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VOLCANOLOGY
Mt Tarawera lies within the Okataina Volcanic Centre, one of five
major active areas within the Taupo Volcanic Zone.
Tarawera
is made up of 11 rhyolite domes and pyroclastics from eruptions
from within the southern part of the Haroharo Caldera formed by
volcanic episodes more than 20,000 years ago.
Tarawera
has erupted five times:
- 1886
basaltic scoria eruption
- 700
yrs ago Kaharoa eruption of rhyolitic lava and pyroclastics
- 11,000
yrs ago Waiohau episode
- 15,000
yrs ago Rerewhakaaitu episode
- 17,000
yrs ago An episode associated with the Okareka ash
The
1886 Tarawera Basalt deposits are well exposed along the rift across
Mt Tarawera. The red and black scoria varies in thickness from 20-60
cm.
The
basalt contrasts with the older grey-white rhyolite lavas and pyroclastics
which make up the bulk of the mountain.
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UNIQUE
FLORA & FAUNA
Flora on the mountain is sub-alpine flora. Mainly ground covers,
moss, lichen, herbs and hebes. Due to the altitude, all flora close
to the summit is slow growing and fragile.
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