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The Marlborough Sounds (te reo Māori: Te Tauihu-o-te-Waka) are an extensive network of sea-drowned valleys at the northern end of the South Island of New Zealand. The Marlborough Sounds were created by a combination of land subsidence and rising sea levels. [1] According to Māori mythology, the sounds are the prows of the many sunken waka of ...
The Marlborough Sounds, a series of deep indentations in the coastline at the northern tip of the South Island, are in fact drowned river valleys, or rias. The deeply indented coastlines of Northland and Auckland also host many rias, such as the Hokianga and Waitematā Harbours .
Pelorus Sound (Māori: Te Hoiere; officially Pelorus Sound / Te Hoiere) is the largest of the sounds which make up the Marlborough Sounds at the north of the South Island, New Zealand. The Marlborough Sounds is a system of drowned river valleys , which were formed after the last ice age around 10,000 years ago.
The Marlborough Sounds Important Bird Areas are four distinct sites comprising several small, rocky islets contained within an area with a maximum linear extent of 40 km, in New Zealand. They lie close to Cook Strait in the outer Marlborough Sounds at the northern end of the South Island. The sites are Duffers Reef, Sentinel Rock, White Rocks ...
Kenepuru Sound from Queen Charlotte Track. Kenepuru Sound is one of the larger of the Marlborough Sounds in the South Island of New Zealand. [1] The drowned valley is an arm of Pelorus Sound / Te Hoiere, it runs for 25 kilometres (16 mi) from the northeast to southwest, joining Pelorus Sound a quarter of the way down the latter's path to the Cook Strait.
Marlborough is known for its dry climate, the Marlborough Sounds, and Sauvignon blanc wine. It takes its name from the earlier Marlborough Province , which was named after John Churchill, 1st Duke of Marlborough , an English general and statesman.