Tschierva Glacier

Tschierva Glacier is an ice field in the Bernina Range, characterized by steep granite walls and broad expanses of white ice that dominate the alpine landscape. The terrain shows the typical features of a high mountain glacier zone with exposed bedrock and seasonal snow cover.

The glacier has been observed since the 19th century, showing continuous retreat over the following decades. This long-term monitoring makes it an important indicator of climate change impacts in the Swiss Alps.

Scientists and researchers gather data from the Tschierva Glacier as part of the Swiss glacier monitoring network to study environmental changes.

The area is reached by marked trails from Roseg Valley, with summer months offering the best accessibility and conditions. Proper hiking boots and alpine experience are necessary, as the routes are steep and demanding.

The meltwater feeds the Ova da Roseg river, which forms a vital water system for the surrounding alpine meadows and valleys. This network of glacier water and vegetation has sustained local communities for centuries.