Lake Rotomahana
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Lake Rotomahana is an
lake A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much large ...
in northern
New Zealand New Zealand ( mi, Aotearoa ) is an island country in the southwestern Pacific Ocean. It consists of two main landmasses—the North Island () and the South Island ()—and over 700 smaller islands. It is the sixth-largest island count ...
, located 20 kilometres to the south-east of
Rotorua Rotorua () is a city in the Bay of Plenty region of New Zealand's North Island. The city lies on the southern shores of Lake Rotorua, from which it takes its name. It is the seat of the Rotorua Lakes District, a territorial authority encompass ...
. It is immediately south-west of the dormant
volcano A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are ...
Mount Tarawera Mount Tarawera is a volcano on the North Island of New Zealand within the older but volcanically productive Ōkataina Caldera. Located 24 kilometres southeast of Rotorua, it consists of a series of rhyolitic lava domes that were fissured d ...
, and its geography was substantially altered by a major
1886 eruption of Mount Tarawera In 1886, a violent eruption occurred at Mount Tarawera, near the city of Rotorua on New Zealand's North Island. At an estimated Volcanic Explosivity Index of 5, the eruption is the largest and deadliest in New Zealand during the past 500 years, w ...
. Along with the mountain, it lies within the Okataina caldera. The New Zealand
Ministry for Culture and Heritage The Ministry for Culture and Heritage (MCH; ) is the department of the New Zealand Government responsible for supporting the arts, culture, built heritage, sport and recreation, and broadcasting sectors in New Zealand and advising government on ...
gives a translation of "warm lake" for , following
Hochstetter The family of Höchstetter (also rendered Hechstetter or Hochstetter), from Höchstädt in western Bavaria near the banks of the Danube, were members of the fifteenth and sixteenth-century mercantile patriciate of Augsburg. For a time, these i ...
. Before the 1886 eruption, only two small lakes were present in the current lake's basin. High quality pictures of the then Lake Rotomahana and associated tourist attractions were widely available in Europe by 1875. Following the eruption, a number of craters filled over the course of 15 years to form today's Lake Rotomahana. It is the most recently formed larger natural lake in New Zealand, and the deepest in the Rotorua district. The lake's northern shore lies close to the lower
Lake Tarawera Lake Tarawera is the largest of a series of lakes which surround the volcano Mount Tarawera in the North Island of New Zealand. Like the mountain, it lies within the Okataina caldera. It is located to the east of Rotorua, and beneath the pea ...
, separated by less than of terrain that is mostly material from the 1886 eruption. Lake Rotomahana has no natural outlet, and its water level varies by about one meter in response to rainfall and evaporation. The lake is a wildlife refuge (and was one prior to first contact), with all hunting of birds prohibited. A healthy population of
black swan The black swan (''Cygnus atratus'') is a large waterbird, a species of swan which breeds mainly in the southeast and southwest regions of Australia. Within Australia, the black swan is nomadic, with erratic migration patterns dependent upon c ...
inhabits the lake, and there are efforts underway to ensure the lake's largest island, Patiti Island, is kept pest-free. Recent research confirms Patiti Island is the closest surviving pre-eruption feature on the old lake, i.e. to survive the 1886 eruption, being formerly known as Rangipakaru Hill.Bunn R (2020) Commentary: Locating Relict Sinter Terrace Sites at Lake Rotomahana, New Zealand, With Ferdinand von Hochstetter’s Legacy Cartography, Historic Maps, and LIDAR. Front. Earth Sci. 8:68. doi: 10.3389/feart.2020.00068 There is no public access to the lake, save for the Tourist Track, overland from Lake Tarawera. A boat cruise on the lake, visiting hydrothermal features on the lake's shore, is available as an additional extra from the Waimangu Volcanic Valley tourism operation.


