Abstract
This chapter focuses on the processes controlling the shallow transfer of magma below and within volcanic edifices. As such, it builds on the knowledge of the previous chapters, which considered the general mechanisms for the rise of magma in the crust (Chap. 3), its arrest and the development of magma chambers nucleating magma-filled fractures (Chap. 4), and the important topographic variations induced by calderas (Chap. 5) and sector collapse (Chap. 6). At the same time, shallow magma transfer generates signals detected by monitoring systems (Chap. 8), which can be used to understand the state of active volcanoes and ultimately improve eruption forecasting (Chap. 9).
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Acocella, V. (2021). Shallow Magma Transfer. In: Volcano-Tectonic Processes. Advances in Volcanology. Springer, Cham. https://doi.org/10.1007/978-3-030-65968-4_7
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