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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 ...
Queen Charlotte Sound / Tōtaranui [a] is the easternmost of the main sounds of the Marlborough Sounds, in New Zealand's South Island.. In 2014, the sound was given the official name of Queen Charlotte Sound / Tōtaranui as part of a Waitangi Tribunal settlement with the Te Āti Awa tribe.
The Marlborough Sounds is a system of drowned river valleys, which were formed after the last ice age around 10,000 years ago. Pelorus Sound has a main channel which winds south from Cook Strait for about 55 kilometres (34 mi), between steeply sloped wooded hills, until it reaches its head close to the Havelock township.
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 .
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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.