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Girraween National Park is not far from my daughter’s place near Stanthorpe. It’s in the Granite Belt which stretches for 250 kilometres from Warwick in Queensland to Armidale in NSW. 

For its creation story, take yourself back 240 million years. Two tectonic plates approach each other and compress the crust of the eastern side of whatever was sort-of Australia then. The heat is intense, and a molten mass of magma invades older rocks. Two kilometres below the earth’s surface, it cools very slowly, creating coarse-textured granite. It’s under an immense weight of older rock which is gradually eroded away. The upper face of the granite expands upwards and cracks and large slabs, sometimes metres thick, break away  from the mother rock. Gradually, where there are a lot of fractures, sheets break into blocks and the roughly rectangular blocks become weathered into rounded boulders, like the ones I’m walking through now. But there are less-fractured places in Girraween, now beyond my aging reach: broad slabs, steep domes and pinnacles of bare granite with names like The Pyramid and Castle Rock. The creation story continues today: chemical reactions dissolve the boulders into a mixture of kaolinite clay and quartz sand; each episode of freeze and thaw enlarges cracks; wind, water, animals, algae, bacteria, lichens and mosses also play a part in weakening and shaping the stone.

My  Girraween walk this visit isn’t a long one (less than 2km): it meanders between boulders, the legacy of the processes of long time, as it makes its way to today’s goal, the Granite Arch. I have two cameras slung around my neck and my sturdy walking stick, just in case I want to venture beyond the well-made track. 

The trail begins with a creek crossing, concrete bridges joining granite slabs. But the main beauty is the rockscape, everywhere rounded boulders, leaning over and resting on each other amongst the scrub, sometimes paddling in bright wattle, sharp leaved bell shaped heath flowers, a couple of white correas. Where the rocks are sparser there is plenty of moss and sundews. 

I round a corner, and there’s the Granite Arch: a huge rounded lintel-rock, supported by two doorposts. 

For once geological information is easy to come by, easily understood and accompanied by explanatory photos. I am grateful! For a photo gallery covering more of the park than my legs can manage, see here.

The panel near the Granite Arch was also informative, although geological processes satisfy me: I don’t need the handiwork of giants. It’s a pity too that the Thoreau quote is so apposite: David Henry is not my favourite person!