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  2. Mount Aniakchak - Wikipedia

    en.wikipedia.org/wiki/Mount_Aniakchak

    Mount Aniakchak (Russian: Аниакчак) is a volcano on the western Alaska Peninsula. Part of the Aleutian Volcanic Arc , it was formed by the subduction of the oceanic Pacific Plate under the North American Plate .

  3. Phreatic eruption - Wikipedia

    en.wikipedia.org/wiki/Phreatic_eruption

    Phreatic eruption at the summit of Mount St. Helens, Washington, in the spring of 1980. A phreatic eruption, also called a phreatic explosion, ultravulcanian eruption or steam-blast eruption, [1] occurs when magma heats ground water or surface water. The extreme temperature of the magma (anywhere from 500 to 1,170 °C (930 to 2,100 °F)) causes ...

  4. Tomb of Kha and Merit - Wikipedia

    en.wikipedia.org/wiki/Tomb_of_Kha_and_Merit

    Fourteen stools of various forms were placed in the tomb; these were all items used by Kha and Merit in life. The most unusual example is a folding stool with a leather seat and legs ending in duck heads inlaid with ivory. The tables found in the tomb were simple, either of wood, or constructed of papyrus stems.

  5. There was once an ancient ocean filled with magma on the moon ...

    www.aol.com/once-ancient-ocean-filled-magma...

    There was once a magma-filled ocean on the south pole of the moon, scientists recently discovered after analyzing lunar soil that revealed ancient information about the moon's origin. The study of ...

  6. Ancient ocean of magma found on Moon south pole

    www.aol.com/ancient-ocean-magma-found-moon...

    The Moon’s south pole was once covered in an ocean of liquid molten rock, according to scientists. The findings back up a theory that magma formed the Moon's surface around 4.5 billion years ago.

  7. Mount Mazama - Wikipedia

    en.wikipedia.org/wiki/Mount_Mazama

    Its collapse, due to the eruption of magma emptying the underlying magma chamber, formed a caldera that holds Crater Lake (Giiwas in the Native American language Klamath). [6] Mount Mazama originally had an elevation of 12,000 feet (3,700 m), but following its climactic eruption this was reduced to 8,157 feet (2,486 m).

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