Chap. 2 Flashcards
The 2 parts of an earthquake are
- surface waves 2. body waves
P waves
Compressional, first to arrive, move through solid liquid and gas
S wave
Shear, second to arrive, Solid
P wave shadow zones
104-140
S wave shadow zones
104-180
Model 1
Core, Mantle, Crust (1. continental 2. Oceanic)
Model 2
Lithosphere, Asthenosphere, Mesosphere, Outer Core, Inner Core
Lithosphere
Crust and upper mantle fused together
Asthenosphere
Deformable region in the mantle
Mesosphere
Solid lower mantle
Isostasy
buoyant support of lithosphere by asthenosphere
Moho
Layer between crust and mantle
Alfred Wagener
proposed the continental drift theory
Supercontinent
Pangaea
Single ocean
Panthalassa
Pangea break-up
200-250 million years ago
Pangea split to make
Laurasia and Gond
Wegeners evidence
Fit on continents fossil distribution ancient mountain belt matching rocks patterns of glaciation
Harry Hess
Mantle convection (slab push & pull)
Subduction Zones
earthquakes
volcanoes
island Arc
Benioff Zone
Large & Deep earthquakes
subduction zone evidence
distribution of EQ epicenter
heat flow
sediment age & thickness
paleomagnetism
Paleomagnetism
Reversal of magnetic poles
magnetic stripes
Rift
sea floor spreading
Divergent
two Plates moving apart (mid-oceanic ridge)
Convergent
two plates moving together, one sinks under another (mantel)
Transform
two plates move in different directions parallel with each other
plate tectonic stages
up warping
Rift Valley
Linear Sea
Mid-ocean ridge
Convection
driven by heat in mantle
Rate of motion
1-20 cm/yr
Hotspots
where you have a volcano, then volcanic island, then seamount, then Guyot
Wilson Cycle
Initial continent Rifting ocean basin subduction closing ocean basin collision new continent