Plate Tectonics Flashcards
Earth’s Structure
Takes up 1% of Earth’s volume
Temp. varies from air temperature (at surface) to 1600℉ (at boundary)
Chemically speaking
- Crust
- Silicates (silicon + oxygen)
Mechanically speaking
- Lithosphere (crust + upper mantle)
- Rigid movement
Mantle
- Silicates at 100-2900km
Asthenosphere
- Ductile movement
Alfred Wegener & Continental Drift Theory
Alfred Wegener - first to propose the idea that continents moved
Evidence
- Apparent fit of the continents
- Glacial evidence in tropical areas
- Distribution of fossils
- Matching geologic units
Convection Currents
Convection current of the mantle is driving force of plate tectonics
Plate Boundaries
Tectonic plates meet at plate boundaries
3 types of plate boundaries: convergent, divergent, and transform
What is an earthquake?
A vibration caused by the sudden breaking or frictional sliding of rock in the Earth
Magnitude
Measurement of energy released at the source, uses seismographs
Intensity
The effect on Earth’s surface, location or site-dependent
Plate Tectonics & Volcanism
Convergent Boundaries
- Subduction - one plate sinks beneath another. As the sinking plate gets closer to the hotter mantle, it melts. Produces magma.
- Continental - Oceanic: Continental Volcanic Arc
- Oceanic - Oceanic: Volcanic Island Arc
Plate Tectonics & Volcanism
Divergent Boundaries
Continental - Continental: Volcanically active rift valleys as lithosphere gets thinner
Oceanic - Oceanic: Mid-ocean ridge volcanism as seafloor spreading pushes plates apart
Convergent Boundaries
Boundary at which two plates are moving towards each other
Subduction - a convergent boundary at which one plate sinks under the other
Oceanic crust is being destroyed
Geologic Features:
Mountains
Earthquakes
Trench - forms as the plate bends and begins to subduct
Volcanic Arc - magma is formed as the subducting plate melts
Continental Volcanic Arc (Continental & Oceanic) vs. Volcanic Island Arc (Oceanic)
Divergent Boundaries
A boundary at which two plates move apart from each other
Oceanic lithosphere (crust) is created at these ridges through seafloor spreading process
Geologic Features:
- Earthquakes
- Mid-ocean ridges
- Rift Valley
Transform Boundaries
Boundary at which two plates slide sideways past each other
No new plate is created, no new plate is destroyed
Often link together ridge segments
Shallow earthquakes common