Plate Tectonics Flashcards
(34 cards)
Evidence for continental drift
Jigsaw fit Geological fit Tectonic fit Glacial deposits Fossil evidence
Types of plate boundaries where volcanoes form
Oceanic oceanic divergent
Continental continental divergent
Oceanic oceanic convergent
Oceanic continental convergent
Type of plate boundaries where ocean ridges form
Oceanic oceanic divergent
Type of plate boundaries where ocean trenches form
Oceanic oceanic convergent
Oceanic continental convergent
Type of plate boundaries where fold mountains form
Oceanic continental convergent
Continental continental convergent
Type of plate boundaries where island arcs form
Oceanic oceanic convergent
Type of plate boundaries where rift valleys form
Continental continental divergent
Hydration melting
Destructive boundary (convergent) Water forced down into mantle Mantle melts at lower temp. As bonds in rock are disrupted my water molecule Liquid mantle = magma which rises up through crust
Decompression melting
Constructive boundary (divergent)
Lower pressure means lower melting point of mantle
Two plates move apart leading to an area of low pressure
Reduction in overlying pressure enable mantle to melt leading to upward movement of magma
No subduction because plate are same density
Evidence for plate tectonics
Theory of Continental Drift 1915 (Alfred Wegener)
Mid oceanic ridges/Sea floor spreading 1962 (Harry Hess)
Paleomagnetism, symmetrical stripes 1963 (Vine and Matthews)
Hotspot theory 1963 and Transform Faults 1965 (John Tuzo Wilson)
Mantle Convection 1966 (Dan McKenzie)
Types of magma and their characteristics
Basaltic: 45-55% silica, 1000-2000C temp, low viscosity, Low gas content
Andesitic: 55-65% silica, 800-1000C temp, medium viscosity, medium gas content
Rhyolitic: 65-75% silica, 650-800C temp, high viscosity, high gas content
6 volcano types by shape
Flood/ Plateau Basalt / Fissure Shield Cinder Cone Composite/ Stratovolcano Volcanic dome/ acid Caldera
Primary volcanic hazards
Lava flows
Pyroclastic flows
Volcanic gases
Ash and tephra fall
Secondary volcanic hazards
Lahars Volcanic landslides Tsunami Flooding Fires
Focus
Location within Earth where underground rock moves and sends out earthquake waves
Epicentre
Location on the surface of the earth directly above focus
Earthquake waves/Seismic waves
Shock waves created at the focus and sent out in all directions
Earthquake
Rapid vibration of earth created by a sudden movement of large sections of rock
Seismograph
A device that reads earthquake waves
Seismogram
The picture drawn by a seismograph indicating earthquake waves
Natural causes of earthquakes
Plate boundaries
Intra plate movement
Isostatic recoil
Quasi-natural / human induced causes of earthquakes
Fracking
Dams
Nuclear testing
Two scales used to measure earthquakes
Richter scale - magnitude determined by logarithm of amplitude of waves recorded by seismograph
Mercalli scale - value assigned to a specific site after assessing damaged caused by an earthquake
Two types of body waves and their characteristics
Body waves: travel through earth itself
P waves (primary): longitudinal waves, push and pull, fastest body wave, average speed 6km/s, travel through both solid and liquid
S waves (secondary): transverse waves, shake side to side, slower, average speed 4km/s, only travel through solid