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 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.
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.
Yes, earthquakes can occur in plate interiors, especially in areas where older faults or weak zones exist within the plate. These intraplate earthquakes are less common than those that occur at plate boundaries, but they can still cause significant damage due to the unexpected nature of their occurrence. Examples include the New Madrid Seismic Zone in the central United States and the seismic activity in the stable interior of the Indian Plate.
Mountain ranges, such as the Himalayas, were formed when 2 plates collided. When 2 tectonic plates crash together, the force pushes the plate boundaries upward and create mountains. So, mountains are formed by convergent plate boundaries. By, Heather (11) ADDED: Correct, though the collision is more a steady push than a "crash". The Himalayas are still forming, with the up-lift slightly faster than the erosion, as India is still colliding with the Asian continental plate.
That would be a hotspot.
A hotspot.
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.
he changed surname, don't know if he's still alive though
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.
they're still alive. they're extinct now though
Will Downing is still alive, though he is wheelchair bound.
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.
As of the 23rd of July 2016, she is still alive, though she abdicated in 2013, so she is no longer the queen.
Yes she's like 80 though she was so pretty titanic and yeah but she is still alive.
As I here she is still alive I dont know though I just met her yesterday
Gillian Ayres was still alive in 2011-not sure about now though (answered in 2012) You can look at the answer to "Is Gillian Ayres still alive?"