Shag River | |
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![]() Route of the Shag River | |
Location | |
Country | New Zealand |
Physical characteristics | |
Source | |
• coordinates | 45°38′38″S 166°36′19″E / 45.6440°S 166.6054°E |
Mouth | |
• location | Goose Cove |
• coordinates | 45°40′38″S 166°33′12″E / 45.6772°S 166.5532°E |
• elevation | 0 m (0 ft) |
Basin features | |
Progression | Shag River → Goose Cove → Tamatea / Dusky Sound → Tasman Sea |
Shag River is a river on Resolution Island in Fiordland, New Zealand.[1] It rises north west of Mount Roa and flows south into the Taumoana (Five Fingers Peninsula) Marine Reserve, part of Tamatea / Dusky Sound.
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The Moeraki boulders - Roadside Stories
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Gold of Otago EP7 - The Northern Route to the Diggings
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First People In New Zealand // Maori History Documentary
Transcription
[Traditional Māori music (14secs)] [Narrator] You would think it unlikely that a series of rocks along a beach should become a tourist attraction, but the spherical Moeraki Boulders are a natural phenomenon that has intrigued people for centuries. Over fifty of these strange spheres lie along a sandy beach near the fishing port of Moeraki. Māori call them Te Kai Hīnaki -- eel pots. Locals call the boulders Hooligan's gallstones. Others have named them giant gob-stoppers, aliens' brains, the bowling balls of giants, or even the Stonehenge of New Zealand. Whalers named the place 'Vulcan's foundry'. The boulders grew in a pile of mud some 60 million years ago. They are called concretions -- lumps of sediment bound together by a mineral cement. Imagine dropping a lump of glue onto sand -- the resulting clump would be a concretion. At Moeraki the glue was calcite which was probably created when a marine animal began to rot. The calcite hardened around the sediment and as more was added it grew just like a massive pearl. The largest boulders weigh 7 tonnes and are 2 metres across. They are among the world's largest concretions and they took around 4 million years to grow. Their roundness is not because they have been tumbled in the surf, as many believe; but simply because they grew evenly in all directions -- forming a perfect sphere. The boulders only recently landed on the beach -- they formed in a layer of mudstone which was lifted above the sea about 15 million years ago. Breaking waves released them from the cliff and they rolled down to the beach. Today some boulders can be seen half-freed in the cliffs. According to Māori stories, many centuries ago, Māori arrived here from their South Pacific ancestral home of Hawaiki. They made the long ocean voyage in canoes carrying people and cargo. Unfortunately one of these canoes, the Ārai-te-uru, was wrecked in a fierce storm on Shag Point or Matakaea, just south of the Moeraki Boulders. The reef there is said to be the remains of the canoe. Just before the canoe was wrecked the travellers threw the food baskets of kūmara and gourds overboard to lighten the load. The baskets washed ashore at Moeraki where they petrified into what we now know as the Moeraki Boulders. Some of the less regular stones along the beach are said to be kūmara. Photographs from the nineteenth century show many more boulders on the beach than are there today. Many smaller boulders were taken as souvenirs or garden ornaments. One even made it to Australia. In 1938 a very large Moeraki boulder was hoisted onto a truck and taken to Otago museum to be preserved 'for all time'. But within 25 years it began to break up while its companions on the beach remained intact. In 1971 as concern mounted that names were being carved into the surface of the boulders and that rock collectors were using explosives, the boulders were given legal protection as a scientific reserve.
See also
References
- ^ "Place name detail: Shag River". New Zealand Gazetteer. New Zealand Geographic Board. Retrieved 9 March 2020.
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