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Tectonic & Seismic Hazards
Volcanoes
The outer layer we live on. 0-60 km thick. Can be
either continental or oceanic.
Semi-molten rock (magma), 2900km thick
Liquid. Made up of iron and nickel
Solid. Hottest part (55000 c), made up of
iron and nickel
• A theory that explains the
global distribution of
earthquakes, active
volcanoes, mountains and
other geologic features
by the movement of large
fragments of the of the
Earth’s crust
• Evidence includes
continental drift &
seafloor spreading
• Earth’s crust is broken into plates
and convection currents in the
mantle cause the movement of
these plates (conveyor belts)
• The tectonic setting of a region
determines if there will be any
volcanoes present and, if so, what
type
Spatial
distribution of
volcanoes is
related to plate
boundaries and
hot spots
Approx. 1500
active volcanoes
Approx. 2/3
volcano activity
occurs along the
‘Ring of Fire’
Mid-ocean ridges Subduction zonesHot Spots
Volcanoes occur at:
• Plates moving away from one
another, basaltic magma rises
to create new crust
• Can also occur on continents –
East Africa rift zone
• Plates moving towards each other.
Denser plate forced under less
dense plate and melts to become
magma. Magma rises to form
volcano
• Typically explosive in nature
Note: all three processes can occur under water or on land
Individual plumes of
magma rise to the crust
Chain of volcanoes produced as the plate moves over the hot spot
Located in the upper mantle and asthenosphere
Fueled by a high concentration of radioactive materials (energy source)
As the plate moves:
Location of volcanic features migrate
Hot spot remains in same location
Hot Spot Volcanoes
• A chain of volcanoes extends
northwest from the big island of
Hawaii
• The age of the volcanoes
gradually increase in this
direction
• The youngest volcano is Loihi (active
submarine volcano)
• The oldest above water volcano is
Kauai (4-6 million years old)
• At the far end of the chain, submarine
volcanoes, now eroded into
seamounts, can be dated to 78 million
years old
Direction of
plate movement
Hawaii, ocean hot spot
Yellowstone National Park,
continental hot spot
Direction of
plate movement
SHIELD VOLCANO
Largest, but much wider than they are tall
Gently sloping slides and broad summits
Non-explosive eruptions of very low-viscosity, basaltic magmas
Lava erupts through openings, or vents, in the volcano and flows down the sides
Muana Loa, Hawaii
Last eruption 1984
Skjaldbreidur, Iceland
Last eruption 9000 years ago
Piton de la Fournaise,
Reunion Island (France)
Last eruption 2017
COMPOSITE VOLCANO
(STRATOVOLCANOES)
Interlayered lava and pyroclastic deposits (debris blown from a volcano during an explosion)
Cone-shaped with steep sides
Combination of lava flow and explosive activity
Responsible for most of the death and destruction in history
Mt. Pinatubo, Phillipines
Mt. Fuji, Japan
Canadian Examples: Mount Meager
& Mount Garibaldi - dormant
Review: https://www.youtube.com/watch?v=yDy28QtdYJY
Watch first 12 minutes: https://www.youtube.com/watch?v=KlbnLnHSRzE
What are secondary
hazards of volcanoes?
MIND MAP PROJECT ( / 20)
Criteria:
• Minimum five secondary hazards (main
themes)
• Each theme needs to include further
detail – could be key facts about the
hazard, examples of when the hazard has
occurred and/or images & diagrams
• Mind map should be organized so
branches go from more general (main
themes) to more specific (detail)
• Use different colours and/or line types to
help distinguish between your main
themes
• Main questing, “What are secondary
hazards of volcanoes?” written in the
centre
What are secondary
hazards of volcanoes?
/5
/10
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