The Difference Between The Tectonic Events Of Eyjafallajokull And Mount Merapi
Figure 1: Eyjafallajokull Figure 2: Mount Merapi
Table of Contents
Introduction 3
Tectonic Plate Theory 3
Plate Boundaries in Iceland and Indonesia 3
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Start My OrderThe Geological Events 3
The Claim and Research Question 3
Analysis 4
The Occurrence of Both Events 4
Trends/ Patterns Seen With Each Event 4
Human, Economic and Geological Impacts Of Both Events 5
Similarities and Differences Between the 2 Geological Events 5
Conclusion 6
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References 7
Introduction
Plate Tectonic Theory
Plate tectonics is a theory which suggests that Earth’s outer shell is divided into several plates which hover over the mantle, the stony inner layer above the core. The reason for plate tectonics moving is due to the convection in the mantle, where hot material near the Earth’s core rises and colder mantle rock sinks. (Lynn S. Fichter, 2000) The movement and interaction of crustal plates in the Earth’s lithosphere results in geological events such as volcanism, continental drift, seafloor spreading, and mountain building.
Plate Boundaries In Iceland And Indonesia According to Figure 3, Iceland emerged as a result of the divergent and spreading at this boundary which is situated between the Eurasian and the North American tectonic plate. (BBC, 2014) As shown in Figure 4, Indonesia is located between two continental plates: the Eurasian Plate and the Australian Plate and between two oceanic plates: the Philippine Sea Plate and Pacific Plate. (Weebly, 2017)
Figure 3: Iceland Mid-Atlantic Ridge Map Figure 4: Plate Tectonics Of Indonesia
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