[Illustration]: Le Glacier d'Argentiere in (a) ca. 1850-60, and (b) 1966Source: Philosophical Transactions of the Royal Society of London. Series A, Mathematical andPhysical Sciences, Vol. 330, No. 1615, The Earth's Climate and Variability of the Sun OverRecent Millennia: Geophysical, Astronomical and Archaeological Aspect (Apr. 24, 1990)Published by: The Royal SocietyStable URL: http://www.jstor.org/stable/53587 .

Accessed: 07/05/2014 21:30

Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at .http://www.jstor.org/page/info/about/policies/terms.jsp

.JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range ofcontent in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new formsof scholarship. For more information about JSTOR, please contact support@jstor.org.

.

The Royal Society is collaborating with JSTOR to digitize, preserve and extend access to PhilosophicalTransactions of the Royal Society of London. Series A, Mathematical and Physical Sciences.

http://www.jstor.org

This content downloaded from 169.229.32.136 on Wed, 7 May 2014 21:30:53 PMAll use subject to JSTOR Terms and Conditions

Phil. Trans. R. Soc. Lond. A, volume 330 Frontispiece

Qua~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~4

Le Glacier d'Argentiere in (a) ca. 1850-60, and (b) 1966. The engraving (a) and the photograph (b) (taken by Madeleine Le Roy Ladurie) are both taken from Histoire du climat depuis l'an mil by Emmanuel Le Roy Ladurie, and reproduced courtesy of Libraire Flammarion, Paris.

This content downloaded from 169.229.32.136 on Wed, 7 May 2014 21:30:53 PMAll use subject to JSTOR Terms and Conditions