Vulcan

Sabancaya vulcan eruptent, Peru in 2017

Un vulcan es un rupture in li cruste de a planetari-masse objecte, quam Terra, que permisse calid lava, vulcanic cindres, e gases a escapar ex un magmic chambre sub li superficie.

Sur Terra, vulcanes es max sovente trovat u tectonic platiles es diverger o converger, e usualmen es trovat submarin. Por exemple, un mid-ocean creste, quam li Mid-Atlantic Creste, have vulcanes causat per divergent tectonic platiles, ma li Pacific Anelle de Foy have vulcanes causat per convergent platiles. Vulcanes anc posse formar u hay tender e tenuar de li platiles de cruste, quam in li Ost African Rift e li Rift del Rio Grande. Vulcanisme for del limites de platiles have esset postulat a resultar de ascendent diapires fro li limite de cordie–mantel, 3000 km profund in li Terra. To causa vulcanisme de calid-locos, de quel li Hawaiian calid-loco es un exemple. Vulcanes rarmen resulta u du tectonic platiles glissa preter unaltru.

Eruptiones grand posse afecter atmosferic temperatura pro que cindres e guttetas de sulfuric acide obscura li Sole e frigida li troposfere del Terra. Historicmen, grand eruptiones vulcanic have esset sequet per vulcanic hivernes, quel have causat catastrofic famines.

Altri planetes adplu Terra have vulcanes. Por exemple, Mercur have piroclastic deposites format per explosiv vulcanic activitá.. Mars have pluri grand vulcanes.

Vide anc

Referenties

  1. Volcanic Winters. In: Annual Review of Earth e Planetary Sciences. 16, Nr. 1, May 1988, S. 73–99
  2. Pitted-Ground Volcanoes on Mercury. In: Remote Sensing. 14, Nr. 17, 2022-08-24, S. 4164