They now understand better how the Earth’s mantle is composed in that particular region and how the magma changes before an eruption. The study is published in Nature Communications.

pm5552_elrsprdczfei11nz2sxx

Frances Deegan, the study’s first author and a researcher at Uppsala University’s Department of Earth Sciences, summarises the findings.

“Magma is formed in the mantle, and the composition of the mantle under Indonesia used to be only partly known. Having better knowledge of Earth’s mantle in this region enables us to make more reliable models for the chemical changes in magma when it breaks through the crust there, which is 20 to 30 kilometres thick, before an eruption.”

The composition of magma varies greatly from one geological environment to another, and has a bearing on the kind of volcanic eruption that occurs. The Indonesian archipelago was created by volcanism, caused by two of Earth's continental tectonic plates colliding there. In this collision, Indo-Australian plate slides beneath the Eurasian plate at a speed of some 7 cm annually. This process, known as subduction, can cause powerful earthquakes. The tsunami disaster of 2004, for example, was caused by movements along this particular plate boundary.

Read more

Noticias Relacionadas

Icy Waters of ‘Snowball Earth’ May Have Spurred Early Organisms to Grow Bigger

Read News

The Climatic Environment to Sustain Permafrost in Daisetsu Mountains, Hokkaido in Japan, Is Projected to Decrease Significantly in the Future

Read News

UN Climate Panel Contends With Models Showing Implausibly Fast Warming

Read News

Stinkweed Could Make a Cleaner Bio-Jet Fuel, Study Finds

Read News