Topography and Tectonics > Step Two

Other types of tectonic activity can be inferred by looking at topography. For example, around the Pacific rim it is common to see deep sea trenches adjacent to chains of volcanoes--either as strings of islands as in Japan and the Phillipines, or along the edges of continents, as in Central and South America. These features mark subduction zones, a second type of convergent plate boundary. Here thin and dense oceanic plates descend into the Earth's mantle. Where the plate bends down there is a topographic low, or trench. In the mantle the plates melt and rise to the surface again, forming the chains of volcanoes.

For this exercise we'll make another topography map using QUEST.

QUESTIONS:

1. Where is the deepest part of the ocean?


2. Where are the ocean's mountain ranges?

 

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