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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 ...
The submerged mountain is about 200 meters taller from base to peak than Mount Olympus, and roughly four times the size of the tallest building in the world (Dubai’s Burj Khalifa), according to ...
For example, the world's second-highest mountain is K2 (height 8,611 m, prominence 4,017 m). While Mount Everest's South Summit (height 8,749 m, prominence 11 m [2]) is taller than K2, it is not considered an independent mountain because it is a sub-summit of the main summit (which has a height and prominence of 8,848 m).
An underwater mountain taller than the world’s highest building has been discovered by scientists in Central America. Schmidt Ocean Institute researchers discovered the seamount while mapping ...
Tallest mountain base-to-peak on land [15] [n 3] Mount Everest: 3.6 to 4.6 km (2.2 to 2.9 mi) [16] 0.072: tectonic: 4.6 km on north face, 3.6 km on south face; [n 4] highest elevation (8.8 km) above sea level, as well as by wet and dry prominence (but not among the tallest from base to peak, and in distance to Earth's center Mt Chimborazo rises ...
A team of oceanographers led by Schmidt Ocean Institute have discovered and mapped a new seamount on the Nazca Ridge 900 miles off the coast of Chile.
Its slopes are very gradual, ranging from less than half a degree to one degree near its summit. The Shatsky Rise oceanic plateau is comparable in size to California or Japan , [ 1 ] but Tamu Massif, which is the plateau's oldest and largest edifice, is comparable in size to New Mexico , [ 1 ] [ 12 ] or Britain and Ireland together. [ 4 ]
Undersea mountain ranges are mountain ranges that are mostly or entirely underwater, and specifically under the surface of an ocean. If originated from current tectonic forces, they are often referred to as a mid-ocean ridge. In contrast, if formed by past above-water volcanism, they are known as a seamount chain.