The Pinnacles is contained within
Natural history
The base material for the limestone came from sea shells which were broken-down into lime-rich sand. This sand was then blown inland by natural wind pattens, forming high sand dunes. Rain caused the lime to seep to the bottom of the dunes, where it stuck together and formed limestone. Small plants began growing on top of the dunes, protecting the dunes from being blown away again by the wind. This also helped to create an acidic layer of soil over the top of the dune, which further contributed to the leaching of the lime from the soil. A layer of calcrete formed over the soft limestone under the dunes. Small cracks in this hard layer allowed plants to send down deeper roots, which had the side-effect of allowing water to flow in also, gradually eroding the soft limestone beneath. This was replaced by quartz sand from the dune above. This continued until only columns of limestone that sat protected from the encroaching water remained. These columns were exposed when the vegetation on top of the dune died, allowing the wind to blow away the dune and sand between from between them.
Tourismus
The Pinnacles remained relatively unknown to most Australians until the 1960s, when the area was added to
As of February 2007, entrance to the park costs AUS$10.00 per car, or AUS$4.00 per person on a tourbus.
The area receives over 250,000 visitors a year. A visitor precinct and interpretive centre was completed in March 2008.
Credited to wikipedia and flickr: 5348 Franco


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