About 6cm a year.
Australia lies on the Indo-Australian plate.
The indo-australian plate is mostly a convergent boundary with the pacific plate.
New Zealand shares the Australian plate.
The Indo-Australian Plate is primarily formed by the collision of the Australian Plate and the Indian Plate. This collision is ongoing and has resulted in the uplift of the Himalayas and the Tibetan Plateau.
in the top of the Australian plate
Australia is located on the Indo-Australian Plate, which is a major tectonic plate that includes the continent of Australia as well as the Indian subcontinent and surrounding oceanic crust.
The indo-Australian plate.
The proposed plate called the Capricorn Plate is a relatively rigid oceanic structure that was the westernmost part of the Indo-Australian Plate, which is now believed to exist as three separate smaller plates: the Indian Plate, the Australian Plate, and the Capricorn Plate.
The Indo-Australian plate moves Northeast as the Pacific Plate moves around it in a Northwest direction as if rotating.
The Indo-Australian plate moves at an average rate of about 6 to 7 centimeters per year in a northeasterly direction. This movement is responsible for seismic activity in the region, particularly along plate boundaries such as the Himalayas and the Sumatra-Andaman fault zone.
The Indo-Australian plate.