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Yes I think ************************************* If the fault is a fissure (crack) without any slippage (movement up or down) then the layers on both sides will remain on the same level. If slippage has occured, there will be no continuity of layers.
Folds are the when the rock layers bend. Faults are breaks in the rock layers. Folds are called anticlines and synclines. Faults are called reverse faults, normal faults, or strike-slip faults.
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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.
if it is a sedimentary rock the fossils get cemented together
Faulting is caused by stress in the rock layers, the stress can break and crack the rock causing a fault. There are two types of faults a normal fault and a reverse fault.
Usually along a fault the rock layers are broken and displaced in some manner so that the rock layers are not continuous across the fault.
Fault
after the fault
normal fault occurs...odyssey
Yes I think ************************************* If the fault is a fissure (crack) without any slippage (movement up or down) then the layers on both sides will remain on the same level. If slippage has occured, there will be no continuity of layers.
Not necessarily. Rock layers along a strike-slip fault may be offset if they are dipping.
thrust or reverse fault,
Folds are the when the rock layers bend. Faults are breaks in the rock layers. Folds are called anticlines and synclines. Faults are called reverse faults, normal faults, or strike-slip faults.
The type of rock layers found on one side of the fault will either be repeated higher or lower on the other side of the fault. This proves that one side of a fault has moved (slipped).
a normal fault
What is the relative age of a fault that cuts across three horizontal sedimentary rock layers?A. The fault is older than the middle layer. B.The fault is younger than all the layers it cuts across.C. The fault is the same age as the top layer. D. The fault is older than all the layers it cuts across == ==