| Usu |
Statistics:
Location: 42.53°N, 140.83°E (Hokkaido, Japan)
Summit elevation: around 3,315 m.a.sea-level
Last eruption: active since several thousand
years. Last big eruption in 2001
Type: Stratovolcano
|
|
|
Abstract:
Usu is a small stratovolcano located astride
the southern topographic rim of the 110,000-year-old Toya caldera.
The center of the 10-km-wide, lake-filled caldera contains Naka-jima,
a group of forested andesitic lava domes. The summit of the dominantly
basaltic edifice of Usu is cut by a somma formed about 7-8,000 years
ago when collapse of the volcano produced a debris avalanche that
reached the sea. Dacitic domes erupted along two NW-SE-trending lines
fill and flank the summit caldera. Three of these domes, O-Usu, Ko-
Usu and Showa-Shinzan, along with seven crypto-domes, were erupted
during historical time. The 1663 eruption of Usu was one of the largest
in Hokkaido during historical time. The war-time growth of Showa-
Shinzan from 1943-45 was painstakingly documented by the local postmaster,
who created the first detailed record of growth of a lava dome.
(From the Global
Volcanism Program) |
Latest Earthquakes in this region
(last updated: 04. January 2006:17:29
MET):
From Swiss
Seismological Service:
D
a t e Time (UTC) Location Dep Magni. Region
03Jan2006 12:26:16.4 42.6N 142.3E132 mb=5.1 A*EMS HOKKAIDO, JAPAN REGION 1333
03Jan2006 12:26:14.7 42.4N 142.2E130 mb=4.9 M*GSR HOKKAIDO, JAPAN REGION 1320
28Dec2005 15:42:06.1 44.0N 145.1E150 mb=4.8 M*GSR HOKKAIDO, JAPAN REGION 2001
21Dec2005 20:47:00.7 43.6N 143.7E150 mb=5.0 M*GSR HOKKAIDO, JAPAN REGION 2219
20Dec2005 22:58:35.6 41.8N 140.6E 33 mb=4.9 A*EMS HOKKAIDO, JAPAN REGION 0037
Only events with an average magnitude larger/equal than
3 are listed.
Go to the
main page of RedPuma
See their Disclaimer.
Other source: NEIC
|
|