Geology
The Flinders Ranges are largely composed of folded and faulted sediments of the Adelaide Geosyncline. This very thick sequence of sediments were deposited in a large basin during the Neoproterozoic on the passive margin of the ancient continent of Rodinia. During the Cambrian, approximately 540 million years ago, the area underwent the Delamerian orogeny where the geosynclinal sequence was folded and faulted into a large mountain range. Since this time the area has undergone erosion resulting in the relatively low ranges today.
Most of the high ground and ridgetops in the Flinders are sequences of quartzites that outcrop along strike. The high walls of Wilpena Pound are formed by the outcropping beds of the eponymous Pound Quartzite in a synclinal structure. The same formation forms many of the other high parts of the Flinders, including the high plateau of the Gammon Ranges and the Heysen Range. Cuesta forms are also very common in the Flinders.
The Ranges are particularly renowned for the Ediacara Hills, north-west of Leigh Creek. This was the site of discovery in 1946 of some of the oldest fossil evidence of animal life. Since then similar fossils have been found in many other parts of the ranges, though their locations are a closely kept secret due to the risk of sites being desecrated. In 2004 a new geological period, the Ediacaran Period was formed to mark the appearance of Ediacara biota.
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