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- W652715511 abstract "In the 1995 Hyogoken Nanbu Earthquake, large earthquake motions struck the Rokko Mountain System and its surrounding areas located 10 to 30 km northeast of the epicenter and in the northern part of Awaji Island located 0 to 30 km southwest of the epicenter. In these areas, many phenomena of slope movement (hillside failures, landslips, landslides) occurred and some of the sediment and slope movement control-related facilities (sediment and erosion control facilities, landslide prevention structures, steep slope failure prevention structures) suffered slight damage. Based on the results of on-site studies, interpretation of aerial photos, slope stability analyses and comparisons with phenomena of debris movement due to earthquakes in the past, this report describes characteristics of the phenomena of slope movement due to this earthquake observed in and around the Rokko Mountain System and northern part of Awaji Island and how the sediment and erosion control facilities were actually hit. Research has revealed that many hillside failures occurred in the eastern and southern part of the Rokko Mountain System and many slope failures occurred to the south of the system. It has also been shown that few landslides occurred and that they occurred mainly along the Nikawa and Arimakawa rivers. The sediment and erosion control facilities did not suffer any great damage that could seriously threaten their safety." @default.
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- W652715511 date "1997-03-01" @default.
- W652715511 modified "2023-09-27" @default.
- W652715511 title "SLOPE MOVEMENT DISASTERS AND DAMAGE TO SEDIMENT & SLOPE MOVEMENT (OR LANDSLIDE) CONTROL FACILITIES (1995 HYOGOKEN NANBU EARTHQUAKE)" @default.
- W652715511 hasPublicationYear "1997" @default.
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