Granite outcrops, more properly known as monadnocks or inselbergs (an isolated hill or small mountain that rises abruptly from a surrounding plain – literally ‘island mountain’), are a feature of the Yilgarn Craton and are dotted conveniently throughout the south-west of Western Australia extending beyond Kalgoorlie.
Although monadnock is a Native American term and inselberg is German for ‘island mountain’ they are particularly suitable terms to describe the granite outcrops in the south west of Australia.
Granite outcrops have their own ecosystem an act as island sanctuaries for a whole range of wildlife. They are characterised by a belt of thick vegetation around the base of the rock. In many cases this vegetation is swamp like, due to the large amount of runoff from the rock.
In remote, low rainfall area these granite outcrops catch and direct precious rain water that, in earlier times, was so vital for aborigines, and later explorers and prospectors as they pushed to the east. David Carnegie, a prospector and explorer active in the 1890s, recorded in his classic book Spinifex and Sand:
“The monotony of the flat timber-clad country was occasionally relieved by the occurrence of large isolated hills of bare granite. But for these the road, except for camels, could never have been kept open; for they represented our source of water supply. On the surface of the rocks numerous holes and indentations are found, which after rain, hold water, and besides these, around the foot of the outcrops, ‘soaks”, or shallow wells, are to be found.”
These granite outcrops were particularly useful for navigating through the dense thickets of tamma. Navigators would climb to the summit, find a distant outcrop in their desired direction of travel, take a sighting on it and then, once down among the thickets again, follow the bearing to the destination.
Granite outcrops support a discrete ecosystem in their vicinity, supporting many organisms that are not found elsewhere.
© Kim Epton 2014-2021
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