Orakei Korako Today
The lowest terrace at Orakei Korako is the jade-green Emerald Terrace, which is the largest of its kind in New Zealand since the destruction of the famed Pink and White Terraces in the Mount Tarawera eruption of 1886. In peak wet conditions up to 20 million litres of silica-enriched water per day may flow over the terrace and into Lake Ohakuri.
The Emerald Terrace continues 35 metres under the lake, which was formed for hydropower generation in 1961. This raised the Waikato River level by 18 metres at Orakei Korako, flooding approximately 200 alkaline hot springs and 70 geysers (or two thirds of the active thermal area). Some of these thermal features still discharge, with their presence evident as gas bubbles rising from the vents in the lake bed.
Despite the loss of so many of its thermal features under the artificial lake, Orakei Korako remains the largest geyser field in New Zealand, with up to 35 active geysers. The most famous of these is the Diamond Geyser, whose unpredictable eruptions can last from a few minutes to many hours, ejecting boiling water as high as nine metres.
The three terraces above the lakeside Emerald Terrace are great fault scarps formed by a massive earthquake in 131 AD, around the time when Lake Taupo (a supervolcano) was last erupting. They are mostly covered in hot water algae, or cyanobacteria, which grows in temperatures between 35-59 degrees Celsius, the colours dependent on the species, with green, yellow and black the most common.
At the base of the two lower terraces – named Rainbow and Cascade Terraces – are several small geysers, including the intermittently active Sapphire Geyser, and the Hochstetter Pool (named after Austrian pioneer geologist Ferdinand von Hochstetter, who visited the area in 1859), which erupted in November 1954 and played as a geyser until mid-1955, ceasing suddenly after swarms of subterranean earthquakes.
The third and largest great fault scarp in the valley is called the Golden Fleece Terrace (named Te Kapua by the Māori people, meaning “The Cloud”), which is five metres high and 40 metres long, with a beautiful white crystal-like sinter coating. At the base are numerous vents where geysers have come and gone over the years, with the most recent, Wairiri Geyser.
Atop this terrace is the Artist’s Palette, a 10,000 m² silica sinter terrace covered with clear blue alkali chloride pools and irregularly erupting geysers. To one side of this topmost terrace a new geyser began to erupt in 2001, possibly the beginnings of a further terrace.
Also at Orakei Korako is the Ruatapu Cave, one of only two caves in the world known to exist in a geothermal field. The cave extends 45 metres, with a vertical drop of 23 metres, to a shallow pool of clear, sulfate-rich, warm acid water. (The pool’s chemical composition gives it the unique ability to clean jewellery.)
Another notable feature at Orakei Korako is the Soda Fountain, which burst into life in 1984 after a 17 year dormancy.
To the south of this feature, high atop a cliff above Lake Ohakuri, are three further geysers, Kurapai, Ellan Vannin and Benedix Washer Geysers, in an area not accessible to the public because it is too dangerous. Temperatures of 100 degrees Celsius have been recorded here just 100 to 150 mm below the ground. Of these geysers, Kurapai Geyser is the most significant, and can sometimes be seen erupting from across the lake in the visitor's centre.
The Orakei Korako geothermal system now has some protection from further development, although the nearby Ngatamariki Geothermal Development at Tahorakuri gained resource consent in 2010 despite its possible effects on Orakei Korako.
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