Victoria (Australia) in the area occurred in 1803 at Sullivan Bay, and much of what is now Victoria was included in 1836 in the Port Phillip District, an administrative division of New South Wales. Named in honour of Queen Victoria, who signed the division's separation from New South Wales, the colony was officially established in 1851 and achieved self government in 1855. The Victorian gold rush in the 1850s and 1860s significantly increased both the population and wealth of the colony, and by the time of the Federation of Australia in 1901, Melbourne had become the largest city and leading financial centre
Geology of the Australian Capital Territory is located on a terrane that is called the Benambra Terrane in Victoria, but the Molong-Monaro Terrane in New South Wales. also known as Canberra-Yass Synclinorial Zone East also known as Canberra-Yass Synclinorial Zone west A plate with a continent fragment on board bumped into the east coast of what is now Australia, forming the Delamerian Orogeny. The remains of the mountains of this orogeny can be found near Broken Hill and in eastern South Australia, western Victoria, and western Tasmania. This happened between 520 and 480 million years ago up to the Cambrian period. No associated ocean floor has