the uneven heat distribution between the plate tectonics
It is a THRUST fault The San Andreas Fault
tsunami
strike slip
transform boundary
Tectonic shear stress.
normal fault and reverse fault.
The 1556 Shaanxi earthquake in China was caused by a thrust fault. This type of fault occurs when two tectonic plates are compressed together, forcing one up and over the other. In this case, the thrust fault caused significant damage and loss of life in the region.
On February 4th, 1965, a reverse fault caused the Rat Islands Earthquake, Alaska, at 5:01 A.M.
The Great Kanto earthquake was a oceanic to continental
The 1964 earthquake in Alaska was caused by a megathrust fault associated with the subduction zone where the Pacific Plate is being pushed beneath the North American Plate. This type of fault is known as a megathrust or subduction zone fault.
The Kansu earthquake took place on the Weihe Basin fault, not on a plate boundary. The Weihe Basin is a normal dip-slip fault.
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.
In all likelihood it was a thrust fault, as most seismicity in New England is associated with thrust faulting.
The 2004 earthquake in northern Sumatra, Indonesia was caused by a megathrust subduction zone fault between the Indian Plate and the Burma Plate. This type of fault is known as a subduction zone fault, where one tectonic plate is forced beneath another.
It is a THRUST fault The San Andreas Fault
tsunami
The Chilean earthquake was caused by subduction zone stress, where the Nazca Plate slid beneath the South American Plate. The fault associated with this event was a megathrust fault, specifically the interface between the two plates.