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t a convergent boundary where a deep-ocean trench occurs, the crust is
Convergent Boundary: continental crust to contental crust
subduction
convection currents
divergent boundary on land
divergent boundary in ocean
plate tectonics
subducting
radiation
A rift valley forms at
Convergent Boundary: continental crust to contental crust
subduction
convection currents
divergent boundary on land
divergent boundary in ocean
plate tectonics
subducting
radiation
The sun warming your skin and a fire providing heat is an example of
Convergent Boundary: continental crust to contental crust
subduction
convection currents
divergent boundary on land
divergent boundary in ocean
plate tectonics
subducting
radiation
Mountain Ranges on land will occur at
Convergent Boundary: continental crust to contental crust
subduction
convection currents
divergent boundary on land
divergent boundary in ocean
plate tectonics
subducting
radiation
The geological theory that states that pieces of Earth’s lithosphere (or crust) are in constant, slow motion is the theory of
Convergent Boundary: continental crust to contental crust
subduction
convection currents
divergent boundary on land
divergent boundary in ocean
plate tectonics
subducting
radiation
Heat transfer within a fluid takes place by
Convergent Boundary: continental crust to contental crust
subduction
convection currents
divergent boundary on land
divergent boundary in ocean
plate tectonics
subducting
radiation
The process by which the ocean floor sinks beneath a deep-ocean trench and back into the mantle is known as
Convergent Boundary: continental crust to contental crust
subduction
convection currents
divergent boundary on land
divergent boundary in ocean
plate tectonics
subducting
radiation
Sea floor spreading and mid-ocean ridges occur at
Convergent Boundary: continental crust to contental crust
subduction
convection currents
divergent boundary on land
divergent boundary in ocean
plate tectonics
subducting
radiation
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