our world - 10 volcano made lakes

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    OUR WORLD

    10 Volcano Made LakesCHRISTINE VREYAUGUST 3, 2011

    Check out our new companion site:http://knowledgenuts.com

    This list will focus on any volcano made lake. Volcano lakes can occur in a

    few different ways: The first would simply be a crater filled with water. Another

    way that these lakes can form is that when a volcano erupts, such large

    amounts of magma are released that the emptied magma chamber beneath it

    collapses under the weight of the earth, thus forming a large indentation called

    a caldera, which eventually fills with water. All these lakes have an explosive

    past, a beautiful and majestic present, and a potentially devastating future.

    They each hold their own story.

    10Ijen Lake

    http://listverse.com/science-nature/our-world/http://listverse.com/science-nature/our-world/http://listverse.com/authors/?Christine%20Vreyhttp://listverse.com/authors/?Christine%20Vreyhttp://knowledgenuts.com/http://knowledgenuts.com/http://knowledgenuts.com/http://knowledgenuts.com/http://listverse.com/authors/?Christine%20Vreyhttp://listverse.com/science-nature/our-world/
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    Ijen Lake is a crater lake that is found in East Java, in Indonesia. It is situated

    in a group of stratovolcanoes, inside the Ijen Volcano. It is a 1km wide acid

    lake which has a beautiful turquoise color. This is also a site for sulphur

    mining, as there is an active vent at the one side of the lake, which continually

    brings sulphur to the surface, from where it is broken into pieces and carried

    out of the crater in baskets. The molten, red hot, sulphur is guided out of the

    vent through ceramic pipes, which deposits it on the floor, where it cools,

    turning into a bright yellow color. [Image Source]

    9Coatepeque Caldera

    Coatepeque Caldera is a volcanic caldera in El Salvador. The Caldera wasformed after a series of huge eruptions 72,000 and 54,000 years ago. Since

    those two large eruptive eras, cinder cones and volcanic domes have formed,

    as well as large areas of lava flow along the western edge of the caldera. On

    the eastern side of the caldera is a crater lake called Lake Coatepeque. This

    lake is about 26km2, making it one of the largest lakes in El Salvador, and it

    http://www.flickr.com/photos/laurentwiart/5819136479/in/photostreamhttp://www.flickr.com/photos/laurentwiart/5819136479/in/photostreamhttp://www.flickr.com/photos/laurentwiart/5819136479/in/photostreamhttp://www.flickr.com/photos/laurentwiart/5819136479/in/photostream
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    has hot springs all along its borders. In the lake there is an Island called

    Teopan, which was a sacred Mayan Site of importance.

    8Lake Towada

    Lake Towada is the largest crater lake in Japan, and the 12th largest lake in

    Japan. It is located in an active volcano caldera, with the last big eruption

    dating back about 13,000 years. The lake is actually situated in a double

    caldera, as a smaller eruption caused another caldera under the lake to

    collapse about 5,400 years ago. The volcanos eruptions stretch well into

    recorded history, and the last known eruption was about 1000 years ago,

    causing devastating ash and pyroclastic flows to retard crops, and lower the

    temperature considerably bringing with it a very cold winter and harsh famine.

    7Mount Katmai

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    Mount Katmai is a complex stratovolcano found on the Alaskan peninsula, in

    Southern Alaska. In the center there is a lake filled caldera, about 4km in

    diameter. The caldera was formed in the Novarupta eruption of 1912, and the

    caldera rim now reaches a maximum 6,716 feet. Little is known about the

    volcano before the huge eruptions in 1912, due to the uninhabitable aspect ofthe area, but some record was left by nearby villages, from the 1800s, that a

    volcano in the area would smoke on occasion.

    The eruption in 1912, was one of the two largest eruptions that the 20th

    century ever saw (the other being Mt Pinatubo in 1991). The 60 hour long

    eruption actually took place about 6 miles away from the mountain, in an

    active vent. The eruption caused the caldera to fall exactly in the crater of the

    mountain, creating a crater caldera lake.

    6Laach Lake

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    Laach Lake, also known as Laacher See, is a caldera lake, about 9km in

    diameter and can be found in Rhineland-Palatinate, Germany, near the towns

    of Koblenz (24 km), Bonn (37 km), Andernach (8 km), and Mayen (11 km),

    and only 8km away from the river Rhine. The caldera was formed after the

    massive Laacher See eruption, which occurred about 12,900 years ago.

    Approximately 6km3 of magma was erupted, causing almost 16km3 of tephrato be blasted into the atmosphere. The eruption had a VEI of 6, the same VEI

    as the massive eruption of Mt Pinatubo in 1991, which blasted less than

    10km3 of tephra out. The Laacher See eruption caused global cooling, and

    the tephra from the eruption can be found across Europe, with many unique

    minerals now being found in the area.

