lecture 9 pt 2 Flashcards
strombolian type eruptions
medium viscosity basaltic to andesitic magmas TRAP MORE of the GAS BUBBLES, producing mildly explosive eruptions as at stromboli italy
scoria cones
strombolian type eruptions: repeated eruptions produce mounds of volcanic rock fragments piled up next to a volcanic vent. Summit crater may hold a lava lake during eruption
BC: stikine volcanic belt and Wells gray-clearwater volcanic field
vulcanian type eruptions
medium to high viscosity magmas, typically andesitic in composition
- magma is sufficiently viscous that explosive eruptions send rock and ash into atmosphere forming a plume
frequency of eruption occurances
strombonian–> occur pretty much daily, 100s a year
plinian: more violent and high visocsity so 1/200 years
ultra plinian: every few millions
stratovolcanoes
vulcanian type eruptions: tall steep sided symmetrical peaks built of alternating ash and viscous magma flows
plinian type eruptions
high viscosity rhyolitic magmas trap gas bubles most effectively producing a violent plinian type eruptions (ex. omunt st helens 1980)
caldera
plinian type eruptions–> associated w/stratovolcanoes but empty magma chamber can lead to collapse of volcanic cone forming caldera
- mountains break apart
pliny the younger
erupted in 79CE, roman city was buried in pyroclastic flow
ultra plinican type eruptions
sixth class of volcanic eruption accounts for largest eruptions of all defined by > 25km high plumes and >10km volumes - 630ka yellowstone: caldera 75 x 45 km volume = 1000km
what is special about yellow stone supervolcano
occupies a continental hot spot, magma is rhytolitic since it must rise through thick continental crust
volcanic explosivity index (VEI)
classifies volcanic eruptions based on
- volume of material erupted
- height of eruption column
- duration fo major eruptive blast
viscosity/volatiles/volume of eruption types
icelandic: basalt, low viscosity, low volatiles, large volume, flood basalt
hawaiin: basalt, low viscosity, low volatiles, large volume, shield volcano
strombolian: basalt/andesite, low/medium viscosity, medium volatiles, small volume and scoria cones
vulcanian: basalt (rhyolite), medium/high viscosity, medium/high volatiles, large volume, stratovolcanoes
plinian: adnesite (rhyolite), high viscosity, high volaties, very large volume and calderas
glass
obsidian: produced when lava comes in contact with cool air or water and can be quenched solidifying so quickly that crystalizzation cannot happen
pumice
gas escapes quickly from lava producing frothy glass
can comprise 90% holes
tephra or pyroclasts
explosive eruptions blast out chunks of magma and surrounding rock