Lake Waikaremoana

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Lake Waikaremoana
Lake Waikaremoana sun set.jpg
Location Wairoa District, Hawke's Bay Region, North Island
Coordinates 38°46′S 177°05′E / 38.767°S 177.083°E / -38.767; 177.083Coordinates: 38°46′S 177°05′E / 38.767°S 177.083°E / -38.767; 177.083
Primary outflows Waikaretaheke River
Basin countries New Zealand
Surface area 54 km²
Max. depth 256 m
Shore length1 102.3 km
Surface elevation 600 m
Settlements Āniwaniwa
1 Shore length is not a well-defined measure.
Location

Lake Waikaremoana is located in Te Urewera National Park in the North Island of New Zealand, 60 kilometres northwest of Wairoa and 80 kilometres west-southwest of Gisborne. It covers an area of 54 km². From the Maori Waikaremoana translates as 'sea of rippling waters'

The lake lies in the heart of Tuhoe country. The hamlet of Āniwaniwa and the Waikaremoana Motor Camp are located on the lakeshore, along SH38 (from Wai-O-Tapu via Murupara to Wairoa), which connects the lake to the central North Island (Rotorua) and Gisborne. There is a Department of Conservation office at Aniwaniwa. Several walks start here, including a short stroll to Aniwaniwa Falls.

Lake Waikaremoana is a holiday destination by people who use the lake for fishing, tramping and other recreational activities. The Lake Waikaremoana Track, one of New Zealand's "Great Walks", is a three to four-day tramp which follows approximately half of the lake's circumference. The track can be walked independently, or as part of a guided group. There are huts dotted on the walk which require booking to use. Camping is permitted unless you are more than 500 metres from the track.

Numbers of visitors to the area are mitigated by the unsealed road that must be taken to reach it. The smaller Lake Waikareiti lies four kilometres to the northeast.

Geography and natural history[edit]

Waikaremoana is the North Island's deepest lake (256 m deep), its surface being an altitude of 600 metres above sea level. The lake has been created by a huge landslide dam about 250 metres high and is believed to be around 2,200 years old.[1] Prior to the landslip being sealed, around 1950, much of the lake outflow flowed through the landslip rather than out an overflow at a low point in the slip.[1]

Other geographical features include Panekiri Bluff and Puketukutuku Peninsula, which is the site of a kiwi conservation programme. Surrounded as it is by mountains clad with native forest which has never been logged, it is regarded as the North Island's most attractive lake. Many native bird species scarce in most other parts of the North Island can be found in the area. A possum-hunting programme operates in the area to help protect the forest. There are numerous understory species within the forested area of the catchment basin, Crown Fern, Blechnum discolor, being an example.[2] Since at least the early 1900s lake bottom molluscs have been studied by Colenso and others.[3]

Hydroelectric power scheme[edit]

The Waikaremoana Hydroelectric Power Scheme appears to be the only example of a hydroelectric power station being built on a natural landslide dam.

Modifying the natural dam[edit]

The stability of the natural dam has been the subject of intense engineering review, both at the time of construction and subsequently. Construction of an outlet tunnel through the slip, which commenced in 1935, required extensive grouting around the control structures and throughout tunnel construction. Work was suspended at the end of 1936 because Bob Semple, the newly elected Minister for Public Works, wanted the tunnelling project reconsidered for "risk, cost and value". A new tunnelling scheme was devised in 1941 based on what had been learned from initial exporatory tunnelling and work recommenced in 1943 and continued for about 5 years because of continual problems with dewatering the tunnels. After the tunnels and intake headworks had been completed the natural dam was sealed for leaks on the lake side by removing submerged timber, a task that took a year and then applying 40,000 cubic metres of crushed rock and clay-like pumice in 6 layers, then covering those layers with a top layer of larger rock and spalls to protect the material from wave action. This sealing reduced the natural flow by about 80%. The sealing of the lake was only done after tunnelling was completed otherise it would have caused the lake level to rise and make tunnelling more difficult. As it was, the lake level had to be lowered by temporary syphons to enable the construction of the headworks and make sealing of the natural dam easier.[1]

Power stations[edit]

Although the Waikare River carries a flow of about 17 m³/s from Lake Waikaremoana, the head of water through the 3 power stations, Kaitawa, Piripura, and Tuai is around 450 metres, allowing the stations to potentially generate 124 megawatts all up. The 250m head of water for the Kaitawa station is the highest for a dam in New Zealand and among the highest in the world.[1]

See also[edit]

References[edit]

Line notes[edit]

  1. ^ a b c d Offer, R.E. (Robert) (1997). Walls for Water: Pioneer Dam Building in New Zealand. Palmerston North: The Dunmore Press Ltd. pp. 191–200. ISBN 0-86469-313-3. 
  2. ^ C. Michael Hogan. 2009
  3. ^ Royal Society of New Zealand. 1905

Gallery[edit]

View of Lake Waikaremoana from Panekiri Bluff


External links[edit]