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unit 1 - plate tectonics

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- moving away from each other
- forms new lithosphere and is the youngest land on
earth
- creates mid-ocean ridges or rift zones (ex. east african rift valley)
- seafloor spreading can lead to mid-ocean ridges
- moving together
- when 2 plates are moving towards each other, 1 plate will eventually be pushed down under the other plate due to variations in density
- 2 continental plates converge: may form mountains
- continental plate and oceanic plate converge: oceanic plate will subduct and create a trench
- 2 oceanic plates converge: process is longer, eventually one will begin to descend and be reclaimed by the mantle (may form a string of volcanic islands)
- where the lithospheric crust is being pushed under and reclaimed by the mantle (where the oldest rock material is found)
- occurs when an oceanic and continental plate meet
- occurs when 2 plates slide horizontally past each other
- surface area is neither created or destroyed
- known as a tear or strike-slip fault
- great friction between the 2 plates, and if they become locked massive earthquakes can occur when the pressure releases

types of faults

  • normal, reverse (compression), strike-slip, horst, graben

normal fault

  • plates move away from each other

  • one goes up, one goes down

* plates move away from each other
* one goes up, one goes down

reverse (compression) fault

  • plates converge, one goes up, one goes down

* plates converge, one goes up, one goes down

strike-slip fault

  • transform boundary

* transform boundary

horst fault

  • block mountain, occurs under tension

  • like a horse, you can mount it

* block mountain, occurs under tension
* like a horse, you can mount it

graben fault

  • rift valley, also created under tension

  • looks like someone grabbed chunks out of it

* rift valley, also created under tension
* looks like someone grabbed chunks out of it
- sedimentary, metamorphic, igneous

igneous rocks

  • formed form melted rock deep inside the earth, found in volcanic regions
    ex. gabbro, basalt (in oceanic crust), granite, andesite (continental crust)

- predominantly found on continents
- made up of acidic lava
- made of layers of cinder and ash
- compact/small in size
- highly violent and explosive
- associated with pyroclastic flows
- fast cooling = can cause clogged neck 
ex. Mt. Fuji
- large and gentle sloping
- basic lava (basaltic lava) = wet like concrete
- do not violently erupt, instead ooze
-> any accounts of violent eruption tend to be from steam as the lava comes in contact with the water
- cools very slowly and spreads over large areas
- predominantly found on ocean floors
ex. Hawaiian Islands
- most often formed over subduction zones (Pacific Ring of Fire)
- symmetrical formation with cake-like layers of lava and ash
- snow and ice-capped
- more moderately sloped than cinder cones
- tend to be larger in size
- sudden and violent eruptions 
ex. Pacific Ring of Fire

lava flows

  • pour or ooze out of vents or cracks

  • causes majority of harm to non-moveable objects (trees, cars)

  • basaltic lava can travels vast distances vs. andesite lava that rarely goes past ~8 km.

  • objects and terrain are either surrounded, buried or ignited

pros of volcanoes

  • creates igneous rocks that can be used as building building materials

  • creates fertile soil

  • a source of geothermal energy

  • tourism! (slay)

- forms because the magma chamber empties/oozes out so fast that the volcanoes lose their structural integrity
- also forms because the explosion is so violent that the volcano blows its top off

batholith

  • largest feature, looks like a giant pool of magma underground

* largest feature, looks like a giant pool of magma underground

laccolith

  • 2nd largest feature

  • found between layers

  • usually dome-shaped but smaller

dike

  • cuts through multiple layers (across)

sill

  • stuck between layers

  • cuts in between layers

- aka compression wave
- a type of body wave (much smaller)
- travels by compressing and expanding the ground
- the fastest
- first to reach the earthquake recording stations
- aka shear wave
- second wave generated by quakes
- slower than the primary waves and travels in a side-to-side motion
- more extreme + aggressive
- travels like ripples through calm water
- responsible for ground shaking which causes much of the damage during earthquakes
- includes love waves (move back + forth) and Rayleigh waves (rolling)
- the location where the fracture/shift occurs and the seismic waves originate
- depth varies but can be as deep as ~700km
- located on the surface of the earth directly above the focus point