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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 ...
Marlborough was an iron-built two-decked merchant sailing ship which disappeared in 1890. She was built by the firm of Robert Duncan and Co., Port Glasgow and launched in 1876. First managed by James Galbraith for the Albion Shipping Company, she was registered in 1880 to the ownership of John Leslie of London, while continuing to operate ...
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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.
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. [1] [2]
Bay of Many Coves is a reference to the many small bays situated within it. A number of these bays, and those throughout the Marlborough Sounds are named after poets and characters from literature. [1] Ironically the Bay of Many Coves only has one of the locality that uses the word cove in its name, and even that was initially called Cockle Bay.
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.