tectonics L1 dynamic landscapes Flashcards
(27 cards)
How are Earthquakes distributed?
on or around a plate boundary
- mid-Atlantic ridge
How is volcanic activity distributed?
along constructive & destructive boundaries
- Nazca-South America Boundary
How are Tsunamis distributed?
happen along mostly destructive boundaries around the pacific
anomaly — many around the mediterranean which is an uncertain boundary
What is the Lithosphere?
The crust & the upper most solid mantle
What is the Asthenosphere?
Semi-molten rock (99% solid) in the upper mantle
Viscous/ductile which allows lithosphere to glide on top
What is the Mesosphere?
lower mantle — high pressure from layers above — more rigid
What is Mohorovičić discontinuity (Moho)?
The boundary between the crust and the mantle — 10-12km under ocean bed
Crust — Temperature
Surface temp to about 400°C
Crust — Density & Composition
Continental - Granite (Less Dense) (up to 100km), Oceanic - Basalt (7km thick)
Crust — Physical state?
solid
Mantle — Temperature
870°C
Mantle — Density & Composition
silicate
less to medium density
700km to 2890km deep
Mantle — Physical State
Phases of liquid and solid in layers
(semi molten)
Outer Core — Temperature
4400 to 6100°C
Outer Core — Density & Composition
dense
12% sulphur
88% iron
2890 to 5150km deep
Outer Core — Physical State
liquid (and generates magnetic field)
Inner Core — Temperature
7000°C
(Radioactive decay & pressure)
Inner Core — Density & Composition
20% nickel
80% iron
5150km to centre deep
very dense
Inner Core — Physical State
Solid (+ radiates heat)
Destructive Plate Boundaries
oceanic plate subducts under continental plate into BENIOFF ZONE
shallow, intermediate & deep focus EQs
Conservative Plate Boundaries
only earthquakes
only shallow (30km) focus EQs
Constructive Plate Boundaries
two oceanic plates
magma rises and cools forming land
effusive volcanic activity
Collision Boundary
Two continental
destructive
fold mountains
What are Intra-Plate Earthquakes?
Earthquakes that occur in the middle of a plate due to pre-existing weaknesses that become reactivated forming seismic waves
— Newcastle in 1989