SlideShare une entreprise Scribd logo
1  sur  66
Télécharger pour lire hors ligne
VOLCANISM
The Walker School
Geology
Volcanism is a Constructive Process
   Atmosphere
   Water
   Crust




     Painting of Early Earth’s Volcanism
Current Volcanism
   Iceland
   Hawaiian Islands
   Azores
   Galapagos Islands


                        Volcanism at Hawaii’s National Park
Notable Volcanic Eruptions




                             Table 5-1, p. 135
Mount Vesuvius Continues to Errupt




                               Fig. 5-1, p. 134
Maps of the World’s Major Volcanoes

                            •550 Are Currently
                            Active

                            •About 1 dozen
                            are erupting at
                            anyone time

                            •Responsible for
                            extrusive igneous
                            rock
Viewing Volcanoes in Google Earth
Basic Volcanic Structure
Pyroclastic Materials
   Blocks
   Bombs
   Lapilli
   Ash

              Size



                     Volcanic Bomb
Lava Tubes at Volcanic National Park, HI




                                    Lava Tube
                                    in Hawaii




                                      Fig. 5-3a, p. 137
Lava Textures
Pahoehoe (pah-hoy-hoy) is            Aa (ah-ah) is characterized by a
characterized by its smooth and      rough, clinkery surface and is
often ropey or wrinkly surface and   what most viscous and hot lava
is generally formed from more        flows look like.
fluid lava flows.




                                                                  Fig. 5-4a, p. 137
Lava Composition
   Felsic Lava: high percentage (>63%) of silica, and
    trapped gasses; highest viscosity, lowest temperatures
   Andesitic Lava: (52-63%) of silica
   Mafic Lava: (45-52%) of silica + high percentage of
    Magnesium (Mg); typically occur at subduction zones
   Balsitic Lava: (45-52%) of silica + high percentage of
    Iron (Fe); typically occur at oceanic divergent pages
   Ultramafic Lava: (=<45%) of silica; lowest vicsosity,
    highest temperatures
Columnar Jointing at Devil’s Post Pile
National Monument, CA




                                         Fig. 5-5b, p. 138
Inversion of Topography
   1. Lava flows into the
    valley
   2. Lava cools and
    crystallizes, forming
    extrusive igneous rocks.
   3. Areas adjacent to
    the flow erode more
    easily then the flow
   4. Over time, an
    inversion is produced.

                               Fig. 5-6ab, p. 139
Craters of the Moon National Monument, ID
http://www.nps.gov/crmo/




                                    Fig. 5-3b, p. 137
VOLCANIC TYPES
Types of Volcanoes
Fig. 5-18, p. 149
Plutonic Bodies
Formation of a Caldera




                         Fig. 5-9a-d, p. 142
Crater Lake, OR Caldera


Caldera Floor of Crater Lake




                               Wizard Island, Crater Lake, OR
Shield Volcanos




                  Fig. 5-10a, p. 143
Shield Volcano, Mauna Loa, HI




                •Low Viscosity Basalt Flows
                •Lava fountains
                •Most common in ocean basins
Cinder Cones




               Fig. 5-11a, p. 144
Cinder Cones, Mojave Desert, CA




                •Eruptions are short-lived.
                •Large, bowl-shaped craters.
                •Ash builds up rapidly.
                •Few lava flows.
                •Lava flows typically from base of cone.
Stratovolcanoes (Composite Cones)




                             Fig. 5-13a, p. 146
Stratovolcano, Mt. Rainier, WA




From Space




             •Composed of layered sills.
             •Lahars, or volcanic mud flows are common.
             •Have steep slops near summit.
             •Lava flows from andesite.
Lahar Flows, Mt. Pinatubo, Philippines




 Mt. Pinatubo
 from Space
                                   Fig. 5-14a, p. 146
Lava Domes




             Fig. 5-15b, p. 147
Lava Dome, Mt. St. Helens, WA




 •Composed of felsic magma.
 •Formed from intermediate magma forced up under great pressure.
 •Highly unstable, will collapse under weight of rock.

                                                              Fig. 5-15a, p. 147
Mt. Saint Helens Eruption
http://www.youtube.com/watch?v=bgRnVhbfIKQ
VOLCANIC ERUPTIONS
Types of Erruptions
Fig. 5-17, p. 148
Fissure Eruptions
   Generated along a
    linear fracture
   Composed of low-
    viscosity melt
   Commonly occur along
    divergent plate
    boundaries
   Also common on the
    edges of large          Fissure eruption in Iceland
    volcanoes.
   Produces a curtain of
    fire.
Columbia River Basalt Plateau




