Volcanic debris flows repeatedly occurred along the Mizunashi River by the eruption of Unzen Volcano since November 1990. Debris flow sediments were dredged on the river mouth area of the Mizunasi River from May 1993 to November 1996. We measured the thickness and analyzed the grain size of these debris flow sediments. The appearance of the debris flow sediments look like the volcanic ash from Unzen Volcano. After the intense debris flow occurred, the debris flow sediments were widely distributed. On March 1994,these sediments have the largest distribution. The river mouth area, sediments were characterized by the mud that median diameter was larger than 4φ. Before the influx of debris flow in this area, most of surface sediments used to be...
Debris flow hazard posts a big threat to the main downstream of Jinsha River where a number of huge ...
This is the fourth of a series of papers on the Ura River basin (AOKI et al 1981, 1982 and 1983) and...
Monitoring of sediment transport from hillslopes to channel networks as a consequence of floods with...
Unzen volcano in wastern Kyushu, southwestern Japan, began a series of eruptions in November 1990. R...
Unzen volcano in wastern Kyushu, southwestern Japan, began a series of eruptions in November 1990. R...
A debris flow occurred in the Tsugaru Juniko Lakes area, NE Japan, due to localized torrential downp...
An observation was made on the occurrence of debris flows and the characteristics of their deposits ...
Among varied topographic changes induced by the eruption and other activities of Mt.Fugen in the Unz...
This report interprets the physical and mechanical properties of the unstable debris deposits in the...
Debris flow deposits, that occurred during the Middle Pleistocene to the present, are widely distrib...
Debris flow composes the important part of mass movement and is called dosekiryu in Japan. Debris fl...
Japan is awarded with a total of about 144 volcanos distributed over the whole country from the sout...
Abstract The present contribution investigates the temporal changes in volcaniclastic sediment trans...
Japan is awarded with a total of about 144 volcanos distributed over the whole country from the sout...
Japan is awarded with a total of about 144 volcanos distributed over the whole country from the sout...
Debris flow hazard posts a big threat to the main downstream of Jinsha River where a number of huge ...
This is the fourth of a series of papers on the Ura River basin (AOKI et al 1981, 1982 and 1983) and...
Monitoring of sediment transport from hillslopes to channel networks as a consequence of floods with...
Unzen volcano in wastern Kyushu, southwestern Japan, began a series of eruptions in November 1990. R...
Unzen volcano in wastern Kyushu, southwestern Japan, began a series of eruptions in November 1990. R...
A debris flow occurred in the Tsugaru Juniko Lakes area, NE Japan, due to localized torrential downp...
An observation was made on the occurrence of debris flows and the characteristics of their deposits ...
Among varied topographic changes induced by the eruption and other activities of Mt.Fugen in the Unz...
This report interprets the physical and mechanical properties of the unstable debris deposits in the...
Debris flow deposits, that occurred during the Middle Pleistocene to the present, are widely distrib...
Debris flow composes the important part of mass movement and is called dosekiryu in Japan. Debris fl...
Japan is awarded with a total of about 144 volcanos distributed over the whole country from the sout...
Abstract The present contribution investigates the temporal changes in volcaniclastic sediment trans...
Japan is awarded with a total of about 144 volcanos distributed over the whole country from the sout...
Japan is awarded with a total of about 144 volcanos distributed over the whole country from the sout...
Debris flow hazard posts a big threat to the main downstream of Jinsha River where a number of huge ...
This is the fourth of a series of papers on the Ura River basin (AOKI et al 1981, 1982 and 1983) and...
Monitoring of sediment transport from hillslopes to channel networks as a consequence of floods with...