Deep in the earth, solid rocks can flow, but the surface layers are cold rigid plates that move across the surface. This means that continents are constantly drifting across the earth and oceanic crust is being created and destroyed. Plate tectonics is one of the most successful scientific theories of the Twentieth Century. It explains… Continue reading Plate tectonics
Category: Deep earth
Beyond plate tectonics
Plate tectonics is the core unifying concept that has underpinned our understanding of the solid earth for over 50 years. To describe your research as moving “beyond plate tectonics” is quite a claim, but Trond Torsvik and the group he leads have some remarkable science to back it up. By tracking the movement of the earth’s plates… Continue reading Beyond plate tectonics
Hot spot volcanoes: no plumes required?
It’s a simple and well-known picture. Volcanoes form either at plate boundaries due to subduction or inside plates due to mantle plumes. Invoking plumes – columns of hot rock rising from deep in the mantle – is an awfully useful way of explaining oddly-placed volcanoes, both ancient and modern. Too useful, many people think. The concept has been… Continue reading Hot spot volcanoes: no plumes required?
Tasting the earth: mantle geochemistry
If seismologists listen to the earth then geochemists taste it. Like experts blind-tasting a glass of wine and recognising where it came from, geochemists studying the deep earth aim to find out where a particular liquid came from. Their liquid – basaltic magma formed from melting of the mantle rocks – is now solid, so ‘tasting it’ involves dissolving… Continue reading Tasting the earth: mantle geochemistry