Plume from Tanzania's Ol Doinyo Lengai Volcano : News Photo

Plume from Tanzania's Ol Doinyo Lengai Volcano

Credit: NASA / Contributor
TANZANIA - JULY 18: In early September 2007, Tanzania's Ol Doinyo Lengai Volcano erupted, sending a cloud of ash into the atmosphere. On September 4, 2007, the Advanced Spaceborne Thermal Emission and Reflection Radiometer (AST ER) on NASA's Terra satellite captured this image of the volcano sending a plume of ash and steam southward. The volcanic plume appears pale blue-gray, distinct near the summit, and growing more diffuse to the south. On the land surface, green indicates vegetation, and beige and gray indicate bare or thinly vegetated ground. The charcoal-colored stains on the volcano's flanks appear to be lava, but they are actually burn scars left behind by fires that were spawned by fast-flowing, narrow rivers of lava ejected by the volcano. An explosive eruption of ash and steam is rare for Ol Doinyo Lengai. Typically, volcanic activity at the volcano consists of lava flows that are restricted to the summit crater. This eruption, however, sent ash downwind at least 18 kilometers (11 miles). Ol Doinyo Lengai is an unusual volcano. Like many other volcanoes on Earth, it is a stratovolcano composed of alternating layers of hardened lava, solidified ash, and rocks from previous eruptions. Unlike other volcanoes, however, Ol Doinyo Lengai is the only active volcano on Earth known to produce natrocarbonatite lava. Natrocarbonatite has a relatively low temperature, about 500 to 600 degrees Celsius (930 to 1,100 degrees Fahrenheit), compared to typical lavas, which are about 700 to 1,200 degrees Celsius (1,300 to 2,200 degrees Fahrenheit). Although still hot enough to burn much of what it directly touches, this lava is cool enough to allow close-up inspection without the routine layers of protective gear that volcanologists use elsewhere. But while it is cooler than other lavas, natrocarbonatite lava is also less viscous. Its more fluid consistency means this lava is also faster than other lavas. (Photo by NASA/SSPL/Getty Images)
Caption:
TANZANIA - JULY 18: In early September 2007, Tanzania's Ol Doinyo Lengai Volcano erupted, sending a cloud of ash into the atmosphere. On September 4, 2007, the Advanced Spaceborne Thermal Emission and Reflection Radiometer (AST ER) on NASA's Terra satellite captured this image of the volcano sending a plume of ash and steam southward. The volcanic plume appears pale blue-gray, distinct near the summit, and growing more diffuse to the south. On the land surface, green indicates vegetation, and beige and gray indicate bare or thinly vegetated ground. The charcoal-colored stains on the volcano's flanks appear to be lava, but they are actually burn scars left behind by fires that were spawned by fast-flowing, narrow rivers of lava ejected by the volcano. An explosive eruption of ash and steam is rare for Ol Doinyo Lengai. Typically, volcanic activity at the volcano consists of lava flows that are restricted to the summit crater. This eruption, however, sent ash downwind at least 18 kilometers (11 miles). Ol Doinyo Lengai is an unusual volcano. Like many other volcanoes on Earth, it is a stratovolcano composed of alternating layers of hardened lava, solidified ash, and rocks from previous eruptions. Unlike other volcanoes, however, Ol Doinyo Lengai is the only active volcano on Earth known to produce natrocarbonatite lava. Natrocarbonatite has a relatively low temperature, about 500 to 600 degrees Celsius (930 to 1,100 degrees Fahrenheit), compared to typical lavas, which are about 700 to 1,200 degrees Celsius (1,300 to 2,200 degrees Fahrenheit). Although still hot enough to burn much of what it directly touches, this lava is cool enough to allow close-up inspection without the routine layers of protective gear that volcanologists use elsewhere. But while it is cooler than other lavas, natrocarbonatite lava is also less viscous. Its more fluid consistency means this lava is also faster than other lavas. (Photo by NASA/SSPL/Getty Images)
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Date created:
July 18, 2011
Editorial #:
138596668
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In early September 2007 Tanzania's Ol Doinyo Lengai Volcano erupted... News Photo 1385966682000-2009,2000s Style,2007,21st Century,Ash,Atmospheric,Cloud,Color Image,NASA,Nature,Ol Doinyo Lengai,Satellite View,Science and Technology,Sending,Smoke,Square,Tanzania,The Natural World,VolcanoPhotographer Collection: SSPL SSPL/NASATANZANIA - JULY 18: In early September 2007, Tanzania's Ol Doinyo Lengai Volcano erupted, sending a cloud of ash into the atmosphere. On September 4, 2007, the Advanced Spaceborne Thermal Emission and Reflection Radiometer (AST ER) on NASA's Terra satellite captured this image of the volcano sending a plume of ash and steam southward. The volcanic plume appears pale blue-gray, distinct near the summit, and growing more diffuse to the south. On the land surface, green indicates vegetation, and beige and gray indicate bare or thinly vegetated ground. The charcoal-colored stains on the volcano's flanks appear to be lava, but they are actually burn scars left behind by fires that were spawned by fast-flowing, narrow rivers of lava ejected by the volcano. An explosive eruption of ash and steam is rare for Ol Doinyo Lengai. Typically, volcanic activity at the volcano consists of lava flows that are restricted to the summit crater. This eruption, however, sent ash downwind at least 18 kilometers (11 miles). Ol Doinyo Lengai is an unusual volcano. Like many other volcanoes on Earth, it is a stratovolcano composed of alternating layers of hardened lava, solidified ash, and rocks from previous eruptions. Unlike other volcanoes, however, Ol Doinyo Lengai is the only active volcano on Earth known to produce natrocarbonatite lava. Natrocarbonatite has a relatively low temperature, about 500 to 600 degrees Celsius (930 to 1,100 degrees Fahrenheit), compared to typical lavas, which are about 700 to 1,200 degrees Celsius (1,300 to 2,200 degrees Fahrenheit). Although still hot enough to burn much of what it directly touches, this lava is cool enough to allow close-up inspection without the routine layers of protective gear that volcanologists use elsewhere. But while it is cooler than other lavas, natrocarbonatite lava is also less viscous. Its more fluid consistency means this lava is also faster than other lavas. (Photo by NASA/SSPL/Getty Images)