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Forfatter: Geoff Corner
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DIVERSE

Norge Sør-Norge N-N / TROMS Svalbard
Berggrunnsgeologi

Løsmasser

Landskapet Spor etter istiden Eldre havnivå

Bruk av geologien

6 End moraines from the ice age (280-320 m.a.s.l.)  

A 15-20-minute walk from the previous locality leads up to a small moraine ridge that gives fine views up the valley. The moraine ridge was formed at the front of the glacier during a short readvance. A similar end moraine can be seen 600 m farther on. The moraine ridges show where the glacier front was located during its general retreat at the end of the last ice age.

 

 

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