World Heritage Site: Uluru-Kata Tjuta National Park
Publication Year: 2012
Publication Type: Article
Publication Identifier: WHE3B722FE667
Summary
Uluru's morphology is a result of episodic exposure, shaped not by uplift but by the lowering of surrounding plains. This inselberg, formed from arkosic sandstone, exhibits features like tafoni and slope breaks due to deep subsurface weathering and stripping of regolith. Indigenous interpretations link its landforms to mythological narratives, while scientific explanations attribute them to processes such as scarp retreat, wind or water erosion, and climatic variations. The study contrasts these contrasting perceptions, highlighting Uluru's geological evolution from the latest Mesozoic to its current form.
Citation
Twidale, C. R., & Bourne, J. A. (2012). Contrasted Perceptions of Uluru. Physical Geography, 33(3), 285–302. https://doi.org/10.2747/0272-3646.33.3.285
You are here:
World Heritage Explorer > World Heritage Research > Publications > Contrasted Perceptions of Uluru