Linked from

The 16 pages that link to Indo-Australian plate, each with the reason it gives.

• 2004 Indian Ocean earthquake and tsunamiRelated: Its convergence with the Burma region drove the subduction loading released in 2004.

• Lesser Sunda IslandsRelated: Its convergence with the overriding plate drives subduction south of the islands.

• Sunda ArcRelated: Its descent beneath the Sunda Plate supplies the arc’s subduction system.

• Sunda StraitRelated: Its subduction beneath the Sunda region contributes to local earthquakes and volcanism.

• Sunda TrenchRelated: Its oceanic crust descends beneath the Sunda region at the trench.

• New Guinea HighlandsRelated: Its complex motion underlies the highlands’ tectonic setting.

• Indonesian archipelagoRelated: Its subduction beneath the archipelago’s southern margin drives earthquakes and volcanism.

• Sunda PlateRelated: Its convergence with the Sunda Plate drives subduction along the region’s southern margin.

• Malay ArchipelagoRelated: Its movement beneath neighboring plates drives uplift, earthquakes, and volcanism across the region.

• KrakatoaRelated: Its subduction beneath the Sunda region supplies the magma that feeds Krakatoa.

• Southeast Indian RidgeRelated: It forms the northern side of the ridge’s plate boundary.

• Greater Sunda IslandsRelated: Its subduction beneath the Sunda margin drives earthquakes and volcanism on the islands’ southern edge.

• Central Indian RidgeRelated: Its western boundary diverges from neighboring plates at the ridge system.

• Mount BromoRelated: Its subduction contributes to the magma that feeds Java’s volcanoes.

• Mount PapandayanRelated: Its subduction helps supply magma to West Java’s volcanoes.