In the early hours of 10th June
1886, after a series of constant quakes since midnight, a
violent eruption occurred near the township of Rotorua.
The top of nearby Mount Wahanga was completely blown off, producing
a dense black cloud extending from Taheke to Paeroa, and
which became a mass of thunder and lightening to continue
incessantly the night long. Shortly after, nearby Mount
Tarawera and its twin cone Ruawahia exploded into action,
belching fire. The process of a volcanic eruption is when the pressure
on a magma chamber deep below the Earth’s surface begins to build up.
This building pressure causes the magma from the chamber to be forced
upward through a series of tubes or conduits. As the magma reaches the
surface, it is thrust through the vents on the volcano, resulting in an
eruption.
Sunday, 18 November 2012
How did this natural disaster happen?
In the early hours of 10th June
1886, after a series of constant quakes since midnight, a
violent eruption occurred near the township of Rotorua.
The top of nearby Mount Wahanga was completely blown off, producing
a dense black cloud extending from Taheke to Paeroa, and
which became a mass of thunder and lightening to continue
incessantly the night long. Shortly after, nearby Mount
Tarawera and its twin cone Ruawahia exploded into action,
belching fire. The process of a volcanic eruption is when the pressure
on a magma chamber deep below the Earth’s surface begins to build up.
This building pressure causes the magma from the chamber to be forced
upward through a series of tubes or conduits. As the magma reaches the
surface, it is thrust through the vents on the volcano, resulting in an
eruption.
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