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Hawaiʻi Volcanoes National Park is a national park of the United States located in Hawaii on the island of Hawaii. The park encompasses two active volcanoes: Kīlauea , one of the world's most active volcanoes, and Mauna Loa , the world's largest shield volcano.
Halemaʻumaʻu Crater Lake in October 2019, the yellow water is the result of dissolved minerals and sulfur 2008 Map of Kīlauea Caldera with Halemaʻumaʻu lower left. Halemaʻumaʻu (six syllables: HAH-leh-MAH-oo-MAH-oo) is a pit crater within the much larger Kīlauea Caldera at the summit of Kīlauea volcano on island of Hawaiʻi.
Mauna Kea (/ ˌ m ɔː n ə ˈ k eɪ ə, ˌ m aʊ n ə-/, [6] Hawaiian: [ˈmɐwnə ˈkɛjə]; abbreviation for Mauna a Wākea) [7] is a dormant shield volcano on the island of Hawaiʻi. [8] Its peak is 4,207.3 m (13,803 ft) above sea level, making it the highest point in Hawaii and the island with the second highest high point, behind New Guinea, the world's largest tropical island with ...
Here’s what travelers should know about Haleakalā, the latest national park in USA TODAY’s yearlong series. Why is Haleakalā so special? The lush Pipiwai trail is located in Haleakalā ...
Haleakalā National Park is a national park of the United States located on the island of Maui, Hawaii.Named after Haleakalā, a dormant volcano within its boundaries, the park covers an area of 33,265 acres (52.0 sq mi; 134.6 km 2), [1] of which 24,719 acres (38.6 sq mi; 100.0 km 2) is a wilderness area. [3]
On Maui, the summit of Haleakalā occasionally experiences snowfall, but snow had never been observed below 7,500 feet (2,300 m) before February 2019, when snow was observed at 6,200 feet (1,900 m) and fell at higher elevations in amounts large enough to force Haleakalā National Park to close for several days. The record low temperature in ...
Like all Hawaiian volcanoes, Mauna Loa was created as the Pacific tectonic plate moved over the Hawaii hotspot in the Earth's underlying mantle. [10] The Hawaii island volcanoes are the most recent evidence of this process that, over 70 million years, has created the 3,700 mi (6,000 km)-long Hawaiian–Emperor seamount chain. [11]
The Puhahonu volcano (Gardner) would be twice as big as Mauna Loa's based on that research. [5] [f] The Pūhāhonu and West Pūhāhonu volcanoes result from the Hawaii hotspot which is fed by the Hawaiian plume which had a major magmatic flux pulse at the time. [2] [c] A longer magmatic flux pulse produced the Hawaiian Islands.