There are three main types of interactions that can occur at the boundaries of Earth's crustal plates:

1. Convergent Boundaries: This occurs when two plates move towards each other. If the two plates are of equal density, they usually push up against each other, forming a mountain range. If they have different densities, one plate typically subducts, or slides under the other. This can create deep ocean trenches and volcanic activity.

2. Divergent Boundaries: This happens when two plates move away from each other. As they separate, magma rises from the mantle to fill the gap. This can create mid-ocean ridges and new crustal material.

3. Transform Boundaries: This occurs when two plates slide past each other horizontally. The friction caused by this movement can trigger earthquakes. The San Andreas Fault in California is an example of a transform boundary.

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There are three main types of interactions that can occur at the boundaries of Earth's crustal plates:

1. Convergent Boundaries: This occurs when two plates move towards each other. If the two plates are of equal density, they usually push up against each other, forming a mountain range. If they have different densities, one plate typically subducts, or slides under the other. This can create deep ocean trenches and volcanic activity.

2. Divergent Boundaries: This happens when two plates move away from each other. As they separate, magma rises from the mantle to fill the gap. This can create mid-ocean ridges and new crustal material.

3. Transform Boundaries: This occurs when two plates slide past each other horizontally. The friction caused by this movement can trigger earthquakes. The San Andreas Fault in California is an example of a transform boundary.

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There are three main types of interactions that can occur at the boundaries of Earth's crustal plates:

1. Convergent Boundaries: This occurs when two plates move towards each other. If the two plates are of equal density, they usually push up against each other, forming a mountain range. If they have different densities, one plate typically subducts, or slides under the other. This can create deep ocean trenches and volcanic activity.

2. Divergent Boundaries: This happens when two plates move away from each other. As they separate, magma rises from the mantle to fill the gap. This can create mid-ocean ridges and new crustal material.

3. Transform Boundaries: This occurs when two plates slide past each other horizontally. The friction caused by this movement can trigger earthquakes. The San Andreas Fault in California is an example of a transform boundary.

List the possible interactions between Earth’s crustal plates that can occur at their boundaries

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