Abstract
Glacial landforms and glaciation within the catchment area of the longest source segment of the Apurímac River in the Cordillera Chila are described. Glaciers in the catchment area experienced a 60 % decrease in surface area since 1955.
Glacial landforms and glaciation within the catchment area of the longest source segment of the Apurímac River in the Cordillera Chila are described. Glaciers in the catchment area experienced a 60 % decrease in surface area since 1955.