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.
|Published (Last):||13 October 2010|
|PDF File Size:||14.11 Mb|
|ePub File Size:||8.21 Mb|
|Price:||Free* [*Free Regsitration Required]|
Legg igjen en kommentar Avbryt svar Skriv din kommentar her The stripes in the rocks is called striae see photo below. Can you give a roughly estimate of sizes of visible grains?
These were formed beneath the Main Ice Sheetthat at its maximum covered most of Scandinavia. Try to describe its appearance and the approximate size length-width-height? The summit is named Trollvasstinden. 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 is taken in a southward direction. Du kommenterer med bruk av din Twitter konto.
There are also some beautiful small-scaled erosional forms southwest of the sign. Answers Read answers to your questions here.
Answers to questions can be found here. Du kommenterer med bruk av din Facebook konto. Legg igjen en kommentar Avbryt svar Skriv din kommentar her Du kommenterer med bruk av din WordPress. Glacial modulation of rocks GPS-coordinates: Du kommenterer med bruk av din Geotopr konto. Du kommenterer med bruk av din WordPress.
The photo shows the ridge down-valley towards east, seen from the signpost. When you look down the valley to the northeast of the sign geotpper to the east and south you see an elongated ridge.
This photo is of the same ridge further up-valley, towards south, and is taken from a position close to 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.
Torghatten locality 3 | Geotoper
What kind of ridge do you think it is? This melt water seeped to the leeward side of the eminence and down into fissures in the bedrock. If you wonder which ridge take a look on figures 2 and 3. The image shows striae in bedrocks at Vegdalsskaret. Read answers to your questions here. See about grain-sizes here. 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.
Which way do you think the glacier has moved in this locality? A figure on this page will help you in your interpretation. The extreme pressure from the glacier declined in the lee-side and water froze to ice again and expanded. Small-scaled erosional forms There are also some beautiful small-scaled erosional forms southwest of the sign. Du kommenterer med bruk av din Facebook konto.