                                Fig. 5-19, p. 150
Volcanic Explosive Index
Primary Effects of Volcanoes
   Pyroclastic Flows
   Fumaroles
   Landslides
   Ash Fall
   Earthquakes
   High Temperatures
Secondary Effects of Explosions
   Suffocation from Ash
   Asphyxiation from Volcanic Gasses
   Tsunamis
   Temperatures Decreases
Environmental Effects
   Involved in the formation of continental crust and
    offset weathering and erosion
   Provide nutrient rich soils
   By trapping clouds at their peaks, water for
    agriculture
   Agriculture based cultures are attracted to their
    bases
Volcanic Gasses
   Water Vapor
   Carbon Dioxide
   Nitrogen
   Sulfur Dioxide
   Hydrogen Sulfide
   Carbon Monoxide
   Hydrogen
   Chlorine
Gasses emitted from fumaroles at the Sulfur Works in
Lassen Volcanic National Park, CA

                                                       Fig. 5-2, p. 136
Effects of Volcanoes on Climate
   Nucleation, condensation, and sedimentation of aerosols (acid rain)
   Change in Albedo from ash cloud
   Tropospheric cooling from the addition of sulfur to the stratsophere
   Ozone destruction through the formation of atomic chlorine
SUPER ERUPTIONS
Supereruptions
http://www.pbs.org/wgbh/nova/megavolcano/about.html
Discovery Questions
   What does it take to be classified as a super
    eruption?
   When did the last one occur? Why is their
    controversy about the date?
   What would be the primary effects of such an
    eruption?
   For those who survived the initial eruption, what
    would happen in the following months, or years?
   How did the Toba explosion effect the evolution of
    humans?
DISTRIBUTION &
MONITORING
Distribution of Volcanoes
   Circum-Pacific
    Belt (60%)
   Mediterranean
    Belt (20%)
   Mid-Oceanic
    Ridges (20%)

   More common along both divergent than convergent plate boundaries.
   Mainly composed of intrusive magma flows.
   Composed of mafic magma that forms beneath spreading plates.
   Pyroclastic materials are not common because lava is fluid.
   Water pressure prevents gasses from expanding and escaping.
                                                                         Fig. 5-20, p. 151
USGS Volcano Hazards Program
http://volcanoes.usgs.gov/
Alaska’s Volcano Observatory
http://www.avo.alaska.edu/
Alaska’s Volcanoes
Cascade Volcano Observatory
http://vulcan.wr.usgs.gov/
The Cascade Range
Lassen Peak, CA




            Largest Lava Dome in the World
Lassen Peak Diagram




                      Concept Art, p. 154
Mid-Atlantic Ridge & Iceland
Formation of Surtsey Island, Iceland
http://www.youtube.com/watch?v=4MmX_i7S9u4
Important Monitoring Techniques




                              Fig. 5-23, p. 159
Fumarole Gas Monitoring
   Chemically-selective sensors
    for SO2 and CO2 measure
    gas concentrations and a wind
    sensor measures wind speed
    and direction.
   Data from solar-powered
    stations are transmitted to
    GOES geostationary satellite
    and then down to
    observatories every 10
    minutes, providing near real
    time data on degassing of
    volcanoes
Ground Deformation Monitoring
   Paint
   Electronic Distance Meters
       determine the horizontal movements
        that occur on active volcanoes
   Tiltmeters
       leveling surveys to measure vertical
        motions
   Global Positioning Systems
       allows us to measure horizontal
        motions much more accurately and
        conveniently, and also to estimate
        vertical motions in the same survey
Remote Sensing
   The Advanced Very High
    Resolution Radiometer (AVHRR)
    is a space-borne sensor
    embarked on the NOAA family
    of polar orbiting platforms.
   The primary purpose of these
    instruments is to monitor clouds
    and to measure the thermal
    emission (cooling) of the Earth.
   The main difficulty associated
    with these investigations is to
    properly deal with the many
    limitations of these instruments,
    especially in the early period
    (sensor calibration, orbital drift,
    limited spectral and directional
    sampling, etc).
WHAT ARE BLACK
SMOKERS?
Hydrothermal Vents
   Distributes heat and
    drives water circulation
    in the ocean through
    convection
   Provides energy source
    in the form of hydrogen
    sulfide to benthic
    chemotrophs
   Distributes minerals and
    influences the
    composition of the ocean
Hydrothermal Plume



                                         White
                         Black smoker   smoker

                           Sulfide
                           deposit

                         Tube worms
                     Magma White clam


                        White crab
Location of Major Vent Systems
Learn More About Vents
http://www.divediscover.whoi.edu/vents/index.html
Hydrothermal Vent Chemistry

Contenu connexe

Tendances

Types Of Volcanoes Powerpoing 2
Types Of Volcanoes Powerpoing 2Types Of Volcanoes Powerpoing 2
Types Of Volcanoes Powerpoing 2
LiveandLearn
 
igneous rocks formation and their classification
igneous rocks formation and their classificationigneous rocks formation and their classification
igneous rocks formation and their classification
Mazhar Ali
 
