The Pinnacles are limestone formations contained within Nambung National Park, near the town of Cervantes, Western Australia.

Formation

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 blown inland to form high mobile dunes. This represented the raw material for the formation the Pinnacles.

The mechanisms through which the Pinnacles were formed from this raw material are the subject of some controversy, with three possible mechanisms having been proposed:

The Pinnacles were formed from lime leaching from the aeolian sand (wind-blown 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 and quartz sand fills the channels that form. Vegetation dies and winds blow away the sand covering the eroded limestone, thus revealing the Pinnacles.

The Pinnacles were formed through the preservation of casts of trees buried in coastal aeolianites where roots became groundwater conduits, resulting in precipitation of indurated (hard) calcrete. Subsequent wind erosion of the aeolianite would then expose the calcrete pillars.

On the basis of the mechanism of formation of smaller “root casts” occurring in other parts of the world, it has been proposed that plants played an active role in the creation of the Pinnacles, rather than the rather passive role detailed in 1 and 2 above. The proposal is that as transpiration draws water through the soil to the roots, nutrients and other dissolved minerals flow toward the root. This process is termed "mass-flow" and can result in the accumulation of nutrients at the surface of the root, if the nutrients arrive in quantities greater than needed for plant growth. In coastal aeolian sands which have large amounts of Ca (derived from marine shells) the movement of water to the roots would drive the flow of Ca to the root surface. This Ca accumulates at high concentrations around the roots and over time is converted into a calcrete. When the roots die, the space occupied by the root is subsequently also filled with a carbonate material derived from the Ca in the former tissue of the roots and possibly also from water leaching through the structures. Although evidence has been provided for this mechanism in the formation of root casts in South Africa, evidence is still required for its role in the formation of the Pinnacles.

Tourism

The Pinnacles remained relatively unknown to most Australians until the 1960s, when the area was added to Nambung National Park. The area receives over 250,000 visitors a year. A visitor precinct and interpretive centre was completed in March 2008.

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.

The Pinnacles were featured in the musical number "Ye Jaan Le Le" in the 1997 Indian film, Daud, starring Sanjay Dutt and Urmila Matondkar. They were also featured in the music video for the song "Standing on the Shore" by Australian electropop duo Empire of the Sun.

credited to wikipedia