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lithosphere
the rigid outer part of the earth, consisting of the crust and upper mantle
Seamount
old eroded volcanoes that are found beneath the ocean surface
Continental crust
thicker, older, and less dense
Sea floor spreading
process where new ocean crust is formed due to the upwelling of magma at mid ocean ridges
Subduction
Process that occurs when denser tectonic plates sinks below a less dense plate, the plate melts and the material can be recycled.
Tectonic plate
A piece of the lithosphere that moves over the asthenosphere
Asthenosphere
a soft, flexible layer responsible for the direction of plate motion
hot spot
an intensely hot zone in the mantle bellow Earth's crust which causes the mantle in that region to melt
oceanic crust
crust that is thinner, newer and more dense
Why didn't the scientific community orignally accept Wegener's Theory of Continental drift ?
Because there was no way to explain how the plates moved
What layer does earths thermal energy come from?
core
Earths magnetic feild is made of what?
Iorn and Nickle (that come from the core)
Convergent: Oceanic- Oceanic crust creates…?
trenches, island arcs ( subduction can occur)
Convergent: Continental- Continental crust creates…?
mountain ranges ( no subduction can occur)
Convergent: Continental- Oceanic crust creates..?
trenches, Volcanic arc (subduction possible)
Divergent: Oceanic- Oceanic creates..?
Mid- ocean ridges (no subduction)
Divergent: Continental- Continental creates…?
Rift valley ( no subduction)
True or false? Eventually the African Rift Valley will fill with water and create a new tectonic plate
True
3 things hot spots and seamounts tell us about plate tectonics
Rate of plate movement
direction of plate movement
how long a spot has been active
Convergent: Oceanic- Oceanic Earthquake distribution
Spread beyond boundary, shallow/deep, often
Convergent: Continental- Continental Earthquake distribution
Spread Beyond boundary, shallow, often
Convergent: Oceanic- Continental Earthquake distribution
Spread Beyond boundary, shallow or deep, often
Divergent : Oceanic- Oceanic Earthquake distribution
along boundary, shallow, not often
Divergent : Continental- Continental Earthquake distribution
spread beyond boundary, shallow, not often