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  2. Helenite - Wikipedia

    en.wikipedia.org/wiki/Helenite

    Helenite, also known as Mount St. Helens obsidian, emerald obsidianite, and ruby obsidianite, is a glass made from the fused volcanic rock dust from Mount St. Helens and marketed as a gemstone. [1] [2] Helenite was first created accidentally after the eruption of Mount St. Helens in 1980.

  3. Volcanic glass - Wikipedia

    en.wikipedia.org/wiki/Volcanic_glass

    Magma rich in silica and poor in dissolved water is most easily cooled rapidly enough to form volcanic glass. As a result, rhyolite magmas, which are high in silica, can produce tephra composed entirely of volcanic glass and may also form glassy lava flows. [2] Ash-flow tuffs typically consist of countless microscopic shards of volcanic glass. [3]

  4. Obsidian - Wikipedia

    en.wikipedia.org/wiki/Obsidian

    Obsidian (/ ə b ˈ s ɪ d i. ən, ɒ b-/ əb-SID-ee-ən ob-) [5] is a naturally occurring volcanic glass formed when lava extruded from a volcano cools rapidly with minimal crystal growth. It is an igneous rock . [ 6 ]

  5. Sideromelane - Wikipedia

    en.wikipedia.org/wiki/Sideromelane

    Sideromelane from Hawaii. Sideromelane is a vitreous basaltic volcanic glass, usually occurring in palagonite tuff, [1] for which it is characteristic. It is a less common form of tachylite, with which it usually occurs together; however it lacks the iron oxide crystals dispersed in the glass, and therefore appears transparent and pure, with yellow-brown color, instead of tachylite opaque ...

  6. Why you absolutely should wash your feet in the shower and ...

    www.aol.com/lifestyle/foot-scrubers-for-shower...

    The soft bristles gently clean in between the toes and cracks on the heels, while the gentle loofah offers an all-over clean for both tops and bottom of the feet. And at under $10, it's a steal! Pros

  7. Rhyolite - Wikipedia

    en.wikipedia.org/wiki/Rhyolite

    The alkaline magmas of volcanic ocean islands will very occasionally differentiate all the way to peralkaline rhyolites, but differentiation usually ends with trachyte. [ 25 ] Small volumes of rhyolite are sometimes erupted in association with flood basalts , late in their history and where central volcanic complexes develop.

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