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Plate boundary
These plates are all moving in different directions and different speeds the place where two plates meet called
Alfred Wegener
the father of the plate tectonics theory
Driving mechanism
aspect of the plate tectonics theory explains how tectonic plates are able to move across the Earth's surface
Lithosphere
The brittle, solid part of Earth
asthenosphere
It is a ductile layer under the solid lithosphere. It is primarily composed of rocks that are partly molten due to high temperature and pressure under the lithosphere.
convection current
is divided into cells that move in the opposite direction. Hot molten materials move up whereas cooler materials move down.
plate margins
also known as plate boundaries, are of three types, namely, convergent, divergent, and transform. Each plate boundary forms different geological features.
convergent boundaries
This is where two plates are colliding Subduction zones occur when one or both of the tectonic plates are composed of oceanic crust.
Where oceanic crust meets ocean crust
Island arcs and oceanic trenches occur when both of the plates are made of oceanic crust.These are often associated with submarine volcanoes.
Where oceanic crust meets continental crust
The denser oceanic plate is subducted, often forming a mountain range on the continent. The Andes is an example of this type of collision.
Where continental crust meets continental crust
too light to subduct so a continentcontinent collision occurs, creating especially large mountain ranges. The most spectacular example of this is the Himalayas.
Subduction
is a geological process that takes place at convergent boundaries of tectonic plates where one plate moves under another and is forced to sink due to high gravitational potential energy into the mantle.
subduction zones
Regions where this process occurs are known as
Divergent Boundaries
This is where two plates are moving apart each other. The space created can also fill with new crustal material sourced from molten magma that forms below.
fracture
Resulting in the production of new seafloor. As the plate moves opposite each other, it causes a __ in the lithosphere, resulting in the upwelling of hot molten materials.
mid-oceanic ridges
The most active divergent plate boundaries are between oceanic plates and are often called
rifts
Divergent boundaries within continents initially produce
rift valley
is another feature that results from plate movement. As plates move apart, they create a depression or a lowland region along the separation of the plates
The Great Rift Valley of Africa
is an example of this rifting due to tectonic movement.
transform boundaries
This is where plates slide passed each other
destroyed nor created
The relative motion of the plates is horizontal. They can occur underwater or on land, and crust is neither
earthquake
Because of friction, the plates cannot simply glide past each other. Rather, stress builds up in both plates and when it exceeds the threshold of the rocks, the energy is released - causing
convection current
is thought to be the driving mechanism for plate movements.
asthenosphere
Even though the mantle is solid, a part of it called the ___ flows like a soft and pliable plastic.
heat transfer
Convection currents are an important form of
photosphere
In the sun, convection occurs when opaque gas absorbs energy emitted by fusion, heats up, and rises to the ___ where the energy is radiated into space.
convection
also occurs in a pot of boiling water, or a convection oven