Convection in Volcanoes

mt_st_helens1The Earth is so fragile. We sit on a thin layer of rock, under which is a seething mass of molten material. If the rock is very thin, the hot magma bursts out of the surface sometimes, cascading down a mountainside, like the pictures of Mount St Helen’s  used in the movie Dante’s Peak.  The Earth consists of rigid  plates called tectonic plates, floating above a layer of molten magma.   With a thickness of about 100 km, this ‘lithosphere’ is composed of an upper layer of crust (~7 km thick under the oceans, and ~35 km thick under the continents) and a lower, denser layer of the earth’s upper mantle. Underneath the lithosphere is a hot, mobile layer of partially molten rock lying within the earth’s upper mantle which is constantly being moved around by convection.

Hot mantle rises beneath mid-oceanic ridges, and cold, denser mantle descends at oceanic trenches. Sideways movement of the plates above these circular convection cells is rather like rigid blocks riding above a rotating conveyor belt. Here’s a little interactive demonstration

which goes with the picture.

 

 

convectcells_s

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