Te Tatua-a-Riukiuta facts for kids
Quick facts for kids Te Tātua-a-Riukiuta |
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| Three Kings | |
Te Tātua-a-Riukiuta from Mt Albert
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| Highest point | |
| Elevation | 133 m (436 ft) |
| Geography | |
| Location | Auckland, North Island, New Zealand |
| Parent range | Auckland volcanic field |
| Geology | |
| Volcanic arc/belt | Auckland volcanic field |
Te Tātua-a-Riukiuta (also known as Three Kings) is a volcano in Three Kings, New Zealand that erupted 28,500 years ago. The volcano had three prominent peaks and a number of smaller peaks until most of them were quarried away, leaving a sole remaining large peak.
Geology
Te Tātua-a-Riukiuta was probably the most complex volcano in the Auckland volcanic field, consisting of five significant scoria cones and about a dozen smaller scoria mounds, sitting inside a large explosion crater. Along the edge of this crater to the south runs Mount Albert Road, and to the north, Landscape Road. At 800 metres (2,600 ft) across and nearly 200 metres (660 ft) deep, the explosion crater, which was caused by the initial eruption, is the largest in Auckland. The three largest scoria cones of the group were Big King at 133 m (436 ft) high, East King at 120 m (390 ft) high, and Highest King, which was 135 m (443 ft) high.
Lava flows ran from here down a stream valley for three kilometres to Western Springs. These flows created lava tunnels which still exist under the surface. Thus, rainwater falling on Te Tātua-a-Riukiuta and the surrounding area is channeled underground for miles until it emerges at Western Springs Lake. Most of these lava tunnels have collapsed but sections of them form caves and can be accessed from private properties in the area. It was formerly believed that the lava had travelled further and formed Meola Reef at Point Chevalier, but in 2008 it was discovered that the Meola Reef lava had come from the older Mount Saint John volcano.
The eruption occurred 28,500 years ago. Charred twigs and wood were found in six boreholes drilled through Te Tātua-a-Riukiuta lava flows in 2006 and carbon dating of the organic material produced six very similar dates around 28,500 years.
History
An earlier name for the volcano was Te Tatua o Mataaho (the war belt of Mataaho), which referred to a deity living in the Maungawhau crater. It was later adapted to Te Tātua-a-Riukiuta, which referred to Riukiuta, a senior priest of the Tainui waka who brought together diverse genealogical lines of the local tribes. The name Three Kings derives from the biblical Magi, and was named by Captain William Hobson's surveyor Felton Mathew in 1841. Big King refers to the second-highest (and only remaining) peak.
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Te Tātua-a-Riukiuta was once the site of a pā, and Big King has retained Māori earthworks from that era such as kumara pits and terracing.
The area has been drastically quarried over the years for the red scoria it contains, and only one of the three large peaks (Big King) remains today, largely because of the water reservoir that was built on its summit at the beginning of the 20th century. The reservoir is below the hydraulic grade of the area and is hence maintained as an emergency supply reservoir only.
However, the large scoria deposits in the surrounding area are still being quarried. The groundwater level became a problem for the quarry in 1995, and Winstone Aggregates, the company operating the quarry, arranged with the Auckland City Council to supply the water to the region. However, as a result of local opposition to this arrangement, the water is instead discarded into the sea. This dewatering has led to concerns about subsidence.
In the 2014 Treaty of Waitangi settlement with Ngā Mana Whenua o Tāmaki Makaurau, a collective of 13 Auckland iwi, the volcano was officially named Te Tātua-a-Riukiuta and ownership was vested to the collective. It is now co-governed by the collective and Auckland Council in common benefit of the iwi "and all other people of Auckland".
