The two plates are; Indo-Australian Plate subducts and Pacific Plate that form the Puysegur Trench.
No. Many faults, especially minor ones, are located far from plate boundaries.
No. Many plate boundaries are on the seafloor far from continents and several are well within continents.
Most tsunamis are tirggered by earthquaes and so usually occur at plate boundaries.
Earthquakes occur more frequently near plate boundaries, where tectonic plates interact and create stress along faults. These interactions often result in sudden release of energy, causing earthquakes. In contrast, earthquakes far away from plate boundaries are less common but can still occur due to other geological processes like volcanic activity or human-induced activities.
The volcanoes in Hawaii and other places far from tectonic plate boundaries are known as hot spot volcanoes. These volcanoes are formed by magma upwelling from deep within the Earth's mantle, creating volcanic islands or features such as seamounts. An example of a hot spot volcano is the Hawaiian Islands.
Shield volcanoes may occur far from any plate boundaries.
No. Many faults, especially minor ones, are located far from plate boundaries.
That would be a hotspot.
A hotspot.
Most tsunamis are tirggered by earthquaes and so usually occur at plate boundaries.
No. Many plate boundaries are on the seafloor far from continents and several are well within continents.
Most tsunamis are tirggered by earthquaes and so usually occur at plate boundaries.
Hot spots!
Earthquakes occur more frequently near plate boundaries, where tectonic plates interact and create stress along faults. These interactions often result in sudden release of energy, causing earthquakes. In contrast, earthquakes far away from plate boundaries are less common but can still occur due to other geological processes like volcanic activity or human-induced activities.
The volcanoes in Hawaii and other places far from tectonic plate boundaries are known as hot spot volcanoes. These volcanoes are formed by magma upwelling from deep within the Earth's mantle, creating volcanic islands or features such as seamounts. An example of a hot spot volcano is the Hawaiian Islands.
As far as the Earth is concerned - plate tectonics has not stopped; the plates are still in motion - which is why we get earthquakes and volcanic eruptions along the plate boundaries.
Earthquakes that occur far from plate boundaries are called intraplate earthquakes. These earthquakes can happen due to the reactivation of ancient faults or the buildup of stress within a tectonic plate caused by various geological processes, such as volcanic activity or the movement of magma. They are less frequent than tectonic earthquakes at plate boundaries but can still be significant due to the accumulated stress in the crust.