Unlike the Aucklands, Campbell and Antipodes, which are primarily volcanic in origin, the Bounties are made of igneous rock, pushed up from the floor of the ocean.

The Bounty Islands are divided roughly into three groups: Main, Centre and East. Their total land mass is only 135ha, with Depot Island being the largest in the group at 800m in length and 88m at its highest point.

The Bounty Islands have virtually no soil or vegetation as they are frequently washed clean by rain and spray from the often huge waves which crash into them.

Despite the hostile conditions, the islands manage to live up to their name during the summer breeding season by hosting thousands of seabirds, including the world’s rarest cormorant, the Bounty Island shag, of which there are only 500-600 individuals. The Bounty Island shag is one of the few birds present on the island throughout the year.

The islands are also the primary breeding area for erect-crested penguins (whose only other breeding site is the Antipodes group) and Salvins mollymawks (75,000 pairs estimated to be breeding here with several hundred pairs breeding on the Snares). Antarctic terns, fulmar prions, Snares cape pigeons and Southern black-backed gulls also nest here in lesser numbers.

The Bounty Islands were discovered and named by Captain William Bligh of the British naval ship 'Bounty' in 1788, just months before the infamous mutiny.

In the early 19th century hunters decimated the large population of fur seals on the islands. The first two years of sealing on the Bounty Islands saw 50,000 seals killed. By the early 1830s just a handful were left.

There were no known shipwrecks on the Bounty Islands, although a castaway depot was established on Depot Island in anticipation of such an event. Nothing remains of the depot today.

source:http://www.doc.govt.nz/parks-and-recreation/places-to-go/southland/places/subantarctic-islands/bounty-islands/