Glacier du Tour, Alpine glacier in Chamonix-Mont-Blanc, France
Glacier du Tour is a large ice mass near Chamonix that extends across several kilometers and defines the surrounding slopes. Its surface displays typical glacial features with crevasses and uneven structures resulting from constant movement and melting.
The ice field formed during the last ice age and has repeatedly advanced and retreated depending on temperature changes. Throughout the 20th century its retreat accelerated noticeably, showing how mountain conditions have shifted.
The glacier serves as a powerful natural landmark that mountain climbers and hikers encounter as they move through this high Alpine region. Its massive ice formations give visitors a direct sense of how nature shapes these mountains over time.
Access is through hiking paths known and used by experienced mountain guides; starting early in the day helps secure stable weather conditions. The altitude requires good physical fitness and proper gear to protect against cold and intense sun exposure.
A striking feature is that the lower tongue descends over large rock steps, making its drop quite dramatic. This steep structure reveals how glacial ice crosses ancient mountain terrain and exposes the underlying topology.
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