An Archival Study of Environmental Change in the Glaciers of the Mer de Glace and La Meije Using Historical Cartography and Photographic Surveys
The masses do not see the Sirens, they do not hear the songs in the air. Blind, deaf, stooping, they pull at their oars in the hold of the earth. But the more select, harken to a Siren within them...and royally squander their lives with her.
---Nikos Kazantzakis
During my visits to the Alps over the last 15 years I have noticed a change. Instead of snow capped and glacier topped mountains, one has begun to see bare, dark rock, where white snow and ice once stood. For anyone who has spent time anywhere in the Alps this fact is a stark reminder of the current effects of global warming on these fragile mountain environments. A glance through the many scientific journals in the field of glaciology shows how many studies have recently been produced that are concerned with attempts to quantify the extent of this melting by calculating the negative change in the mass balances of glaciers in mountain ranges al of the world. There are few studies however, that have looked at this melting using archival and historic sources. An exception to this can be found in the work of Daniel Steiner, Heinz J. Zumbuhl and Anderas Bauder. Their article, "Two Alpine Glaciers over the Past Two Centuries: A Scientific View Based on Pictorial Sources", (in Darkening Peaks: Glacier Retreat, Science and Society, edited by Ben Orlove (2008)) details the use of historical maps and both early panoramic and stereo photography to study the historical flow of Unterer Grindelwald and Unteraar glaciers in Switzerland. The Unteraar glacier of course being the site where Louis Agassiz did his famous experiments on glacial motion. Others, such as H. Holzhauser, have examined glacier fluctuations in the western Swiss and French Alps using historical sources dating back into the early 16th century. (see his article in Climate Change 43: 223-37 (1999)). Their results show that it is possible to create DEMs (digital elevation models) using various types of historical data and to calculate changes in glacier volume, area, and length over long periods of recent history.

Author at the glacial lake around the Arsine Glacier near La Meije in the Parc Nationale des Ecrins (click on images to enlarge)
The geographic region around both of these glacier systems was well traveled, photographed and mapped through the 19th century, with some studies surviving from earlier times. The historical record for the glaciers in the Mont Blanc region being especially rich. The first quantifiable map of the region around Mont Blanc and the Mer de Glace was made by the Scottish scientist James Forbes in 1842, and the triangulations found in his field notebooks (shown on the map below) provide a baseline to compare later cartography of the region and to map the extent of glacial retreat. The map below is found in Tydall's collection of Forbes letters shows the location of the triangulation points on the Mer de Glace that Forbes used in the creation of his map and in the measuring of glacier flows. Forbes tells us in his Travels through the Alps of Savoy that, "Topographical literature, more than almost any other, is diffused over bulky and unindexed compilations, or more irrevocably lost in fugitive pamphlets." It is this very information that we seek to use in this project.
45: 575-83.Map based on Forbes survey found in Alps glacier systems, published in 1854
In the coming months there will be more posts and photographs on this subject as I work out the georectification of many of the early glacial maps of these areas and travel to the Mont Blanc and La Meije to record and photograph the conditions as they exist today. Steiner et. al. note, in regards to the type of sources used in this study, "with methods based on historical records a temporal resolution of decades or, in some cases, even individual years can be achieved in the reconstruction of glacier time series."




























