Tectonic Processes And Hazards Flashcards
Convergent plate
. Denser oceanic crust is forced underneath the continental rust. This is know as slab pull
. Deep trench forms where oceanic plate is pushed under
. Composite volcanoes
. Tsunamis
. Earthquakes
Divergent
. Magma rises and seeps through the gap created as the plates move apart
. A ridge underwater
. Volcanic mountains
. Earthquakes
Collision
. Plates of similar weight collide and force upwards
. Built up of pressure suddenly releases
. Earthquakes
. Fold mountains
Conservative
. Plates rub against eachorher because they’re going at different speeds causing friction
. Release of friction causes fault lines in the ground
. Fault lines
. Earthquakes
Hotspots
. Occur in centre of plates where there is a hot mantle plume rising to surface that triggers the coast
Why do plates move?
Heat rises and falls, pulling the plated apart and making them move. This is done using convection currents
Tsunamis
. Triggered by an earthquake which occurs under an ocean
. When plate jolts, ocean above is forced upwards providing extra energy to the waves
Time of evidence supporting plate tectonics
. 1915: fossils collected by Wegener
. WW1: Found geologic features on ocean floor
. 1919: proposed concection currents exist
. 1946: ocean floor is mapped with solar technology
. 1954: first world mapf of volcanic eruptions is published
. 1960: hess and Dietz develop theory of sea floor spreading
. 1963: magnetic Rock reveals pattern of spreading away from centre of Atlantic ocean
. 1965: Wilson proposed idea that earth’s crust made of plates
. 1983: first gps made available
Shockwave body
. Two types- primary and secondary
. Travel through interior of earth’s layers
. Primary- faster but not felt
. Secondary- slower and do most damage
Shockwave surface
. Two types- love and Rayleigh
. On the surface and cause the most damage
. Love are transverse
. Rayleigh push ground forward and back
. Only found on shallow earthquakes
Secondary earthquake impacts
. Tsunamis
. Landslides
. Liquefaction
. General groun displacement
Volcanic explosivity
. Has a range from gentle fissures to explosive composite areas
. Links to energy of eruption
. Supervolcanoes are the largest
. Basaltic and andesitic
. Use of volcanic expolsivity index
Secondary volcano impacts
. Jokulhoup- flood causes by melted glacier
. Lahars- water mixed with volcanic deposits
. Most significant things involve water
Basaltic lava
. Hottest (1000-1200)
. Low gas content
. Thin and runny
. Gentle
. Location: ocean hot spots, mid ocean ridges and shield volcanoes
Andesitic lava
. Temp: 800-1000
. Gas content 3-4%
. Slow flow
. Violent eruption
. Location: composite cone volcanoes