Uluru is a large sandstone monolith rising from flat scrubland in central Australia's Northern Territory, within Uluru-Kata Tjuta National Park. Geologically it is an inselberg, an isolated remnant hill left standing after the erosion of a much larger mountain range that once covered the region. The rock began forming roughly 500 million years ago as sediment deposited in an ancient inland sea, was compressed into arkose sandstone rich in feldspar, and was later uplifted and tilted onto its side so that its original rock layers now stand nearly vertical. Iron oxidation on its exposed surface gives Uluru its distinctive red to orange color, though the sandstone beneath is grey. It rises 863 meters above sea level, about 348 meters above the surrounding plain, with a base circumference of roughly 9.4 kilometers.
Facts
Highest Elevation (m) Connections
Associated With
Source Australia (Wikipedia)
Source Encyclopaedia Britannica
Demonstrates
Uluru's weathered outer surface, shaped by physical and chemical breakdown in place, is a well-documented example of weathering acting on a single exposed monolith.
Source British Geological Survey
Shaped By
Source Uluru (Wikipedia)
Sources
1. Uluru (Wikidata)
Wikimedia FoundationWikidata item Q33910Quote, Wikidata item Q33910
P31 monolith/inselberg, matched by enwiki sitelink title Uluru
View the Source 2. Uluru (Wikipedia)
Wikimedia FoundationInfobox coordinates
25.34500°S 131.03611°E
Shaped By: Erosion, Formation statement for target 23652
An inselberg is a prominent isolated residual knob or hill that rises abruptly from and is surrounded by extensive and relatively flat erosion lowlands in a hot, dry region.
View the Source Encyclopaedia Britannica
Encyclopaedia Britannica, Inc.- Uluru/Ayers Rock
- Associated With: Oceania
View the Source Wikidata: Uluru
British Geological Survey
Australia (Wikipedia)
Reader Challenges (0)
No disputes yet. Spotted an error or a better source? Open the first one.
Sign in to dispute this or suggest a correction.