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Explanation: A fault where 2 plates slide against each other, parallel to the fault line.
Stress that Causes this: Shearing causes the rock layers to slide.

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Explanation: a downward fold in the rock layers.  The rock layers sink down to form a upside down arch or u-shape.
Stress that causes it: Compression causes the rock layers in a syncline to fold in a u like shape.

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Explanation: a upwards fold in the rock layers.  The layers of rock push up into a arch shape.
Stress that causes it: Compression causes the rock layers in an anticline to form their arch shape fold.

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A bend in rock layers

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Explanation: A fault where the hanging wall moves downwards, in relation to the foot wall.
Stress that Causes this: Tension causes the rock layers to change its shape/break.

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Explanation: a reverse is the opposite to a normal fault. In a normal fault the hanging wall moves downward, while in a reverse fault the hanging wall moves upward, relative to foot wall.
Stress that causes it: Compression stress, which occurs at a convergent boundary, causes a reverse fault to happen.

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The cause of stress for these types of faults/folds are convection currents. The convection currents are always moving. This shapes the land in many different ways. The convection currents pushes the land upwards, downwards, and sideways. This results in faults and folds.