The rocks on opposite sides of a fault that move in opposite directions or in the same direction at different rates are called fault blocks. These blocks can move horizontally, vertically, or rotationally along the fault line.
The stress force that causes a mass of rock to pull or twist in opposite directions is called tension. Shearing is the stress force that causes a mass of rock to pull or twist in opposite directions.
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.
This is called wind shear.
The area you are referring to is called a transform boundary. At a transform boundary, tectonic plates slide past each other horizontally, typically in opposite directions. This movement can cause earthquakes due to the friction and pressure buildup along the fault line.
The rocks on opposite sides of a fault that move in opposite directions or in the same direction at different rates are called fault blocks. These blocks can move horizontally, vertically, or rotationally along the fault line.
Two forces acting in opposite directions are called balanced forces. When balanced forces act on an object, the object's motion remains constant or remains at rest.
A force that is pulled in opposite directions is called tension. Tension is the force experienced by an object when it is pulled on both ends in opposite directions, creating stress within the object.
stress that pushes a mass of rock in two opposite directions is called shearing
It is known as a fault line. (or a fault zone if the fault is complex rather than a single slippage of two surfaces.)
The stress force that causes a mass of rock to pull or twist in opposite directions is called tension. Shearing is the stress force that causes a mass of rock to pull or twist in opposite directions.
The forces are called balanced forces. When equal strength forces act in opposite directions, they cancel each other out, resulting in no change in the object's motion.
The stress force that causes a mass of rock to pull or twist in opposite directions is called tension. Shearing is the stress force that causes a mass of rock to pull or twist in opposite directions.
Strike Slip Fault.
The process is called bidirectional replication. In this process, DNA polymerases synthesize new strands in opposite directions on each template strand.
The wheels of a vehicle may rotate in different directions if they have a system that is called "spur-gear differential." Pinion pairs are displaced axially, and mesh part of the length between two spur gears, results in rotation in opposite directions.
Because we can't see the image you're referring to, we can't give the answer to which ray is opposite to BA. However, we can help. Opposite rays are two rays that both start from a common point and go off in exactly opposite directions. So, if there are two rays (BA and BC) with a common endpoint (B) going in different directions, they are called opposite rays.