COMPARE AND CONTRAST THE TWO TYPES OF DIVERGENT BOUNDARIES
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Divergent boundaries: where new crust is generated as the plates pull away from each other. Convergent boundaries: where crust is destroyed as one plate dives under another. Transform boundaries: where crust is neither produced nor destroyed as the plates slide horizontally past each other.
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Two types of divergent boundaries.
EXPLANATION:
There are two significant types of divergent boundaries:
- Continental, and
- Oceanic.
- In divergent boundaries two of the plates create some distance from one another.
- At the point when this occurs, magma surges up to fill the hole, making shiny new outside.
- At the point when two continental plates veer, incredible break valleys can be formed.
Components regularly found at divergent plate boundaries are:
(1) mid-sea edges and crack valleys.
(2) wide valleys and deltas.
(3) sea channels and subduction zones.
- The Mid-Atlantic Ridge is an illustration of divergent plate boundaries.
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