geology comprises hard volcanic rocks overlying soft Tertiary sediments.
thumbnail
The April 1998 El Niño-Triggered Anzar Road landslide, San Benito County, California. El Niño-driven rainfall triggered many landslides and debris flows in northern and north-central California during the winter and spring of 1997-98. The 1997-98 rainy season began normally in the fall of 1997, but turned unusually wet in late November. The 1998 Anzar Road landslide occurred as a reactivation of an old landslide in Pleistocene nonmarine claystone, sandstone and conglomerate immediately adjacent to the San Andreas rift Zone. Destructive movement began during the early morning of april 22 as a moderately deep-seated earth slide within the area of the old landslide. This slide, on an average slope of 12 degrees,...
thumbnail
The Aratozawa Dam landslide in Japan, was triggered by the 7.2 magnitude Iwate-Miyagi-Nariku earthquake which occurred on 14 June 2008. The landslide at the Aratozawa Dam in Kurihara measures over 1km in length and is 0.8 km wide. The landslide body mass is around 6700 million cubic meters and the amount of displacement was around 300 meters in the main section. The landslide was translational in nature and the geology comprises hard volcanic rocks overlying soft Tertiary sediments.
thumbnail
The April 1998 El Niño-Triggered Anzar Road landslide, San Benito County, California El Niño-driven rainfall triggered many landslides and debris flows in northern and north-central California during the winter and spring of 1997-98. The 1997-98 rainy season began normally in the fall of 1997, but turned unusually wet in late November. The 1998 Anzar Road landslide occurred as a reactivation of an old landslide in Pleistocene nonmarine claystone, sandstone and conglomerate immediately adjacent to the San Andreas rift Zone. Destructive movement began during the early morning of april 22 as a moderately deep-seated earth slide within the area of the old landslide. This slide, on an average slope of 12 degrees,...
thumbnail
The Aratozawa Dam landslide in Japan, was triggered by the 7.2 magnitude Iwate-Miyagi-Nariku earthquake which occurred on 14 June 2008. The landslide at the Aratozawa Dam in Kurihara measures over 1km in length and is 0.8 km wide. The landslide body mass is around 6700 million cubic meters and the amount of displacement was around 300 meters in the main section. The landslide was translational in nature and the geology comprises hard volcanic rocks overlying soft Tertiary sediments.
thumbnail
The Aratozawa Dam landslide in Japan, was triggered by the 7.2 magnitude Iwate-Miyagi-Nariku earthquake which occurred on 14 June 2008. The landslide at the Aratozawa Dam in Kurihara measures over 1km in length and is 0.8 km wide. The landslide body mass is around 6700 million cubic meters and the amount of displacement was around 300 meters in the main section. The landslide was translational in nature and the geology comprises hard volcanic rocks overlying soft Tertiary sediments.
thumbnail
The Aratozawa Dam landslide in Japan, was triggered by the 7.2 magnitude Iwate-Miyagi-Nariku earthquake which occurred on 14 June 2008. The landslide at the Aratozawa Dam in Kurihara measures over 1km in length and is 0.8 km wide. The landslide body mass is around 6700 million cubic meters and the amount of displacement was around 300 meters in the main section. The landslide was translational in nature and the geology comprises hard volcanic rocks overlying soft Tertiary sediments.
thumbnail
The Aratozawa Dam landslide in Japan, was triggered by the 7.2 magnitude Iwate-Miyagi-Nariku earthquake which occurred on 14 June 2008. The landslide at the Aratozawa Dam in Kurihara measures over 1km in length and is 0.8 km wide. The landslide body mass is around 6700 million cubic meters and the amount of displacement was around 300 meters in the main section. The landslide was translational in nature and the geology comprises hard volcanic rocks overlying soft Tertiary sediments.
thumbnail
The Aratozawa Dam landslide in Japan, was triggered by the 7.2 magnitude Iwate-Miyagi-Nariku earthquake which occurred on 14 June 2008. The landslide at the Aratozawa Dam in Kurihara measures over 1km in length and is 0.8 km wide. The landslide body mass is around 6700 million cubic meters and the amount of displacement was around 300 meters in the main section. The landslide was translational in nature and the geology comprises hard volcanic rocks overlying soft Tertiary sediments.


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