The Pinnacles Desert

The Pinnacles is contained within Nambung National Park, near the town of Cervantes, Western Australia. The Pinnacles are limestone formations. The raw material for the limestone of the Pinnacles came from seashells in an earlier epoch rich in marine life. These shells were broken down into lime rich sands which were carried inland to form high mobile dunes. The Pinnacles were formed from lime leaching from the sand and by rain cementing the lower levels of the dune into a soft limestone. Vegetation forms an acidic layer of soil and humus. A hard cap of calcrete develops above the softer limestone. Cracks in the calcrete are exploited by plant roots. The softer limestone continues to dissolve. Quartz sand fills the channels that form. Vegetation dies and winds blow away the sand covering the eroded limestone, thus revealing the Pinnacles.

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.

Tourism

The Pinnacles remained relatively unknown to most Australians until the 1960s, when the area was added to Nambung National Park. [M. Bright, 1001 Natural Wonders You Must See before You Die, Quintet Publishing, London 2005] The best season to see the Pinnacles is spring from August to October, as the days are mild and wildflowers start to bloom. The pinnacle formations are best viewed in the early morning or late afternoon as the play of light brings out the colours and the extended shadows of the formations delivers a contrast that brings out their features. Most animals in the park are nocturnal, but emus and kangaroos can also be seen during the daytime, more commonly in the evening or early morning.

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 new Visitor precinct and interpretive centre will be completed in March 2008. [ [http://www.naturebase.net/component/option,com_hotproperty/task,view/id,61/Itemid,755/ Nambung National Park (Pinnacles)] NatureBase. Retrieved 2007-03-24.]

The Pinnacles were featured in the musical number "Ye Jaan Le Le" in the Indian film, Daud: Fun on the Run (1997) starring Sanjay Dutt and Urmila Matondkar

References

Further reading

* Stephens, Alan.(1989) "Pinnacles : Nambung National Park, Western Australia" (photography, Alan Stephens - text, Sue Hughes) Mulgrave, Vic. : Nucolorvue Productions, ISBN 085858106X

External links

* [http://www.thepinnacles.com.au Pinnacles Tour Guide]
* [http://www.kissthetime.org/Day70.htm Images of the Pinnacles]