The three events that can be observed at transform plate boundaries are the earthquakes, faults, and formation of mountains.
Explanation:
The transform plate boundaries are the boundaries between two plates that are sliding past each other. This means that there is no collision between the plates, as they move in opposite direction, so they just rub off one another. That rubbing between them actually causes lot of stress to the crust. The stress on the crust manifests itself in multiple ways, like the creation of faults, common earthquakes, as well as the formation of mountains in some cases.
The faults are the trademark of the transform plate boundaries. They form when the crust is lengthening, so a gap opens up, while one side moves up, and the other side moves down, or one side moves up or down, while the other is static.
The faults actually manage to create small to medium size mountains in some cases. That can happen when one of the sides of the faults moves significantly up, while the other side moves significantly down, thus forming a mountain and a valley.
Because of the constant stress on the crust, it breaks, and when it does, the crust from above is falling in the gap and adjusts itself, resulting in release of lot of power which creates the earthquakes.
There are threetypes of plate boundary such as Constructive, destructive and transform plate boundary. The primary landform in the Transform boundary are faults which is caused by the Earthquakes. Many transform boundary landforms are in the ocean floor which is responsible for the island formation. Fault is found due to the two process such as Ridgepush and ridge pull. Transform boundary neither creates and nor destroys any land in the region.
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