Chapter 4 igneous rocks
Chapter 4   igneous rocksChapter 4   igneous rocks
Chapter 4 igneous rocks
jjones0227
 
Plate Tectonics
Plate TectonicsPlate Tectonics
Plate Tectonics
itutor
 
landforms (geomorphology) presentation
landforms (geomorphology) presentationlandforms (geomorphology) presentation
landforms (geomorphology) presentation
Vera Nataa
 

Tendances (20)

Forms of igneous rocks
Forms of igneous rocksForms of igneous rocks
Forms of igneous rocks
 
Types Of Volcanoes Powerpoing 2
Types Of Volcanoes Powerpoing 2Types Of Volcanoes Powerpoing 2
Types Of Volcanoes Powerpoing 2
 
Volcanoes2009
Volcanoes2009Volcanoes2009
Volcanoes2009
 
Igneous rocks
Igneous rocksIgneous rocks
Igneous rocks
 
igneous rocks formation and their classification
igneous rocks formation and their classificationigneous rocks formation and their classification
igneous rocks formation and their classification
 
Earthquake and volcanoes
Earthquake and volcanoesEarthquake and volcanoes
Earthquake and volcanoes
 
volcanic eruptions
volcanic eruptionsvolcanic eruptions
volcanic eruptions
 
Chapter 4 igneous rocks
Chapter 4   igneous rocksChapter 4   igneous rocks
Chapter 4 igneous rocks
 
Study of Volcanism and volcano
Study of Volcanism and volcanoStudy of Volcanism and volcano
Study of Volcanism and volcano
 
Deformation and .mountain building
Deformation and  .mountain buildingDeformation and  .mountain building
Deformation and .mountain building
 
Volcanism
VolcanismVolcanism
Volcanism
 
Igneous rocks
Igneous rocksIgneous rocks
Igneous rocks
 
Plate Tectonics
Plate TectonicsPlate Tectonics
Plate Tectonics
 
landforms (geomorphology) presentation
landforms (geomorphology) presentationlandforms (geomorphology) presentation
landforms (geomorphology) presentation
 
All about - Volcanoes
All about - VolcanoesAll about - Volcanoes
All about - Volcanoes
 
Metamorphic rocks
Metamorphic rocksMetamorphic rocks
Metamorphic rocks
 
Types of Rock
Types of RockTypes of Rock
Types of Rock
 
Intrusive igneous rocks
Intrusive igneous rocks Intrusive igneous rocks
Intrusive igneous rocks
 
How are Mountains formed?
How are Mountains formed?How are Mountains formed?
How are Mountains formed?
 
Magmatism.pptx
Magmatism.pptxMagmatism.pptx
Magmatism.pptx
 

En vedette

The 3 volcano types
The 3 volcano typesThe 3 volcano types
The 3 volcano types
xi11um
 
2 Intro To Landforms And Landscapes
2 Intro To Landforms And Landscapes2 Intro To Landforms And Landscapes
2 Intro To Landforms And Landscapes
Ecumene
 
PPT - Ring of Fire
PPT - Ring of FirePPT - Ring of Fire
PPT - Ring of Fire
jaymz0949
 
Solar system 05 terrestrial planets
Solar system 05 terrestrial planetsSolar system 05 terrestrial planets
Solar system 05 terrestrial planets
BHSEarthScience
 
Factors Affecting Climate
Factors Affecting ClimateFactors Affecting Climate
Factors Affecting Climate
David Rogers
 
Landscapes presentation
Landscapes presentationLandscapes presentation
Landscapes presentation
angelammoyano
 

En vedette (20)

Topic 4 volcanism
Topic 4 volcanismTopic 4 volcanism
Topic 4 volcanism
 
8.1 Mass Movements
 8.1 Mass Movements 8.1 Mass Movements
8.1 Mass Movements
 
Lava textures
Lava texturesLava textures
Lava textures
 
Ring of fire
Ring of fireRing of fire
Ring of fire
 
Pacific ring of fire
Pacific ring of firePacific ring of fire
Pacific ring of fire
 
Teaching the Food Cycle to Students
Teaching the Food Cycle to StudentsTeaching the Food Cycle to Students
Teaching the Food Cycle to Students
 
CHMSC Lab. School Science 6 - Food Cycle
CHMSC Lab. School Science 6 - Food CycleCHMSC Lab. School Science 6 - Food Cycle
CHMSC Lab. School Science 6 - Food Cycle
 
The 3 volcano types
The 3 volcano typesThe 3 volcano types
The 3 volcano types
 
Food cycle
Food cycleFood cycle
Food cycle
 
Types of volcanoes
Types of volcanoesTypes of volcanoes
Types of volcanoes
 
2 Intro To Landforms And Landscapes
2 Intro To Landforms And Landscapes2 Intro To Landforms And Landscapes
2 Intro To Landforms And Landscapes
 
