Editing Mount Conner (section)

==Geology==
The sides of Mount Conner are blanketed by [[scree]] (talus) and its top is blanketed by [[colluvium]]. The base of Mount Conner is surrounded by [[alluvium]].<ref name="YoungOthers2002a">Young, DN, N Duncan, A Camacho, PA Ferenczi, and TLA Madigan (2002a) ''Ayers Rock, SG 52-8 map, 1:250 000 Geological Series (Second Edition), Northern Territory Geological Survey.'' scale 1:250 000, Darwin, Northern Territory Geological Survey, Australia.</ref><ref name="YoungOthers2002b">Young, DN, N Duncan, A Camacho, PA Ferenczi, and TLA Madigan (2002b) ''Ayers Rock, SG 52-8 Explanatory Text, 1:250 000 Geological Series (Second Edition).'' scale 1:250 000, Darwin, Northern Territory Geological Survey, Australia.</ref><ref name="Edgoose2012a">Edgoose, CJ (2012) ''The Amadeus Basin, central Australia.'' Episodes. 35(1):257-263.</ref>

The summit of Mount Conner, along with the summits of low domes in the [[Kata Tjuta]] complex and summit levels of Uluru, is an erosional remnant of a [[Cretaceous]] geomorphic surface. It is considered to be a classic example of an [[inselberg]] created by erosion of surrounding strata.<ref name="Twidale2007a">[[Charles Rowland Twidale|Twidale, C.R.]] (2007) ''Ancient Australian Landscapes.'' Rosenberg Publishing, Kenthurst, New South Wales. 144 pp.</ref>