@article{ref1,
title="Instability of magma flow from volatile-dependent viscosity",
journal="Science",
year="1999",
author="Wylie, JJ and Voight, B and Whitehead, JA",
volume="285",
number="5435",
pages="1883-1886",
abstract="Volatiles dissolved in silicic magma at depth exsolve as the magma nears the surface and cause an increase in viscosity of the magma. A model of a volcanic conduit within an elastic medium and a viscosity dependent on the volatile content of the magma produces oscillatory magma flow for a critical range of steady input flow rates. Oscillatory flow is recognized as a fundamental mode of behavior at silicic volcanoes, and understanding it allows improved short-term forecasting of timing and eruption style.<p /><p>Language: en</p>",
language="en",
issn="0036-8075",
doi="",
url="http://dx.doi.org/"
}