Asthenosphere
Along with their attached rigid uppermost mantle, they are referred to as tectonic plates.
Shifting,sliding,diverging ,converging etc . of tectonic plates.
along tectonic plate boundaries.
The mountain is likely growing in elevation due to the tectonic plate movement along the boundary, resulting in compression and uplift of the sedimentary layers. This compression causes the layers to fold and deform, creating the rugged mountain structure. Over time, continued tectonic activity will further elevate the mountain.
When tectonic plates collide, the extreme pressure and forces involved can cause the rocks to deform, leading to the creation of folds and faults. Folds are bends or curves in rock layers, while faults are fractures along which movement has occurred. These geological structures are a result of the tectonic forces exerted during plate collisions.
The tectonic plates located along the Prime Meridian are the Eurasian Plate and the African Plate.
Earthquakes along the seafloor, tsunamis, and changed water movements.
Faults are formed at the outer solid layers of the Earth. They are developed within the earths crust or Lithosphere.
The movement of Earth's plates can create geological features like mountains and volcanoes through processes such as subduction and continental collision. It can also lead to earthquakes when plates shift along faults in the Earth's crust.
Earthquakes occur most often along the boundaries of tectonic plates.
Along with their attached rigid uppermost mantle, they are referred to as tectonic plates.
earthquakes
Shifting,sliding,diverging ,converging etc . of tectonic plates.
because the tectonic plates are moving beneth the earths crust, colliding with each other. if someone live along one of these fault lines between the plates they would experience a large earthquake.
along tectonic plate boundaries.
Bali is located on two tectonic plates, the Australian Plate and the Eurasian Plate. These plates interact along the Sunda Megathrust, which can result in seismic activity in the region.
The mountain is likely growing in elevation due to the tectonic plate movement along the boundary, resulting in compression and uplift of the sedimentary layers. This compression causes the layers to fold and deform, creating the rugged mountain structure. Over time, continued tectonic activity will further elevate the mountain.