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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 ...
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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.
00:48. Includes weather reports from an extended list of coastal stations at 00:52 and an inshore waters forecast at 00:55 and concludes with a brief UK weather outlook for the coming day. The broadcast finishes at approximately 00:58. 05:20. Includes weather reports from coastal stations at 05:25, and an inshore waters forecast at 05:27.
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.
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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.
The bay, one of the larger of numerous bays in the crenellated coast of the sounds, is 10 kilometres (6 mi) wide at its mouth and extends 8 kilometres (5 mi) south. The peninsula into which it cuts is almost bisected by the bay, with a narrow isthmus only some 900 metres (3,000 ft) wide lying between the bay's southernmost extent and Hallam ...