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Te Awamutu. Te Kuiti.
Own or manage this property? Claim your listing for free to respond to reviews, update your profile and much more. Skip to main content. Log in to get trip updates and message other travelers. Review of Bistro Lago. Bistro Lago. Improve this listing. Ranked 28 of Restaurants in Taupo. Certificate of Excellence. Description: From lake, land and ocean, our seasonal New Zealand a la carte lunch and dinner brings the region's best offerings to your plate.
Located at the elegant Hilton Lake Taupo, boasting stunning lake views and guided by the expertise of celebrity Chef Gareth Stewart, Bistro Lago is a culinary experience not to be missed. Reviewed January 8, via mobile. Dinner date. Date of visit: January Ask carhbs59 about Bistro Lago. Thank carhbs Report response as inappropriate Thank you. We appreciate your input.
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Palmer, J. Close banner Close. Our reanalysis of the radiocarbon ages for the Taupo ignimbrite eruption provides the first demonstration of regional biasing of 14 C eruption ages by magmatic carbon Supplementary Information. In the meantime, to ensure continued support, we are displaying the site without styles and JavaScript.
Reviewed January 4, Go for the lamb! Ask maxwelltham about Bistro Lago. Magma typically ranges from the fluid, hot, basaltic types, to viscous, cooler, less dense, paler coloured rhyolitic forms. All varieties contain gas which is given off when it reaches the surface and gases are the driving force behind explosive eruptions—the mingling of steam with magma adds significantly to the scale of a detonation.
Wiggle-match radiocarbon dating of the Taupo eruption
The Oruanui eruption at Taupo occurred 27, years ago and was the largest eruption worldwide since Toba in Indonesia, around 74, years ago. Oruanui ignimbrite rock solidified from magmatic material flowing as a dense gas and ash cloud can be readily seen in road cuttings along the Desert Road, draped by the layers of younger tephra tephra is a collective term for airborne volcanic ejecta, also referred to as pyroclastic deposits.
Fine ash from this event, found throughout New Zealand and in numerous offshore core samples, indicates the pre-existence of a lake at this site. This eruption is listed as VEI-8, having produced km 3 of ejecta, km 3 of which was magma. Magma rises through fractures in the crust and, if it cannot progress any further, it pools to form a magma chamber. As more magma rises up from below, pressure in the chamber grows. If it finds a way to the surface, the result will be a volcanic eruption. This illustration shows the structure and range of ejecta typical in the magmatic eruption of a stratovolcano like Ngauruhoe although lava flows, lava fountains and ash plumes do not occur simultaneously.
The massive Taupo and Whakamaru events were phreatomagmatic eruptions resulting from an interaction between water and magma.
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The scale and form of these eruptions means that no cone formed—materials were blasted away as voluminous ash fall and widespread pyroclastic flows—and the chamber collapsed to form caldera. Radiocarbon Dating places the most recent eruption of Taupo at around AD. It was the 28th post-Oruanui eruption of Taupo and evidence from trees preserved at Pureora Forest suggest it occurred in late summer. Links have been drawn to descriptions of unusual meteorological phenomena noted in Rome by Herodian of Antioch and in the Book of Later Han by Fan Ye in China, which would exactly date the eruption to AD, but such correlations are tenuous and unsupported.
While not the largest eruption in historic times Tambora in expelled more material , it was the most violent and complex. In the first phases minor activity was followed by the dry vent Hatepe plinian outburst. Large amounts of water then entered the vent, pausing the eruption.
With vent collapse came the catastrophic eruption of Taupo ignimbrite, a large and very energetic pyroclastic flow that devastated an area of about 20, square kilometres and filled all the major river valleys of the central North Island with pumice and ash. Many of the major rivers in the North Island still carry large amounts of this pumice when in flood. Most importantly, Taupo shows no signs of being finished—it is extremely likely to erupt again and the timing and scale of its next episode cannot be predicted.
For as long as the Tuwharetoa have lived beneath the steaming cliffs of the Hipaua thermal area, they have been subjected to its volatility. More than 60 people were killed when a prolonged period of rain brought down a torrent of loose earth upon Te Rapa village. After a second large slide in , they moved their pa beyond the path of imminent destruction to Waihi, where it remains today.
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Now the thermal field appears to be migrating towards the village and it once again threatens Tuwharetoa. In July this year, they were evacuated by Civil Defence in anticipation of another large landslip. The steaming Hipaua thermal area marks the edge of the Waihi Fault and contains a significant amount of geologically weak, fractured fault-zone material. Beneath this ominous but striking feature is the deeply incised Waimatai Valley, slopes thick with native vegetation flourishing in the volcanic soil.
Debris from the slip is still visible, broadening into the lake just north of the mouth of the Waimatai Stream.
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The combination of these conditions amount to a particularly hazardous area that Environment Waikato and the Taupo District Council have monitored for 20 years. For anyone visiting the area for the first time, the instability of the land is immediately evident; steam rises from the ground and creates a veil that floats across the bush.
One might think that this dangerous area would be some threat to the community. Rather it makes their home a vibrant place rich in tradition. Maria Hoko, a resident and my hospitable guide to the area, recalls a childhood deeply connected to the land: collecting koura in the lake and then cooking them with crab apples in the hot springs. The marae and the church stand side by side at the centre of the village, and at the top is an old buttery, a relic from an industrious past, now used as a pumice chalkboard for declarations of love.
At the shore, two lines of whare face one another, the lake lapping at their foundations. This feature has become a significant cause for concern.
In the event of another major landslide, a slip-wave would cause extensive damage to the village even if the falling earth skirted it. Maria Hoko is only too aware of the destructive capacity of the land. The tragic loss of life in is memorialised through song, which the Tuwharetoa perform whenever there is a large gathering or funeral.