The debris flow that occurred at the foot of Hieda-yama on July 13, 1985, struck the observatory of the Ministry of Construction, and totally destroyed a substantial part of the facilities. Another debris flow, probably of concurrent occurrence, took place in old Kanayama-zawa. The authors have investigated the cause of these debris flows and the landform changes at the debris flow sites, and have reconstructed the physical feature of down-flowing
A large number of debris flows occurred in the northwestern part of Hiroshima Prefecture on July 21s...
The background and mechanism of the Gamahara Torrent debris flow of 6 December, 1996 is reported. It...
Many debris flows caused by heavy rainfall have occurred at mountains in crystalline schist area, Sh...
This is the fourth of a series of papers on the Ura River basin (AOKI et al 1981, 1982 and 1983) and...
This second paper as continued first paper (AOKI et al 1982) deals with the results of research in t...
The Ura river, a tributary of the Hime river running through Nagano and Niigata Prefectures, covers ...
This report interprets the physical and mechanical properties of the unstable debris deposits in the...
The background and the process of the Hachimantai debris flows of 11 May 1997 are reported. At first...
Systematic observation was carried out on the eastern slope of Mt. Yakedake in JapanAlps, in order t...
An observation was made on the occurrence of debris flows and the characteristics of their deposits ...
From July to October in 1983, twenty-one debris flows were recorded in the Ura River. The author use...
Torrential rainfall in mid-July 2009 triggered numerous geodisasters such as slope failure and debri...
Serious damages occurred in the area of headwaters of Hitotsuse River in Miyazaki prefecture extendi...
The debris avalanche occurred in Kitamura area, Kurashiki City, Okayama Prefecture caused by the har...
A large number of debris flows occurred in the northwestern part of Hiroshima Prefecture on July 21s...
A large number of debris flows occurred in the northwestern part of Hiroshima Prefecture on July 21s...
The background and mechanism of the Gamahara Torrent debris flow of 6 December, 1996 is reported. It...
Many debris flows caused by heavy rainfall have occurred at mountains in crystalline schist area, Sh...
This is the fourth of a series of papers on the Ura River basin (AOKI et al 1981, 1982 and 1983) and...
This second paper as continued first paper (AOKI et al 1982) deals with the results of research in t...
The Ura river, a tributary of the Hime river running through Nagano and Niigata Prefectures, covers ...
This report interprets the physical and mechanical properties of the unstable debris deposits in the...
The background and the process of the Hachimantai debris flows of 11 May 1997 are reported. At first...
Systematic observation was carried out on the eastern slope of Mt. Yakedake in JapanAlps, in order t...
An observation was made on the occurrence of debris flows and the characteristics of their deposits ...
From July to October in 1983, twenty-one debris flows were recorded in the Ura River. The author use...
Torrential rainfall in mid-July 2009 triggered numerous geodisasters such as slope failure and debri...
Serious damages occurred in the area of headwaters of Hitotsuse River in Miyazaki prefecture extendi...
The debris avalanche occurred in Kitamura area, Kurashiki City, Okayama Prefecture caused by the har...
A large number of debris flows occurred in the northwestern part of Hiroshima Prefecture on July 21s...
A large number of debris flows occurred in the northwestern part of Hiroshima Prefecture on July 21s...
The background and mechanism of the Gamahara Torrent debris flow of 6 December, 1996 is reported. It...
Many debris flows caused by heavy rainfall have occurred at mountains in crystalline schist area, Sh...