Ōkārito Lagoon
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Ōkārito Lagoon
Ōkārito Lagoon is a coastal lagoon on the west Coast, New Zealand, West Coast of New Zealand's South Island. It is located south of Hokitika, and covers an area of about , making it the largest unmodified coastal wetland in New Zealand. It preserves a sequence of vegetation types from mature Dacrydium cupressinum, rimu forest through Leptospermum scoparium, mānuka scrub to brackish water that has been lost in much of the rest of the West Coast. The settlement of Ōkārito is at the southern end of the lagoon. Name The lagoon's name is from the Māori language, Māori , place of, and , the young shoots of the bulrush or Typha orientalis, raupō (''Typha orientalis''), a valued food source. Another account has Ōkārito taking its name from a rangatira named Kārito, whose daughters Mapourika and Wahapako gave their names to nearby Lake Mapourika and Lake Wahapo. The lagoon's official name has been spelled with Macron (diacritic), macrons over the vowels since 2010, althoug ...
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Westland District
Westland District is a territorial authority district on the West Coast of New Zealand's South Island. It is administered by the Westland District Council. The district's population is History Westland was originally a part of Canterbury Province, administered from Christchurch, on the east coast. The booming population as a result of the gold rush, together with the difficulty of travel and communication across the Southern Alps, led first to the creation of a special Westland County, then the formal separation of Westland from Canterbury to form the short-lived Westland Province (1873–1876). Westland Province also included what is now the southern portion of Grey District, with the provincial boundary at the Grey and Arnold rivers. Greymouth proper was in Westland Province, Cobden, on the north bank of the Grey River, was in Nelson Province. After the abolition of the provinces in 1876, a new Westland County was created with roughly the same borders as the province ...
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Ōkārito + Whitebaiting • Nimmo • MRD 7
Ōkārito is a small coastal settlement on the West Coast of New Zealand's South Island, southwest of Hokitika, and from . It is built at the southern end of the Ōkārito Lagoon at the mouth of the Ōkārito River. The settlement of The Forks is located just inland, on the banks of the river. Name Ōkārito's name is from the Māori , place of, and , the young shoots of the bulrush or raupō (''Typha orientalis''), a valued food source. Another account has Ōkārito taking its name from a rangatira named Kārito, whose daughters Mapourika and Wahapako gave their names to nearby Lake Mapourika and Lake Wahapo. The settlement's official name has been spelled with macrons over the vowels since 2010, although it is still commonly seen written as "Okarito". History Māori occupation and seasonal harvesting in area began over 600 years ago. The Ōkārito historic gold mining settlement is home to Donovan's Store, the oldest known building on the West Coast, and the Ōkā ...
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Spit (landform)
A spit (cognate with the word for a rotisserie bar) or sandspit is a deposition (geology), deposition shoal, bar or beach landform off coasts or lake shores. It develops in places where re-entrance occurs, such as at a cove's headlands, by the process of longshore drift by longshore currents. The drift occurs due to waves meeting the beach at an oblique angle, moving sediment down the beach in a zigzag pattern. This is complemented by longshore currents, which further sediment transport, transport sediment through the water alongside the beach. These currents are caused by the same waves that cause the drift. Hydrology and geology Where the direction of the shore inland ''re-enters'', or changes direction, for example at a headland, the longshore current spreads out or dissipates. No longer able to carry the full load, much of the sediment is dropped. This is called deposition. This submerged bar of sediment allows longshore drift or littoral drift to continue to transport sed ...
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Estuary
An estuary is a partially enclosed coastal body of brackish water with one or more rivers or streams flowing into it, and with a free connection to the open sea. Estuaries form a transition zone between river environments and maritime environments and are an example of an ecotone. Estuaries are subject both to marine influences such as tides, waves, and the influx of saline water, and to fluvial influences such as flows of freshwater and sediment. The mixing of seawater and freshwater provides high levels of nutrients both in the water column and in sediment, making estuaries among the most productive natural habitats in the world. Most existing estuaries formed during the Holocene epoch with the flooding of river-eroded or glacially scoured valleys when the sea level began to rise about 10,000–12,000 years ago. Estuaries are typically classified according to their geomorphological features or to water-circulation patterns. They can have many different names, such as ba ...
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Earthquakes In New Zealand
This is a list of large earthquakes that have occurred in New Zealand. Only earthquakes with a magnitude of 6.0 or greater are listed, except for a few that had a moderate impact. Aftershocks are not included, unless they were of great significance or contributed to a death toll, such as the M 6.3 2011 Christchurch earthquake and the M 7.3 aftershock to the 1931 Hawke's Bay earthquake. Earthquakes occur frequently in New Zealand as the country is situated in the collision zone between the Indo-Australian and Pacific plates, part of the Pacific Basin Ring of Fire, where many earthquakes and volcanoes occur. Most events occur along the main ranges running from Fiordland in the southwest to East Cape in the northeast. This axis follows the boundary between the Indo-Australian and Pacific plates. Large earthquakes are less common, where the plates are not subducting and the forces are accommodated in different ways. The largest city within the highest-risk zone is the nation's ...
