Subscribe now

Letter: Crusty creation

Published 9 January 2008

From Tim Sprod

Lawrence D’Oliveiro wonders whether continental crust is disappearing (17 November 2007, p 24). In fact, new continental crustal material is continually created by partial melting of rocks in the denser and silica-poor mantle and partial solidification of existing magmas. Both processes produce magmas richer in silica – the building blocks of continents. These rise and solidify, forming new crustal material. When teaching this to students, I likened it to the formation of scum when you boil fruit to make jam. The continents, I would tell them, are truly the scum of the Earth.

Taroona, Tasmania, Australia

Issue no. 2638 published 12 January 2008

Sign up to our weekly newsletter

Receive a weekly dose of discovery in your inbox. We'll also keep you up to date with New Scientist events and special offers.

Sign up
Piano Exit Overlay Banner Mobile Piano Exit Overlay Banner Desktop