Dakataua

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Dakataua
Ulawun steam plume.jpg
Dakataua lake on the North tip of the Willaumez Peninsula, left of the Pago volcano. On the right there is a steam plume over the sea from the Ulawun volcano.
Highest point
Elevation 400 m (1,300 ft)
Coordinates 5°3′20″S150°6′30″E / 5.05556°S 150.10833°E / -5.05556; 150.10833
Geography
Geology
Mountain type Stratovolcano
Volcanic arc/belt Bismarck volcanic arc
Last eruption 1895 ± 5 years

The Dakataua Caldera is located at the northern tip of the Willaumez Peninsula, New Britain, Papua New Guinea. The peninsula includes the 350 m high andesitic Mount Makalia stratovolcano. [1] The last major collapse of Dakataua was during the Holocene around 800 CE. [2] The most recent eruption on the caldera's rim was Mount Makalia in 1890, producing lava flows and cinder cones. [3]

Contents

Caldera lake

Dakataua's caldera lake is about 76 m above sea level; it has a total surface area of 48 km2 (19 sq mi) and a maximum depth of approximately 120 m. [4] It is horseshoe shaped, roughly bisected by a peninsula. [1] It is a freshwater lake that is alkaline with a pH of up to 8.2. It is presumed to be formed by rainwater gradually filling in the caldera. [5] While the lake supports various kinds of life, it does not support any species of fish. [6]

Migo the Lake Monster

There is a folk legend that a monster called the migo (or masali) inhabits the lake. In 1993 a Japanese film crew led by Tetsuo Nagata captured what they claimed to be the migo on film. It is presumed that the creature in the video is actually a saltwater crocodile from the ocean surrounding the lake. [7]

Related Research Articles

A caldera is a large cauldron-like hollow that forms shortly after the emptying of a magma chamber in a volcano eruption. When large volumes of magma are erupted over a short time, structural support for the rock above the magma chamber is gone. The ground surface then collapses into the emptied or partially emptied magma chamber, leaving a large depression at the surface. Although sometimes described as a crater, the feature is actually a type of sinkhole, as it is formed through subsidence and collapse rather than an explosion or impact. Compared to the thousands of volcanic eruptions that occur each century, the formation of a caldera is a rare event, occurring only a few times per century. Only seven caldera-forming collapses are known to have occurred between 1911 and 2016. More recently, a caldera collapse occurred at Kīlauea, Hawaii in 2018.

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<span class="mw-page-title-main">Rabaul caldera</span> Large volcano on the tip of the Gazelle Peninsula in East New Britain, Papua New Guinea

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<span class="mw-page-title-main">Sulu Range</span>

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<span class="mw-page-title-main">Timeline of volcanism on Earth</span>

This timeline of volcanism on Earth includes a list of major volcanic eruptions of approximately at least magnitude 6 on the Volcanic explosivity index (VEI) or equivalent sulfur dioxide emission during the Quaternary period. Other volcanic eruptions are also listed.

References

  1. 1 2 "Dakataua". Global Volcanism Program . Smithsonian Institution . Retrieved 2021-06-25.
  2. "Holocene explosive eruptions of Witori and Dakataua caldera volcanoes in West New Britain, Papua New Guinea" . Retrieved August 19, 2020.
  3. "Dakataua Volcano World" . Retrieved August 19, 2020.
  4. E. BALL, J. GLUCKSMAN A limnological survey of Lake Dakataua, a large calderalake on West New Britain, Papua New Guinea, with comparisons to Lake Wisdom, a younger nearby caldera lake. Freshwater Biology (10)73, 1980
  5. "Lake Dakataua" . Retrieved August 19, 2020.
  6. "A liminological survey of Lake Dakataua". doi:10.1111/j.1365-2427.1980.tb01182.x . Retrieved August 19, 2020.{{cite journal}}: Cite journal requires |journal= (help)
  7. "Filming Migo the Monster" . Retrieved August 19, 2020.