Global Tectonics: Plates and Plumes Flashcards
How does continental drift relate to plate tectonics?
Wegner saw the continents as a jigsaw puzzle that fit together into a prior single supercontinent, Pangea, surrounded by the sea Panthalassa
The earth is made up of what 3 layers?
- core
- mantle
- crust
The crust:
- Is where we live
The Earth’s crust is made of:
- Continental and Oceanic crust
Continental crust
- 10-70km thick
- Buoyant (less dense than oceanic)
- Mostly old
Oceanic Crust
- Thin (~7km)
- Dense (sinks under continental crust
- Young
How many plates is the earths crust divided in to?
The earth is divided into 12 major plates which are moved in various directions
What does the word tectonic refer to?
It refers to the deformation of the crust as a consequence of plate interaction
Plates are made of:
rigid lithosphere
What lies beneath the tectonic plates?
- The asthenosphere
The lithosphere makes up:
The tectonic plates
Plate Movement
Plates of lithosphere are moved around by the underlying hot mantle connection cells
Plate Tectonic Theory
- Strong lithospheric plates move atop the weaker, plastic asthenosphere
- Deformation occurs at or near the edges of plates where they interact with other plates
- The interiors of the plates are relatively undeformed
Three types of plate boundary:
- Divergent
- Convergent
- Transform
Divergent plate boundaries
- Show the creation of new oceanic lithosphere from the upwelling mafic magmas as well as a widening of the ocean basin
Eg.) Iceland is an example of a mid-ocean ridge exposed above sea level - widening at the rate of ~4 mm/year
Convergent Boundaries
Three types:
- Continent-oceanic crust collision
- Ocean-ocean collision
- Continent-continent collision
Oceanic-continental boundary
- Much of the western boundary of South America is this type of boundary.
- Denser oceanic lithosphere flexes under the less dense, much older, continental crust.
- When oceanic and continental plates converge, the oceanic plate must subduct beneath the continental plate because the density of thick continental crust is too low to permit it to sink into the asthenosphere
Oceanic-oceanic boundary
- When a convergent boundary forms between plates of oceanic lithosphere, the plate that is older, thicker, and denser subduct the less dense plate.
- Several areas of the western Pacific typify this boundary, such as the area around Japan
How is a Subduction Zone formed?
They are formed when two oceanic plates collide. One runs over the other which causes it to sink into the mantle
Continental-continental boundaries
When subduction brings two continents together limited subduction may occur, but the buoyancy of continental crus eventually stops the subduction. The contraction of crust in the collision zone doubles the thickness of continental crust and creates high mountains.
Volcanoes are formed by:
- Subduction
- Rifting
- Hotspots
Hotspots
- Form where narrow columns (plumes) of unusually hot mantle convectively rise from the core-mantle boundary
- They leave tracks on moving plates.
Plumes
are an upwelling of abnormally hot rock within earths mantle. They are stationary in the mantle and other data indicates that they move slowly, if at all