Summary:
The layers of Uluṟu were deposited flat, but then tipped to the angles we see today during the Alice Springs Orogeny. Uluru’s distinctive colour is due to oxidation of small amounts of iron minerals – it’s rust!
Type:
Figure
Sub Component:
Normal
Slug:
F32
Highwire: Type:
fragment
Highwire: Parent:
HighWire: Journal/Corpus Code:
csirobk
Highwire: pisa_id:
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Highwire: pisa_master:
csirobk;9781486310975/1/BK07864_ch04/F32
HighWire: Atom Path:
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Image - Large:
Highwire: cpathalias:
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Image - Medium:
Highwire: Variants:
expansion
Image - Small:
Highwire: State:
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Contributors:
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