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at9 italy
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Volcanoes and Volcanism - Learn with Professor Agust Gudmundsson
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- 1 Introduction
- 2 Monitor volcanoes
- 3 Inside volcanoes
- 4 My background
- 5 Classification of volcanoes
- 6 Monogenetic volcanoes
- 7 Lava shields
- 8 Volcano geometry
- 9 Volcano magma chambers
- 10 Satellite measurements
- 11 Inside a volcano
- 12 How deep are they
- 13 In the field
- 14 Magma chamber
- 15 How magma chambers form
- 16 Icelander
- 17 Acid magma chambers
- 18 Fractures
- 19 dike paths
- 20 dike segments
- 21 vertical segments
- 22 propagation direction
- 23 Irregular paths
- 24 dikes
- 25 santorini
- 26 at9 italy
- 27 at8 Iceland
- 28 can we forecast dive paths
- 29 sizes of eruptions
- 30 Typical eruption in Iceland
- 31 How much magma goes out
- 32 It is surprisingly little
- 33 Why does the dike close so easily
- 34 How large are the volcanic eruptions
- 35 How big are the biggest eruptions
- 36 How can we get this kind of volume
- 37 What we need to look for
- 38 Elastic and strain energy
- 39 Summary
