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Answer:
A Wilson cycle consists of six stages: embryonic, juvenile, mature, declining, terminal, and suturing. The cycle begins because thick continental crust does not conduct heat as readily as thinner oceanic crust. The Pacific Ocean is an example of stage D. Terminal Ocean Basin (Closing Remnant Ocean Basin) Stage E: At this stage, the continents are almost colliding. Formation of magma happens deep in the subduction zone and small mountains are building up. There are some stages of ocean basin evolution. The evolution contains five stages which are embryonic stage, juvenile stage, mature stage, declining stage, terminal stage, mature stage, and continental collision.
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