Lake_Okataina
Lake Ōkataina
Volcanic crater lake in New Zealand
Lake Ōkataina (also spelled Okataina; Māori: Te Moana i kataina ā Te Rangitakaroro or Ōkataina) is the northernmost and largest of four smaller lakes lying between Lake Rotorua and Lake Tarawera in the Bay of Plenty Region of New Zealand's North Island. The others are Lake Rotokakahi (Green Lake), Lake Tikitapu (Blue Lake), and Lake Ōkareka. All lie within the Ōkataina caldera, along its western edge.
| Lake Ōkataina | |
|---|---|
| Lake Okataina | |
| Te Moana i kataina ā Te Rangitakaroro (Māori) | |
Aerial view from the south | |
| Location | Bay of Plenty, North Island |
| Coordinates | 38°07′S 176°25′E |
| Type | crater lake |
| Primary inflows | Herupapaoa Stream, Pukahu Stream [1]: 50 |
| Primary outflows | subsurface |
| Catchment area | 59.8 km2 (23.1 sq mi)[1]: 56 |
| Basin countries | New Zealand |
| Max. length | 6.2 km (3.9 mi)[2] |
| Max. width | 5.0 km (3.1 mi)[2] |
| Surface area | 10.7 km2 (4.1 sq mi)[1]: 55 |
| Average depth | 44.0 m (144.4 ft)[2] |
| Max. depth | 78.5 m (258 ft)[2] |
| Surface elevation | 309.1 m (1,014 ft)[1]: 24 |
| References | [1]: 55–6 [2] |
Unlike many other lakes in the region, Lake Ōkataina is completely encircled by native forest. Over the past 30 years, the level of the lake has risen and fallen in a range of about 5 metres. The mean autumn lake level is 309.1 m (1,014 ft).[1]: 24
The lake can be accessed by road via Hinehopu on the southern shores of Lake Rotoiti. At the end of the road there is a large sandy beach, a massive grassed area and the privately owned Okataina Lodge. Due to changes in the surface level of the lake, the lodge jetty has at times been either completely submerged or left high and dry.
On its south-western arm is a small island, Motuwhetero Island.
Water Flow
The lake is feed by multiple unnamed and often transient streams with a total catchment precipitation inflow average of 3,841 L/s (135.6 cu ft/s).[1]: 56 The only named streams that empty into the lake are the Herupapaoa Stream and Pukahu Streams.[1]: 50 The Te Rereoterangi Stream joins the permanent Herupapaoa Stream before it enters the lake.[1]: 50 The lake has no surface outflow and a outflow to Lake Tarawera of 399 L/s (14.1 cu ft/s) has been estimated.[1]: 70
Geology
It is located in the Ōkataina Caldera and some of its south-eastern shore has discoloured hot water sources in the lake.[1]: 50 The western shore is underlaid by Mamaku ignimbrite from the Rotorua Caldera eruption of 240,000 years ago.[3] The rest of the lake catchment has rhyolite formations from Ōkataina eruptions.[1]: 8
After the 1886 eruption of Mount Tarawera the lake level increased, to a maximum height about 1930 which dropped to present levels after the 1931 Hawke's Bay earthquake. The lake is now about 10 m (33 ft) above its pre 1886 level.[4]: 16
The New Zealand Ministry for Culture and Heritage gives a translation of "place of laughter" for Ōkataina.[5] The lake and surrounds were occupied by the Ngāti Tarāwhai iwi.
Te Koutu Pā was located on the north-east shore of Lake Ōkataina.[6] The carved entrance gate, is to be found in the Auckland War Memorial Museum.[7]
Because of war raids before 1886,[6] and flooding after 1886, the previous sites of occupation on the lake shore were abandoned by the Māori Ngāti Tarāwhai inhabitants.[4]: 16, 27 Both a drowned Pā and shine has been found.[4]: 56 A palisade post found under water near Motuwhetero Island confirms that the older low lake level had been present for at least about 100 years before the eruption.[4]: 132 Rock art in the form of a canoe in red ochre has been described.[4]: 56
The lake is surrounded by pristine virgin native forest and has good fishing for Rainbow trout.[8]
The area around the Okataina Lodge is heavily populated by tammar wallabies introduced from Australia in the 19th century.[9] It is known that these have impacted on the seedling layer of the forest, drastically reducing seedling density and diversity, and causing the disappearance of preferred food species. The local Red deer prevent seedlings from maturing into saplings and the combined effect has been a profound depletion of the forest understorey.[10]
Its trophic level index was 2.7 in 2014, being the lowest of the Ōkataina Caldera lakes.[1]: 5
- White, P; Toews, M; Tschritter, C; Lovett, A (2016). "Nitrogen discharge from the groundwater system to lakes and streams in the greater Lake Tarawera catchment GNS Science Consultancy Report 20151108" (PDF). Retrieved 26 August 2023.
- Lowe, D.J.; Green, J.D. (1987). Viner, A.B. (ed.). Inland waters of New Zealand. Wellington: DSIR Science Information Publishing Centre. pp. 471–474. ISBN 0-477-06799-9.
- Bégué, F.; Deering, C. D.; Gravley, D. M.; Kennedy, B. M.; Chambefort, I.; Gualda, G. A. R.; Bachmann, O. (2014). "Extraction, Storage and Eruption of Multiple Isolated Magma Batches in the Paired Mamaku and Ohakuri Eruption, Taupo Volcanic Zone, New Zealand". Journal of Petrology. 55 (8): 1653–1684. doi:10.1093/petrology/egu038. hdl:20.500.11850/88102.
- Law, Garry (2008). Archaeology of the Bay of Plenty (PDF). Science and Technical Publishing, Department of Conservation, New Zealand. ISBN 9780478144307. Retrieved 10 September 2023.
- "1000 Māori place names". New Zealand Ministry for Culture and Heritage. 6 August 2019.
- "New Zealand National Library:Te Koutu Pā". Retrieved 10 September 2023.
- "Lake Okataina". NZFishing.com. Retrieved 27 August 2023.
- MacFarlane, Kristin (20 August 2006). "Where are the wallabies?". Rotorua Daily Post. Retrieved 7 September 2010.
- "Impact of dama wallaby and red deer in Lake Okataina Scenic Reserve". Retrieved 27 August 2023.
Media related to Lake Okataina at Wikimedia Commons
