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Mauna Loa Research Paper

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Mauna Loa is located in the island of Hawaii and is 4170 meters above the ground. Ever since 1832, Mauna Loa has shot out explosions of sultry lava 39 times and its last sudden eruption was in 1984. The USGS cerebrates the volcano has erupted about of once every 6 years over the past 3000 years. The Hawaiian Volcano Observatory celebrated the 30th anniversary of Mauna Loa's last eruption (in 1984) on March 25, 2014.

Mauna Loa is the worlds most sizably voluminous mountain and volcano, it is a basaltic shield volcano in its tardy mature stage of life about 600,000-1,000,000 years old. Albeit it does not erupt as much as the volcano adjacent to it (Kilauea) it is still one of the most active volcanos in the world. When it erupts, its eruptions are customarily astronomically immense and engender immensely colossal rivers of lava that have perpetually threatened the town of Hilo. Mauna Loa elevates virtually 9 km above the sea floor and the weight of the mountain has caused the sea floor below it sink down by eight kilometers. Virtually 90% of Mauna Loa's surface is covered by lavas less than 4000 years old, while about 50% of its surface is covered by lavas no older than about 1500 years old, while about 25% are covered by lava flows younger than about 750 years, i.e. emplaced after the formation of the Mokuaweoweo summit …show more content…
Mauna Loa is one of five volcanoes that form the Island of Hawaii in the Pacific Ocean. Being the largest subaerial volcano in both mass and volume, it has been kenned as the most immensely colossal volcano in the world. It is an shield volcano with gentle slopes and a volume of 18,000 cubic miles. Lava eruptions from Mauna Loa are silica-poor and very fluid, and they incline to be non-explosive.

A shield volcano is a broad, domed volcano with gently sloping sides, characteristic of the eruption of fluid, basaltic

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