What is a volcano? A point on the earths crust where magma forces - - PowerPoint PPT Presentation

what is a volcano
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What is a volcano? A point on the earths crust where magma forces - - PowerPoint PPT Presentation

What is a volcano? A point on the earths crust where magma forces its way to the surface Ash and gases may also escape Where do they occur? On subduction zones On constructive plate boundaries On hot spots What types of


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What is a volcano?

  • A point on the earth’s crust where magma

forces its way to the surface

  • Ash and gases may also escape
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Where do they occur?

  • On subduction zones
  • On constructive plate boundaries
  • On hot spots
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What types of volcanoes are there?

Acid id vo volc lcano anoes es

  • Highly explosive
  • Magma/lava is viscous

(thick)

  • Found where oceanic crust is

subducted under continental crust

Basa salti ltic c vo volc lcano anoes es

  • Less explosive*
  • Magma/lava less viscous

(runny)

  • Found at rift zones (constructive

boundaries) and hotspots * Continental hotspots are basaltic but potentially highly explosive

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Acid (rhyolitic) volcanoes

Lava va dom

  • mes
  • Formed of layers of lava high in

silica

  • Lava is viscous and does not run

very far

  • Rounded form
  • composed completely of lava

Stratovo atovolcanoes lcanoes

  • Also called composite

volcanoes

  • Formed of layers of lava and

ashes

  • Lava is viscous
  • Distinct cone shape
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Example – lava dome

  • Mount St Helens - Washington state, USA

befo fore re dur urin ing

after ter

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Example - stratovolcano

  • Mount Pinatubo, Luzon, Philipines

before

During… after

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Other famous stratovolcanoes

Fuji, dormant Krakatoa, active Vesuvius, active Kilamanjaro, dormant

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Location of stratovolcanoes

  • Along subduction

zones

  • Often found in

volcanic arcs*

  • E.g. Cascade

range, USA

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Ba Basic sic (ba basalti saltic) c) vo volc lcanoes anoes

  • Also known as shield volcanoes
  • Formed of widespread layers of lava low in silica –

low viscsity, lava travels very far

  • Low form spread over a great distance
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Exa Examp mple le – basi asic c vo volca lcano no

  • Eyjafjallajökull, Iceland
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Ex Exam ample 2 ple 2

  • Kilauea, Hawaii
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Calderas

  • Collapsed volcanoes
  • Magma chamber has emptied and the ground has

sunk

  • Often becomes a lake
  • New volcanoes can form, or pressure can build from

below, lifting the ground

  • If acidic, this can cause a catastrophic eruption in

the form of a ”super-volcano volcano”

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Caldera - Santorini

  • Destroyed the Minoan civilization due to

tsunamis circa 1600BC

  • May have given rise to the Atlantis myth
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Yellowstone national park

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Yellowstone is a hotspot

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Hotspots

  • Tectonic plate moves
  • ver a magma

”plume”

  • Occasionally erupts,

creating a volcano

  • Hawaii – basic
  • Yellowstone - acid
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Volcanic hazards

  • Most hazards during

eruptions are caused by what comes out of a volcano

  • In worst case scenarios

then a volcano may violently explode

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  • Slow moving
  • Weight of ash can

collapse buildings

  • Destroys crops, pollutes

water

  • Affects air traffic
  • Can enter high

atmosphere and cause cooling – disrupting climate

Hazards – ash clouds

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Hazards – lava bombs

  • Molten rocks thrown out of volcano
  • Pummice – smaller rocks
  • Travel short distances
  • Can start fires
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An acid volcano

  • Potential for

violent eruptions

  • Slow moving lava
  • Explosions
  • Hot ash/cinders
  • Pyroclastic flows
  • Real danger!
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History of eruptions

  • 1800 BC – destruction of Bronze age

settlements – then several more times

  • 79 AD – destruction of Pompeii
  • At least 40 times until the last eruption

in 1944 – witnessed by allied troops towards the end of WWII

  • = once every 40-50 years
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Buried alive!

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Reducing the risks

  • Round-the-clock monitoring of the volcano

–Tremors, gasses, changes in water

  • Identifying hazard areas

–Weak spots, secondary vents, predicting routes of pyroclastic flows

  • Creating an evacuation plan

–Zoning, warning systems, public education