Vega Vegdalsskaret Lokalitet 3 12_ Figure 1: The photo above is taken on the way up to the locality along the path from its beginning in Bjørnlia, and shows a. Geotoper 3 – Elevbog ebog – Ivan Jacobsen, Tom Døllner, Jørgen Steen, Nils Hansen, Lennie Boesen, Ole Chir. tom. iii. Diss. Gunzii Libell. de hern. &c — -Hernie de la vessie urin- aire, Mery Mem. de l’Acad. R. des Sc Garen- geot Oper. de Chir. Levret Obs.
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Legg igjen en kommentar Avbryt svar Skriv din kommentar her A figure on this page will help you in your interpretation.
Modsætning rig/fattig by Nikolaj Therkildsen on Prezi
Striae are thus traces of glacier movement. There are also some beautiful small-scaled erosional forms southwest of the sign. Du kommenterer med bruk av din Twitter konto. The summit is named Geotoprr. The extreme pressure from the glacier declined in the lee-side and water froze to ice again and expanded. See about grain-sizes here. 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 geotiper an elongated ridge. The stripes in the rocks is called striae see photo below. Small-scaled erosional forms There are also some beautiful small-scaled erosional forms southwest of the sign. This is called ice-scouring.
Vega locality 3 | Geotoper
Try to describe its appearance and the approximate size length-width-height? Answers Read answers to your questions here. Vegdalsskaret A ridge-shaped goetoper When you look down the valley to the northeast of the sign and heotoper the east and south you see an elongated ridge. It was formed under the ice sheet during last Ice Age, where multiple processes were involved in the formation. 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 geotopeer rock was extreme.
Du kommenterer med bruk av din WordPress. Read answers to your questions here. Glacial modulation of rocks GPS-coordinates: Du kommenterer med bruk av din Twitter konto. Answers to questions can be found here. You see a large depression behind the ridge, in the shadow-part of the photo in the foot of Trollvasstinden.
What kind of ridge do you think it is? The image shows striae in bedrocks at Vegdalsskaret.
The photo shows the ridge down-valley towards east, seen from the signpost. Legg igjen en kommentar Avbryt svar Skriv din kommentar her The photo is taken in a southward direction.
Geotoperr melt water seeped to the leeward side of the eminence and down into fissures in the bedrock. Answers Answers to questions can be found here.
If you wonder which ridge take a look on figures 2 and 3. These were formed beneath the Main Ice Sheetthat at its maximum covered most of Scandinavia.
Du kommenterer med bruk av din Facebook konto. Du kommenterer med bruk av din Facebook konto. Can you give a roughly estimate of sizes of visible grains? Which way do you think the glacier has moved in this locality? This photo is of the same ridge further up-valley, towards south, and is taken from a position close to the signpost.