Rocks and weathering 3.1 Flashcards
1
Q
What are the three mechanisms of plate movement?
A
- Ridge push: intrusion of magma into the spreading ocean ridges such as the Mid-Atlantic ridge propels plates apart.
- Convection drag: convection currents in the plastic mantle drag the overlying lithosphere.
- Slab pull: cold and dense lithosphere sinking due to gravity pulls the rest of the plate with it.
2
Q
Convergent plate boundaries: continental/oceanic
A
- Form fold mountains and ocean trenches
- Less dense, oceanic plate subducts beneath the continental plate.
- Subduction causes layers of rock to be forced upwards causing anticlines and synclines - fold mountains.
- Material at depth is also forced downwards, deepening crust in the mountain belt.
- Sediments scraped off the plate and in the trench builds up an accretionary wedge.
- Subducted plate is partially melted and small pockets of magma rise to form volcanoes - orogenesis.
- The ocean floor drops steeply to form an ocean trench.
- Sloping zone of earthquake foci is known as the Benioff zone.
3
Q
Convergent plate boundaries: oceanic/oceanic
A
- All similar to continental/oceanic except no fold mountains.
- Instead, main features are island arcs and ocean trenches.
- Example is the Philippines and the Philippine trench.
4
Q
What are island arcs?
A
- Island chains with the same convexo-concave form.
- Made of active stratovolcanoes and sediment from accretionary wedges.
5
Q
Convergent plate boundaries: continental/continental
A
- Compressional stresses lead to the formation of earthquakes but with shallower foci.
- Example: the alps.
6
Q
Divergent plate boundaries
A
- Found at great ocean ridges.
- Example: Mid Atlantic Ridge.
- The ridge has a higher relief than the rest of the ocean floor as the ridges consist of hot, expanded rock.
- Magma rises in between gaps from two plates separating, forming new land as it cools.
7
Q
What is the evidence of continental drift?
A
- Coastline fit: Africa and South America
- Fossils, flora, and fauna: similarities in animal and plant fossils in South America and Africa.
- Fit of orogenic belts (fold mountain belts): Norway and Britain
- Fit of rock types: Precambrian rocks on either side of the Atlantic.
8
Q
What is sea floor spreading?
A
- The process of creation of new oceanic lithosphere at the ocean ridges as magma cools.
- Magma extruded along the ridge as dark-colored basalt.
9
Q
What is the evidence of sea floor spreading?
A
- Age of rocks on the ocean floor: radiometric dating.
- Thickness of sediment: increases with increasing distance from the ridge as more time to accumulate.
- Direct satellite measurements of ocean width.
- Magnetic stripes
10
Q
What are hot spots?
A
- Areas of volcanic activity not related to plate boundaries.
- Hot magma plumes from the mantle rise and burns through weak parts of the crust, creating volcanoes and islands.
- The plume remains in the same place but plates continue to move which causes chains of islands.
- Example: Hawaii