no the mid- Atlantic ridge is a transform boundary
A reverse fault occurs when rock above the fault moves upward at the fault line. This type of fault is associated with compressional stress where the hanging wall moves up relative to the footwall. Reverse faults are common in regions undergoing compression, such as convergent plate boundaries.
A transform fault is a general term to describe a plate boundary where the lithosphere is not destroyed or created. A transverse fault is a type of transform fault also known as a strike-slip fault.
A strike-slip fault has a shearing force, where the two blocks on either side of the fault move horizontally past each other. This type of fault is characterized by lateral movement along the fault line caused by horizontal forces.
A normal fault occurs when rock is pulled apart, causing one block of rock to move downward relative to the other. This displacement is due to tensional forces acting on the earth's crust, causing the hanging wall to drop relative to the footwall along the fault plane.
A fault with horizontal movement is called a strike-slip fault. In strike-slip faults, the movement is primarily horizontal, with one block of rock sliding past the other horizontally. This type of fault is characterized by lateral displacement along the fault line.
At a spreading ocean ridge, you are likely to find a divergent boundary fault, known as a mid-ocean ridge fault. This type of fault is created as two tectonic plates move apart, causing magma to rise from the mantle and create new oceanic crust at the ridge.
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The Niagara Escarpment is not a fault line at all; it appears to be a fault line due to unequal erosion. It spans about 650 miles in the Great Lakes region.
A reverse fault occurs when rock above the fault moves upward at the fault line. This type of fault is associated with compressional stress where the hanging wall moves up relative to the footwall. Reverse faults are common in regions undergoing compression, such as convergent plate boundaries.
A transform fault is a general term to describe a plate boundary where the lithosphere is not destroyed or created. A transverse fault is a type of transform fault also known as a strike-slip fault.
Divergent. This is because the two fault lines are pushing away from each other which allows the magma to come up through the crust from the mantle and core. This is what makes the volcanos which create islands such as Iceland.
On a fault line. For example, California is on the San Andreas fault, and as such is very earthquake prone.
In a normal fault the hanging wall moves downward. With this type of fault, the hanging wall also shifts horizontally away from the fault line.
Dynamic Metamorphism >.<
Mt Tambora is on a Tectonic fault line called the Jave Trench System. Mt Tambora is an active stratovolcano. It is located in Indonesia.
A strike-slip fault has a shearing force, where the two blocks on either side of the fault move horizontally past each other. This type of fault is characterized by lateral movement along the fault line caused by horizontal forces.
An asymmetrical fault is a type of power system fault that results in an imbalance of currents and voltages in the system. This imbalance can cause different magnitudes and phases of currents flowing through the system components, leading to potential equipment damage and system instability. Asymmetrical faults are typically caused by line-to-line or line-to-ground faults.