Mount Oakan
Encyclopedia
is a shield volcano
located in Akan National Park
in Hokkaidō
, Japan
.
. The volcano rises some 900 metres (2,952.8 ft) above the surrounding terrain. The top of the volcano is 1370 metres (4,494.8 ft) above sea level. The volcanic cone is some 8 kilometres (5 mi) in diameter. There are three explosion craters at the summit. At at about 800 metres (2,624.7 ft), there is a fumarole
. The volcano is made mostly from non-alkalai mafic
volcanic rock. The main rock type is andesite
and dacite
.
dropping pumice on Minamishikata. After that, continuous lava flows formed the bulk of the volcano. In the final stages of its life, a parasitic volcano formed a lava dome
at the summit.
According to its name and local legend, Mount Oakan is the male counterpart to Mount Meakan
on the other side of Lake Akan.
Shield volcano
A shield volcano is a type of volcano usually built almost entirely of fluid lava flows. They are named for their large size and low profile, resembling a warrior's shield. This is caused by the highly fluid lava they erupt, which travels farther than lava erupted from more explosive volcanoes...
located in Akan National Park
Akan National Park
is a national park located on the island of Hokkaidō, Japan. Along with Daisetsuzan National Park, these are the two oldest national parks in Hokkaidō. The park was established December 4, 1934....
in Hokkaidō
Hokkaido
, formerly known as Ezo, Yezo, Yeso, or Yesso, is Japan's second largest island; it is also the largest and northernmost of Japan's 47 prefectural-level subdivisions. The Tsugaru Strait separates Hokkaido from Honshu, although the two islands are connected by the underwater railway Seikan Tunnel...
, Japan
Japan
Japan is an island nation in East Asia. Located in the Pacific Ocean, it lies to the east of the Sea of Japan, China, North Korea, South Korea and Russia, stretching from the Sea of Okhotsk in the north to the East China Sea and Taiwan in the south...
.
Geography and geology
Mount Oakan sits in the Akan caldera northeast of Lake AkanLake Akan
is a lake in Kushiro, Hokkaidō, Japan. It is located in Akan National Park and is a Ramsar Site.-History:Volcanic activity formed the lake some 6,000 years ago, when a dam was formed. The lake used to have a clarity of 8–9 meters in the 1930s. Pollution from local hotspring resorts has decreased...
. The volcano rises some 900 metres (2,952.8 ft) above the surrounding terrain. The top of the volcano is 1370 metres (4,494.8 ft) above sea level. The volcanic cone is some 8 kilometres (5 mi) in diameter. There are three explosion craters at the summit. At at about 800 metres (2,624.7 ft), there is a fumarole
Fumarole
A fumarole is an opening in a planet's crust, often in the neighborhood of volcanoes, which emits steam and gases such as carbon dioxide, sulfur dioxide, hydrochloric acid, and hydrogen sulfide. The steam is created when superheated water turns to steam as its pressure drops when it emerges from...
. The volcano is made mostly from non-alkalai mafic
Mafic
Mafic is an adjective describing a silicate mineral or rock that is rich in magnesium and iron; the term is a portmanteau of the words "magnesium" and "ferric". Most mafic minerals are dark in color and the relative density is greater than 3. Common rock-forming mafic minerals include olivine,...
volcanic rock. The main rock type is andesite
Andesite
Andesite is an extrusive igneous, volcanic rock, of intermediate composition, with aphanitic to porphyritic texture. In a general sense, it is the intermediate type between basalt and dacite. The mineral assemblage is typically dominated by plagioclase plus pyroxene and/or hornblende. Magnetite,...
and dacite
Dacite
Dacite is an igneous, volcanic rock. It has an aphanitic to porphyritic texture and is intermediate in composition between andesite and rhyolite. The relative proportions of feldspars and quartz in dacite, and in many other volcanic rocks, are illustrated in the QAPF diagram...
.
History
Mount Oakan emerged in the Late PleistoceneLate Pleistocene
The Late Pleistocene is a stage of the Pleistocene Epoch. The beginning of the stage is defined by the base of the Eemian interglacial phase before the final glacial episode of the Pleistocene 126,000 ± 5,000 years ago. The end of the stage is defined exactly at 10,000 Carbon-14 years BP...
dropping pumice on Minamishikata. After that, continuous lava flows formed the bulk of the volcano. In the final stages of its life, a parasitic volcano formed a lava dome
Lava dome
|250px|thumb|right|Image of the [[rhyolitic]] lava dome of [[Chaitén Volcano]] during its 2008–2009 eruption.In volcanology, a lava dome is a roughly circular mound-shaped protrusion resulting from the slow extrusion of viscous lava from a volcano...
at the summit.
According to its name and local legend, Mount Oakan is the male counterpart to Mount Meakan
Mount Meakan
is an active stratovolcano located in Akan National Park in Hokkaidō, Japan. It is the tallest mountain in the Akan Volcanic Complex.The volcano consists of nine overlapping cones that grew out of the Akan caldera, on the shores of Lake Akan. Mount Meakan has a triple crater at its summit...
on the other side of Lake Akan.