It seems like you're asking about the types of faults and their corresponding plate boundaries. Here's a step-by-step explanation:

1. Normal Fault: This type of fault occurs when the crust is extended. It is associated with Divergent Boundaries, where two tectonic plates move away from each other. An example of this is the Mid-Atlantic Ridge.

2. Strike-Slip Fault: This type of fault occurs when the crust neither extends nor shortens. It is associated with Transform Boundaries, where two tectonic plates slide past each other horizontally. The San Andreas Fault in California is an example of this.

3. Reverse Fault: This type of fault occurs when the crust is compressed. It is associated with Convergent Boundaries, where two tectonic plates move towards each other. The Himalayan Mountain Range was formed by this type of fault.

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It seems like you're asking about the types of faults and their corresponding plate boundaries. Here's a step-by-step explanation:

1. Normal Fault: This type of fault occurs when the crust is extended. It is associated with Divergent Boundaries, where two tectonic plates move away from each other. An example of this is the Mid-Atlantic Ridge.

2. Strike-Slip Fault: This type of fault occurs when the crust neither extends nor shortens. It is associated with Transform Boundaries, where two tectonic plates slide past each other horizontally. The San Andreas Fault in California is an example of this.

3. Reverse Fault: This type of fault occurs when the crust is compressed. It is associated with Convergent Boundaries, where two tectonic plates move towards each other. The Himalayan Mountain Range was formed by this type of fault.

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It seems like you're asking about the types of faults and their corresponding plate boundaries. Here's a step-by-step explanation:

1. Normal Fault: This type of fault occurs when the crust is extended. It is associated with Divergent Boundaries, where two tectonic plates move away from each other. An example of this is the Mid-Atlantic Ridge.

2. Strike-Slip Fault: This type of fault occurs when the crust neither extends nor shortens. It is associated with Transform Boundaries, where two tectonic plates slide past each other horizontally. The San Andreas Fault in California is an example of this.

3. Reverse Fault: This type of fault occurs when the crust is compressed. It is associated with Convergent Boundaries, where two tectonic plates move towards each other. The Himalayan Mountain Range was formed by this type of fault.

Normal fault Strike-slip fault Reverse faultDivergent boundary Convergent boundary Transform boundary Divergent boundary Convergent boundary Transform boundary

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