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):||8 February 2016|
|PDF File Size:||6.97 Mb|
|ePub File Size:||14.11 Mb|
|Price:||Free* [*Free Regsitration Required]|
When you look down the valley to the northeast of the sign and to the east and south you see an elongated ridge. 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 Twitter konto. These were formed beneath the Geotpper Ice Sheetthat at its maximum covered most of Scandinavia.
The stripes in the rocks is called striae see photo below.
It was formed under the ice sheet during last Ice Age, where multiple processes were involved in the formation. This is called ice-scouring. Answers Read answers to your questions here. Rock particles geotoepr 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.
Answers to questions can be found here. Du kommenterer med bruk av din WordPress. This photo is of the same geotopfr further up-valley, towards south, geoyoper is taken from a position close geotopeer the signpost.
Du kommenterer med bruk av din Facebook konto. Which way do you think the glacier has moved in this locality? Small-scaled erosional forms There are also some beautiful small-scaled erosional forms southwest of the sign. Du kommenterer med bruk av din Twitter konto. This melt water seeped to the leeward side of geotope eminence and down into fissures in the bedrock.
If you wonder which ridge take a look on figures 2 and 3. Try to describe its appearance and the approximate size length-width-height? Striae are thus traces of glacier movement. The extreme pressure from the glacier declined in the lee-side and water froze to ice again and expanded. Du kommenterer med bruk av din Facebook konto. You see a large depression behind the ridge, in the shadow-part of the photo in the foot of Trollvasstinden.
Torghatten locality 3: answer | Geotoper
Read answers to your questions here. Answers Answers to questions can be found here.
Legg igjen en kommentar Avbryt svar Skriv din kommentar her 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 geotoepr elongated ridge. The photo shows the ridge down-valley towards east, seen from the signpost.
A figure on this page will help you in your interpretation.
See about grain-sizes here. The summit is named Trollvasstinden. The image shows striae in bedrocks at Vegdalsskaret. What kind of ridge do you think it is?
The photo is taken in a southward direction. There are also some beautiful small-scaled erosional forms southwest of the sign. Can you give a roughly estimate of sizes of visible grains?