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The Pinnacles Desert #1
A Sunset Tour of The Pinnacles Desert in Nambung National Park, located about 260 kms north of Perth, Western Australia. This unique landscape where thousands of huge limestone pillars rise from the shifting yellow sands is a photographer’s paradise. The colours of the Pinnacles change with the mood of the day and the angle of the light. This Sunset Tour with ‘Turquoise Coast Enviro Tours’ brings you views of The Pinnacles as seen from late afternoon until sunset. Some sunset photos were taken with a fill-in flash to highlight the Pinnacles, while others are silhouettes, but all are shown in natural colours and not enhanced. After you have enjoyed this Sunset tour, I hope you will join a Morning Tour to see this unique landscape by day — http://imageevent.com/gladysclancy/ecotours/thepinnaclesdesert2

 

October 2009Showing 1-40 of 10517097 visitsAlbum by gladysclancyPhotos by Gladys
Enlarge photo 1 Dunes carpeted with Wildflowers
The Pinnacles Desert is surrounded by Dunes which are carpeted with Wildflowers during Spring
Enlarge photo 2 Rose Banjine (Pimelea rosea)
Enlarge photo 3 Rose Banjine (Pimelea rosea) close-up
Enlarge photo 4 Common Clematis (Clematis pubescens)
Enlarge photo 5 Thick-leaved Fanflower (Scaevola crassifolia)
Enlarge photo 6 Silky Hemigenia (Hemigenia incana)
Enlarge photo 7 Wattle (Acacia species)
Enlarge photo 8 Wattle (Acacia species)
Enlarge photo 9 Mike is a dedicated Tour Guide
'Turquoise Coast Enviro Tours'
www.thepinnacles.com.au

Enlarge photo 10 Entering the Pinnacles Desert
Nambung National Park, Western Australia.
Located on the Swan Coastal Plain, 260 kms north of Perth.

Enlarge photo 11 Pinnacles formations
The formation of the Pinnacles would have taken many thousands of years.
Enlarge photo 12 Vegetation beside Pinnacle
In winter, rain, which is slightly acidic, dissolves small amounts of calcium carbonate as it percolates down through the sand.
Enlarge photo 13 The Pinnacles Desert
As the dune dries out during summer, this is precipitated as a cement around grains of sand in the lower levels of the dunes, binding them together and eventually producing a hard limestone rock.
Enlarge photo 14 The Pinnacles Desert
At the same time, vegetation that became established on the surface, aided this process. Plant roots stabilised the surface, and encouraged a more acidic layer of soil and humus (containing decayed plant and animal matter) to develop over the remaining quartz sand.
Enlarge photo 15 In Shadow of encroaching Sand Dune
The acidic soil accelerated the leaching process, and a hard layer of calcrete formed over the softer limestone below.
Enlarge photo 16 'Chocolate-coated' Pinnacles
Cracks which formed in the calcrete layer were exploited by plant roots.
Enlarge photo 17 The Pinnacles Desert
When water seeped down along these channels, the softer limestone beneath was slowly leached away and the channels gradually filled with quartz sand.
Enlarge photo 18 The Pinnacles Desert
This subsurface erosion continued until only the most resilient columns remained.
Enlarge photo 19 Emu Footprint in the Sand
The Pinnacles, are the eroded remnants of the formerly thick bed of limestone.
Enlarge photo 20 The Pinnacles Desert
As bush fires denuded the higher areas, south-westerly winds carried away the loose quartz sands and left these limestone pillars standing up to three and a half metres high.
Enlarge photo 21 The Pinnacles Desert
Although the formation of the Pinnacles would have taken many thousands of years, they were probably only exposed in quite recent times.
Enlarge photo 22 Yellow Sands of the Pinnacles
Aboriginal artefacts at least 6,000 years old have been found in the Pinnacles Desert despite no recent evidence of Aboriginal occupation.
Enlarge photo 23 Pinnacles Landscape
This tends to suggest that the Pinnacles were exposed about 6,000 years ago and then covered up by shifting sands, before being exposed again in the last few hundred years.
Enlarge photo 24 White Sand Dunes in the Distance
This process can be seen in action today - with the predominantly southerly winds uncovering pinnacles in the northern part of the Pinnacles Desert but covering those in the south.
Enlarge photo 25 The Pinnacles
Over time, the limestone spires will no doubt be covered again by other sand drifts and the cycle repeated, creating weird and wonderful shapes over and over again.
Enlarge photo 26 The Pinnacles
The first known European recording of the Nambung area dates back to 1658, when the North and South Hummocks first appeared on Dutch maps.
Enlarge photo 27 The Pinnacles
The Hummocks were also mentioned in navigator Philip Parker King's journal in about 1820.
Enlarge photo 28 The Pinnacles
Nambung is an Aboriginal word that means crooked or winding and it was from this river that the park was named.
Enlarge photo 29 The Pinnacles
The Pinnacles Desert remained relatively unknown until the late 1960s, when the Department of Lands and Surveys agreed to add the area to the already existing national park, which had been established in 1956.
Enlarge photo 30 The Pinnacles
Today the park is visited by approximately 250,000 visitors, from all over the world, each year.
Enlarge photo 31 The Pinnacles
Information courtesy:--
http://www.dec.wa.gov.au/hotproperty/property/national-parks/nambung-national-park-pinnacles.html

Enlarge photo 32 The Pinnacles
Nambung National Park, Western Australia
Enlarge photo 33 Parrotbush (Dryandra sessilis)
Enlarge photo 34 Opening flower of Parrotbush (Dryandra sessilis)
Enlarge photo 35 The Pinnacles
Nambung National Park, Western Australia
Enlarge photo 36 The Pinnacles
Nambung National Park, Western Australia
Enlarge photo 37 Galahs perched on a Pinnacle
Galahs(Cacatua roseicapilla)are common in Nambung National Park.
Enlarge photo 38 Nankeen Kestrel (Falco cenchroides)
This bird of prey is also known as Australian Kestrel.
Enlarge photo 39 Nankeen Kestrel (Falco cenchroides)
Enlarge photo 40 The Pinnacles
Nambung National Park, Western Australia