Mount Takahe is a 3,460-metre-high (11,350 ft) snow-covered
shield volcano in
Marie Byrd Land,
Antarctica, 200 kilometres (120 mi) from the
Amundsen Sea. It is a
c. 30-kilometre-wide (19 mi) mountain with
parasitic vents and a
caldera up to 8 kilometres (5 mi) wide. Most of the volcano is formed by
trachytic lava flows, but
hyaloclastite is also found. Snow, ice, and
glaciers cover most of Mount Takahe. With a volume of 780 km
3 (200 cu mi), it is a massive volcano; the parts of the edifice that are buried underneath the
West Antarctic Ice Sheet are probably even larger. It is part of the
West Antarctic Rift System along with eighteen other known volcanoes.
The volcano was active in the
Quaternary age, from 2.5 million years ago to the present.
Radiometric dating has yielded ages of up to 300,000
years for its rocks, and it reached its present height about 200,000
years ago. Several
tephra layers encountered in
ice cores at
Mount Waesche and
Byrd Station have been attributed to Mount Takahe, although some of them were later linked to eruptions of
Mount Berlin instead. The tephra layers were formed by
explosive or
phreatomagmatic eruptions. Major eruptions took place around 17,700
years ago—possibly forming an
ozone hole over Antarctica—and in the early
Holocene. Mount Takahe's last eruption occurred about 7,600 years ago, and there is no present-day activity. (
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