PPT - Ring of Fire
PPT - Ring of FirePPT - Ring of Fire
PPT - Ring of Fire
 
Solar system
Solar systemSolar system
Solar system
 
Solar system 05 terrestrial planets
Solar system 05 terrestrial planetsSolar system 05 terrestrial planets
Solar system 05 terrestrial planets
 
Factors Affecting Climate
Factors Affecting ClimateFactors Affecting Climate
Factors Affecting Climate
 
Types of Volcanoes
Types of VolcanoesTypes of Volcanoes
Types of Volcanoes
 
CAMBRIDGE GEOGRAPHY AS ULTRA REVISION TEST 1 HYDROLOGY
CAMBRIDGE GEOGRAPHY AS ULTRA REVISION TEST 1 HYDROLOGYCAMBRIDGE GEOGRAPHY AS ULTRA REVISION TEST 1 HYDROLOGY
CAMBRIDGE GEOGRAPHY AS ULTRA REVISION TEST 1 HYDROLOGY
 
Geomorophology presentation
Geomorophology presentationGeomorophology presentation
Geomorophology presentation
 
Landscapes presentation
Landscapes presentationLandscapes presentation
Landscapes presentation
 
Factors affecting climate
Factors affecting climateFactors affecting climate
Factors affecting climate
 

Similaire à Volcanism

Presentation on volcanos
Presentation on volcanosPresentation on volcanos
Presentation on volcanos
Anjali Patra
 
The san joaquin fault
The san joaquin faultThe san joaquin fault
The san joaquin fault
berbs27
 
Weathering/EPCC/LM5
Weathering/EPCC/LM5Weathering/EPCC/LM5
Weathering/EPCC/LM5
tcarrick
 
Field assignment part 1-2
Field assignment part 1-2Field assignment part 1-2
Field assignment part 1-2
karastangle
 
Francisco Rosas Manzo Field Lab Assingment
Francisco Rosas Manzo Field Lab AssingmentFrancisco Rosas Manzo Field Lab Assingment
Francisco Rosas Manzo Field Lab Assingment
jrosas_83
 
03 boberg 2012 iaea - wy uranium province
03 boberg 2012   iaea - wy uranium province03 boberg 2012   iaea - wy uranium province
03 boberg 2012 iaea - wy uranium province
Monatom Mgl
 

Similaire à Volcanism (20)

Volcanoes
VolcanoesVolcanoes
Volcanoes
 
Intorduction to Volcanology, Weathering, Erotion, Dispertion and Soil.
Intorduction to Volcanology, Weathering, Erotion, Dispertion and Soil.Intorduction to Volcanology, Weathering, Erotion, Dispertion and Soil.
Intorduction to Volcanology, Weathering, Erotion, Dispertion and Soil.
 
Geology of Hawai'i - Lava
Geology of Hawai'i - LavaGeology of Hawai'i - Lava
Geology of Hawai'i - Lava
 
Presentation on volcanos
Presentation on volcanosPresentation on volcanos
Presentation on volcanos
 
Volcanoes
VolcanoesVolcanoes
Volcanoes
 
Field lab part 2
Field lab part 2Field lab part 2
Field lab part 2
 
Erosion
ErosionErosion
Erosion
 
Plates of the earth
Plates of the earthPlates of the earth
Plates of the earth
 
Chapter fourteen
Chapter fourteenChapter fourteen
Chapter fourteen
 
Geology lab field assignment
Geology lab field assignmentGeology lab field assignment
Geology lab field assignment
 
Volcanoes
VolcanoesVolcanoes
Volcanoes
 
Hopson 2001 Potential Impact On Water Resources From Eruptions Near Mammoth L...
Hopson 2001 Potential Impact On Water Resources From Eruptions Near Mammoth L...Hopson 2001 Potential Impact On Water Resources From Eruptions Near Mammoth L...
Hopson 2001 Potential Impact On Water Resources From Eruptions Near Mammoth L...
 
The san joaquin fault
The san joaquin faultThe san joaquin fault
The san joaquin fault
 
Intro to volcanoes module
Intro to volcanoes moduleIntro to volcanoes module
Intro to volcanoes module
 
Weathering/EPCC/LM5
Weathering/EPCC/LM5Weathering/EPCC/LM5
Weathering/EPCC/LM5
 
Field assignment part 1-2
Field assignment part 1-2Field assignment part 1-2
Field assignment part 1-2
 
Francisco Rosas Manzo Field Lab Assingment
Francisco Rosas Manzo Field Lab AssingmentFrancisco Rosas Manzo Field Lab Assingment
Francisco Rosas Manzo Field Lab Assingment
 
03 boberg 2012 iaea - wy uranium province
03 boberg 2012   iaea - wy uranium province03 boberg 2012   iaea - wy uranium province
03 boberg 2012 iaea - wy uranium province
 
