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Quanta Magazine


Eruption forecasting asks a lot of questions. Chief among them is: When? At its core, this question is equivalent to asking when magma from below will travel up through a conduit (the pipe between the magma and the surface opening) and break through, as lava flows and ash, as volcanic glass and bombs.
When magma ascends from depth, it can alter a volcano’s architecture, literally changing the shape of the land above. Migrating magma flows can also force rock apart, generating volcano-tectonic earthquakes. And when the pressure keeping magma trapped underground declines, it liberates trapped gas, which can escape to the surface. ....

Diana Roman , Carnegie Institution For Science , Last December , Reykjanes Peninsula , Carnegie Institution , டயானா ரோமன் , கார்னகி நிறுவனம் க்கு அறிவியல் , கடந்த டிசம்பர் , கார்னகி நிறுவனம் ,