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DISCOVER — BASÒDINO<br />

11<br />

GLACIER MINI<br />

GLOSSARY<br />

Front of the glacier<br />

The front is the lower<br />

edge of the tongue,<br />

to which the glacier<br />

length and regression<br />

measurements refer.<br />

Glacial lakes<br />

The meltwater can<br />

form lakes at the front<br />

or sides of the glacier<br />

(proglacial lakes), on<br />

the surface of the<br />

glacier (epiglacial)<br />

or inside the glacier<br />

(endoglacial).<br />

Crevasses<br />

These are cracks<br />

in the ice and can<br />

be transverse,<br />

longitudinal or<br />

terminal.<br />

Seracs<br />

These are blocks of<br />

ice separated by large<br />

crevasses, formed due<br />

to a marked increase<br />

in the angle and<br />

speed of the glacier.<br />

03<br />

01. Discovering the glacier on<br />

the snowy slopes of the Upper<br />

Maggia Valley.<br />

02. With a surface area of 1.6 km 2 ,<br />

the Basòdino glacier is the<br />

largest in Ticino.<br />

03. Mattia and Giovanni often<br />

work together to perform<br />

measurements on the Basòdino<br />

glacier.<br />

04. The various measurements<br />

are made at least once a year,<br />

usually between April and<br />

September.<br />

Moraines<br />

Moving ice carries<br />

rocky debris with it,<br />

which is deposited at<br />

the sides and in front<br />

of the ice, giving rise<br />

to moraines.<br />

04<br />

TO THE<br />

VIDEO

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