Volcanoes by James Aquilina, 4.03
Volcanoes by James Aquilina, 4.03Volcanoes by James Aquilina, 4.03
Volcanoes by James Aquilina, 4.03
 
4qdr3l2partsofavolcano-210310034653 (1).pdf
4qdr3l2partsofavolcano-210310034653 (1).pdf4qdr3l2partsofavolcano-210310034653 (1).pdf
4qdr3l2partsofavolcano-210310034653 (1).pdf
 

Plus de tcooper66

Designing And Leading Collaborative Projects
Designing And Leading Collaborative ProjectsDesigning And Leading Collaborative Projects
Designing And Leading Collaborative Projects
tcooper66
 
C:\Fakepath\Designing And Managing Collaborative Projects
C:\Fakepath\Designing And Managing Collaborative ProjectsC:\Fakepath\Designing And Managing Collaborative Projects
C:\Fakepath\Designing And Managing Collaborative Projects
tcooper66
 
Ge Tutorials Part Vi Design Principles
Ge Tutorials Part Vi   Design PrinciplesGe Tutorials Part Vi   Design Principles
Ge Tutorials Part Vi Design Principles
tcooper66
 
GE Tutorials Part VI Design Principles
GE Tutorials Part VI   Design PrinciplesGE Tutorials Part VI   Design Principles
GE Tutorials Part VI Design Principles
tcooper66
 
Cooper Family Reunion 2009
Cooper Family Reunion 2009Cooper Family Reunion 2009
Cooper Family Reunion 2009
tcooper66
 
Kml Basics Chpt 5 Overlays
Kml Basics Chpt  5   OverlaysKml Basics Chpt  5   Overlays
Kml Basics Chpt 5 Overlays
tcooper66
 
Kml Basics Chpt 4 Styles &amp; Icons
Kml Basics Chpt  4   Styles &amp; IconsKml Basics Chpt  4   Styles &amp; Icons
Kml Basics Chpt 4 Styles &amp; Icons
tcooper66
 
Kml Basics Chpt 3 Geometry
Kml Basics Chpt  3   GeometryKml Basics Chpt  3   Geometry
Kml Basics Chpt 3 Geometry
tcooper66
 
Kml Basics Chpt 2 Placemarks
Kml Basics Chpt  2   PlacemarksKml Basics Chpt  2   Placemarks
Kml Basics Chpt 2 Placemarks
tcooper66
 
Kml Basics Chpt 1 Overview
Kml Basics Chpt  1   OverviewKml Basics Chpt  1   Overview
Kml Basics Chpt 1 Overview
tcooper66
 

Plus de tcooper66 (20)

Java Koch Curves
Java Koch CurvesJava Koch Curves
Java Koch Curves
 
Java tree fractals
Java tree fractalsJava tree fractals
Java tree fractals
 
Waitomo slideshow
Waitomo slideshowWaitomo slideshow
Waitomo slideshow
 
Energy Facts and Fiction
Energy Facts and FictionEnergy Facts and Fiction
Energy Facts and Fiction
 
Designing And Leading Collaborative Projects
Designing And Leading Collaborative ProjectsDesigning And Leading Collaborative Projects
Designing And Leading Collaborative Projects
 
C:\Fakepath\Designing And Managing Collaborative Projects
C:\Fakepath\Designing And Managing Collaborative ProjectsC:\Fakepath\Designing And Managing Collaborative Projects
C:\Fakepath\Designing And Managing Collaborative Projects
 
Ge Tutorials Part Vi Design Principles
Ge Tutorials Part Vi   Design PrinciplesGe Tutorials Part Vi   Design Principles
Ge Tutorials Part Vi Design Principles
 
GE Tutorials Part VI Design Principles
GE Tutorials Part VI   Design PrinciplesGE Tutorials Part VI   Design Principles
GE Tutorials Part VI Design Principles
 
Ge Tutorials Part V Embedding Objects
Ge Tutorials Part V   Embedding ObjectsGe Tutorials Part V   Embedding Objects
Ge Tutorials Part V Embedding Objects
 
Cooper Family Reunion 2009
Cooper Family Reunion 2009Cooper Family Reunion 2009
Cooper Family Reunion 2009
 
Kml Basics Chpt 5 Overlays
Kml Basics Chpt  5   OverlaysKml Basics Chpt  5   Overlays
Kml Basics Chpt 5 Overlays
 
Kml Basics Chpt 4 Styles &amp; Icons
Kml Basics Chpt  4   Styles &amp; IconsKml Basics Chpt  4   Styles &amp; Icons
Kml Basics Chpt 4 Styles &amp; Icons
 
Kml Basics Chpt 3 Geometry
Kml Basics Chpt  3   GeometryKml Basics Chpt  3   Geometry
Kml Basics Chpt 3 Geometry
 
