Yes.
Normal faults, where the hanging wall drops down relative to the footwall, typically do not generate tsunamis. These faults are more common in areas of active stretching of the Earth's crust and are not usually associated with the sudden vertical displacement of large volumes of water required to trigger a tsunami.
Tsunamis are primarily generated by underwater earthquakes, particularly those associated with subduction zone faults, where one tectonic plate is forced under another. Other types of faults that can create tsunamis include strike-slip faults, which can displace the seafloor laterally, and normal faults, which can cause vertical displacements. Additionally, volcanic eruptions and landslides into the ocean can also trigger tsunamis. The magnitude of the tsunami is influenced by the size and nature of the fault movement.
Different types of faults can lead to various disasters. For example, strike-slip faults can cause earthquakes that result in ground shaking and infrastructure damage. Normal faults often lead to tectonic uplift, which can trigger landslides or tsunamis if they occur under the ocean. Reverse faults, associated with compressional forces, can also generate significant earthquakes and potentially lead to secondary disasters like fires or flooding due to ruptured pipelines and infrastructure failures.
Folding is usually the result of compressional stress. This may also cause thrust / reverse faults.
the best answer is reverse boundary
Normal faults, where the hanging wall drops down relative to the footwall, typically do not generate tsunamis. These faults are more common in areas of active stretching of the Earth's crust and are not usually associated with the sudden vertical displacement of large volumes of water required to trigger a tsunami.
Tsunamis are primarily generated by underwater earthquakes, particularly those associated with subduction zone faults, where one tectonic plate is forced under another. Other types of faults that can create tsunamis include strike-slip faults, which can displace the seafloor laterally, and normal faults, which can cause vertical displacements. Additionally, volcanic eruptions and landslides into the ocean can also trigger tsunamis. The magnitude of the tsunami is influenced by the size and nature of the fault movement.
Rocks moving apart can cause normal faults to form, as opposed to reverse and strike-slip faults.
reverse fault
Thrust faults and reverse faults can result in mountain formation. Thrust faults occur when rocks are pushed up and over each other, while reverse faults involve compressional forces causing rocks to move vertically. Both of these fault types contribute to the uplift and formation of mountain ranges.
Different types of faults can lead to various disasters. For example, strike-slip faults can cause earthquakes that result in ground shaking and infrastructure damage. Normal faults often lead to tectonic uplift, which can trigger landslides or tsunamis if they occur under the ocean. Reverse faults, associated with compressional forces, can also generate significant earthquakes and potentially lead to secondary disasters like fires or flooding due to ruptured pipelines and infrastructure failures.
reverse faults move from compression when the hanging wall moves up
Reverse and thrust faults are both under compressive stress.
Folding is usually the result of compressional stress. This may also cause thrust / reverse faults.
compression
The three major types of faults are normal faults, reverse faults, and strike-slip faults. Synclines are not faults but rather geological structures that describe the folding of rock layers.
The main direction of the stress on blocks of rock at normal faults, reverse faults and the strike slip faults usually happens at the weak areas.