Steven C.
Google
Spectacular view of entire city of Hobart up here! Dress warmly, even on a sunny summer day, specially in the afternoon.
Rising 1,271 meters above Hobart, kunanyi / Mt Wellington is a geological masterpiece. Its striking appearance is defined by a dramatic interplay of sedimentary and igneous rock.
The mountain’s base and foothills consist of Permian mudstone and Triassic sandstone, formed over 200 million years ago when the area was a shallow seabed. However, the summit is dominated by massive Jurassic dolerite.
This dark, durable stone intruded as molten magma approximately 170 million years ago during the breakup of Gondwana. As it cooled, it fractured into the iconic vertical columns known as the Organ Pipes, creating a rugged silhouette that defines the Tasmanian skyline.