The devils marbles are large granitic boulders that form the exposed top layer of an extensive and mostly underground granite formation.
The devils marbles formation.
When i see fields of boulders i think glaciers.
The devils marbles are made of large granitic boulders which were formed millions of years ago as a result of the hardening of magma within the earth s crust the natural processes of weathering and erosion have created the various shapes of the boulders.
Standing at up to 6 metres high and formed over millions of years they continue to crack and change.
The devils marbles are a collection of massive granite boulders strewn across a valley south of tennant creek.
The marbles have been formed over millions of years by the act of erosion and rise up out of the desert scenery in a surreal display of granite kind of like a natural art exhibition.
It s the meeting place of four different language groups.
A sacred aboriginal site.
What are the devils marbles and how were they formed.
Located near the geology gifted town of natural bridge virginia the devil s marbleyard is a jumbled morass of refrigerator car and bus sized boulders strewn over eight acres on the side of a mountain.
Many of them seem impossibly balanced on top of each other just like the two marbles in the famous picture.
An ancient aboriginal meeting point naming the devils marbles.
These impressive granite boulders are peppered around a sprawling valley about 100 kilometres to the south of tennant creek.
The devils marbles or karlu karlu as they are known by the local warumungu aboriginals are a collection of huge red rounded granite boulders.
Actually they vary in size from 50 cm up to six metres across and they are strewn across a large area.
Forming one of the northern territory s most impressive geological wonders the devil s marbles can be found not too far from uluru.
The devils marbles are located within the karlu karlu devils marbles conservation reserve.
The devils marbles are called karlu karlu in alyawarre pronounced al yow worrah a local aboriginal language.
The large boulders are culturally and spiritually significant to the land s traditional.
The marbleyard is a unique geological feature that can best be described as a huge rock field with boulders ranging from the size of coffee tables to those of large vans.
The formation of the devils marbles are a result of the erosion of the sandstone on top of granite which was formed millions of years ago due to the hardening of magma within the earth s crust which the marbles are made up of.
The devil s marbleyard is a 3 mile hike located in the james river face wilderness area as part of the belfast trail.
The natural processes of weathering and erosion have created the various shapes of the boulders.
