volcanic activity. magma reaching the surface materials of asthenosphere under great pressure...
TRANSCRIPT
Magma Reaching the Magma Reaching the SurfaceSurface
Materials of asthenosphere under great Materials of asthenosphere under great pressurepressure
Magma less dense than surrounding Magma less dense than surrounding rockrock
Magma rises until it reaches the Magma rises until it reaches the surface or becomes trapped by rock surface or becomes trapped by rock layerslayers
A Volcano EruptsA Volcano Erupts
Dissolved gases in magma are under Dissolved gases in magma are under tremendous pressuretremendous pressure
As magma rises pressure decreasesAs magma rises pressure decreases
Gases dissolved in magma rush out, Gases dissolved in magma rush out, carrying magma when an opening carrying magma when an opening develops in weak rock on the surfacedevelops in weak rock on the surface
Characteristics of MagmaCharacteristics of Magma
Force of volcanic eruption impacted Force of volcanic eruption impacted by:by:– Gas dissolved in magmaGas dissolved in magma– Thickness of magmaThickness of magma– TemperatureTemperature– Silica contentSilica content
Characteristics of MagmaCharacteristics of Magma
Some magma thick- flows slowlySome magma thick- flows slowly Some more fluid- flows easilySome more fluid- flows easily Viscosity describes a liquids Viscosity describes a liquids
resistance to flow- higher viscosity, resistance to flow- higher viscosity, greater resistancegreater resistance
http://www.seed.slb.com/en/scictr/lab/visco_exp/index.htm
Characteristics of MagmaCharacteristics of Magma
Temperature impacts thickness- Temperature impacts thickness- hotter, more fluidhotter, more fluid
More silica- thicker magmaMore silica- thicker magma– High silica- light lava, too sticky, doesn’t High silica- light lava, too sticky, doesn’t
flow far, forms rhyolite, pumice, & flow far, forms rhyolite, pumice, & obsidianobsidian
– Low silica- flows easily, dark colored, Low silica- flows easily, dark colored, forms basaltforms basalt
Types of EruptionsTypes of Eruptions
Quiet EruptionsQuiet Eruptions– Quiet eruption if magma flows easilyQuiet eruption if magma flows easily– Gases bubble out gentlyGases bubble out gently– Lava oozes quietly from ventLava oozes quietly from vent– Ex. Hawaii, IcelandEx. Hawaii, Iceland– Forms from basaltic material, low in Forms from basaltic material, low in
silicasilica– Type of crust?!?Type of crust?!?
Types of Volcanic EruptionsTypes of Volcanic Eruptions
Explosive eruptionsExplosive eruptions– Thick & sticky magma- explosive eruptionThick & sticky magma- explosive eruption– Dissolved gases can’t escape, pressure Dissolved gases can’t escape, pressure
builds up, it explodesbuilds up, it explodes– Magma pushed out of volcano w/incredible Magma pushed out of volcano w/incredible
forceforce– Pyroclastic flow hurls ash, cinders, bombsPyroclastic flow hurls ash, cinders, bombs– Forms from granitic material, high in silicaForms from granitic material, high in silica– Crust type?!?Crust type?!?
Stages of a VolcanoStages of a Volcano
Active- erupting or shows signs of Active- erupting or shows signs of erupting in near futureerupting in near future
Dormant- sleeping, expected to Dormant- sleeping, expected to awaken in future & become activeawaken in future & become active
Extinct- unlikely to erupt againExtinct- unlikely to erupt again