1. Tectonic Uplift: Uluru is a large rock formation that was formed as part of the Petermann Ranges, which were uplifted due to tectonic forces. The uplift occurred around 550 million years ago, and it resulted in the formation of a large dome-shaped rock structure.
2. Erosion: After the uplift, Uluru was subjected to various erosional processes. Wind erosion, water erosion, and freeze-thaw cycles have all played a role in shaping the rock formation. The softer layers of rock have been eroded away, while the more resistant layers have remained intact.
3. Weathering: The harsh desert climate has also contributed to the weathering of Uluru. The extreme temperature fluctuations, as well as the presence of water and salts, have caused the rock to break down and form small fragments. These fragments have been transported away by wind and water, further shaping the rock formation.
4. Exfoliation: Exfoliation is the process of rock splitting into thin layers and breaking away from the main rock mass. This process is caused by the expansion and contraction of the rock due to changes in temperature. Over time, this process has created the distinctive onion-like layers that are visible on Uluru.
5. Jointing and Fracturing: Uluru is also characterized by the presence of joints and fractures. These are natural cracks and weaknesses in the rock that have been caused by tectonic forces, weathering, and erosion. The joints and fractures have allowed water and wind to penetrate the rock, further contributing to its shaping and erosion.
6. Sediment Deposition: Over time, sediment and debris from the surrounding desert have accumulated around the base of Uluru. This sediment has been transported by wind and water and has helped to shape the surrounding landscape.
These geomorphic processes have acted over millions of years to create Uluru's unique shape and features. The rock formation continues to be shaped by these processes, albeit at a slower rate due to the arid climate and the lack of water.