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478:
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102:
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has been used to correlate the
Annijokka Member of the BĂĄtsfjord Formation with other Neoproterozoic successions around the world, suggesting it was deposited approximately 811 million years ago, during the Bitter Springs carbon isotope excursion.
454:. Two ancient fault systems divide the geology of the peninsula into three groups, where the NE side of the peninsula (North Varanger region) is separated from the SW by the Trollfjord-Komagelva
101:
497:, when the Løkvifjell Group was deposited. Notable strata of the Barents Sea Group are the Kongsfjord and Båsnæring formations, which form prominent ridges and cliffs along the
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share the 2,069-square-kilometre (799 sq mi) peninsula. Nesseby and Tana are only partially on the peninsula, with the rest being entirely on the peninsula. The
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133:
889:"Supralittoral ponded algal stromatolites of the late Precambrian Annijokka Member of the BĂĄtsfjord formation, Varanger peninsula, north Norway"
965:
Crockford, Peter W.; Hodgskiss, Malcolm S.W.; Uhlein, Gabriel J.; Caxito, Fabricio; Hayles, Justin A.; Halverson, Galen P. (2017-12-12).
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climate but with the updated 1991-2020 climate normals, this is mostly gone. However, much of the peninsula is at some altitude and are
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The area has rugged mountain terrain with altitudes of up to 633 metres (2,077 ft). Much of the relief of the peninsula is a
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similar to the one found in the highlands of southern Norway. In the peninsula the paleic surface is made up of an undulating
832:
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along the coast of the peninsula; some arctic species of birds spend the winters along the coast of the peninsula.
517:, and other sedimentary structures that indicate deposition in an inter-tidal, intermittently exposed environment.
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road. Outcrops of the overlying BĂĄtsfjord
Formation are generally not as prominent, but are notable for containing
778:]. Meddelanden frĂĄn Lunds universitet geografiska institution. Avhandlingar XCIII (in Swedish). Lund, Sweden:
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632:
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Neoproterozoic glacial and associated facies in the
Tanafjord-Varangerfjord area, Finnmark, north Norway
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crystals related to 'Snowball Earth' deglaciation are found locally on outcrops of the Baltic Shield.
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470:
400:. Blockfields are most extensive on the northern half of the peninsula, chiefly in the plateau area.
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110:
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on the
Norwegian mainland. In addition to introducing animals into nature, the larger and stronger
459:
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739:"Origin of the palaeic landforms and glacial impact on the Varanger Peninsula, northern Norway"
267:
226:
63:
926:
Hodgskiss, Malcolm S. W.; Kunzmann, Marcus; Poirier, André; Halverson, Galen P. (2018-01-15).
928:"The role of microbial iron reduction in the formation of Proterozoic molar tooth structures"
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Strata deposited on the SW half of the
Varanger Peninsula mostly formed during the mid-late
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858:"Strike-slip restoration of the Barents Sea Caledonides Terrane, Finnmark, north Norway"
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The higher parts of the undulating plateau are made up by erosion-resistant rocks like
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827:. Marc B. Edwards, T. A. Hansen. Boulder, Colo.: The Geological Society of America.
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is common. Some parts of the paleic surface in
Varanger Peninsula are a re-exposed
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378:) age. The paleic surface might have been uplifted as much as 200–250 meters since
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572:(located on an island just off the coast of the peninsula), earlier had an Arctic
493:(Barents Sea Group), followed by a depositional hiatus that lasted until the late
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Glacial and
Periglacial Geomorphology on the Varanger Peninsula, Northern Norway
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Barite crystals in the
Smalfjord Formation (The diameter of the coin is 24 mm.)
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to the south, and the
Barents Sea to the north and east. The municipalities of
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has a project on the peninsula for the reintroduction and protection of the
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In the North
Varanger region, sedimentary rocks were deposited during the
417:
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Rice, A. H. N.; Gayer, R. A.; Robinson, D.; Bevins, R. E. (April 1989).
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294:. It is located in the northeasternmost part of Norway, along the
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1007:
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On the northern shore of the Varangerfjord between Vardø and Vadsø
967:"Linking paleocontinents through triple oxygen isotope anomalies"
925:
611:
347:
1004:
https://www.sagat.no/nyheter/rekordmange-fjellrevvalper/19.42068
556:' of the Nyborg Formation (Vestertana Group). Small outcrops of
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are recurrent across the peninsula. Among the most common are
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Glacial och periglal gemorfologi på Varangerhalvön, Nordnorge
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584:, there is sufficient summer heat for birch trees to grow.
