A volcano is best described as an opening in the Earth's crust through which
The shape of a volcano depends on a number of factors:
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Here, the shadow of the Mauna Kea volcano cast by the setting sun shows its gentle slopes.
(The hill in the sunlight is one of the small peaks which make up the summit, 4206m above sea level)
The type of lava depends on the composition of the molten rock (magma) which rises within the crust to erupt through the volcano.
This in turn controls
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The structure of volcanoes shows a number of variations:
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In some cases, a layer of lava will cool down to form the characteristic pillar-like structure called columnar jointing. This photograph shows a section of the longest outcrop of columnar jointing in Iceland.
Modern volcanoes are found in certain zones of volcanoes around the world. This suggests that these belts are particularly active; they provide much of the evidence on which the theory of Plate Tectonics is based.
The Study Topics
TENERIFE
Some individual areas show a wide range of volcanic features and a visit - either in real life or on a virtual tour
- can be used to discuss the origins and shapes of volcanoes in general. Tenerife is
one such area. Developed at a hot spot, the island is made of three basalt shield volcanoes surmounted by a large
strato-volcano whose top has collapsed to form a caldera. Within the caldera, the modern volcano of El Teide now sits,
waiting to erupt again.