Kawakawa River | |
---|---|
Location | |
Country | New Zealand |
Physical characteristics | |
Source | Mount Hikurangi |
• elevation | 631 m (2,070 ft) |
Mouth | |
• location | Bay of Islands |
Basin size | 443 km2 (171 sq mi) |
The Kawakawa River is in the Northland Region of New Zealand's North Island. It flows predominantly eastward to Opua, where it joins the Waikare Inlet to flow into the Veronica Channel at the southern end of the Bay of Islands.
The river starts near the town of Kawakawa, at the convergence of the Otiria and Waiharakeke Streams, and is soon joined by the Waiomio Stream. About half the river's length is an estuary, over 500 m (550 yd) wide in places. The estuary is joined by that of the Karetu River. The name was officially gazetted on 21 June 2019. [1]
Long Bridge, the longest wooden railway bridge in the Southern Hemisphere, crosses the river at Taumarere as part of the Bay of Islands Vintage Railway. [2] The river is tidal up to the Long Bridge. [3]
The River Severn, at 220 miles (354 km) long, is the longest river in Great Britain. It is also the river with the most voluminous flow of water by far in all of England and Wales, with an average flow rate of 107 m3/s (3,800 cu ft/s) at Apperley, Gloucestershire. It rises in the Cambrian Mountains in mid Wales, at an altitude of 2,001 feet (610 m), on the Plynlimon massif, which lies close to the Ceredigion/Powys border near Llanidloes. The river then flows through Shropshire, Worcestershire and Gloucestershire. The county towns of Shrewsbury, Worcester and Gloucester lie on its course.
The Hutt River flows through the southern North Island of New Zealand. It flows south-west from the southern Tararua Range for 56 kilometres (35 mi), forming a number of fertile floodplains, including Kaitoke, central Upper Hutt and Lower Hutt.
The Waikato River is the longest river in New Zealand, running for 425 kilometres (264 mi) through the North Island. It rises on the eastern slopes of Mount Ruapehu, joining the Tongariro River system and flowing through Lake Taupō, New Zealand's largest lake. It then drains Taupō at the lake's northeastern edge, creates the Huka Falls, and flows northwest through the Waikato Plains. It empties into the Tasman Sea south of Auckland, at Port Waikato. It gives its name to the Waikato region that surrounds the Waikato Plains. The present course of the river was largely formed about 17,000 years ago. Contributing factors were climate warming, forest being reestablished in the river headwaters and the deepening, rather than widening, of the existing river channel. The channel was gradually eroded as far up river as Piarere, leaving the old Hinuera channel through the Hinuera Gap high and dry. The remains of the old course are seen clearly at Hinuera, where the cliffs mark the ancient river edges. The Waikato's main tributary is the Waipā River, which converges with it at Ngāruawāhia.
The Waimakariri River is one of the largest rivers in Canterbury, on the eastern coast of New Zealand's South Island. It flows for 151 kilometres (94 mi) in a generally southeastward direction from the Southern Alps across the Canterbury Plains to the Pacific Ocean.
The Rangitata River is one of the braided rivers of the Canterbury Plains in southern New Zealand. It flows southeast for 120 kilometres (75 mi) from the Southern Alps, entering the Pacific Ocean 30 kilometres (19 mi) northeast of Timaru. The river has a catchment area of 1,773 square kilometres (685 sq mi), and a mean annual flow of 95 cubic metres per second (3,400 cu ft/s) at Klondyke.
Kawakawa is a small town in the Bay of Islands area of the Northland Region of New Zealand. Kawakawa developed as a service town when coal was found there in the 1860s, but coal mining ceased in the early 20th century. The economy is now based on farming. The town is named after the kawakawa shrub.
Waikanae River is located on the Kāpiti Coast in the North Island of New Zealand.
The Opua Branch or Otiria-Opua Industrial Line, partially still operational as the Bay of Islands Vintage Railway, is a former section of the North Auckland Line in the Northland Region of New Zealand, between Otiria and the Bay of Islands township of Opua. The first section was constructed as a bush tramway in 1867 and converted to a railway in the next decade. Today the railway is partially used by the Bay of Islands Vintage Railway, which runs tourist services between Kawakawa and Te Akeake. The line's centrepiece is the section where it runs down along the main street of Kawakawa.
Taumarere is a locality in the Bay of Islands in Northland, New Zealand. The Kawakawa River and State Highway 11 run through Taumarere. The town of Kawakawa is 3 km to the southwest. Opua is 7 km to the north and Paihia 14 km.
The Bay of Islands Vintage Railway Trust (BOIVRT) is a heritage railway in Kawakawa, in Northland, New Zealand. The railway operates on part of the former Opua Branch railway.
The Ngunguru River is a river of the Northland Region of New Zealand's North Island. It initially flows southwest before turning east to flow into a long, wide estuary which empties into Ngunguru Bay to the northwest of Whangārei. The town of Ngunguru sits on the estuary's north bank at its opening to the bay.
The Waiariki River is a river of the Northland Region of New Zealand's North Island. It forms at the confluence of the Waikiore and Pukekaikiore Streams and is in the catchment of the Wairua River, which it reaches by the Waiotu River, approximately halfway between Whangārei and Kawakawa.
The Waiotu River is a hard sediment bottomed river of the Northland Region of New Zealand's North Island. One of the headwaters of the Wairua River system, it flows generally south from its sources 15 kilometres southeast of Kawakawa. Its waters join with those of the Whakapara River to form the Wairua River.
The Whangae River is a short river of the Northland Region of New Zealand's North Island. It flows generally northeast to reach a southwestern arm of the Bay of Islands. The estuary is about 2 km (1.2 mi) and the river about 5 km (3.1 mi) long. Like much of the coast north of Whangārei, the valley is formed of Waipapa greywacke.
The Waingaro River is a river of the Waikato region of New Zealand's North Island. It flows generally southwest from its origins near Glen Afton and Glen Massey, west of Ngāruawāhia, to reach a northern arm of Raglan Harbour. Its main tributary is Kahuhuru Stream, which Highway 22 follows for several kilometres. Tributaries total about 170 kilometres (110 mi). At Waingaro it is fed by a hot spring.
The Waitangi River is a river of the Northland Region of New Zealand's North Island. It originates close to the northern shore of Lake Ōmāpere and flows eastwards to the Bay of Islands. It is considered to end either where it drops over Haruru Falls into a tidal estuary, or where the estuary opens into Te Tī Bay, just below the bridge between the historic locality of Waitangi and the town of Paihia.
Te Akeake railway station, is a station on the Opua Branch in New Zealand.
Kawakawa railway station was a station on the Opua Branch in New Zealand. and is the terminus of the Bay of Islands Vintage Railway (BoIVR) in the small town of Kawakawa. It was also the terminus of the oldest railway on the North Island, opened in 1867, before being joined to the rest of the North Auckland Line in 1912.
Taumarere railway station was a station on the Opua Branch in New Zealand and is a stop on the Bay of Islands Vintage Railway near Taumarere village. It is on the oldest railway built on the North Island, which opened in 1867. Taumarere station has had three locations, east of the village, west of the village and at the rugby ground.
The Awaroa River is a short river in the Waikato District of New Zealand's North Island. It flows east from its source in the dunes near Karioitahi Beach and Lake Puketi, then south from Waiuku joining with the Aka Aka Stream before reaching the Waikato River in its tidal reaches close to Motutieke Island.
35°20′S174°06′E / 35.333°S 174.100°E