Week 3: Plate tectonics Flashcards
Layer of earth that consists of plate tectonics
Lithosphere
The scientific method
- Observe
- Hypothesise
- Predict
- Test predictions
- Repeat, repeat, repeat
A scientific hypothesis is only credible if it is
Capable of being tested and proven wrong
Sea floor spreading hypothesis
- Ocean floor sediment thickens away from mid-ocean ridges
- New crust moves away from ridges and gathers sediment
- Earthquakes and high heat flow at mid-ocean ridges > seafloor spreading forms new crust at mid ocean ridges
- At trenches, sea-floor dives back into the mantle
- Mechanism for continental drift
Primary waves travel fast through what temperature material
Cold
Do primary or secondary waves travel liquid
Primary liquid
Earths interior strength layers
Lithosphere = strong, cool, rigid
Asthenosphere = high temperature, weak, easily deformed, solid
Mesosphere = high temperature and pressure, strong solid
Mantle is made of
Solid rock that deforms in a ductile (plastic) way when at high pressures and temperatures
How heat is transferred from earths interior towards the surface
Convection
Heat is transferred from the convecting asthenosphere to the non-convecting lithosphere by
Conduction
Plate boundaries where plates move apart and have shallow earthquakes
Divergent
Examples of divergent plates
- Mid ocean ridges
- Continental rifts
Mid ocean ridge formation
- Plates pull apart
- Asthenosphere wells up to fill gap, melting to produce magma
- Magma cools, creating new oceanic crust (basalt/gabbro)
- Normal fault scarps
Types of faults
- Normal fault (block above fault moves down)
- Reverse fault (block above the fault moves up)
- Strike-slip fault (blocks move side by side, no vertical movement)
- Oblique fault (mix between normal and strike slip)
Plate boundaries where plates move together resulting in reverse faults
Convergent