| Solander Islands / Hautere | |
| Local Name: | Māori Hautere |
| Location: | Southland District |
| Coordinates: | -46.5667°N 219°W |
| Area Ha: | 120 |
| Length Km: | 1.6 |
| Elevation M: | 330 |
| Country: | New Zealand |
| Additional Info: | Age Pleistocene Arc volcano |
The Solander Islands / Hautere are three eroded remnants volcanic islets towards the western enterance of the Foveaux Strait just beyond New Zealand's South Island. The islands lie 40km (30miles) south of the coastline of Fiordland.[1]
The islands are andesite rocks with the tip being a larger submerged volcano, roughly equivalent in size to Mount Taranaki.[2] [3] It was formerly believed that the volcano last erupted roughly 2 million years ago, but in 2008 radiometric dating of rock samples from the main island found that it was between 150,000 and 400,000 years old.[4] In 2013 it was discovered that Little Solander Island had been active even more recently at between 20 and 50,000 years ago.[5]
Administratively, the islands form part of Southland District, making them the only uninhabited outlying island group of New Zealand to be part of a local authority.
Solander Island / Hautere (also known in Māori as Te Niho a Kewa), the main island,[6] covers around 1km2, rising steeply to a peak 330m (1,080feet) above sea level. It is wooded except for its northeast end, mainly a bare, white rock. A deep cave is on the east side, Sealers Cave. Little Solander Island is 1.9km (01.2miles) west. It reaches 1480NaN0 high yet covers 4ha. It has a barren appearance and is guano-covered. Pierced Rock is 2500NaN0 south of the main island. It rises to 540NaN0 and covers 2000m2 (0.2 ha).
Administratively, the islands form part of Southland District, making them the only uninhabited outlying island group of New Zealand to be part of a local authority.
The Māori name for the summit of Solander Island is Pukekohu, and the side of the summit is known in Māori as Pukepari.[7] "Hautere" is the father of Moko, a Ngāti Kurī chief, who notably murdered a Kāti Māmoe chief called Tūtewaimate.[8] [9]
The island chain was sighted by Captain James Cook on 11 March 1770 and named by him after the Swedish naturalist Daniel Solander, one of the scientific crew aboard Cook's ship, Endeavour.[10]
The islands are geographically forbidding and weather conditions often confound the approach of ships, dissuading attempts at permanent habitation. Australian sealers briefly made use of the islands during the early 19th century, likely living on small flats between the island's cliffs and its shoreline for stints of a few months.[11] Castaways would occasionally end up on the islands, and in 1813, a passing ship bound for Stewart Island found five men in need of rescue. The men - four Europeans and one Australian Aboriginal - were marooned there between 1808 and 1813, representing the longest continuous period of habitation on the islands. They are thought to have been left ashore in two groups for seal hunting (sealing), but the sea prevented the approach of any ship to recover them. In 1810, sealing moved to Macquarie Island, farther to the west, and they were effectively abandoned. When rediscovered in 1813, it is likely that they had amassed many dried seal pelts.[11]
The islands are remnants of an isolated extinct trachyandesite and andesite Pleistocene volcano whose volcanics have geochemical affinities with modern adakites.[12] [13] The andestic dome of Little Solander Island was active between 20 and 50,000 years ago.[5] The age of the main island is 150 to 400 thousand years old, backed up by pollen data, with in one set of analysis the eruptives having a mean age of 344 ± 10 ka and another mean age of 247 ± 8 ka.[5] [4] The islands lie on a bank with depths less than 1000NaN0, separated from the continental shelf along Foveaux Strait by a 4km (02miles) but narrow trough 2000NaN0 deep (at least 237m (778feet)). Therefore, the islands are included in the New Zealand Outlying Islands.
The islands are the only volcanic land in New Zealand recently related to the subduction of the Australian Plate beneath the Pacific Plate[4] [14] along the Puysegur Trench, which extends southwards from the end of the Alpine Fault.[15] The current estimated rate of subduction is 35–36 mm per year.[12] The Solander Basin Mesozoic continental basement rock consists of diorite and subordinate gabbro overlaid by Oligocene to Pliocene sediment.[12] This is isotopically distinct continental crust from the Solander Islands, excluding partial melting of the lower crust as creating the volcanic magma.[13] It has been suggested that the melt that formed the islands comes from a peridotitic source enriched by the addition of a slab-derived melt with subsequent open-system fractionation, resulted in the evolved andesitic adakites.[13]
There are 53 vascular plant species, one third of which are very rare. The flora is dominated by ferns and orchids. The southern, and nominate, subspecies of Buller's albatross (Thalassarche b. bulleri) breeds only on the Solanders and the Snares.
The Solander Islands were historically a well-known area for migrating whales, especially southern right and sperm whales. Sperm whales in this area were said to be exceptionally large.
The islands are home to a variety of bird life.[16]
The Solander group has been identified as an Important Bird Area (IBA) by BirdLife International because of its significance as a breeding site for Buller's albatrosses (with about 5000 pairs) and common diving petrels.[17]