What controls volcanic eruptions
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What Controls Volcanic Eruptions?. Ch 12.2. Some eruptions are quiet…. Kilauea, Hawaii. Some eruptions are EXPLOSIVE!. Mt. Pinatubo. Montserrat. Mt. St. Helens. What Controls Volcanic Eruptions?. How much water vapor (a gas) and other gases are trapped in the erupting magma

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Some eruptions are explosive
Some eruptions are EXPLOSIVE!

Mt. Pinatubo

Montserrat

Mt. St. Helens


What controls volcanic eruptions1
What Controls Volcanic Eruptions?

  • How much water vapor (a gas) and other gases are trapped in the erupting magma

  • How much silica is contained in the magma


Trapped Gases

  • water vapor and carbon dioxide are dissolved in magma

    • When magma rises to surface, gases escape because they are under less pressure

    • Some magma is thin and fluid- this lets gases escape easily- resulting in quiet eruption

    • Other magma is thick and stiff- when gases erupt it results in explosive eruption


Water VaporWater may be added to magma when ocean crust rock is melted at convergent plate boundaries


Composition of magma

Silica-rich magma is called granitic/rhyolitic magma

Results in explosive eruptions

Ex. Soufriere Hills in Montserrat

Characteristic of convergent plates

Silica-poor magma is called basaltic magma

Results in quiet eruptions

Ex. Iceland

Characteristic of divergent plates

Composition of magma


Basaltic magma may result in different three lava types
Basaltic magma may result in different three lava types:

  • Pahoehoe

  • Aa

  • Pillow (cools

    the fastest)


Pahoehoe lava:

  • Hot, thin, fast flowing

  • harden with a relatively smooth surface

  • Often has a ropy or wrinkled appearance



Aa lava:

  • Cooler, thicker, slow moving

  • Hardens with a rough, jagged, sharp edge surface


Pillow Lava:

  • Lava cools underwater

  • resembles stuffed pillows


Explosive magma lava
Explosive Magma/Lava

Granitic/Rhyolitic Magma

high in silica

high amount of trapped gases

very viscous

lead to explosive type eruptions

Soufriere Hills volcano-active since 1995

At what type of boundary would granitic/rhyolitic magma form?

convergent boundaries


Composition of magma1
Composition of magma

  • Andesitic magma – more silica than basaltic magma, but less than granitic magma

    • Common at convergent boundaries

    • Named after the Andes Mountains in South America

    • Also violent eruptions

    • Ex. Krakatau- one of the most violent eruptions in history



Krakatau 1883
Krakatau 1883

Sound heard 3,000 mi away!

13,000 x more powerful than nuclear blast at Hiroshima in WWII


Anak Krakatau (Child of Krakatau)


Forms of volcanoes
Forms of Volcanoes

  • Depends on:

    • Type of magma it was formed from

    • Type of eruption- quiet or explosive

  • 3 basic types of volcanoes

    • Shield

    • Cinder cone

    • Composite


1 shield volcanoes
1. Shield volcanoes

  • Result of quiet eruptions of basaltic lava flows (no ash)

  • May form volcanic cones or fissures- long cracks that result if flood basalts (Ragged Mtn, Lamentation Mtn)

  • Ex. Hawaiian Islands and the Columbia Plateau of Northwest US


Shield volcanoes
Shield volcanoes

Mauna Kea, Hawaii


Shield volcanoes1
Shield volcanoes

Mauna Loa, Hawaii







2 cinder cones
2. Cinder Cones

  • Small base, steep-sided, loosely consolidated

  • Up to 1000 feet tall

  • Life span of a few years

  • Commonly built from solidified rock thrown through the air called tephra

  • Has violent eruptions, dangerous when close


2 cinder cone volcanoes
2. Cinder Cone Volcanoes

Paricutin, Mexico (1943-1952, newest volcano in Western Hemisphere, 1000 killed)



Cinder cone volcanoes1
Cinder Cone Volcanoes

Pu'u ka Pele on flank of Mauna Kea volcano, Hawaii




Composite volcano aka stratovolcano
Composite Volcano (aka stratovolcano)

  • most beautiful, but most deadly

  • characteristic shape

  • made of alternating layers of lava and tephra- periods of quiet, then explosive eruptions

Mt. Fuji, Japan- one of the most photographed volcanoes in the world because of its near perfect symmetry

Ex. Mt. St. Helens



What are the three types of magma in order from least viscous to most viscous
What are the three types of magma in order from least viscous to most viscous?

  • a. Basaltic

  • b. Andesitic

  • c. Granitic


Tephra
Tephra viscous to most viscous?

  • Names are based on size:

  • Ash

  • Lapilli/Cinders

  • Bombs/Blocks


Volcanoes
Volcanoes viscous to most viscous?

Volcanoes eject different types of material. This material is known as tephra or pyroclastic material.

There are 3 main types:

Ash-less than 2 mm in diameter

Lapilli/cinders-2mm-64 mm in diameter

Blocks orBombs-larger than 64mm


Ash viscous to most viscous?


Lapilli cinders
Lapilli/Cinders viscous to most viscous?

Mt Pinatubo, Philippines 1991


Bombs
Bombs viscous to most viscous?


Blocks
Blocks viscous to most viscous?


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