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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 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 ...
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 spelling fiord is used in New Zealand rather than fjord, although all the maritime fiords instead use the word sound in their name. 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.
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Waikawa Bay opens onto Queen Charlotte Sound. [3] [4] The New Zealand Ministry for Culture and Heritage gives a translation of "bitter water" for Waikawa. [5] Waikawa is an important New Zealand tourist destination because its large marina acts as gateway to the Marlborough Sounds and famous treks (hikes) such as the Queen Charlotte Track.
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