core
mantle
The layer of Earth above the core, containing magma
magma
Molten rock
asthenosphere
the layer of the earth located in the outer part of the mantle, composed of semi molten rock
crust
earth’s thin outermost solid layer, rocky shell
lithosphere
the outermost layer of the earth, including the solid upper mantle and crust
hot spot
a place where the molten material from earth’s mantle reaches the lithosphere
plate tectonics
The theory that the lithosphere of Earth is divided into plates, most of which are in constant motion
tectonic cycle
the process that builds up and break down the lithosphere
convection and plate movement
Convection in the mantle causes oceanic plates to spread apart as new rock rises to the surface at spreading zones.
subduction
Earth is covered with tectonic plates, most of which are in constant
motion.
tectonic plates
Earth is covered with tectonic plates, most of which are in constant
motion.
new lithosphere added at spreading g zones and old recycled and subduction zones
volcano
Earth is covered with tectonic plates, most of which are in constant
motion.
divergent plate boundary
plates pull away from eachother
seafloor spreading
new ocean crust is created because of magma pushes upward and outward from Earth’s mantle to the surface.
convergent plate boundary
plates move toward each other
transform fault boundary
plates slide past each othet
Convergent oceanic continential
oceanic plate is pulled under (subducts) continential plate - volcanoes
convergent oceanic oceanic
one oceanic plate is pulled under another - volcanic island
convergent continental continental
formation of mountain range
formation of oceanic crust
occurs near spreading zones
volcanic activity
you can find this at subduction zones, convergent divergent, and seafloor spreading
mountain ranges
continental continental convergent only
increased seismic activity
mostly happens at transform faults, can occur at subduction zones