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THE GLACIER PART 2. The glacier Basei viewed from the north, almost completely devoid of snow. We live in a hot natural phase, but in particular the human activities have helped to increase this phenomenon. The rate of melting of glaciers has tripled since 1970.
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THE GLACIER PART 2
The glacier Basei viewed from the north, almost completely devoid of snow
We live in a hot natural phase, but in particular the human activities have helped to increase this phenomenon. The rate of melting of glaciers has tripled since 1970. In 2030, the glaciers could be just a memory
THE LAKE BORN BETWEEN THE CLOUDS Ghiaccio del Rocciamelone
The glacial erosion Strong pressure exercised by the glacier moving and by the friction enhanced by the presence of debris.
Ample funds and often stepped, flanked by steep scarps U valleys
Moraine accumulationJumble of boulder scattered in a matrix of sand and silt
Lateral moraine The lateral moraine that blocks the pond indicates the greater level reached by the glacier
The amphitheatre of the Lake of Miage (Monte Bianco) is composed of twenty concentric moraines (pile of rock debris)
Glacial strip (Valley of Funes – Alto Adige)
Sheepbacks (or back of whale) Striped rocks
The sheepbacks are generally rounded on the top and in the side, oriented according to the direction of glacier
The big rocks Erratic rocks The erratic rocks can be transported over long distances by glaciers
Caselette The big rock in the entrance of the village
Pianezza Il “Roc”
The rock of Castellazzo The block rocky region Castellazzo is a typical example of a boulder, fell for landslide on the surface of a glacier and transported in the valley
threshold navel Germanasca’s Valley – Torino – I tredici laghi
Rock glaciers characteristic accumulations of large blocks with their lobed shape