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The Maori River is a river of the West Coast Region of New Zealand's South Island. It flows from several sources in the Mataketake Range east of Haast , passing through the small Tawharekiri Lakes before becoming a tributary of the Waita River , which flows into the Tasman Sea 15 kilometres north of Haast.
Land Information New Zealand – Search for Place Names; Booker, D.J.; Whitehead, A.L. (2017). "NZ River Maps: An interactive online tool for mapping predicted freshwater variables across New Zealand". niwa.co.nz. Christchurch: National Institute of Water and Atmospheric Research (NIWA). Young, David. "Rivers – Types of river.
Waiwawa River - 21 km (13 mi) (longest river on the Coromandel Peninsula) Waimata River (NI) - 20 km (16 mi) Makara River (Chatham Island) - 16 km (10 mi) (longest New Zealand river not in New Zealand's main island chain) Avon River / Ōtākaro (SI) - 15 km (9.5 mi) Water of Leith (SI) - 14 km (9 mi)
Travel+Leisure 2 days ago This 500-year-old Caribbean Capital Has Beautiful Beaches, a Growing Food Scene, and the Best Cocktail Bar in the Region — and Now Is the Time to Visit
InterCity has been the only New Zealand-owned long-distance bus service since Nakedbus was acquired by foreign-owned ManaBus [1] in 2015; ManaBus ceased operating in 2018. [2] In November 2018, InterCity started a new express bus service, SKIP, [ 3 ] [ 4 ] offering affordable, reliable and faster connections between major North Island cities.
The longest river in New Zealand is the Waikato River with a length of 425 kilometres (264 miles). The largest river by rate of flow is the Clutha River / Mata-Au with a mean discharge of 613 cubic metres per second (21,600 cu ft/s). [1] The shortest river is claimed to be the Tūranganui River in Gisborne at 1,200 metres (3,900 feet) long. [2]
The following is a list of rivers in the Wellington Region. The list is arranged in arranged by the location of the river mouth clockwise around the bottom of the North Island.
The Wairoa River carries large quantities of fine sediment (clays, silts and sands) that cloaks both the bed and the banks of the river. The rate of sediment loss has increased because of changes in land use from native forest to pasture, and forestry and farming land use practices, with current sediment losses estimated to be approximately 240% higher than before human arrival.