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Mil'na

Milna

Stratovulcano · Russia · 1504 m

Milne, the southernmost volcano on Simushir Island, lies immediately SE of Goriaschaia volcano (far left) in this Space Shuttle image (N is to the upper left). The walls of a 3-km-wide Pleistocene crater that opens towards the sea are visible in the lower half of the image. The small, mostly snow-free central cone near the crater headwall contains a lava dome that was constructed during postglacial time and forms the highest point on the island.
Milne, the southernmost volcano on Simushir Island, lies immediately SE of Goriaschaia volcano (far left) in this Space Shuttle image (N is to the upper left). The walls of a 3-km-wide Pleistocene crater that opens towards the sea are visible in the lower half of the image. The small, mostly snow-free central cone near the crater headwall contains a lava dome that was constructed during postglacial time and forms the highest point on the island. · Foto: NASA International Space Station image ISS005-E-6511, 2002 (http://eol.jsc.nasa.gov/). · Wikimedia Commons
Tipo
Stratovulcano
Paese
Russia
Regione
Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
Altitudine
1504 m
Coordinate
46.815, 151.786
Ultima eruzione
1914
Contesto tettonico
Subduction zone / Oceanic crust (< 15 km)
Forma vulcanica
Composite
Roccia principale
Andesite / Basaltic Andesite
Sintesi geologica

Milna (or Mil'na) is the southernmost volcano on Simushir Island in the central Kuriles, and includes the Goriaschaia Sopka lava dome on the NW flank. The outer flanks of the steep-sided 1500-m-high volcano are dissected by deep gullies. A 3-km-wide caldera breached widely to the SE was formed during the Pleistocene and became a center of glaciation. A small central cone capped by an andesitic lava dome was constructed within the caldera during postglacial time and forms the highest point on Simushir Island. Lava flows from the cone descend 4-5 km to the sea. Goriaschaia Sopka, previously identified as a distinct volcano, is a historically active andesitic lava dome that grew just beyond what appears to be a NE-SW erosional scarp along the NW flank. Numerous fresh lava flows with prominent marginal levees extend from the dome, with some reaching the sea. It may have formed as recently as the late-19th century; dominantly mild-to-moderate explosive eruptions have occurred since 1842.

Sintesi da Wikipedia

Il Milna è un vulcano somma situato sull'isola di Simušir, nella Grande catena delle Curili (Russia). Appartiene al distretto Kuril'skij dell'oblast' di Sachalin.

Wikipedia · CC BY-SA · Leggi l'articolo completo

Storia delle eruzioni

Riepilogo (VEI nel tempo)
Fai clic su una barra per vedere le singole eruzioni
1842~1852 · 2 eruzioni · VEI max. 31873~1883 · 1 eruzioni · VEI max. 21883~1893 · 1 eruzioni · VEI max. 11913~1924 · 1 eruzioni · VEI max. 21934~1944 · 1 eruzioni · VEI max. 218421862189319131934

Cronologia dettagliata

  1. 1944VEI 2Stima geologica
    1944 – In corso
    Goriaschaia Sopka
  2. 1914VEI 2Osservata
    1914-06-04 – 1914-06-04
    Goriaschaia Sopka
  3. 1883VEI 1Osservata
    1883-04-15 – In corso
    Goriaschaia Sopka
  4. 1881VEI 2Osservata
    1881-09 – In corso
    Goriaschaia Sopka
  5. 1849VEI 2Osservata
    1849 – In corso
    Goriaschaia Sopka
  6. 1842VEI 3Osservata
    1842-06 – In corso
    Goriaschaia Sopka

Link esterni

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