Faults are breaks in the crust where the crust has moved. The types of dip-slip faults are normal and reverse faults. In both of these, the movement is along the slope of the fault. Sudden movements along these faults can produce fault scarps. Layers of rock being misaligned is evidence of fault movement. Fault creep is caused by slow movement along the fault.In a normal fault, the plates are moving away from each other. This is due to tension. When the fault moves, the footwall rises relative to the hanging wall. Normal faults occur at divergent boundaries, such as ocean ridges. Normal faults can produce fault-block mountains.In a reverse fault, the plates are moving towards each other. This is due to compression. Here, the footwall falls relative to the hanging wall. A thrust fault is a special type of reverse fault, where the angle is shallow. Reverse faults occur at convergent boundaries, like subduction zones.A strike-slip fault is where the two plates move horizontally past each other. The force between them is called shearing. This type of fault is often called a transform fault, because they occur at transform boundaries.
There are 3 main types of faults 1. Normal 2. Strike slip 3. Reverse(Thrust) In a normal fault the foot wall stays in place while the hanging wall moves DOWNWARDS In a strike slip the tectonic plate(s) slide past each other horizontally In a reverse fault, the hanging wall gets pushed UPWARDS over the foot wall (The pictures are in the reverse order)
No earthquake having solely terrestrial causes can be stronger than 10 on the Richter scale, because no type of rock is strong enough to store that much energy without breaking before then (and thus causing a smaller earthquake). The strongest earthquake ever recorded so far was a 9.5 earthquake. In principle larger earthquakes could be caused by impacts with very big asteroids or comets, but no impacts that large have occurred in recorded history.
Dynamic Metamorphism >.<
um.....yes?
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.
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.
The Haiti earthquake in 2010 was caused by a strike-slip fault interaction along the Enriquillo-Plantain Garden Fault Zone. This fault zone is located along the boundary between the Caribbean Plate and the North American Plate.