Yankin da ke da alaƙa da tarihi

**Fuskar paleic** ko **palaeic surface** ( Norwegian  , from Tsohon Girkanci palaios '    wani yanki ne na zazzagewar tudu mai laushi da ke a Kudancin Norway .  Sassansa ci gaba ne na peneplain na Sub-Cambrian da Muddus Plains da aka samu gabas   ko kuma daidai da filayen bakin teku na bakin teku na Norway.  Hardangervidda, wani yanki na musamman mai lebur da tsayin daka na Paleic surface da aka kafa a cikin Miocene a matakin teku. 

Kodayake an lura da yanayin da ya dace da kudancin Norway tun daga farkon shekarun 1800, bayanin farko na Hans Reusch ne a cikin 1901, ta amfani da tsarin lokaci na denudation wanda ke kiran ra'ayoyin W.M. Davis da yawa na sake zagayowar lalacewa. Reusch kuma ya kirkiro sunan Paleic surface . 

Yankin Paleic wani lokacin ana ɗaukarsa daidai da "farashin pre-glacial" na Norway - farfajiyar da ta wanzu a Norway kafin glaciations na Quaternary.

## Kudancin Norway: irin yankin
An yi ƙoƙari daban-daban don bayyana ƙananan abubuwan da suka hada da farfajiyar paleic a kudancin Norway. Masanin ilimin ƙasa Karna Lidmar-Bergström da abokan aiki sun gane wurare biyar da aka shimfiɗa. [A] Koyaya, ba duk matakai ba ne za a iya daidaita su cikin tsarin matakai biyar, watakila saboda mamayewa gida. A gabashin Norway wasu daga cikin matakai sun haɗu cikin farfajiyar guda ɗaya. A kudu maso yammacin Norway, kwari da fjords sun rarraba Paleic sosai. Dovre da Jotunheimen su ne sauran duwatsu da ke tashi daga mafi girman matakan da aka ɗora. Wadannan duwatsu suna bayyana tsohuwar ambulaf ɗin da aka warped. Wataƙila warping na farfajiyar ambulaf yana nuna mamayewar ɓawon burodi da ke da alaƙa da hauhawar Dutsen Scandinavia a cikin Cenozoic. An sake gina farfajiyar Paleic a kan yankin fjord na yammacin Norway.   A cikin farfajiyar paleic da aka sake ginawa, kwari masu laushi suna bin wannan hanyar kamar Sognefjord, Hardangerfjord, Gudbrandsdalen da Østerdalen, amma ba na wasu kwari da fjords na yammacin Norway ba.  

A arewa ƙananan matakan Paleic suna ɗaukar daidai da Filayen Muddus a arewacin Sweden, ma'ana cewa yanayin ƙasa mai yiwuwa ya ci gaba a lokaci ɗaya da matakin, kuma ta hanyar matakai iri ɗaya.

Ana zaton ƙananan matakan Paleic sun samo asali ne ta hanyar etching da cirewa da pediplanation. Yanayin da waɗannan matakai suka faru ya fi na yanzu zafi.

### Tectonics da rushewa
Yawancin farfajiyar paleic a kudancin Norway ya kasance a matakin teku ko ƙasa a lokacin Miocene .  A cikin Farkon Pliocene (shekaru miliyan 5-4 da suka gabata) an ɗaga saman kamar Hardangervidda ta hanyar dakarun tectonic 1.2 km. Yankin peneplain na farfajiyar paleic a bayyane yake an rushe shi ta hanyar motsi na tsaye tare da kuskuren, biyo bayan tsarin NNE-SSW.&nbsp;

Filayen bakin teku na Norway, strandflat, mai yiwuwa tsoffin wurare ne da za a iya kwatanta da farfajiyar paleic wanda ya tsere wa hauhawar da ta shafi Dutsen Scandinavia. Tun lokacin da farfajiyar ta kafa kogin da Rushewar kankara ya lalata yawancin sa a Yammacin Norway, amma ragowar da aka warwatsa suna ko'ina.

## Paleic surface a wasu wurare a Norway
A arewacin Norway wani wuri mai laushi ya shimfiɗa a cikin Varanger Peninsula . A cikin tsibirin farfajiyar farfajilar ta ƙunshi tudu mai tsayi tsakanin tsawo na 200 da 600 m.a.s.l. Sassan da suka fi tsayi na tsaunuka sun ƙunshi duwatsu masu tsayayya da rushewa kamar Quartzite. Sassan da ke ƙasa sun ƙunshi duwatsu masu rauni kamar shale da mudstone. A matsakaiciyar matakan sandstone ya zama ruwan dare. Wasu sassan farfajiyar paleic a cikin Varanger Peninsula sun sake nuna rashin daidaituwa wanda ke haifar da dutse mai laushi na Vendian (Late Neoproterozoic) shekaru. Yankin paleic na iya tashi har zuwa mita 200-250 tun tsakiyar zamanin Pliocene.

Sassan nahiyar Norway sun dace da wuraren da ake kira bankflats. Wadannan farfajiyar suna iyaka zuwa ƙasa tare da gangaren ruwa wanda ke raba su daga strandflat.

## Manazarta