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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 ...
Penzance's beach is of gravel, which is unusual for this area of the Marlborough Sounds. This gives the beach a good reputation for safe and pleasant swimming. The bay contains a boat ramp, a large wharf, and a swimming island. These facilities coupled with ease of access gives the bay a great reputation for boating activities and fishing.
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.
Long Island-Kokomohua Marine Reserve is a marine reserve, in the Marlborough Region of New Zealand's South Island. It covers an area of 619 hectares at the entrance to the Queen Charlotte Sound in the Marlborough Sounds. [1] [2] It was the first marine reserve established on the South Island. [3]
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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