Pink and White Terraces

The
Pink and White Terraces The Pink and White Terraces ( and ), were natural wonders of New Zealand. They were reportedly the largest silica sinter deposits on earth. Until recently, they were lost and thought destroyed in the 1886 eruption of Mount Tarawera, while new hy ...
were a natural wonder on the shores of the lake before the 1886 eruption. They were considered to be the eighth wonder of the natural world and were New Zealand's most famous tourist attraction during the 19th century, from c. 1870-1886; but were buried or destroyed by the eruption. Scientists thought they had rediscovered the lower tiers of the Pink and White Terraces on the lake bed at a depth of in 2011. More recent research reports over 2016-2020 suggest the upper parts of both terraces lie on land and may therefore be accessed for physical evidence the terraces or sections of them survived in their original locations. The 2017- research relied on the journals of German-Austrian geologist
Ferdinand von Hochstetter Christian Gottlieb Ferdinand Ritter von Hochstetter (30 April 1829 – 18 July 1884) was a German-Austrian geologist. Career Having received his early education at the evangelical seminary at Maulbronn, Ferdinand proceeded to the University o ...
, who visited the lake in 1859. Hochstetter's journals are the only known survey of the terraces before the eruption. Using Hochstetter's field diaries and compass data, a team of New Zealand researchers identified a location where they believe the Pink and White Terraces lie preserved at a depth of 10–15 metres (32–49 ft). The researchers were hoping to raise funds for a full survey of the area, but any work would first have to be approved by the local Maori tribe on whose sacred ancestral land the Pink and White Terraces are situated. Ground penetrating radar searches were undertaken in 2017 but the equipment failed to penetrate sufficiently deeply to show whether or not the Terraces lay in their surveyed locations. Later Hochstetter survey research refined the Pink, Black and White Terrace locations.


Green Lake

A small lake, Green Lake, lies close to the eastern shore of Lake Rotomahana at . It should not be confused by the much larger Lake Rotokakahi (Green Lake), which lies to the west of Rotomahana. Green Lake was formed in a roughly circular crater and is some 100 metres in diameter. It takes its name from its distinctive colour, which is considerably greener and darker than that of Rotomahana. The lake formed after the 1886 eruption of Mount Tarawera. Prior to the eruption, a small (~12m diameter) lakelet also known as Green Lake (Lake Rotopounamu) had existed to the north of Lake Rotomahana in Waikanapanapa Valley but this was exhumed during the Tarawera eruption. After the eruption, water flowed into the new Green Lake crater, which was given the same name as the older lake. Other pre-eruption lakes and lakelets about Lake Rotomahana included Lakes Rotomakariri, Rangipakaru, Ruahoata and Wairake. The shape, location and orientation of Lake Makariri in Cole, 1970 (cited herein) is incorrect. He followed August Petermann's flawed map. Hochstetter shows the lake axis lay at an azimuth of 355 degrees. Recent research into these lake levels gave insight into changes at Lake Rotomahana in the lead-up to the eruption.


The Sunken Totara Forest Myth

One forgotten lake feature is the semi-mythical ''sunken totara forest'' of Lake Rotomahana. In 2016 when a scuba team first dove the lake, they found no evidence of a sunken forest or trees, as reported by Fitzgerald off Moura. While there were forests over the pre-eruption Mt Tarawera, Totara trees were scattered and only recorded over the western and southern mountain flanks.  Given Totara tree groves could hardly appear in the eruption craters; it appears likely any sunken forest lies in the north-east corner of the new lake. The placement of the sunken forest would have been post-eruption, via the mechanism described by the US Forest Service after the Mt. St. Helens eruption.Walker, T. (2017) “Learning the Lessons of Mount St Helens”, ''Creation'' 39'', 3, 26'' The trees were uprooted in the eruption and propelled into the crater during or after the eruption. As the new lake formed over decades, the trunks floated for a time, then tipped vertically; later descending into a vertical lie, and became embedded into the lake floor coming to resemble a sunken forest. Hence, another myth about the Tarawera eruption and Lake Rotomahana is explained.  


References


External links


Pink & White Terraces photos

The 1886 eruption

The Pink and White terraces 2011
{{DEFAULTSORT:Rotomahana Lakes of the Bay of Plenty Region Okataina Volcanic Centre Volcanic crater lakes 1886 eruption of Mount Tarawera Taupō Volcanic Zone