Southland District, South Island
Le Secrétariat de l’UNESCO et le Centre du patrimoine mondial ne garantissent pas l’exactitude et la fiabilité des avis, opinions, déclarations et autres informations ou documentations fournis au Secrétariat de l’UNESCO et au Centre du patrimoine mondial par les États Parties à la Convention concernant la protection du patrimoine mondial, culturel et naturel.
La publication de tels avis, opinions, déclarations, informations ou documentations sur le site internet et/ou dans les documents de travail du Centre du patrimoine mondial n’implique nullement l’expression d’une quelconque opinion de la part du Secrétariat de l’UNESCO ou du Centre du patrimoine mondial concernant le statut juridique de tout pays, territoire, ville ou région, ou de leurs autorités, ou le tracé de leurs frontières.
Les noms des biens figurent dans la langue dans laquelle les États parties les ont soumis.
Most of the 15 fiords of Fiordland are 200-300 m deep, usually with a pronounced shallower ‘lip' near the mouth of the fiord, indicating ‘over-deepening' by the glacial ice. The longer fiords reach back into the heart of the mountains of Fiordland National Park; the head of Hall Arm, for instance, is 40 km from the mouth of Doubtful Sound.
The marine environment of Fiordland is quite different from the rest of New Zealand. The deeply indented coastline has given rise to two contrasting marine environments:
(a) the wild, exposed outer coastline, with typical west coast New Zealand marine community and zonation patterns, and the preferred breeding habitat for fur seals and a wide range of ocean birds such as petrels, prions, shearwaters and penguins; and
(b) the sheltered, steep-walled fiords, which have a total shoreline length of nearly 1000 km, depths up to 420 m, and a unique inversion of usual patterns of coastal marine life.
The fiords are an integral part of the Fiordland landscape and ecosystems, which were included until the early 1960s within Fiordland National Park. However they were not included in the site when Fiordland National Park was listed as natural World Heritage in 1986. When the World Heritage Committee listed the park as World Heritage, one of its recommendations to the New Zealand government was "...to note the importance of the waters of the fiords as an integral part of the area and welcome any initiatives to bring them under the control of the park authorities".
In 1990, when Fiordland National Park was incorporated into the much larger (2.6 million ha) Te Wahipounamu (South-West New Zealand) World Heritage Area, the issue of listing the seabed and waters of the fiords was again raised by the IUCN (The World Conservation Union) to enhance the integrity of this outstanding World Heritage site.
In April 2005, after the passing of the Fiordland Marine Management Act, the Fiordland (Te Moana o Atawhenua) Marine Area and management regime was enacted:
With these legal protection measures now adopted, the seabed and waters of the fiords have been placed on the New Zealand tentative World Heritage list, as an addition to Te Wahipounamu (South-West New Zealand) World Heritage Area.