Primrose Terrace and Bridal Veil Falls at Wai-O-Tapu, Rotorua

The Primrose Terrace is a landform created by silica deposits. Covering an area of 3 acres, it is the largest in New Zealand since the famed Pink and White Terraces were destroyed in the eruption of Mt Tarawera in 1886. The Primrose Terrace is formed by water from the Champagne Pool which contains dissolved silica. As the water evaporates, the silica is left on the ground. It is a very gradual process of formation, very much like how stalactites and stalagmites are formed. It is estimated that the Primrose Terrace have been forming over the past 700 years since the last major geothermal activity in Wai-O-Tapu.

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The Primrose Terrace on the left side of the boardwalk
Wai-O-Tapu, Rotorua, May 2006
On the left side of the boardwalk, the Primose Terrace is relatively flat with a down slope gradient. Towards the end of the boardwalk, the slope becomes more prominent. Below photo continues with the view of Primrose Terrace after the boardwalk crossing.

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The Primrose Terrace
Wai-O-Tapu, Rotorua, May 2006
It may not be apparent in above photo but there is only a thin layer of water trickling over the silica deposits. The graduated lines of the terraces can be seen in the foreground of above photo and the formation follows the pattern of water trickling down slope.

The Primrose Terrace ends with a drop and as seen in below photo, there is no longer any graduated lines of the terraces but an uneven splattering of deposits. Where this drop begins, the silica deposits has been named the Bridal Veil Falls and we can see why it was named as such.

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Bridal Veil Falls
Wai-O-Tapu, Rotorua, May 2006

Champagne Pool at Wai-O-Tapu, Rotorua

One of the most photographed sections of Wai-O-Tapu is the Champagne Pool. It gets its name from the constant bubbling of its water. The water fizzles and reminds of champagne though its colour is a tinge of blue and green. Along the edge of the lake, is a brilliant shade of orchre.

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Champagne Pool
Wai-O-Tapu, Rotorua, May 2006
Unfortunately, the day I was there, it was raining and the raindrops and runoffs into the the pool had made the water murky. Otherwise, on a sunny day, the colours in the photos would have turned out brilliant!

Champagne Pool is the largest spring in the area. It has a diameter of 65m and is 62m deep! It’s surface temperature is 74 degrees Celsius and steam constantly arises from the pool. The bubbles in the pool are due to carbon dioxide, just like champagne! Like all the natural features in Wai-O-Tapu, Champagne Pool was formed by geothermal activity. From the nearby rocks found at the embankment, it is believed that the pool was formed by a hydrothermal eruption 700 years ago.

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Crossing the Primrose Terrace on the boardwalk
Wai-O-Tapu, Rotorua, May 2006
Across the boardwalk, on the right side where the steam arises, the blue & orange shade of water indicates where the Champagne Pool is.

On the extreme right side is Artist’s Palette. When water overflows from the Champagne Pool, it brings with it minerals which are deposited on this side of the pool which results in a multitude of colours in the water. Hence, this side of the pool has been named Artist’s Palette.

On the left side of the boardwalk lies the Primrose Terrace which I will mention more in a subsequent posting.