what do you already know? what do you want to learn? seec ecuador 2010 presentation by: mary d....
TRANSCRIPT
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What do you already know?
What do you want to learn?
SEEC Ecuador 2010Presentation by:Mary D. CurtisBrittany L. Heller iwith.org
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• Continental Drift – theory, first advanced by Alfred Wegener, that Earth's continents were originally one land mass. Pieces of the land mass split off and migrated to form the continents.
• Plate Tectonics – theory that the Earth's crust and upper mantle (the lithosphere) is broken into a number of more or less rigid, but constantly moving, segments or plates.
• Plate boundary – The place where two or more plates in the Earth's crust meet.
• Lithosphere – the rigid, brittle layer made up of the crust and the uppermost part of the mantle. It is broken up into pieces called tectonic plates.
• Plates – large pieces of the lithosphere that slowly move on top of the mantle. There are seven primary plates and many smaller ones.
• Convection – transfer of heat by movement of a fluid. Example: (Convection currents in the mantle occur because hot rock in
the lower part of the mantle is less dense and rises, and cooler rock in the upper part of the mantle cools, becomes more dense, and sinks. Mantle convection is thought to be the mechanism driving the movement of tectonic plates.)
Terms To Know
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• Divergent Plate Boundaries – where plates are moving apart and new crust is being created. Also called Spreading Center, Rift Valley, Sea-floor spreading, Mid-oceanic Ridge.
• Convergent Plate Boundaries – where plates are moving together• Transform Plate Boundaries – where plates slide past one another. Example:
San Andreas Fault• Subduction – the process by which one tectonic plate sinks below another,
returning to the mantle where the rock is re-melted. Subduction takes place at convergent plate boundaries
• Hot spots – isolated, roughly circular plumes of melted rock (magma) that rise from deep in the mantle (Mantle Plume) to the earth's surface
• Volcano – a vent (opening) in the Earth’s surface through which magma erupts• Composite volcano – a steep-sided volcano built by lava flows and deposits• Magma – melted rock below the Earth’s surface• Lava – term used for magma once it has erupted onto the Earth's surface• Shield Volcano – a broad volcano with repeated non-explosive eruptions of
basalt that forms a low dome or shield• Archipelago – a group of islands
Terms To Know
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Lithosphere = The crust and part of the upper mantle
–The crust is broken into small parts called plates
–Plates move due to the movement of the magma in the upper mantle
–Magma moves due to convection (heating & cooling of magma)
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Continental Drift Theory (Alfred Wegener):- Continents once formed supercontinent,
Pangaea, that later broke apart.
- Look at the map and see how continents “fit.”
Theory of Plate Tectonics
geology.rutgers.edu
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Plate Tectonics:- Crust is broken into many small and large plates- Plates “float” on top of magma in upper mantle- Magma moves due to convection- Plates move toward, away, and next to one another - Plate movement causes: - Mountains and valleys to form- Natural hazards like earthquakes, volcanoes,
tsunamis, landslides, lahars, etc.
Theory of Plate Tectonics
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• Oceanic plates - denser rock composition located below the ocean water
• Continental plates – lighter rock composition located below the continents
• Three types of Plate Boundaries• Divergent• Convergent• Transform (also called Transverse)
Types of Plates & Plate Boundaries
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Types of Plates & Plate Boundaries
Transform
DivergentConvergent
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Divergent Boundaries• Boundary between two plates
that are moving apart or rifting
• A valley forms with some active volcanoes along center – On land: Rift Valley– In the Ocean: Seafloor
spreading, Mid-Oceanic Ridges
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Convergent Boundaries• Boundaries between two plates that are
colliding (coming together)• There are 2 types:
– Type 1: Oceanic plate to
Continental plate (subduction)– Type 2: Same plates move towards each
other (collide)
divediscover.whoi.edu
geologytimes.com
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Convergent 1: Subduction Zone• Oceanic plate colliding with a less dense
continental plate• Oceanic plate moves beneath the
continental plate; it melts into mantle.• Volcanoes (mountains), trenches,
earthquakes occur at subduction zones. (Ex. Andes Mts.)
livescience.com
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Convergent 2: Colliding Plates (Same Composition)
• A continental (or oceanic) plate colliding with another continental (or oceanic) plate
• Have Collision Zones: a place where folded mountains form.
- Earthquakes, landslidesConvergence3.gif
atmos.washington.edu
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Transform Fault Boundaries• Plates slide past each other causing a rubbing
motion.• Motion causes earthquakes
inkycircus.comsanandreas.jpggeomaps.wr.usgs.gov
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Ecuador: A Latin American
Plate Tectonics Example
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• Continental Drift – theory, first advanced by Alfred Wegener, that Earth's continents were originally one land mass. Pieces of the land mass split off and migrated to form the continents.
• Plate Tectonics – theory that the Earth's crust and upper mantle (the lithosphere) is broken into a number of more or less rigid, but constantly moving, segments or plates.
• Plate boundary – The place where two or more plates in the Earth's crust meet.
• Lithosphere – the rigid, brittle layer made up of the crust and the uppermost part of the mantle. It is broken up into pieces called tectonic plates.
• Plates – large pieces of the lithosphere that slowly move on top of the mantle. There are seven primary plates and many smaller ones.
