


The slope opposite, on the right-hand side of the Chambran valley, is part of the crystalline basement of the Les Écrins massif. The peaks and needles of granite and gneiss are quite unlike the imposing limestone cliffs overlooking the path! The glaciers left their mark here, carving out the rock and then leaving behind vast stretches of moraine as they retreated. Unfortunately, the Séguret glacier up ahead, extremely reduced in size and having retreated to the bottom of its cirque, has not escaped the effects of climate change.