    5Lake Taupo

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    Lake Taupo is situated on the North Island of New Zealand, and is the largest

    lake in New Zealand. It has a surface area of about 616km2 and is believed to

    have been created around 26,500 years ago. The eruption is the largest

    known eruption in at least 69,000 years and it measured 8 on a VEI scale. It

    blasted an estimated 1170km3 of material into the atmosphere, which causedthe large caldera to collapse and create the lake. It is believed to have erupted

    about 27 times after the initial event, and the last big eruption can be dated

    back to 180 CE, when 30km3 of materials was blasted out of the volcano

    within 5 minutes, in a VEI 7 eruption. The eruption column would have been

    twice as high as the one from the Mount St Helen eruption, and historical

    records from both China and Rome stated that the sky turned red. This

    volcano is currently considered dormant but will probably wake from its long

    slumber in a few hundred years.

    4Lake Toba

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    Lake Toba is a huge caldera lake found on Sumatra Island, in Indonesia. It is

    over 100km long and 30km wide, and is the largest lake in Indonesia, and the

    largest Volcano Lake in the world. It was created +/- 70,000 years ago when a

    massive super volcano erupted in the largest volcanic explosion in at least 25

    million years. The eruption is believed to have had a VEI reading of 8, and it

    caused a global winter, in which most of the humans alive at the time died.

    This created a population bottleneck in Central Eastern Africa and in India,

    which has affected the genetic diversity of everyone on earth today.

    3Crater Lake

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    Crater Lake is a beautiful caldera lake found in South-central Oregon State,

    USA. It has a stunning deep blue color and brilliant water clarity, and forms

    the main feature in Crater Lake National Park. The lake has almost no signs

    of pollution, and is one of the purest bodies of water in the States, with a

    record clarity of 43.3 meters. The lake was formed about 7,700 years ago

    when volcano Mount Mazama, fell into the caldera beneath it. It is believed

    that the Native American Klamath tribe saw Mount Mazama fall and the

    formation of Crater Lake. Their legends and stories tell of a great battle

    between the sky god, Skell and Llao, the god of the underworld. The Mountain

    was destroyed during the battle and the lake was created. The Klamath

    people used the lake for vision quests, and the lake is still held in high spiritualregard by the tribe. The lake is also known for the old man of the lake, which

    is a full tree, now a stump, which has been bobbing around, vertically, in the

    lake for over a century. It has been very well preserved due the cold water

    inside the lake.

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    other. He said they swam around for almost 1 hour and a before retreating

    under the water.

    1Lake Nyos

    Lake Nyos is a 2km long crater lake located in the North Western part of

    Cameroon. The lake has a magma chamber beneath it, which constantly

    seeps Carbon dioxide into the lake, changing the water into carbonic acid.

    Over thousands of years of carbon dioxide seeping into the lake, it has

    become saturated with carbon dioxide, which had some devastating effects,

    on 2 August, 1986. A land slide caused the lake to release 1.6 million tons ofcarbon dioxide, which rose at about 100 km per hour and came spilling over

    the lip of the lake. The cloud suffocated over 1,700 people and 3,500 livestock

    which were in a 25km radius of the lake. This is the first known mass

    asphyxiation due to a natural event, and the lake was named the most

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    dangerous lake by Guinness World records after the event. Scientists are still

    working at degassing the lake to render it safer.

    +Lava Lakes

    Even though these are not lakes, in the general sense, they are still of

    volcanic origin, and very interesting, so I decided to add a bonus

    A lava lake is a rare occurrence, which can happen in three ways. Either a

    new vent erupts enough lava just to partly fill the crater, Lava flows into a

    depression or a new vent erupts for several weeks, building a crater around its

    self. The result is a lake of molten lava. There are currently just 5 lava lakes

    on earth: Erta Ale (pictured above), Ethiopia; Mount Erebus, Antarctica;

    Klauea, Hawaii; Nyiragongo, Democratic Republic of the Congo; Marum,

    Ambrym, Vanuatu.

    ++

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    Chapagne Pool

    Again this is not strictly a lake but it is a stunning consequence of a volcanic

    eruption. Champagne Pool is a prominent geothermal feature within the Wai-

    O-Tapu geothermal area in the Bay of Plenty Region of the North Island of

    New Zealand. The terrestrial hot spring is located about 30 km (20 mi)southeast of Rotorua and about 50 km (30 mi) northeast of Taupo. The name

    Champagne Pool is derived from the abundant efflux of carbon dioxide (CO2),

    similar to a glass of bubbling champagne. The hot spring was formed 900

    years ago by a hydrothermal eruption, which makes it, in geological terms, a

    relatively young system. Its crater is around 65 m (213 ft) in diameter with a

    maximum depth of approximately 62 m (203 ft) and is filled with an estimated

    volume of 50,000 m3 (1,800,000 cu ft) of geothermal fluid. The orange tinge

    around the edges is due to deposits of arsenic.