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When friction between the opposite sides of a fault is low, it allows for easier movement along the fault line, often resulting in more frequent and potentially larger earthquakes. This low friction can be caused by factors such as the presence of lubricating materials, fluid pressure, or the nature of the rocks involved. The reduced resistance means that stress can accumulate until it is released suddenly, leading to seismic activity. Consequently, areas with low friction faults are closely monitored for earthquake risks.
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Where rocks on opposite sides of a fault move in opposite directions or in the same direction of different rates?
strike slip fault
How do geologists collect data on friction along the sides of faults?
Geologists study the types of movement that occurs along faults. How rocks move along a fault depends on how much friction there is between the sides of the fault. Friction is the force that opposes the motion of one surface as it moves across another surface. Friction exists because surfaces are not perfectly smooth.Along parts of some faults, the rocks on both sides of the fault slide by each other without much sticking. Therefore stress does not build up, and big earthquakes are unlikely. Along many faults, the rocks lock together. In this case, stress increases until it is large enough to overcome the friction force. Stress builds up until an earthquake occurs.
What is the relationship between opposite sides of a parrelogram?
They are parallel sides that are equal in length
Can a square have a line of symmetry?
Diagonals between two opposite corners, and a vertical line between midpoints of 2 opposite sides, and a horizontal line between midpoints of the other pair of sides.
Are 2 pair of parallel sides and opposite angle are congruent?
The angles between the sides that are parallel are congruent.The angles between the sides that are parallel are congruent.The angles between the sides that are parallel are congruent.The angles between the sides that are parallel are congruent.
What happens when friction between opposute sides of a fault is high?
High friction between opposite sides of a fault can cause stress to build up, leading to a potential earthquake when that stress is released suddenly as the fault slips. This can result in intense shaking and ground displacement along the fault line.
What happens when friction on opposite side of a fault is high?
High friction on opposite sides of a fault can cause stress to build up in the rocks. When the stress exceeds the strength of the rocks, it can result in an earthquake as the rocks suddenly shift along the fault line.
What are called Where rocks on opposite sides of a fault move in opposite directions or in the same direction at different rates?
These types of rocks are known as "fault rocks" or "fault gouge." The movement of rocks on opposite sides of a fault can create various structures such as slickensides, cataclasite, or mylonite, depending on the amount of movement and deformation that has occurred.
Where rocks on opposite sides of a fault move in opposite directions?
Strike Slip Fault
Where rocks on opposite sides of a fault move in opposite direction?
Strike Slip Fault
What is it called when rocks on opposite sides of a fault move in opposite directions?
Strike Slip Fault.
Where rocks move on opposite sides of a fault move in opposite directions?
Strike Slip Fault
Where rocks on opposite sides of fault move in opposite directions or in the same direction at different?
strike slip fault
What is a strike-slip fault fault?
Strike-slip fault -a boundary where rocks on opposite sides of the fault move in opposite or the same directions at different rates.
If rocks on opposite sides of a fault move in opposite directions or in the same direction at different rates what kind of fault exists?
strike slip fault
What is a strike slipe fault?
Strike-slip fault -a boundary where rocks on opposite sides of the fault move in opposite or the same directions at different rates.
What is a strike-slipe fault?
Strike-slip fault -a boundary where rocks on opposite sides of the fault move in opposite or the same directions at different rates.
