quit unit 2 Flashcards
layers of the eart deepest to outer
core
mantle
lithosphere
crust
core
most dense
made of nickle and iron
solid inner core, liquid outer core
mantle
where convection occurs
hot, semi-solid rock influences, tectonic activity
asthenosphere
crust
5 km thick below the ocean
70 km thick below the continents
lithosphere
continental
forms all land masses
older, thicker, and less dense
Granite- 2.7g/cm3
oceanic
under oceans
younger, thinner, and more dense
Basalt- 2.9 g/cm3
theory of continental drift
alfred wegener, 1912
continents have been moving around
and single continent pangea broke up 175-200 million years ago
theory of plate tectonics
explains how and why the continents move
heat from core causes uneven heating and convention occurs within the mantle
as these currents move magma the plates above collide seperate and slide
crust is destroyed and created reforming earths surface
what provides evidence for the theory of plate tectonics
mid atlantic ridge and seafloor of atlantic ocean
mariana trench
deepest trench on earth
indo australian and pacific plates colliding
deepest point is challenger deep
mid ocean ridge
run direct down center of atlantic
rocks at equal distance from ridge same age
sediment builds up gets thicker the further from the ridge
seismic activity is frequent
paleomagnetic stripes match both sides
hot spot theory
magma plumes rise and break through the crust at host spots
creates volcanoes farfrom plate boundaries (hawaii)
hot spots stay in one place but the plate moves over top of it which creates line of volcanoes
earthquakes
when plates stuck together and dont move for a long time so
pressure builds
burst of energy releases when movment occurs energy released moves as seismic waves through lithosphere
tsunamis
caused by sudden release of energy on the seafloor(earthquake/volcanic eruption)
energy displaces a large volume of water and moves quickly through deep water
as approaches shallow coast line waves slow and build height
hydrothermal vents
cracks in crust along plate boundaries and water seeps down
gets heated by mantle and dissolves mineral by surrounding rocks
pressure forces water back up
as superheated mineral rick water meets cold deep water it rapidly cools and the minerals recrystalized and build vent structure
creates small plume of water in cold sea ecosysten formed here