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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Torghatten locality 3 | Geotoper
The photo shows the ridge down-valley towards east, seen from the signpost. What kind of ridge do you think it is? Legg igjen en kommentar Avbryt svar Skriv din kommentar her This melt water seeped to the leeward side of the eminence and down into fissures in the bedrock. When you look down the valley geotopper the northeast of the sign and to the east and south you see an elongated ridge. The summit is named Trollvasstinden. Legg igjen en kommentar Avbryt svar Skriv din kommentar her Answers Read answers to your questions here.
Striae are thus traces of glacier movement.
Du kommenterer med bruk av din WordPress. It was formed under the ice geotkper during last Ice Age, where multiple processes were involved in the formation.
Du kommenterer med bruk av din WordPress. This is called ice-scouring.
See about grain-sizes here. Du kommenterer med bruk av din Twitter konto. The image shows striae in bedrocks at Vegdalsskaret.
Vegdalsskaret 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. Teotoper stripes in the rocks is called striae see photo below. Read answers to your questions here. Can you give a roughly estimate of sizes of visible grains? If you wonder which ridge take a look on figures geotopeg and 3.
The extreme pressure from the glacier declined in the lee-side and water froze to ice again and expanded. The photo is taken in a southward direction. This photo is of the same ridge further up-valley, towards south, and is taken from a position close to the signpost. Du kommenterer med bruk av din Twitter konto. These were formed beneath the Main Ice Sheetthat at its maximum covered most of Scandinavia. There are also some beautiful small-scaled erosional forms southwest of the geofoper.
A figure on this page will help you in your interpretation. Glacial modulation of rocks GPS-coordinates: Du kommenterer med bruk av din Facebook konto.
Answers Answers to questions can be found here. Try to describe its appearance and the approximate size length-width-height? Du kommenterer med bruk av din Facebook konto. Small-scaled erosional forms There are also some beautiful small-scaled erosional forms southwest of the sign. Answers to questions can be found here.
Torghatten locality 3: answer | 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.
Which way do you think the glacier has moved in this locality?
You see a large depression behind the ridge, in the shadow-part of the photo in the foot of Trollvasstinden.