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Tokyo and Yokohama, Japan, Earthquake September 1, 1923. "A good idea of the tremendous devastation in Tokyo wrought by earthquake and fire. Enclosed find a few snaps taken on the top of the Imperial Hotel in Tokyo which is the only hotel in the earthquake district that survived." J.H. Messervey, letter dated March 5, 1924.
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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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Unzen Volcano, Japan, 1991. View looking southsouthwest of north flank of Unzen volcano complex. Active dome growth forms highest point on skyline, slightly left of center of photograph, USGS photo by T. J. Casadevall. Japan, Nov 20, 1991.
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Unzen Volcano, Japan, 1991. Aerial view of east face, Unzen volcano showing lava dome and paths of pyroclastic flows of June 3 & 8 (left side) and September 15 (right side). Mayoyama dome, site of 1792 collapse event, is located in lower right side of photograph. Photo by T. Kobayashi, Univ. Kagoshima. Japan, Nov 5, 1991.
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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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Tokyo and Yokohama, Japan, Earthquake September 1, 1923. "I enclose also a photo of the ruins of the Grand Hotel at Yokohama where I stopped last year." J.H. Messervey, letter dated March 5, 1924.
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Oblique aerial view of four-story apartment building in Niigata that settled and tipped because of loss of strength in supporting soils during the 1964 Niigata earthquake. Loss of bearing strength was caused by liquefaction of a sand layer that extends 10 to 15 feet below the base of the foundations. Photo by T. L. Youd. Japan. 1964.
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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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Unzen Volcano, Japan, 1991. Aerial view of northeast side of Unzen lava dome. USGS photo by T. J. Casadevall. Japan, November 20, 1991.
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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.


map background search result map search result map Aerial view of east face of volcano showing lava dome and paths of pyroclastic flows. Unzen Volcano, Japan, 1991. Landslide, Aratozawa Dam, Japan, 2008. Landslide, Aratozawa Dam, Japan. 2008. Landslide, Aratozawa Dam, Japan, 2008. Landslide, Aratozawa Dam, Japan, 2008. Landslide, Aratozawa Dam, Japan, 2008. Landslide, Aratozawa Dam, Japan, 2008. Landslide, Aratozawa Dam, Japan, 2008. Landslide, Aratozawa Dam, Japan. 2008. Landslide, Aratozawa Dam, Japan. 2008. Landslide, Aratozawa Dam, Japan. 2008. Landslide, Aratozawa Dam, Japan. 2008. Landslide. Aratozawa Dam, Japan. 2008 Landslide. Aratozawa Dam, Japan. 2008 Landslide, Aratozawa Dam, Japan. 2008. Aerial view of east face of volcano showing lava dome and paths of pyroclastic flows. Unzen Volcano, Japan, 1991. Landslide, Aratozawa Dam, Japan, 2008. Landslide, Aratozawa Dam, Japan. 2008. Landslide, Aratozawa Dam, Japan, 2008. Landslide, Aratozawa Dam, Japan, 2008. Landslide, Aratozawa Dam, Japan, 2008. Landslide, Aratozawa Dam, Japan, 2008. Landslide, Aratozawa Dam, Japan, 2008. Landslide, Aratozawa Dam, Japan. 2008. Landslide, Aratozawa Dam, Japan. 2008. Landslide, Aratozawa Dam, Japan. 2008. Landslide, Aratozawa Dam, Japan. 2008. Landslide. Aratozawa Dam, Japan. 2008 Landslide. Aratozawa Dam, Japan. 2008 Landslide, Aratozawa Dam, Japan. 2008.