Kml Basics Chpt 2 Placemarks
Kml Basics Chpt  2   PlacemarksKml Basics Chpt  2   Placemarks
Kml Basics Chpt 2 Placemarks
 
Kml Basics Chpt 1 Overview
Kml Basics Chpt  1   OverviewKml Basics Chpt  1   Overview
Kml Basics Chpt 1 Overview
 
Creating Tours in Google Earth
Creating Tours in Google EarthCreating Tours in Google Earth
Creating Tours in Google Earth
 
Google Earth Tutorials Part III
Google Earth Tutorials Part IIIGoogle Earth Tutorials Part III
Google Earth Tutorials Part III
 
Wind Energy
Wind EnergyWind Energy
Wind Energy
 
Google Earth Tutorials Part II
Google Earth Tutorials Part IIGoogle Earth Tutorials Part II
Google Earth Tutorials Part II
 
Google Earth Tutorials - Part I
Google Earth Tutorials - Part IGoogle Earth Tutorials - Part I
Google Earth Tutorials - Part I
 

Dernier

Histor y of HAM Radio presentation slide
Histor y of HAM Radio presentation slideHistor y of HAM Radio presentation slide
Histor y of HAM Radio presentation slide
vu2urc
 
CNv6 Instructor Chapter 6 Quality of Service
CNv6 Instructor Chapter 6 Quality of ServiceCNv6 Instructor Chapter 6 Quality of Service
CNv6 Instructor Chapter 6 Quality of Service
giselly40
 

Dernier (20)

Handwritten Text Recognition for manuscripts and early printed texts
Handwritten Text Recognition for manuscripts and early printed textsHandwritten Text Recognition for manuscripts and early printed texts
Handwritten Text Recognition for manuscripts and early printed texts
 
08448380779 Call Girls In Friends Colony Women Seeking Men
08448380779 Call Girls In Friends Colony Women Seeking Men08448380779 Call Girls In Friends Colony Women Seeking Men
08448380779 Call Girls In Friends Colony Women Seeking Men
 
Boost Fertility New Invention Ups Success Rates.pdf
Boost Fertility New Invention Ups Success Rates.pdfBoost Fertility New Invention Ups Success Rates.pdf
Boost Fertility New Invention Ups Success Rates.pdf
 
2024: Domino Containers - The Next Step. News from the Domino Container commu...
2024: Domino Containers - The Next Step. News from the Domino Container commu...2024: Domino Containers - The Next Step. News from the Domino Container commu...
2024: Domino Containers - The Next Step. News from the Domino Container commu...
 
Histor y of HAM Radio presentation slide
Histor y of HAM Radio presentation slideHistor y of HAM Radio presentation slide
Histor y of HAM Radio presentation slide
 
🐬 The future of MySQL is Postgres 🐘
🐬  The future of MySQL is Postgres   🐘🐬  The future of MySQL is Postgres   🐘
🐬 The future of MySQL is Postgres 🐘
 
Powerful Google developer tools for immediate impact! (2023-24 C)
Powerful Google developer tools for immediate impact! (2023-24 C)Powerful Google developer tools for immediate impact! (2023-24 C)
Powerful Google developer tools for immediate impact! (2023-24 C)
 
Mastering MySQL Database Architecture: Deep Dive into MySQL Shell and MySQL R...
Mastering MySQL Database Architecture: Deep Dive into MySQL Shell and MySQL R...Mastering MySQL Database Architecture: Deep Dive into MySQL Shell and MySQL R...
Mastering MySQL Database Architecture: Deep Dive into MySQL Shell and MySQL R...
 
Understanding Discord NSFW Servers A Guide for Responsible Users.pdf
Understanding Discord NSFW Servers A Guide for Responsible Users.pdfUnderstanding Discord NSFW Servers A Guide for Responsible Users.pdf
Understanding Discord NSFW Servers A Guide for Responsible Users.pdf
 
Partners Life - Insurer Innovation Award 2024
Partners Life - Insurer Innovation Award 2024Partners Life - Insurer Innovation Award 2024
Partners Life - Insurer Innovation Award 2024
 
Exploring the Future Potential of AI-Enabled Smartphone Processors
Exploring the Future Potential of AI-Enabled Smartphone ProcessorsExploring the Future Potential of AI-Enabled Smartphone Processors
Exploring the Future Potential of AI-Enabled Smartphone Processors
 
From Event to Action: Accelerate Your Decision Making with Real-Time Automation
From Event to Action: Accelerate Your Decision Making with Real-Time AutomationFrom Event to Action: Accelerate Your Decision Making with Real-Time Automation
From Event to Action: Accelerate Your Decision Making with Real-Time Automation
 
Presentation on how to chat with PDF using ChatGPT code interpreter
Presentation on how to chat with PDF using ChatGPT code interpreterPresentation on how to chat with PDF using ChatGPT code interpreter
Presentation on how to chat with PDF using ChatGPT code interpreter
 
Apidays Singapore 2024 - Building Digital Trust in a Digital Economy by Veron...
Apidays Singapore 2024 - Building Digital Trust in a Digital Economy by Veron...Apidays Singapore 2024 - Building Digital Trust in a Digital Economy by Veron...
Apidays Singapore 2024 - Building Digital Trust in a Digital Economy by Veron...
 
