The Asosan core (JMA-V40) was drilled at a site 1.2km WSW of Nakadake crater, Aso Volcano in 2009. The core consists of the following nine units: 1)alternating beds of ash-fall deposits and buried soil layers (0-3.49m in depth); 2)alternating beds of ash including Nakadake N2 scoria (N2S; 1.5ka) (3.49-4.46m); 3)scoria-fall deposits from Kishimadake scoria cone (4ka; 4.46-9.00m); 4)a basaltic andesite lava (lava 1, 9.00-23.72m); 5)alternating beds of ash, soils and lahar deposits including the Kikai Akahoya tephra (K-Ash; 7.3ka) (23.72-31.00m); 6)a basaltic andesite lava (lava 2, 31.00-76.11m); 7)lahar deposits (76.11-86.47m); 8)a basaltic andesite lava (lava 3, 86.47-91.64m); 9)lahar deposits (91.64-100.00m). The three lavas recognized in u...
Aso valley (Asodani) is the northern part of Aso Caldera crater which made by depression after the f...
It is very important for reconstructing volcano eruptive history to identify paleosols interbedded b...
Intense rainfall on 11-12 July 2012( maximum total 572 mm; maximum 4-hour rainfall 385mm) triggered ...
The Asosan core (JMA-V40) was drilled at a site 1.2km WSW of Nakadake crater, Aso Volcano in 2009. T...
Aso central cones initiated their eruptive activity just after the Aso-4 eruption, about 90,000 yrs ...
The western part of post-caldera central cones of Aso Volcano, southwestern Japan, is characterized ...
Three lava flows: Nakahono, Nagano, Otogase lava flows and Otogase debris avalanche deposit were new...
Aso central cones located within Aso caldera, central Kyushu, southwestern Japan, initiated their ac...
Ash emissions occurred from a hot water pool of one of the craters of Nakadake, the only active cent...
Nakadake volcano is located in the swarm of central cones within Aso caldera, central Kyusyu, southw...
Komezuka Volcano, located in the northwestern part of the post-caldera central cones of Aso Volcano,...
The stratigraphy and chronology of late-Pleistocene (after deposition of AT ash) tephra layers erupt...
A small ash deposit was recognized on snowpack around the Nakadake crater, Aso Volcano, SW Japan, on...
Jigoku spa is located west of Ikenokubo basin of Yomineyama volcano, southwestern part of the centra...
Take tephra occurs on the northern slope of Kitadake cone, which is one of the main edifices of Saku...
Aso valley (Asodani) is the northern part of Aso Caldera crater which made by depression after the f...
It is very important for reconstructing volcano eruptive history to identify paleosols interbedded b...
Intense rainfall on 11-12 July 2012( maximum total 572 mm; maximum 4-hour rainfall 385mm) triggered ...
The Asosan core (JMA-V40) was drilled at a site 1.2km WSW of Nakadake crater, Aso Volcano in 2009. T...
Aso central cones initiated their eruptive activity just after the Aso-4 eruption, about 90,000 yrs ...
The western part of post-caldera central cones of Aso Volcano, southwestern Japan, is characterized ...
Three lava flows: Nakahono, Nagano, Otogase lava flows and Otogase debris avalanche deposit were new...
Aso central cones located within Aso caldera, central Kyushu, southwestern Japan, initiated their ac...
Ash emissions occurred from a hot water pool of one of the craters of Nakadake, the only active cent...
Nakadake volcano is located in the swarm of central cones within Aso caldera, central Kyusyu, southw...
Komezuka Volcano, located in the northwestern part of the post-caldera central cones of Aso Volcano,...
The stratigraphy and chronology of late-Pleistocene (after deposition of AT ash) tephra layers erupt...
A small ash deposit was recognized on snowpack around the Nakadake crater, Aso Volcano, SW Japan, on...
Jigoku spa is located west of Ikenokubo basin of Yomineyama volcano, southwestern part of the centra...
Take tephra occurs on the northern slope of Kitadake cone, which is one of the main edifices of Saku...
Aso valley (Asodani) is the northern part of Aso Caldera crater which made by depression after the f...
It is very important for reconstructing volcano eruptive history to identify paleosols interbedded b...
Intense rainfall on 11-12 July 2012( maximum total 572 mm; maximum 4-hour rainfall 385mm) triggered ...