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The lithosphere is part of the
crust
boundary
asthenosphere
convergent
subduction
hotspot
Theory of Plate Tectonics
convection
The process of one plate sliding under another plate at a convergent boundary is
crust
boundary
asthenosphere
convergent
subduction
hotspot
Theory of Plate Tectonics
convection
The layer that supports and moves the tectonic plates is
crust
boundary
asthenosphere
convergent
subduction
hotspot
Theory of Plate Tectonics
convection
The border between two tectonic plates
crust
boundary
asthenosphere
convergent
subduction
hotspot
Theory of Plate Tectonics
convection
Plates move on the surface of the Earth because of
crust
boundary
asthenosphere
convergent
subduction
hotspot
Theory of Plate Tectonics
convection
Plates continually move a little bit each year
crust
boundary
asthenosphere
convergent
subduction
hotspot
Theory of Plate Tectonics
convection
The Hawaiian Islands are an example
crust
boundary
asthenosphere
convergent
subduction
hotspot
Theory of Plate Tectonics
convection
Mountains form at this boundary as plates push together
crust
boundary
asthenosphere
convergent
subduction
hotspot
Theory of Plate Tectonics
convection
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