Axa Assurance Maroc - Insurer Innovation Award 2024
Axa Assurance Maroc - Insurer Innovation Award 2024Axa Assurance Maroc - Insurer Innovation Award 2024
Axa Assurance Maroc - Insurer Innovation Award 2024
 
Boost PC performance: How more available memory can improve productivity
Boost PC performance: How more available memory can improve productivityBoost PC performance: How more available memory can improve productivity
Boost PC performance: How more available memory can improve productivity
 
CNv6 Instructor Chapter 6 Quality of Service
CNv6 Instructor Chapter 6 Quality of ServiceCNv6 Instructor Chapter 6 Quality of Service
CNv6 Instructor Chapter 6 Quality of Service
 
TrustArc Webinar - Stay Ahead of US State Data Privacy Law Developments
TrustArc Webinar - Stay Ahead of US State Data Privacy Law DevelopmentsTrustArc Webinar - Stay Ahead of US State Data Privacy Law Developments
TrustArc Webinar - Stay Ahead of US State Data Privacy Law Developments
 
A Domino Admins Adventures (Engage 2024)
A Domino Admins Adventures (Engage 2024)A Domino Admins Adventures (Engage 2024)
A Domino Admins Adventures (Engage 2024)
 
Evaluating the top large language models.pdf
Evaluating the top large language models.pdfEvaluating the top large language models.pdf
Evaluating the top large language models.pdf
 

