Volcanic activity l.jpg
This presentation is the property of its rightful owner.
Sponsored Links
1 / 71

Volcanic Activity PowerPoint PPT Presentation


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

Volcanic Activity. Plumbing System of a Volcano. Fig. 5.1. Cross Section of the East Pacific Rise. Fig. 5.29. Volcanic Materials. Lavas – appearance depends upon viscosity Low viscosity – low SiO 2 lavas; high T; low volatile content - smooth lava

Download Presentation

Volcanic Activity

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


Volcanic activity l.jpg

Volcanic Activity


Plumbing system of a volcano l.jpg

Plumbing System of a Volcano

Fig. 5.1


Cross section of the east pacific rise l.jpg

Cross Section of the East Pacific Rise

Fig. 5.29


Volcanic materials l.jpg

Volcanic Materials

  • Lavas – appearance depends upon viscosity

    • Low viscosity – low SiO2 lavas; high T; low volatile content - smooth lava

    • High viscosity – high SiO2 lavas; low T; high volatile content – rough lava

  • Pyroclastic material – fragmented material due to explosive volcanic activity

    • Associated with magmas with high volatile gas content

  • Volcanic gases – water, carbon dioxide, sulfur, sulfur dioxide, hydrogen sulfide


  • Basaltic lavas l.jpg

    Basaltic Lavas

    • Pahoehoe – rope-like, glassy

    • Aa – fragmented, dull surfaces

    Aa

    Pahoehoe


    Basaltic lavas6 l.jpg

    Basaltic Lavas

    • Pillow lavas – underwater “pillow” or “tube” shaped lava flow


    Pyroclastic materials l.jpg

    Pyroclastic Materials

    • Pyroclastic name based upon fragment size

      ash – sand size

      lapilli – walnut size

      bombs (> 1 inch, cools in flight)

      blocks (> 1 inch, solid before ejection)


    Volcanic bombs l.jpg

    Volcanic Bombs


    Volcanic blocks l.jpg

    Volcanic Blocks


    Volcanic tuff l.jpg

    Volcanic Tuff


    Volatile gases associated with volcanism l.jpg

    Volatile Gases Associated with Volcanism

    • Steam (H2O)

    • Carbon dioxide (CO2 )

    • Hydrogen sulfide (H2S)

    • Sulfur vapor

    • Many other constituents


    Sulfur encrusted fumerole galapagos islands l.jpg

    Sulfur-encrusted fumerole:

    Galapagos Islands

    Sulfur-encrusted fumerole:Galapagos Islands

    Fig. 5.26

    Christian Grzimek/Photo Researchers


    Volcanic landforms l.jpg

    Volcanic Landforms

    • Shield volcanoes

    • Cinder cones

    • Sratovolcanoes or composite volcanoes

    • Domes

    • Calderas

    • Volcanic Necks and Pipes

    • Fissure Eruptions


    Shield volcanoes l.jpg

    Shield Volcanoes

    • Very large

    • Composed of low viscosity basalt

    • Volcanoes have a gentle, shield shape

    • Example: Mauna Loa, Hawaii


    Mauna loa hawaii l.jpg

    Mauna Loa, Hawaii


    Shield volcano l.jpg

    Shield Volcano

    Fig. 5.10


    Cinder cone l.jpg

    Cinder Cone

    • A relatively small volcanic cone composed of unconsolidated pyroclastic material

    • Cinder cones may be composed of basalt, andesite, or rhyolite fragments

    • Usually active for a short period of time

    • Example: Paŕicutin, Mexico


    Slide18 l.jpg

    Cinder Cone

    Fig. 5.12


    Pa icutin mexico l.jpg

    Paŕicutin, Mexico


    Pa icutin mexico20 l.jpg

    Paŕicutin, Mexico


    Cerro negro cinder cone near managua nicaragua in 1968 l.jpg

    Cerro Negro Cinder Cone, near Managua, Nicaragua in 1968

    Fig. 5.13

    Mark Hurd Aerial Surveys


    Stratovolcanoes or composite volcano l.jpg

    Stratovolcanoes or Composite Volcano

    • Steep, symmetrical volcanic cones

    • Composed of alternating layers of lava and volcanic ash

    • Usually composed of andesitic material

    • Examples: Fujiyama, Japan; Mt. Saint Helens, Wa


    Stratavolcano l.jpg

    Stratavolcano


    Fujiyama japan l.jpg

    Fujiyama, Japan


    Mount saint helens before may 1980 l.jpg

    Mount Saint Helens – Before May 1980

    Mount Saint Helens, Before May, 1980

    Emil Muench/Photo Researchers


    Mount saint helens after may 1980 l.jpg

    After May, 1980

    Mount Saint Helens – After May, 1980

    David Weintraub/Photo Researchers


    Volcanic domes l.jpg

    Volcanic Domes

    • Small, dome or “inverted” cup-shaped landforms

    • Usually composed o rhyolie

    • Example: Lava Dome in the Mount Saint Helens crater


    Slide32 l.jpg

    Fig. 5.11


    Mount st helens lava dome l.jpg

    Mount St. Helens lava dome

    Lava

    Dome

    Fig.

