What controls volcanic eruptions
This presentation is the property of its rightful owner.
Sponsored Links
1 / 42

What Controls Volcanic Eruptions? PowerPoint PPT Presentation


  • 198 Views
  • Uploaded on
  • Presentation posted in: General

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

Download Presentation

What Controls Volcanic Eruptions?

An Image/Link below is provided (as is) to download presentation

Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author.While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server.


- - - - - - - - - - - - - - - - - - - - - - - - - - E N D - - - - - - - - - - - - - - - - - - - - - - - - - -

Presentation Transcript


What controls volcanic eruptions

What Controls Volcanic Eruptions?

Ch 12.2


Some eruptions are quiet

Some eruptions are quiet…

Kilauea, Hawaii


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


What controls volcanic eruptions

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


What controls volcanic eruptions

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)


What controls volcanic eruptions

Pahoehoe lava:

  • Hot, thin, fast flowing

  • harden with a relatively smooth surface

  • Often has a ropy or wrinkled appearance


What controls volcanic eruptions

Pahoehoe lava


What controls volcanic eruptions

Aa lava:

  • Cooler, thicker, slow moving

  • Hardens with a rough, jagged, sharp edge surface


What controls volcanic eruptions

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


What controls volcanic eruptions

Andes Mtns


Krakatau 1883

Krakatau 1883

Sound heard 3,000 mi away!

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


What controls volcanic eruptions

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


Shield volcanoes2

Shield volcanoes


5 shield volcanoes make up the island of hawaii

5 Shield volcanoes make up the island of Hawaii


Fissure eruption

Fissure eruption


Fissure eruptions

Common at divergent plate boundaries, mid-ocean ridges

Fissure eruptions


Columbia plateau

Columbia Plateau


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 volcanoes

Cinder Cone Volcanoes

Paricutin


Cinder cone volcanoes1

Cinder Cone Volcanoes

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


Cinder cone example paricut n mexico

Cinder cone example: Paricutín, Mexico

1943


Cinder cone volcanoes2

Cinder Cone Volcanoes


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


Composite volcanoes

Composite Volcanoes


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

  • Names are based on size:

  • Ash

  • Lapilli/Cinders

  • Bombs/Blocks


Volcanoes

Volcanoes

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


What controls volcanic eruptions

Ash


Lapilli cinders

Lapilli/Cinders

Mt Pinatubo, Philippines 1991


Bombs

Bombs


Blocks

Blocks


  • Login