Walga (Walganna) Rock, 1.8 km long and composed of post-tectonic granite, is one of the many whalebacks scattered throughout the Yilgarn Craton. Situated on the Western section of the craton which consists of rocks of every Archean era with zircons dating back to the Hadean also clastic sedimentary rock. It consists of K-feldspar porphyritic monogranite that forms the type area thought to be approx. 2.5 billion years old.

Above the gallery situated on the cave wall are large slabs of granite in the process of ‘peeling off’  the main rock form. This process is caused by expansion and contraction of the surface because of extreme seasonal and diurnal temperatures in this inland (300 km), arid climate. Rain water and wind erosion molded and eroded the lower recessed section of the rock.

The rock overhang protected the array of paintings. The depiction of a masted boat was quoted by archaeologists  as evidence of contact with sailors of European origin, firstly Dutch and then later archaeological evidence suggested a similarity between this depiction and the nineteenth century coastal steamer SS Xantho. (Bigourdan, 2006)

I took a rubbing/frottage from rocks as well as rice paper stains from soil far from the enclosure. They are a way for me to connect with the place via a tactile experience when I return to my studio. Often I adhere them with gesso to the canvas surface.

This technique is one that includes quick sketches done on site. Below are previous examples of this mixing of different media which I meld into large oil paintings. They may be viewed on my website : desterreart.com.au and are part of a series titled An Archaeology of Landscape.

P.S.  Correction: Feldspar should read K-feldspar. The “K”, refers to the Potassium content of feldspar. There are 3 K feldspars: microcline, sanidine and orthoclase (orthoclase and plagioclase, another type of feldspar, are often easily seen in volcanic rocks, they’re usually a milky to pinkish white).