This week, Rover decided it was time to answer a question which one of his friends asked him some time ago. This friend was travelling through the Central West area, and saw lots of huge, rounded rocks in the paddocks and along the side of the road. The question was, what were they? Rover is fascinated by these rocks, which are not only geologically interesting, but really quite beautiful. What are the rocks called? Granite Tors.
These particular tors were photographed in Cowra, but granite tors are scattered throughout the Central West. You can see them on hill tops, in paddocks, and even just beside the road. They’re fascinating rocks, weathered over many, many years to be their distinctive shape. In the Central West, most of them are quite rounded.
Granite tors are extraordinary, jutting out the landscape seemingly randomly, or appearing in groups. They are often quite massive, and look like some giant threw them randomly, allowing them to settle into the landscape thousands of years ago. So how were they created? Granite tors are, essentially, large lumps of granite, but how they form is something of a mystery. Many believe that tors were once surrounded by other outcrops of granite, but the granite which became tors weathered more slowly. According to this theory the surrounding granite would have had many fault lines and joints, which helped normal weathering processes to speed up. The tors though had few joints and faults, so they weathered slowly, and were left in place long after the surrounding granite was gone.
The tors weathered slowly, over a long period of time, which is why they remain in the landscape. Yet they do weather, just like any other rock. They often weather in a very specific way though - a type of weathering called onion-skin weathering (or sometimes called exfoliation). Essentially, when onion-skin weathering occurs, the outer layer of the rock peels off, like the skin of an onion. This type of weathering occurs because of extreme variations in temperature - the rock becomes very hot during the day, and very cold in the nighttime. Sometimes, water might even freeze inside the rock, and all of these changes in temperature force the rock to split and the outer layer to fall away. You can see an example of onion skin weathering in the photo above.