Plate tectonics is driven by deep convection in Earth's mantle. In convection, hot material moves up in one place, while cooler material moves down in another place. Match the seafloor feature or plate tectonic process with up-going or down-going material. mid-ocean ridges down-going trenches down-going seafloor spreading down-going subduction down-going convergent boundary (ocean- ocean) down-going convergent boundary (ocean- continent) down-going divergent boundary down-going
Plate tectonics is driven by deep convection in Earth's mantle. In convection, hot material moves up in one place, while cooler material moves down in another place. Match the seafloor feature or plate tectonic process with up-going or down-going material. mid-ocean ridges down-going trenches down-going seafloor spreading down-going subduction down-going convergent boundary (ocean- ocean) down-going convergent boundary (ocean- continent) down-going divergent boundary down-going
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
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Transcribed Image Text:Plate tectonics is driven by deep convection in Earth's mantle. In convection, hot
material moves up in one place, while cooler material moves down in another place.
Match the seafloor feature or plate tectonic process with up-going or down-going
material.
mid-ocean ridges
down-going
trenches
down-going
seafloor spreading
down-going
subduction
down-going
convergent boundary (ocean-
ocean)
down-going
convergent boundary (ocean-
continent)
down-going
divergent boundary
down-going
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