Volcanism

  • 2. Volcanism is a Constructive Process  Atmosphere  Water  Crust Painting of Early Earth’s Volcanism
  • 3. Current Volcanism  Iceland  Hawaiian Islands  Azores  Galapagos Islands Volcanism at Hawaii’s National Park
  • 4. Notable Volcanic Eruptions Table 5-1, p. 135
  • 5. Mount Vesuvius Continues to Errupt Fig. 5-1, p. 134
  • 6. Maps of the World’s Major Volcanoes •550 Are Currently Active •About 1 dozen are erupting at anyone time •Responsible for extrusive igneous rock
  • 7. Viewing Volcanoes in Google Earth
  • 9. Pyroclastic Materials  Blocks  Bombs  Lapilli  Ash Size Volcanic Bomb
  • 10. Lava Tubes at Volcanic National Park, HI Lava Tube in Hawaii Fig. 5-3a, p. 137
  • 11. Lava Textures Pahoehoe (pah-hoy-hoy) is Aa (ah-ah) is characterized by a characterized by its smooth and rough, clinkery surface and is often ropey or wrinkly surface and what most viscous and hot lava is generally formed from more flows look like. fluid lava flows. Fig. 5-4a, p. 137
  • 12. Lava Composition  Felsic Lava: high percentage (>63%) of silica, and trapped gasses; highest viscosity, lowest temperatures  Andesitic Lava: (52-63%) of silica  Mafic Lava: (45-52%) of silica + high percentage of Magnesium (Mg); typically occur at subduction zones  Balsitic Lava: (45-52%) of silica + high percentage of Iron (Fe); typically occur at oceanic divergent pages  Ultramafic Lava: (=<45%) of silica; lowest vicsosity, highest temperatures
  • 13. Columnar Jointing at Devil’s Post Pile National Monument, CA Fig. 5-5b, p. 138
  • 14. Inversion of Topography  1. Lava flows into the valley  2. Lava cools and crystallizes, forming extrusive igneous rocks.  3. Areas adjacent to the flow erode more easily then the flow  4. Over time, an inversion is produced. Fig. 5-6ab, p. 139
  • 15. Craters of the Moon National Monument, ID http://www.nps.gov/crmo/ Fig. 5-3b, p. 137
  • 20. Formation of a Caldera Fig. 5-9a-d, p. 142
  • 21. Crater Lake, OR Caldera Caldera Floor of Crater Lake Wizard Island, Crater Lake, OR
  • 22. Shield Volcanos Fig. 5-10a, p. 143
  • 23. Shield Volcano, Mauna Loa, HI •Low Viscosity Basalt Flows •Lava fountains •Most common in ocean basins
  • 24. Cinder Cones Fig. 5-11a, p. 144
  • 25. Cinder Cones, Mojave Desert, CA •Eruptions are short-lived. •Large, bowl-shaped craters. •Ash builds up rapidly. •Few lava flows. •Lava flows typically from base of cone.
  • 26. Stratovolcanoes (Composite Cones) Fig. 5-13a, p. 146
  • 27. Stratovolcano, Mt. Rainier, WA From Space •Composed of layered sills. •Lahars, or volcanic mud flows are common. •Have steep slops near summit. •Lava flows from andesite.
  • 28. Lahar Flows, Mt. Pinatubo, Philippines Mt. Pinatubo from Space Fig. 5-14a, p. 146
  • 29. Lava Domes Fig. 5-15b, p. 147
  • 30. Lava Dome, Mt. St. Helens, WA •Composed of felsic magma. •Formed from intermediate magma forced up under great pressure. •Highly unstable, will collapse under weight of rock. Fig. 5-15a, p. 147
  • 31. Mt. Saint Helens Eruption http://www.youtube.com/watch?v=bgRnVhbfIKQ
  • 35. Fissure Eruptions  Generated along a linear fracture  Composed of low- viscosity melt  Commonly occur along divergent plate boundaries  Also common on the edges of large Fissure eruption in Iceland volcanoes.  Produces a curtain of fire.
  • 36. Columbia River Basalt Plateau Fig. 5-19, p. 150
  • 38. Primary Effects of Volcanoes  Pyroclastic Flows  Fumaroles  Landslides  Ash Fall  Earthquakes  High Temperatures
  • 39. Secondary Effects of Explosions  Suffocation from Ash  Asphyxiation from Volcanic Gasses  Tsunamis  Temperatures Decreases
  • 40. Environmental Effects  Involved in the formation of continental crust and offset weathering and erosion  Provide nutrient rich soils  By trapping clouds at their peaks, water for agriculture  Agriculture based cultures are attracted to their bases
  • 41. Volcanic Gasses  Water Vapor  Carbon Dioxide  Nitrogen  Sulfur Dioxide  Hydrogen Sulfide  Carbon Monoxide  Hydrogen  Chlorine Gasses emitted from fumaroles at the Sulfur Works in Lassen Volcanic National Park, CA Fig. 5-2, p. 136
  • 42. Effects of Volcanoes on Climate  Nucleation, condensation, and sedimentation of aerosols (acid rain)  Change in Albedo from ash cloud  Tropospheric cooling from the addition of sulfur to the stratsophere  Ozone destruction through the formation of atomic chlorine
  • 45. Discovery Questions  What does it take to be classified as a super eruption?  When did the last one occur? Why is their controversy about the date?  What would be the primary effects of such an eruption?  For those who survived the initial eruption, what would happen in the following months, or years?  How did the Toba explosion effect the evolution of humans?
  • 47. Distribution of Volcanoes  Circum-Pacific Belt (60%)  Mediterranean Belt (20%)  Mid-Oceanic Ridges (20%)  More common along both divergent than convergent plate boundaries.  Mainly composed of intrusive magma flows.  Composed of mafic magma that forms beneath spreading plates.  Pyroclastic materials are not common because lava is fluid.  Water pressure prevents gasses from expanding and escaping. Fig. 5-20, p. 151
  • 48. USGS Volcano Hazards Program http://volcanoes.usgs.gov/
  • 53. Lassen Peak, CA  Largest Lava Dome in the World
  • 54. Lassen Peak Diagram Concept Art, p. 154
  • 56. Formation of Surtsey Island, Iceland http://www.youtube.com/watch?v=4MmX_i7S9u4
  • 57. Important Monitoring Techniques Fig. 5-23, p. 159
  • 58. Fumarole Gas Monitoring  Chemically-selective sensors for SO2 and CO2 measure gas concentrations and a wind sensor measures wind speed and direction.  Data from solar-powered stations are transmitted to GOES geostationary satellite and then down to observatories every 10 minutes, providing near real time data on degassing of volcanoes
  • 59. Ground Deformation Monitoring  Paint  Electronic Distance Meters  determine the horizontal movements that occur on active volcanoes  Tiltmeters  leveling surveys to measure vertical motions  Global Positioning Systems  allows us to measure horizontal motions much more accurately and conveniently, and also to estimate vertical motions in the same survey
  • 60. Remote Sensing  The Advanced Very High Resolution Radiometer (AVHRR) is a space-borne sensor embarked on the NOAA family of polar orbiting platforms.  The primary purpose of these instruments is to monitor clouds and to measure the thermal emission (cooling) of the Earth.  The main difficulty associated with these investigations is to properly deal with the many limitations of these instruments, especially in the early period (sensor calibration, orbital drift, limited spectral and directional sampling, etc).
  • 62. Hydrothermal Vents  Distributes heat and drives water circulation in the ocean through convection  Provides energy source in the form of hydrogen sulfide to benthic chemotrophs  Distributes minerals and influences the composition of the ocean
  • 63. Hydrothermal Plume White Black smoker smoker Sulfide deposit Tube worms Magma White clam White crab
  • 64. Location of Major Vent Systems
  • 65. Learn More About Vents http://www.divediscover.whoi.edu/vents/index.html