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is found in some places, but there are no known modern
416:, and in a few places this permafrost had originated
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358:. The lower parts are made up by weak rocks like
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568:A part of the peninsula, including the town of
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595:exist, and 79 cubs were registered in 2023.
580:. On the south coast, including the town of
334:protects most of the land on the peninsula.
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600:Norwegian Directorate for Nature Management
374:that underlie sedimentary rock of Vendian (
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544:sedimentary rocks that formed during the
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802:Malmström & Palmér 1985, pp. 91–92.
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469:Outcrops of the Båsnæring Formation on
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117:on the northern coast of the peninsula
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350:between the altitudes of 200 and 600
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27:Peninsula in Finnmark county, Norway
932:Earth and Planetary Science Letters
770:Malmström, Bo; Palmér, Owe (1985).
435:episode. It is largely composed of
428:The peninsula gave its name to the
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737:Fjellanger, J; Sørbel, L (2007).
662:Highway from Vardø to Hamningberg
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638:The Arctic beach at Hamningberg
412:was as of 1985 only known from
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887:Siedlecka, Anna (July 1982).
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332:Varangerhalvøya National Park
905:10.1016/0301-9268(82)90007-9
747:Norwegian Journal of Geology
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519:Stable carbon isotope ratio
124:Interactive map of the lake
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944:10.1016/j.epsl.2017.10.037
617:There are many species of
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1010:.no. Retrieved 2023-12-28
682:"Informasjon om stadnamn"
540:. Notably, this includes
385:Landforms resulting from
366:. At intermediate levels
298:. The peninsula has the
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462:over the Baltic Shield.
460:Scandinavian Caledonides
874:10.1029/TC008i002p00247
821:Rice, A. H. N. (2012).
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1057:Peninsulas of Finnmark
503:molar tooth structures
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111:BĂĄtsfjord Municipality
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713:Store norske leksikon
608:critically endangered
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179:Offshore water bodies
149:70.48361°N 29.54056°E
893:Precambrian Research
448:crystalline basement
446:, locally overlying
376:Late Neoproterozoic
145: /
782:. pp. 86–87.
542:glacial diamictite
511:desiccation cracks
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398:solifluction lobes
256:Varanger Peninsula
154:70.48361; 29.54056
34:Varanger Peninsula
18:Varanger peninsula
834:978-0-8137-0026-7
717:"Varangerhalvøya"
522:chemostratigraphy
507:teepee structures
456:strike-slip fault
444:sedimentary rocks
302:to the west, the
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16:(Redirected from
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394:block fields
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372:unconformity
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489:/early-mid
418:thermokarst
300:Tanafjorden
296:Barents Sea
197:Native name
187:Tanafjorden
183:Barents Sea
152: /
107:Hamningberg
1026:Categories
754:: 223–238.
723:2013-02-25
695:2024-06-27
690:Kartverket
686:Norgeskart
668:References
604:Arctic fox
593:Arctic fox
530:Cryogenian
491:Cryogenian
433:glaciation
410:Permafrost
406:ice wedges
387:Quaternary
140:29°32′26″E
137:70°29′01″N
1037:BĂĄtsfjord
991:0091-7613
952:0012-821X
913:0301-9268
862:Tectonics
843:778988053
619:sea birds
538:Paleozoic
534:Ediacaran
495:Ediacaran
441:Paleozoic
430:Varangian
368:sandstone
356:quartzite
338:Geography
312:BĂĄtsfjord
284:peninsula
272:Várnjárga
260:Norwegian
220:Várnjárga
212:Norwegian
93:Peninsula
57:Várnjárga
49:Norwegian
1032:BerlevĂĄg
938:: 1–11.
546:Marinoan
364:mudstone
352:m.a.s.l.
316:BerlevĂĄg
290:county,
288:Finnmark
169:Finnmark
165:Location
1052:Nesseby
971:Geology
612:red fox
564:Climate
450:of the
424:Geology
382:times.
348:plateau
328:Nesseby
282:) is a
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950:
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574:tundra
558:barite
536:, and
487:Tonian
471:Fv 341
326:, and
292:Norway
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173:Norway
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1047:Vadsø
1042:Vardø
1008:Sagat
774:[
742:(PDF)
588:Fauna
582:Vadsø
570:Vardø
499:Fv341
360:shale
320:Vardø
308:Vadsø
987:ISSN
948:ISSN
909:ISSN
839:OCLC
829:ISBN
784:ISBN
598:The
414:bogs
396:and
362:and
324:Tana
276:Kven
254:The
242:Kven
79:Kven
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439:to
286:in
109:in
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