Mount Haddington
Encyclopedia
Mount Haddington 64.21°S 57.63°W is a massive high shield volcano
located on James Ross Island
, Antarctica. It is 60 kilometers wide and has had numerous subglacial eruption
s throughout its history, forming many tuya
s. Some of its single eruptions are bigger in volume than a whole normal-sized volcano. Old eruption shore lines are found everywhere on the volcano's deeply-eroded
flanks.
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 on James Ross Island
James Ross Island
James Ross Island is a large island off the southeast side and near the northeastern extremity of Antarctic Peninsula, from which it is separated by Prince Gustav Channel. Rising to , it is irregularly shaped and extends in a north-south direction. It was charted in October 1903 by the Swedish...
, Antarctica. It is 60 kilometers wide and has had numerous subglacial eruption
Subglacial eruption
A subglacial eruption is a volcanic eruption that has occurred under ice, or under a glacier. Subglacial eruptions can cause dangerous floods, lahars and create hyaloclastite and pillow lava. Subglacial eruptions sometimes form a subglacial volcano called a tuya. Tuyas in Iceland are called table...
s throughout its history, forming many tuya
Tuya
A tuya is a type of distinctive, flat-topped, steep-sided volcano formed when lava erupts through a thick glacier or ice sheet. They are somewhat rare worldwide, being confined to regions which were covered by glaciers and also had active volcanism during the same time period.-Formation:Tuyas are...
s. Some of its single eruptions are bigger in volume than a whole normal-sized volcano. Old eruption shore lines are found everywhere on the volcano's deeply-eroded
Erosion
Erosion is when materials are removed from the surface and changed into something else. It only works by hydraulic actions and transport of solids in the natural environment, and leads to the deposition of these materials elsewhere...
flanks.