    5.11

    Lyn Topinka/USGS


    Inyo obsidian domes california l.jpg

    Inyo Obsidian Domes-California

    P. L. Kresan


    Caldera l.jpg

    Caldera

    • A large, circular depression produced by the collapse of a volcano following the emptying of a subterranean magma chamber

    • Example: Crater lake, Oregon


    Formation of a caldera l.jpg

    Formation of a Caldera

    Fig. 5.16


    Crater lake oregon l.jpg

    Crater Lake, Oregon

    Fig. 5.17

    Greg Vaughn/Tom Stack


    Volcanic necks and pipes l.jpg

    Volcanic Necks and Pipes

    • Remnants of volcanic vents and conduit systems

    • Exposed after erosion has removed the surrounding, soft volcanic rubble and country rock

    • Examples: Shiprock, N.M.


    Shiprock n m l.jpg

    Shiprock, N.M.


    Fissure eruptions l.jpg

    Fissure Eruptions

    • Very extensive, sheet-like lava flows that originate from long cracks (fissures) rather than central vents or volcanoes.

    • Flood lavas or basalts are associated with this type of activity

    • Example: Columbia river basalts, Washington and Oregon


    1971 fissure eruption kilauea hawaii l.jpg

    1971 Fissure Eruption, Kilauea, Hawaii


    Fissure eruptions form lava plateaus l.jpg

    Fissure Eruptions Form Lava Plateaus

    Fig. 5.20


    Extent of columbia river basalts l.jpg

    Extent of Columbia River Basalts

    Fig. 5.22


    Columbia plateau flow basalts l.jpg

    Columbia Plateau Flow Basalts

    Fig. 5.2

    Martin G. Miller


    Relationship of volcanism and plate tectonics l.jpg

    Relationship of Volcanism and Plate Tectonics

    • Volcanoes of the Earth are associated with:

      • Plate Boundary Volcanism

        Divergent Plates

        Convergent Plate

    • Interplate Volcanism

      Hot spot or plume volcanoes


    The world s active volcanoes l.jpg

    The World’s Active Volcanoes

    Fig. 5.28


    Volcanism associated with plate tectonics l.jpg

    Volcanism Associated with Plate Tectonics

    Fig. 5.30


    Types of volcanic hazards l.jpg

    Types of Volcanic Hazards

    • Lava Flows: e.g. Hawaii, 1998

    • Gas: e.g. Lake Nyos (Cameroon), 1984

      • 1700 people killed

    • Ash fall: e.g. Mt. Pinatubo, 1991

    • Pyroclastic flows: e.g. Mt. Pelee, 1902

      • 28,000 killed

    • Lahars (mudflows): e.g. Nevado del Ruiz, 1985

      • 23,000 killed

    • Tsunami: e.g. Krakatoa, 1883

      • 36,417 killed


    Volcanic hazards l.jpg

    Volcanic Hazards

    • Basaltic lavas (flows) may cover homes and roads, but flows move so slow that there is little loss of life


    May 1990 eruption of kilauea hawaii l.jpg

    May 1990 Eruption of Kilauea, Hawaii

    James Cachero/Sygma


    January 17 2002 nyiragongo volcano d r congo l.jpg

    January 17, 2002 Nyiragongo Volcano D.R. Congo


    January 17 2002 nyiragongo volcano d r congo52 l.jpg

    January 17, 2002 Nyiragongo Volcano D.R. Congo


    January 17 2002 nyiragongo volcano d r congo53 l.jpg

    January 17, 2002 Nyiragongo Volcano D.R. Congo


    January 17 2002 nyiragongo volcano d r congo54 l.jpg

    January 17, 2002 Nyiragongo Volcano D.R. Congo


    January 17 2002 nyiragongo volcano d r congo55 l.jpg

    January 17, 2002 Nyiragongo Volcano D.R. Congo


    Pyroclastic activity l.jpg

    Pyroclastic Activity

    • Usually rapid and explosive, accompanied by large volumes of poisonous gases. Can produce large losses of life and property.


    Vesuvian type pyroclastic eruption l.jpg

    Vesuvian Type Pyroclastic Eruption

    • Mount Vesuvius, Italy (79 A.D.)

    • Three day rain of volcanic ash buried the cites of Pompeii and Herculaneum

    • The cities along with >2000 people were buried intact by large ash falls.


    Slide60 l.jpg

    Escaping a Pyroclastic Flow at Mount Unzen, Japan, 1991A type of Nuee Ardente (“glowing ash flow” eruption)

    Fig. 5.9

    AP/Wide World Photos


    Mt pelee 1902 l.jpg

    Mt. Pelee, 1902


    Pyroclastic flow from the 1998 eruption on montserrat l.jpg

    Pyroclastic Flow from the 1998 Eruption on Montserrat

    R.S.J. Sparks


    Phreatic explosion l.jpg

    Phreatic explosion

    • Produced by groundwater seepage into the interior of a volcano

    • Water is converted into superheated steam with subsequent explosive release (flash vaporization)

    • Example – Krakatoa, Indonesia (1883) >100 megaton explosion; 36,000 people killed by tsunami or “tidal wave” produced by the explosion


    Slide65 l.jpg

    Fig. 5.18

    Maritime Safety Agency, Japan


    Volcanic mudflows lahars l.jpg

    Volcanic Mudflows - Lahars

    • Hot volcanic gases and phyroclastic eruptions can melt glacial ice on the flanks of volcanoes, producing a fast moving wall of mud that can travel tens of miles

    • Example Nevado del Ruíz, Colombian Andes (1985) 20,000 deaths


    Lahar from nevado del ru z 1985 l.jpg

    Lahar from Nevado del Ruíz (1985)

    Barbara and Robert Decker


    U s active volcanoes l.jpg

    U.S. Active Volcanoes


  • Login