Guest Blog

Glaciers have carved some of Earth’s most beautiful landscapes by steepening and deepening valleys through erosion. Think of the Scottish Highlands, Yosemite National Park in the US, or the Norwegian Fjords. But big questions remain about how glacial erosion works.

A problem for scientists seeking to understand how glaciers affect the landscape is that the processes of glacial erosion are very complex and not fully understood. For the most part that’s because these processes occur under tens, hundreds or even thousands of metres of ice – we simply can’t observe them.

In the Andes of Peru and adjacent arid lowlands, human subsistence often depends on year-round streamflow from glaciers and lakes, particularly in the dry season. However, global change impacts increasingly affect local hydrology and associated livelihoods which is clearly demonstrated by the impacts of glacier shrinkage. Rapidly growing lakes (Fig. 1) in deglaciating mountain regions potentially imply severe risks but also options for human livelihoods.