Mauna kea vulkan typ
Mauna kea unter wasser Summary. Mauna Kea, like Hawai‘i's other older volcanoes, Hualālai and Kohala, has evolved beyond the shield-building stage, as indicated by (1) the very low eruption rates compared to Mauna Loa and Kīlauea; (2) the absence of a summit caldera and elongated fissure vents that radiate its summit; (3) steeper and more irregular topography.
Mauna kea teleskop
Mauna Kea is unusually topographically prominent for its height, with a wet prominence fifteenth in the world among mountains, and a dry prominence second in the world, after only Mount Everest. Because the Hawaiian Islands slope deep into the ocean, Mauna Kea has a dry prominence of 9, m (30, ft).Mauna loa letzter ausbruch The top of Mauna Kea falls far below the lofty zenith of its Himalayan rival, however it is more than a kilometre taller than Everest when comparing the two from base to pinnacle. But more than half of this dormant volcano lies unseen underwater. Indeed, of Mauna Kea’s c. 10, m (33, ft) total height, only 4, m (13, ft) is above.
Mauna loa Mauna Kea Observatory, astronomical observatory in Hawaii, U.S., that has become one of the most important in the world because of its outstanding observational conditions. The Mauna Kea Observatory is operated by the University of Hawaii and lies at an elevation of 4, metres (13, feet) atop the peak of Mauna Kea, a dormant volcano on north-central Hawaii island. The observatory was.