Mount Komagatake in Japan is considered dormant and has no recorded historical eruptions.
ls it formed due to a hot spot or a plate boundary Komagatake
Mount Komagatake, located in Japan, typically produces explosive eruptions characterized by the expulsion of ash and volcanic gases. Its eruptions are often associated with the formation of pyroclastic flows and lava domes. The volcano is known for its stratovolcano structure, which contributes to its explosive potential. Overall, its eruptions can be quite hazardous due to the combination of ashfall and pyroclastic activity.
The Komagatake volcano in Japan is classified as a stratovolcano. The definition of a stratovolcano is a volcano that is conical in shape and composed of layers of material expelled from previous eruptions.
The volume of Mt Fuego can vary depending on its current size and shape due to eruptions and volcanic activity. The most recent volume estimate for Mt Fuego was around 10 cubic kilometers in 1974, but this may have changed since then.
Mount Komagatake in Japan is considered dormant and has no recorded historical eruptions.
ls it formed due to a hot spot or a plate boundary Komagatake
in 1934
Mount Komagatake, located in Japan, typically produces explosive eruptions characterized by the expulsion of ash and volcanic gases. Its eruptions are often associated with the formation of pyroclastic flows and lava domes. The volcano is known for its stratovolcano structure, which contributes to its explosive potential. Overall, its eruptions can be quite hazardous due to the combination of ashfall and pyroclastic activity.
The Komagatake volcano in Japan is classified as a stratovolcano. The definition of a stratovolcano is a volcano that is conical in shape and composed of layers of material expelled from previous eruptions.
Lake Ashi
The volume of Mt Fuego can vary depending on its current size and shape due to eruptions and volcanic activity. The most recent volume estimate for Mt Fuego was around 10 cubic kilometers in 1974, but this may have changed since then.
in 1640 and the the las t one was in 2000
The volume of Mt. Hibok-Hibok, an active stratovolcano on the island of Camiguin in the Philippines, is estimated to be around 2 cubic kilometers.
There can be no conversion.A MT is a measure of mass. A KL is a measure of volume. The two measure different things and, according to basic principles of dimensional analysis, conversion from one to the other is not valid.Consider a KL of air. How many MT? Next consider the same volume of lead. How many MT?
Since the density of water is 1 MT/m3 Mass = Volume*SpGr So mass = 384.64*0.939 MT = 361.177 MT (to 3 dp)
The nearest toown is Nanae, part of the town is 'Onuma' followed by Mori. The nearest big cities are 'Hokuto shi' and 'Hakodate'.