when a trent is created
An earthquake
When the 2 plates strike and then slip. Or faulting.
The earthquake in Japan is a result of the Pacific Plate subducting under the North American Plate. The earthquake was caused by thrust faulting.
The 1960 Valdivia earthquake was caused by thrust faulting along what is known as a subduction zone boundary. This type of faulting occurs when one tectonic plate is forced under another, leading to a sudden release of stress and energy in the form of an earthquake.
The Meckering earthquake occurred in the Australian town on October 14, 1968 and destroyed the town. It occurred due to surface faulting up to 3 meters high and 40 kilometers long.
EARTHQUAKES - the sudden, intense shift along already formed fault cause earthquake to occur -earthquake occur around plate boundary where plate movement occur in the form of faulting
In all likelihood it was a thrust fault, as most seismicity in New England is associated with thrust faulting.
Faulting of the Earth's layers occurs when stress builds up within the crust, leading to the rock breaking and sliding along a fault plane. This movement releases energy in the form of an earthquake. Faulting can happen due to tectonic plate movements, volcanic activity, or regional stress within the Earth's crust.
The Chilean earthquake had a magnitude of 8.8 and was a thrust fault earthquake that occurred at a convergent plate boundary where subduction of the Nazca plate under the South American plate is occurring. This type of thrust faulting at subduction zones is commonly referred to as a megathrust earthquake. Please see the related question for further information.
The magnitude 9.0 Tohoku earthquake on March 11, 2011, which occurred near the northeast coast of Honshu, Japan, resulted from thrust faulting on or near the subduction zone plate boundary between the Pacific and North America plates.
Faulting on the lithosphere can result in earthquakes as the stress built up along the fault is released suddenly. This can cause the rocks on either side of the fault to move relative to each other. Additionally, faulting can lead to the formation of new landforms such as mountains or valleys depending on the type of fault.
The focus of an earthquake is the underground spot where the rock movement came from. The epicenter is the point on the surface above the focus.