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Ōkārito Lagoon • Okarito Kayaks • MRD 03 (cropped)
Ōkārito is a small coastal settlement on the West Coast of New Zealand's South Island, southwest of Hokitika, and from . It is built at the southern end of the Ōkārito Lagoon at the mouth of the Ōkārito River. The settlement of The Forks is located just inland, on the banks of the river. Name Ōkārito's name is from the Māori , place of, and , the young shoots of the bulrush or raupō (''Typha orientalis''), a valued food source. Another account has Ōkārito taking its name from a rangatira named Kārito, whose daughters Mapourika and Wahapako gave their names to nearby Lake Mapourika and Lake Wahapo. The settlement's official name has been spelled with macrons over the vowels since 2010, although it is still commonly seen written as "Okarito". History Māori occupation and seasonal harvesting in area began over 600 years ago. The Ōkārito historic gold mining settlement is home to Donovan's Store, the oldest known building on the West Coast, and the Ōkā ...
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Dacrycarpus Dacrydioides
''Dacrycarpus dacrydioides'', commonly known as kahikatea (from Māori) and white pine, is a coniferous tree endemic to New Zealand. A podocarp, it is New Zealand's tallest tree, gaining heights of over a life span of 600 years. It was first described botanically by the French botanist Achille Richard in 1832 as ''Podocarpus'' ''dacrydioides'', and was given its current binomial name ''Dacrycarpus dacrydioides'' in 1969 by the American botanist David de Laubenfels. Analysis of DNA has confirmed its evolutionary relationship with other species in the genera ''Dacrycarpus'' and ''Dacrydium''. In Māori culture, it is an important source of timber for the building of waka and making of tools, of food in the form of its berries, and of dye. Its use for timber and its damp fertile habitat, ideal for dairy farming, have led to its decimation almost everywhere except South Westland. Kahikatea seeds have fleshy structures called receptacles attached to them, which encourage bi ...
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Tide
Tides are the rise and fall of sea levels caused by the combined effects of the gravitational forces exerted by the Moon (and to a much lesser extent, the Sun) and are also caused by the Earth and Moon orbiting one another. Tide tables can be used for any given locale to find the predicted times and amplitude (or " tidal range"). The predictions are influenced by many factors including the alignment of the Sun and Moon, the phase and amplitude of the tide (pattern of tides in the deep ocean), the amphidromic systems of the oceans, and the shape of the coastline and near-shore bathymetry (see '' Timing''). They are however only predictions, the actual time and height of the tide is affected by wind and atmospheric pressure. Many shorelines experience semi-diurnal tides—two nearly equal high and low tides each day. Other locations have a diurnal tide—one high and low tide each day. A "mixed tide"—two uneven magnitude tides a day—is a third regular category. ...
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Ōkārito River
The Ōkārito River is a river of the West Coast Region of New Zealand's South Island. It flows northwest from the northern end of Lake Mapourika, reaching the Ōkārito Lagoon 15 kilometres west of Whataroa. See also *List of rivers of New Zealand This is a list of all waterways named as rivers in New Zealand. A * Aan River * Acheron River (Canterbury) * Acheron River (Marlborough) * Ada River (New Zealand), Ada River * Adams River (New Zealand), Adams River * Ahaura River * Ahuriri R ... References Rivers of the West Coast Region Westland District Rivers of Westland Tai Poutini National Park {{WestCoastNZ-river-stub ...
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Whataroa River
The Whataroa River, sometimes the Wataroa River, is a river in the southern West Coast, New Zealand, West Coast region of New Zealand's South Island. Its source is below Hochstetter Dome in the Southern Alps and it flows north and northwest, passing the township of Whataroa on the eastern side before reaching the Tasman Sea just south of Abut Head. The river is fed by many tributaries, such as the Perth River, and is crossed by on its route between Whataroa and Te Taho. Recreation Whitewater rafting takes place on the river as an adventure tourism activity. Access to the upper reaches of the river for rafting is either via hiking or helicopter. The river also flows through areas used for tramping and climbing. References

Westland District Rivers of the West Coast Region Rivers of New Zealand {{WestCoastNZ-river-stub ...
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Waiho River
The Waiho River (traditionally the Waiau River) is a river of the West Coast region of New Zealand's South Island. It is fed by the meltwater of the Franz Josef Glacier and skirts the main township of Franz Josef to its south, where its river bed is crossed by on a long single-lane bridge. Due to changes in rainfall and snow melt, the river's water flow varies greatly. In a severe rain storm on 26 March 2019, the bridge was destroyed after of rain had fallen. The bridge and one abutment was rebuilt, and the road link reopened after 18 days. The works cost NZ$6m. Waiho River merges with Docherty Creek just before reaching the Tasman Sea southwest of Ōkārito. Gallery Franz Josef Glacier (4673959511).jpg, The origin of the river is at Franz Josef Glacier St James Church Franz Josef from Waiho River bridge.jpg, The Waiho River flows through the town of Franz Josef, passing features such as the St James Church St James river comparisons MRD.jpg, The rise of the Waiho Ri ...
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