fennoscandian - EAS

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  1. Fennoscandia - Wikipedia

    https://en.wikipedia.org/wiki/Fennoscandia

    WebFennoscandia (Finnish, Swedish and Norwegian: Fennoskandia; Russian: Фенноскандия, romanized: Fennoskandiya) or the Fennoscandian Peninsula is the geographical peninsula in Europe, which includes the Scandinavian and Kola peninsulas, mainland Finland, and Karelia. Administratively this roughly encompasses the mainlands of Finland, Norway and …

  2. Cross-country skiing - Wikipedia

    https://en.wikipedia.org/wiki/Cross-country_skiing

    WebCross-country skiing is a form of skiing where skiers rely on their own locomotion to move across snow-covered terrain, rather than using ski lifts or other forms of assistance. Cross-country skiing is widely practiced as a sport and recreational activity; however, some still use it as a means of transportation.

  3. Deutsche Entomologische Zeitschrift

    https://dez.pensoft.net

    WebFounded in 1857 as Berliner Entomologische Zeitschrift, Deutsche Entomologische Zeitschrift (DEZ) is one of the World’s oldest international journals in systematic Entomology. It publishes original research papers in English on the systematics, taxonomy, phylogeny, comparative morphology, and biogeography of insects. Other arthropods are also …

  4. Geology of Wales - Wikipedia

    https://en.wikipedia.org/wiki/Geology_of_Wales

    WebThe geology of Wales is complex and varied; its study has been of considerable historical significance in the development of geology as a science.All geological periods from the Cryogenian (late Precambrian) to the Jurassic are represented at outcrop, whilst younger sedimentary rocks occur beneath the seas immediately off the Welsh coast. The effects …

  5. Subregion - Wikipedia

    https://en.wikipedia.org/wiki/Subregion

    WebThe Statistics Division of the United Nations (UN) is in charge of the collection, processing, and dissemination of statistical information for the UN. In 1999, it developed a system of macro-geographical (continental) regions, subregions, and other selected economic groups to report advances towards achieving numerous millennial development goals worldwide.

  6. Cronologia degli impatti astronomici sulla Terra - Wikipedia

    https://it.wikipedia.org/wiki/Cronologia_degli_impatti_astronomici_sulla_Terra

    WebQuesta cronologia degli impatti astronomici sulla Terra è un elenco dei più significativi eventi d'impatto astronomico sulla Terra (prodotti da asteroidi, comete e meteoriti).Va specificato che la Terra è un pianeta geologicamente attivo e dinamico, soggetto a trasformazioni geologiche nel corso del tempo per via dei vari agenti corrosivi che la …

  7. Alpine orogeny - Wikipedia

    https://en.wikipedia.org/wiki/Alpine_orogeny

    WebThe cause of Alpine orogeny. The Alpine orogeny is caused by the continents Africa and India and the small Cimmerian Plate colliding (from the south) with Eurasia in the north. Convergent movements between the tectonic plates (the African Plate and the Indian Plate from the south, the Eurasian Plate from the north, and many smaller plates and …

  8. Werewolf - Wikipedia

    https://en.wikipedia.org/wiki/Werewolf

    WebNames. The Modern English werewolf descends from the Old English werewulf, which is a cognate (linguistic sibling of the same origin) of Middle Dutch weerwolf, Middle Low German werwulf, Middle High German werwolf, and West Frisian waer-ûl(e).These terms are generally derived from a Proto-Germanic form reconstructed as *wira-wulfaz ('man-wolf'), …

  9. Kenorland - Wikipedia

    https://en.wikipedia.org/wiki/Kenorland

    WebKenorland was one of the earliest known supercontinents on Earth.It is thought to have formed during the Neoarchaean Era c. 2.72 billion years ago (2.72 Ga) by the accretion of Neoarchaean cratons and the formation of new continental crust.It comprised what later became Laurentia (the core of today's North America and Greenland), Baltica (today's …

  10. Abrupt Climate Change During the Last Ice Age - Nature

    https://www.nature.com/scitable/knowledge/library/...

    WebDuring the last ice age, massive continental ice sheets up to five km high covered much of North America and northern Europe (the Laurentide and Fennoscandian ice sheets, respectively).



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