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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
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Acid magma chambers
18
Fractures
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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
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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
Description:
Explore the explosive world of volcanoes and volcanism in this 41-minute lecture by Professor Agust Gudmundsson from the Department of Earth Sciences at Royal Holloway, University of London. Delve into the classification of volcanoes, their internal structures, and the formation of magma chambers. Discover how scientists monitor volcanic activity using satellite measurements and field observations. Examine the mechanics of magma movement, including dike paths and propagation directions. Learn about eruption sizes, from typical Icelandic events to the largest known volcanic eruptions in history. Gain insights into forecasting dike paths and understanding the factors that influence eruption volumes. Conclude with an overview of elastic and strain energy in volcanic systems, providing a comprehensive understanding of these powerful geological phenomena.

Volcanoes and Volcanism - Learn with Professor Agust Gudmundsson

Royal Holloway, University of London
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