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volcano: from Latin, referring to volcano; coni: from ancient Greek (κόνις, kónis) which means dust-osis: from ancient Greek, suffix to indicate a medical condition; This word was invented in the daily meeting from the National Puzzlers' League (N.P.L.) by its president Everett M. Smith.
It is the only volcano in the world where visitors can take an elevator and safely descend into the magma chamber. The magma that would normally fill the chamber and become sealed is believed to have drained away, to the bewilderment of scientists, revealing the rift beneath the surface.
Hualālai (pronounced [huwəˈlaːlɐi] in Hawaiian) is an active volcano on the island of Hawaiʻi in the Hawaiian Islands. [4] It is the westernmost, third-youngest and the third-most active of the five volcanoes that form the island of Hawaiʻi, following Kīlauea and the much larger Mauna Loa.
Öræfajökull (Icelandic pronunciation: [ˈœːrˌaiːvaˌjœːkʏtl̥] ⓘ; 'Öræfi glacier' or 'wasteland glacier') is an ice-covered volcano in south-east Iceland. The largest active volcano and the highest peak in Iceland at 2,110 metres (6,920 ft), it lies within the Vatnajökull National Park and is covered by part of the glacier.
The ice cap covers the caldera of a volcano with a summit elevation of 1,651 metres (5,417 ft). The volcano has erupted relatively frequently since the Last Glacial Period, most recently in 2010, [7] [8] when, although relatively small for a volcanic eruption, it caused enormous disruption to air travel across northern and western Europe for a ...
Highest point; Elevation: 305 m (1,001 ft) Coordinates: Naming; English translation: The summit where Tamatea, the man with the big knees, the slider, climber of mountains, the land-swallower who travelled about, played his kōauau (flute) to his loved one.
Grímsvötn (Icelandic pronunciation: [ˈkrimsˌvœhtn̥] ⓘ; [2] vötn = "waters", singular: vatn) is an active volcano with a (partially subglacial) fissure system located in Vatnajökull National Park, Iceland. The central volcano is completely subglacial and located under the northwestern side of the Vatnajökull ice cap.
The subglacial volcano is located within the Reykjanes volcanic system [4] or Svartsengi volcanic system, [5] depending on author, and enclosed by Holocene lava fields. A visible tectonic graben [6] runs over the top of the mountain [7] forming a small canyon, up to 80 m deep. [8] The mountain is a symbol of Reykjanes' geology. [9]