they cause the world to spin
A normal fault is the result of the downward movement of rock along the fault line.
it shakes and moves
Dip-slip faults is the term used for any fault that has movement in the vertical direction. One side moves up where as the other side moves down. Examples are Normal Fault and Reverse fault.
A simple answer is: Colliding and subductive as they consume the Earth as a portion of the plate is moved beneath another plate and remelted into magma. A common example is the western side of South America where the denser oceanic Pacific Plate moves under the less dense continental South American Plate. The Pacific melts into magma and the South American rises to form the Andes Mts. with a great deal of volcanic activity.
A Normal fault
A transform plate boundary shears horizontally against each other. When one crust moves up, the other one moves down. A transform plate boundary produces the second worst earthquakes with (S) waves (Shear or secondary waves). Every boundary including a transform plate boundary are located on a fault.
a boundary at which two plates moves past each other horizontally
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.
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.
A transform boundary, or conservative plate boundary, is a type of fault at the margin of two adjacent tectonic plates were the relative motion is horizontal in either sinistral or dextral direction between the two.
A normal fault is the result of the downward movement of rock along the fault line.
a boundary at which two plates moves past each other horizontally
it shakes and moves
Dip-slip faults is the term used for any fault that has movement in the vertical direction. One side moves up where as the other side moves down. Examples are Normal Fault and Reverse fault.
Dip-slip faults is the term used for any fault that has movement in the vertical direction. One side moves up where as the other side moves down. Examples are Normal Fault and Reverse fault.
A sudden movement of the Earth's crust is called an earthquake.
The sudden movement could result in an earthquake.