3) Discuss changes in the lithosphere that occur between an oceanic ridge and an oceanic trench.
Answer: The mid-ocean ridge is a continuous underwater mountain range that winds through
every ocean basin in the world. It is entirely volcanic in origin, wraps one-and-a-half times
around the globe, and rises more than 2.5 kilometers (1.5 miles) above the surrounding deep-
ocean floor. New ocean floor forms at the crest, or axis, of the mid-ocean ridge. By the process
of sea floor spreading, new ocean floor is split in two and carried away from the axis, replaced
by the upwelling of volcanic material that fills the void with new strips of sea floor. Sea floor
spreading occurs along the axis of the mid-ocean ridge, which is referred to as a spreading center.
At the same time, ocean floor is being destroyed at deep ocean trenches. Trenches are the deepest
parts of the ocean floor and, on a map of the sea floor, resemble a narrow crease or trough. The
largest earthquakes in the world occur near these trenches; they are caused by a plate bending
downward and slowly plunging back into Earth’s interior. This process is called subduction, and
the sloping area from the trench along the downward-moving plate is called a subduction zone.
Diff: 2
Bloom’s Taxonomy: Remembering/Understanding
Section: 2.3 What Features Occur at Plate Boundaries?
Essent’l Concept: 2.3 Discuss the origin and characteristics of features that occur at plate
boundaries
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