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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.
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.
Forsyth Island lies in the outer Marlborough Sounds of New Zealand's South Island and is separated from the mainland by the 300m wide Allen Strait (also known as Guards Pass). The island comprises a mixture of farm land and native bush on hills rising to over 350 metres (1,148 ft) with views into the Marlborough Sounds and east towards the ...
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Download as PDF; Printable version; In other projects ... Pages in category "Marlborough Sounds" The following 39 pages are in this category, out of 39 total.
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]
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