Te Hoe River

Last updated

Te Hoe River
Location
Country New Zealand
Physical characteristics
Mouth  
  location
Mohaka River
Length23 km (14 mi)
Basin features
Tributaries 
  right Hautapu River

The Te Hoe River is a river of the Hawke's Bay region of New Zealand's North Island. It flows south from its sources west of Lake Waikaremoana to reach the Mohaka River 20 kilometres north of Lake Tutira.

The river and its tributary streams, including Mangahouanga, flow through the Tahora Formation, and is a location where many Mesozoic fossils have been uncovered since the 1970s. [1] In 1999, palaeontologist Joan Wiffen discovered the vertebra bone of a titanosaur in a tributary of the Te Hoe River. [2]

See also

Related Research Articles

<span class="mw-page-title-main">Hawke's Bay</span> Region of New Zealand

Hawke's Bay is a region on the east coast of New Zealand's North Island. The region is named for Hawke Bay, which was named in honour of Edward Hawke. The region's main centres are the cities of Napier and Hastings, while the more rural parts of the region are served by the towns of Waipukurau, Waipawa, and Wairoa.

<span class="mw-page-title-main">Waikato River</span> Longest river in New Zealand

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.

<span class="mw-page-title-main">Ruahine Range</span> Mountain range

The Ruahine Range is the largest of several mountain ranges in the North Island of New Zealand that form a ridge running parallel with the east coast of the island between East Cape and Wellington. The ridge is at its most pronounced from the central North Island down to Wellington, where it comprises the Ruahine, Tararua and Remutaka Ranges.

<span class="mw-page-title-main">Wairoa River (Hawke's Bay)</span> River in New Zealand

The Wairoa River of the Hawke's Bay region in New Zealand runs south for 65 kilometres from the inland east coast region of the North Island, west of Gisborne, before flowing into northern Hawke Bay at the town of Wairoa.

<span class="mw-page-title-main">Tutaekuri River</span> River in New Zealand

The Tutaekuri River flows eastward for 99.9 kilometres through the Hawke's Bay Region of the eastern North Island of New Zealand into the Pacific Ocean. It starts in the Kaweka Range roughly 50 kilometres north-east of Taihape, and reaches the sea just to the south of Napier, where the Ngaruroro and Clive Rivers join it.

<span class="mw-page-title-main">Mohaka River</span> River in Hawkes Bay, New Zealand

The Mohaka river is on the North Island of New Zealand in the east central region of Hawke’s Bay. Mohaka is a Maori word, roughly translated it means “place for dancing”. The iwi associated with the Mohaka River are Ngāti Pāhauwera, Ngāti Hineuru, Ngāti Tūwharetoa and Mana Ahuriri. The headwaters are found in the Kaweka and Kaimanawa ranges. From the range it winds southeast before twisting northeast and finally southeast again to empty into the Pacific Ocean near the town of Mohaka. There are many gorges on the Mohaka; some as steep as 200m. Its main tributaries are the Waipunga, Taharua, Hautapu rivers. The full length is 172 kilometres (107 mi) and it drains a basin of 2,357 square kilometres (910 sq mi).

<span class="mw-page-title-main">Waipawa River</span> River in New Zealand

The Waipawa River is a braided river of southern Hawke's Bay, in New Zealand's eastern North Island. It flows southeast from the slopes of 1,687 m (5,535 ft) Te Atuaoparapara in the Ruahine Range, past the town of Waipawa, before joining the Tukituki River. The river rises at the 1,326 m (4,350 ft) Waipawa Saddle, which is also the source of the Waikamaka River. The Mangaonuku Stream is a tributary on the northern bank, west of Waipawa, near Ruataniwha. The Waipawa's flow is generally greater than that of the Tukituki River, into which it flows.

