Diamantina Fracture Zone Ridge Plateau. All these features are mirrored by corresponding topography on the other side of the Southeast Indian Ridge. Broken Ridge Plateau was formed at the ridge together with the Kerguelen Plateau. Diamantina Fracture Zone was first detected by and RV Argo in 1960. It is named after , which did further exploration in 1961. The Diamantina Deep is the zone's deepest location, located about 1 125 km West-South-West of Perth, Western Australia, at . This is not the deepest point in the Indian Ocean: the CIA's Physical Map of the World lists the Java Trench as such. On the
Diamantina Lakes Station Diamantina Lakes Station Diamantina Lakes Station most commonly known as Diamantina Lakes was a pastoral lease that once operated as a cattle station in central west Queensland, and is now Diamantina National Park a national park. Diamantina Lakes station was located about south east of Boulia and north west of Windorah in the Channel Country of Queensland. The area is a mix of landscapes including sand dunes, claypans, sandstone mesas, gibber plains and river channels. The Diamantina River traverses the area meaning the plains are able to support extensive grasslands and have near-permanent naturally deep waterholes, fed by seasonal rains