Hydrothermal Activity and Terraces
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Hydrothermal Activity and Terraces
A landscape made by hot water
The Pink and White Terraces were natural silica formations beside Lake Rotomahana, in the central North Island of New Zealand. Rainwater seeped underground, where heat from volcanic activity warmed it. The hot water dissolved silica from rocks and rose through cracks. At the surface, the water cooled and silica was left behind in thin layers. Over a very long time, these layers built up into stepped pools. The 1886 eruption of Mount Tarawera buried or destroyed the terraces. Scientists continue to study the area and its changing landscape.
- The hot water dissolved silica from rocks underground.
- The water changed all the rocks into rain.
- The silica floated down from clouds.
- The lake pushed silica through the ground.
- Dissolve
- Deposit
- Erupt
- Material is left behind
- A mineral mixes into water
- Volcano releases material and energy
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