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Fri frakt – när du handlar för 795 kr. de Geer moraine A type of moraine landscape that consists of a series of separate, narrow ridges trending parallel to a former ice front, and which can form annually. The ridges may be up to 300 m apart and up to 15 m high. They consist typically of a till core, capped by a layer of partly rounded boulders. De Geer moraines are generally considered ridges that reflect a saccadic, annual retreat of a stable ice margin in contact with a water body.

They were formed along the ice margin trasversal to ice flow (see fig. 1). av M Lindén · 2006 · Citerat av 7 — were focused on to provide a process and depositional model for De Geer moraine and Niemisel moraine and to reveal their internal and spatial relationship, av C Öhrling · 2020 · Citerat av 2 — mapped; end moraines, De Geer moraines, drumlins, crag-and-tails, hummock tracts and corridors, irregular ridges, murtoos, eskers, 18 juni 2020 — och drumlinoid landform, korsande De Geer-moräner, spår av glacialt end moraines, De Geer moraines, drumlins, crag-and-tails, hummock De Geer moraines on sight this weekend? tower where you have a wonderful view of the archipelago and the world heritage De Geer-morain from the ice age. De Geer moraines. De Geer-moräner. Ice marginal moraines.

2012 — Grunden för min tanke med världsarvs-pedagogiken började i Bodback I Finland 2007 Hur ska man förstå De Geer moränbildningen i Bodback 7 sep. 2019 — Då inlandsisen började smälta formades moränformationer, s.k.

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29 nov. 2020 — betydelse av tvärryggar (de Geer moraines) intill Moray Firth, NE Skottland · Ardesierhalvön del av en svit av glaciomarin iskontaktfyndigheter 6 jan.

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De Geer moraines in a Swedish mountain area? / by Ingmar Borgström Borgström, Ingmar, 1951- (författare) Stockholm, 1979 Engelska S. 35-42 Serie: Meddelanden från Naturgeografiska institutionen vid Stockholms universitet, 0348-9264 ; A 99 Bok De Geer moraines are ridges up to 5 m high, 10-50 m wide, and in some cases 1000 m or more in length.

2020-03-04 · De Geer moraine formations create the iconic views of the Kvarken Archipelago.
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We refer to these new landforms as ‘murtoos.’ 3. Morphometric measurements show murtoos to be 50 to 200 m long and 50 to 100 m wide. The orientation of their apices strongly correlates with local ice- flow orientation. They form Sedimentology and architecture of De Geer moraines in the western Scottish Highlands, and implications for grounding-line glacier dynamics Nicholas R. Golledge 1,2, Emrys Phillips 1British Geological Survey, Murchison House, West Mains Road, Edinburgh, EH9 3LA* 2Institute of Geography, University of Edinburgh, Drummond Street, Edinburgh, EH8 9XP email n.golledge@bgs.ac.uk, phone +44 131 6671000. Occurrence of De Geer moraines in Finland based on LiDAR DEM A.E.K.

J. Quaternary Sci., Vol. 20 pp. 113–133. ISSN 0267‐8179.
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113–133. ISSN 0267‐8179. De Geer Moraine Map Symbol: MG First publication: 21 January 2021 Last modification: EtymologyThe De Geer moraines owe their name (Hoppe, 1959) to Baron Gerald Jacob De Geer (1858-1943), a pioneering geologist who was the first to observe these sedimentary structures in Sweden (De Geer, 1889).

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Using airborne 2000: Common origin for De Geer moraines of variable composition in Raudvassdalen, northern Norway. Journal of Quaternary Science 15, 633–644. Page 55 av K Lidmar-Bergström · 1991 · Citerat av 46 — limitation and areal extent of the hummocky moraine in the As the moraines in the 10 - 20 km wide, NW-SE The Andrarum esker (De Geer 1889, Bergdahl. Ribbed moraine formed by subglacial folding, thrust stacking and lee-side cavity infill Marginal formation of De Geer moraines and their implications to the Panorama of the view from Saltkaret in Svedjehamn, Mustasaari. This is a view over the De Geer-moraines, the Kvarken Archipelago World Heritage site.

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2000-06-01 · De Geer moraines are small moraine ridges formed partly in crevasses at the base of glacier ice.

The 5,600 islands of the Kvarken Archipelago feature unusual ridged washboard moraines, 'De Geer moraines', formed by the melting of the continental ice V. = the lake in the moraine hill account_balance De Geer 1919 a Karta över Spetsbergens inland mellan Belsund och Storfjorden med Sveagruvans kolfält The tower, located in the fish harbour Svedjehamn, offers a beautiful view over the De Geer-moraines. This unique moraine archipelago affirms the enormous Gerard Jakob De Geer, den föregåendes broder, son till D. 8, f. On the solar curve as dating the ice age, the New York moraine and Niagara falls through the Panorama of the view from Saltkaret in Svedjehamn, Mustasaari. This is a view over the De Geer-moraines, the Kvarken Archipelago World Heritage site. were focused on to provide a process and depositional model for De Geer moraine and Niemisel moraine and to reveal their internal and spatial relationship, av G Dannstedt · 1947 · Citerat av 15 — De Geer i stor utstrickning baserat denna Kalmarmorinernas dragning i sydlig riktning stage in the Goti-glacial ice recession (the #Kalmar moraines)). (9) Bouldery end moraines and bouldery ground in generai register Bromma-området karaktäriseras av mycket blockrika öndmcräner (De Geer 1932, 1940). Björköby.sijainti.svg 1,750 × 2,950; 1.14 MB. Björköby.vaakuna.svg 500 × 545; 17 KB. De Geer moraines at Kvarken.JPG 4,608 × 3,456; 3.83 The 5,600 islands of the Kvarken Archipelago feature unusual ridged washboard moraines, 'De Geer moraines', formed by the melting of the continental ice betydelse av tvärryggar (de Geer moraines) intill Moray Firth, NE Skottland · Ardesierhalvön del av en svit av glaciomarin iskontaktfyndigheter 51 (1996): Estuaries of the Outer Moray Firth · Morphology and significance of transverse ridges (de Geer moraines) adjacent to the Moray Firth, NE SCotland säregen samling av istida landsformer såsom De Geer-moräner, vilka ger mer formations, such as De Geer moraines, which add to the variety of glacial land-.