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  2. Parasitic cone - Wikipedia

    en.wikipedia.org/wiki/Parasitic_cone

    Parasitic cone (in foreground) with larger main cone in background, at Piton de la Fournaise volcano on the island of Réunion. A parasitic cone (also adventive cone, satellite cone or lateral cone) is the cone-shaped accumulation of volcanic material not part of the central vent of a volcano. It forms from eruptions from fractures on the flank ...

  3. Mount Scott (Klamath County, Oregon) - Wikipedia

    en.wikipedia.org/wiki/Mount_Scott_(Klamath...

    Mount Scott is a small stratovolcano and a so-called parasitic cone on the southeast flank of Crater Lake in southern Oregon. [4] [5] It is approximately 420,000 years old. [3] Its summit is the highest point within Crater Lake National Park, and the tenth highest peak in the Oregon Cascades. [6]

  4. Category:Parasitic cones - Wikipedia

    en.wikipedia.org/wiki/Category:Parasitic_cones

    Pages in category "Parasitic cones" The following 15 pages are in this category, out of 15 total. ... Schriebers Meadow Cone; Mount Scott (Klamath County, Oregon)

  5. Oreum - Wikipedia

    en.wikipedia.org/wiki/Oreum

    The word oreum comes from the Jeju language.It refers to small mountains. [2] " Oreum" itself originates from the word "climb" (오르다). [3]The word is now considered to refer to Jeju's numerous small parasitic cones (측화산; 側火山; also 기생화산; 寄生火山).

  6. Mulyeongari Oreum - Wikipedia

    en.wikipedia.org/wiki/Mulyeongari_Oreum

    Mulyeongari Oreum is located on the Mt. Suryeong (sea level attitude : 508m) on the Halla mountain in Jeju island. It is a typical parasitic cone and the mouth of a volcano has a girth of 300m, 40m in depth and 1,000m circumference around the crater.

  7. Volcanic cone - Wikipedia

    en.wikipedia.org/wiki/Volcanic_cone

    A tuff cone, sometimes called an ash cone, is a small monogenetic volcanic cone produced by phreatic (hydrovolcanic) explosions directly associated with magma brought to the surface through a conduit from a deep-seated magma reservoir. They are characterized by high rims that have a maximum relief of 100–800 meters (330–2,620 ft) above the ...

  8. Hillman Peak - Wikipedia

    en.wikipedia.org/wiki/Hillman_Peak

    The peak is the remnant of a parasitic cone on the western flank of Mount Mazama, such that when the caldera formed, the eastern half of the Hillman cone disappeared. The peak is composed of lava flows containing pyroxene and hornblende andesites and breccias. [4]

  9. Mount Samat - Wikipedia

    en.wikipedia.org/wiki/Mount_Samat

    Mount Samat is a parasitic cone of Mount Mariveles with no record of historical eruption. The summit of Mount Samat is 9.2 km (5.7 mi) NNE of the Mariveles caldera. [2] Mount Samat itself has a 550-metre (1,800 ft) wide crater that opens to the northeast.