GEOTOPER 3 PDF

Mikanos Can you give a roughly estimate of sizes of visible grains? Answers Read answers to your questions here. Read answers to your questions here. Geotopfr A ridge-shaped deposition When you look down the valley to the northeast of the sign and to the east and south you see an elongated ridge. This is called ice-scouring. See about grain-sizes here.

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Nejas Leka locality 3 Geotoper Du kommenterer med bruk av din Facebook konto. Which way do you think the glacier has moved in this locality?

Du kommenterer med bruk av din Twitter konto. The extreme pressure from the glacier declined in the lee-side and water geeotoper to geotopper again and expanded. If you wonder which ridge take a look on figures 2 and 3. This melt water seeped to the leeward side of the eminence and down into fissures in the bedrock.

Nylige innlegg Du kommenterer med bruk av din Facebook konto. Du kommenterer med bruk av din WordPress. When you look down the valley to the northeast of the sign and to the east and south you see an elongated ridge.

These were formed beneath the Main Ice Sheetthat at its maximum covered most of Scandinavia. The image shows striae in bedrocks at Vegdalsskaret. Read answers to your questions here. The summit is named Trollvasstinden. Answers Read answers to your questions here. Small-scaled erosional forms There are also some beautiful geotopfr erosional forms southwest of the sign. Try to describe its appearance and the approximate size length-width-height? Answers Answers to questions can be found here.

Can you give a roughly estimate of sizes of visible grains? Striae are thus traces of glacier movement. See about grain-sizes here. Vega locality 3 Geotoper Rock particles frozen to the base of the glacier was scoured along the rock-surface, so that the glacier acted as a gigantic sand paper, where the pressure towards the underlying rock was extreme. This photo is of the same ridge further up-valley, towards south, and is taken from a position close to the signpost.

Glacial modulation of rocks GPS-coordinates: A figure on this page will help you in your interpretation. You see a large depression behind the ridge, in the shadow-part of the photo in the foot of Trollvasstinden.

Legg igjen en kommentar Avbryt svar Skriv din kommentar her This is called ice-scouring. It was formed under the ice sheet during last Ice Age, where multiple processes were involved in the formation. The photo shows the ridge down-valley egotoper east, seen from the signpost. There are also some beautiful small-scaled erosional forms southwest of the sign. Answers to questions can be found here. The photo is taken in a southward direction. Related Posts

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Geotoper 3

Brazshura The photo shows the ridge down-valley towards east, seen from the signpost. Rock particles frozen to the base of the glacier was scoured along the rock-surface, so that the glacier acted as a gigantic sand paper, where the pressure towards the underlying rock was extreme. The summit is named Trollvasstinden. Answers Answers to questions can be found here. Try to describe its appearance and the approximate size length-width-height?

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GEOTOPER 3 PDF

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