• Convection – transfer of heat by movement of a fluid. Example: (Convection currents in the mantle occur because hot rock in
the lower part of the mantle is less dense and rises, and cooler rock in the upper part of the mantle cools, becomes more dense, and sinks. Mantle convection is thought to be the mechanism driving the movement of tectonic plates.)
Terms To Know
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• Divergent Plate Boundaries – where plates are moving apart and new crust is being created. Also called Spreading Center, Rift Valley, Sea-floor spreading, Mid-oceanic Ridge.
• Convergent Plate Boundaries – where plates are moving together• Transform Plate Boundaries – where plates slide past one another. Example:
San Andreas Fault• Subduction – the process by which one tectonic plate sinks below another,
returning to the mantle where the rock is re-melted. Subduction takes place at convergent plate boundaries
• Hot spots – isolated, roughly circular plumes of melted rock (magma) that rise from deep in the mantle (Mantle Plume) to the earth's surface
• Volcano – a vent (opening) in the Earth’s surface through which magma erupts• Composite volcano – a steep-sided volcano built by lava flows and deposits• Magma – melted rock below the Earth’s surface• Lava – term used for magma once it has erupted onto the Earth's surface• Shield Volcano – a broad volcano with repeated non-explosive eruptions of
basalt that forms a low dome or shield• Archipelago – a group of islands
Terms To Know
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http://www.trekearth.com/gallery/South_America/Ecuador/photo1150399.htm
Ecuador: Land of Tectonic Activity
Fact: Nine large plates and a number of smaller plates on EarthKey Terms: Plate Boundaries: Convergent, Divergent, Transform
http://facstaff.gpc.edu/~pgore/Earth&Space/GPS/platetect.html
What do you already know?
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geol.umd.edu
Nazca Plate is moving away from the Cocos Plate in a South, southwest direction (Divergent Plate Boundary).
A small area of the Nazca Plate (northwest of the Galapagos) is rubbing along the Cocos Plate (Transform Plate Boundary).Nazca Plate moving toward and
under the South American Plate (Convergent Plate Boundary).
Plate Boundaries: Ecuador
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oceanexplorer.noaa.gov
The Galapagos Islands are formed by a Hot Spot.
A Hot Spot is an area on a plate where magma wells up in what is called a Mantle Plume. When the magma reaches the surface in the ocean, islands are formed.
facility.unavco.org
Ecuador experiences a divergent (spreading zone) and transform plate boundary near the Galapagos Islands.
The Galapagos
Plate Boundaries Near Galapagos Transform
Hot Spot
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tulane.edu
cotf.edu
• Create a series of islands.• Move with the plate movement.
• Islands directly over the mantle plume have active volcanoes (Shield Volcanoes).
• Islands erode over time and may become sea mounts.
Hot Spots
Shield Volcanoes - relatively low, broad volcanoes with repeated non-explosive eruptions of basalt that form a low dome or shield-like shape.
http://pubs.usgs.gov/gip/dynamic/world_map.html
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The Northern Galápagos is made up of Wolf, Darwin, Pinta, Marchena, and Genovesa islands. These islands may have formed from the hotspot “leaking” northward.
The Central Galápagos comprises three main islands, San Cristobal, Santa Cruz and Floreana and is where most of the population of the Galápagos lives.
The Western Galápagos are made up of Isabela and Fernandina. These are the youngest islands in the archipelago with the most active volcanoes.
bizz-101.com
The Galápagos is a group of volcanic islands (archipelago); each of the 13 major islands is made up of at least one volcano. The Galápagos Islands have three different geographic and geologic regions: Northern, Central, and Western.
Northern
WesternCentral
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fuvirese.org
pugsjones.wikispaces.com
Geologic Formations:• Mountain Ranges/ Volcanic Arc• Volcanoes• Ocean Trenches• Valleys
Subduction Zone
A subduction zone is a convergent plate boundary
Subduction- the process by which one tectonic plate sinks below another, returning to the mantle.
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geology.com
peer.berkeley.edu
Andes Mountains
Formed on top of a subduction zone.
(Here, the Nazca Plate is descending under the South American Plate.)
As the Nazca Plate melts, pressure and friction occur resulting in the formation of stratovolcanoes.
Stratovolcanoes
Andes Mts.
MantleMantle
Ecuador
Natural Hazards:• Earthquakes• Volcanoes• Lahars/mudslides• Tsunamis
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whirley.wordpress.com
• 30 Volcanoes (most are active)
• Stratovolcano (most dangerous)
• Active volcanoes are near population centers
• Recent eruption: Tungurahua (2010)
A Country on a Subduction Zone: Ecuador
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http://www.msnucleus.org/membership/html/jh/earth/dictionary/patedictionary.htmlhttp://csmres.jmu.edu/geollab/Fichter/PlateTect/definitions.htmlhttp://www.brighthub.com/education/homework-tips/articles/55610.aspxhttp://www.pbs.org/wgbh/aso/tryit/tectonics/intro.htmlhttp://facstaff.gpc.edu/~pgore/Earth&Space/GPS/platetect.htmlhttp://geology.rutgers.edu/https://www.cia.gov/library/publications/the-world-factbook/geos/ec.htmlgeol.umd.eduoceanexplorer.noaa.govdivediscover.whoi.eduhttp://pubs.usgs.gov/gip/dynamic/world_map.htmlpeer.berkeley.edugeology.comhttp://facility.unavco.org/highlights/2009/galapagos.htmltulane.edu