Lake Poukawa is a small shallow hardwater lake in the Hawke's Bay Region, North Island, New Zealand. It is located about 20 km south-west of Hastings, New Zealand, close to the settlement of Te Hauke. It is the largest lake lying within a peatland in the active tectonic Poukawa depression, between the Raukawa Range and Kaokaoroa Range of central Hawke's Bay. Its maximal depth is less than one metre and its diameter is ca. 1.5 km. It was deeper in the past but it was artificially drained after the 1931 Hawke's Bay earthquake. Lake Poukawa is drained by the Poukawa Stream, which flows north-eastward through the Pekapeka Wetland and eventually into the Clive River.

<span class="mw-page-title-main">Te Awa o Mokotūāraro</span> River in New Zealand

Te Awa o Mokotūāraro, formerly known as the Clive River, is a river in Hawke's Bay, New Zealand. At 33 kilometres (21 mi) long, it is the shortest of the main rivers flowing through the Heretaunga Plains.

The Mangatewai River is a river of the Hawke's Bay Region of New Zealand's North Island. It flows generally east from the Ruahine Range to reach the Tukipo River 5 kilometres (3 mi) north of the township of Takapau.

The Old Bed of Waipawa River is a river of the Hawke's Bay region of New Zealand's North Island. It flows roughly parallel with and north of the Waipawa River, which it almost meets to the east of Waipawa. It flows into the Tukituki River via the Papanui Stream, south west of Lake Poukawa. The Waipawa changed its course during a flood in 1868. In the Cyclone Gabrielle event of February 2023 the flooded river broke its banks south of Waipapa town and reverted to its old bed, causing significant damage to farms and property. The Coronation Park stop bank in Waipawa was repaired on 16 February, returning the Waipawa to its post 1868 course.

The Ripia River is a river of the Hawke's Bay region of New Zealand's North Island. A major tributary of the Mohaka River, it flows generally southeast from its sources at the northern end of the Ahimanawa Range 25 kilometres east of Lake Taupō, reaching the Mohaka 40 kilometres northwest of Napier.

The Ruakituri River is a river of the Gisborne and Hawke's Bay Region of New Zealand's North Island. It initially flows northeast from its sources north of Lake Waikareiti. Within its course are the 72 m high Waitangi Falls. Afterwards it turns southeast for the majority of its course, reaching the settlement of Te Reinga, 25 kilometres (16 mi) north of Wairoa. It merges with the Hangaroa River resulting in the Wairoa River.

The Taharua River is a river of the northwestern Hawke's Bay region of New Zealand's North Island. It flows south from its origins 25 kilometres southwest of Taupō to reach the Mohaka River of which it is one of the earliest tributaries.

<span class="mw-page-title-main">Joan Wiffen</span> New Zealand paleontologist

Joan Wiffen was a self-taught New Zealand paleontologist known for discovering the first dinosaur fossils in New Zealand.

The Otamatea River is a river of the northwestern Hawke's Bay region of New Zealand's North Island. It flows generally north from its origins in the northern foothills of the Ahimanawa Range, reaching the Rangitaiki River 25 kilometres southwest of Taupō amid the Kaingaroa Forest.

<span class="mw-page-title-main">Ahuriri Lagoon</span> Historic lagoon in New Zealand

Ahuriri Lagoon was a large tidal lagoon at Napier, on the east coast of New Zealand's North Island, that largely drained when the area was raised by the 1931 Hawke's Bay earthquake.

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.

The Hautapu River is a river in the Hawkes Bay region of New Zealand. Its catchment is almost entirely forested.

References

  1. Gill, B. J.; Eagle, Michael K. (2014). "New Zealand Mesozoic marine reptiles in the Auckland Museum collection". Records of the Auckland Museum . 49: 21–28. ISSN   1174-9202. JSTOR   43264619. Wikidata   Q58629014.
  2. "Giant dinosaur fossil find in Hawke's Bay". stuff.co.nz. 24 June 2008. Retrieved 29 June 2011.

38°54′36″S176°48′58″E / 38.910°S 176.816°E / -38.910; 176.816