"This white lake, the Lac de la Glière, is not covered by ice, despite appearances. It actually dried up in the 19th century. In 1818, people lived in the ""small ice age"", a colder climatic period that began in the late 16th century in Western Europe and whose end we are now seeing. As a result, the Rosolin glacier ""licks"" the edge of the lake. Seracs, or pieces of glacier detached from the main tongue, then fell into its waters, blocking the natural flow at the outlet of the lake. The water ended up overflowing, carrying along its course the seracs, mud and rocks downstream. After this natural disaster of 1818, the lake dried up, taking on a new appearance. After draining, the sediment deposited at the bottom of the basin then came to light. The historic mountain pasture around the lake has not been affected, having been frequented since the thirteenth century."