The Austral islands include two island groups, the Tubuai Group and the Bass Islands. The Tubuai Group (22–23º S, 147–152º W) includes the four inhabited islands of
Rimatara,
Rurutu,
Tubuai, and
Raivavae, along with the uninhabited
Îles Maria atoll. The
Bass Islands (27º 35' S, 144º W) include inhabited
Rapa island (or Rapa Iti) and the uninhabited
Marotiri or Bass Rocks to the southeast. Tubuai is the largest of the Austral islands at 44 km2. The total land area of the ecoregion is 142 km2. The islands are volcanic in origin, formed as the
Pacific Plate moved west-northwest over a geologic
hotspot. The inhabited islands have volcanic rocks at the center of the island, with rings of coralline limestone, known as makatea, in the coastal lowlands. Makatea was created when the islands were uplifted to expose ancient coral reefs, and often forms rough and uncultivable terrain. Tubuai has two central peaks which rise above 400 meters, and are surrounded and separated by makatea at lower elevations. Rurutu Island has volcanic hills at the center of the island, with Manureva reaching 385 meters elevation. The island was geologically uplifted, creating a continuous makatea rim along the shore that reaches 50 to 60 meters high. Rimatara Island also has a makatea rim, with low and weathered central volcanic hills. Maria is a low coral atoll. Raivavae is an heavily eroded extinct volcano with a central peak (Hiro, 438 meters), with makatea outcrops along the shore, and surrounded by a lagoon and encircling barrier reef. Rapa is an ancient crescent-shaped volcanic caldera. Its highest point is Perau at 633 meters, which is also the highest peak in the ecoregion. Marotiri consists of very young, steep volcanic crags with no fringing reef. ==Flora==