Finland

Natural features Finland fit(p) by its situation in the north-centralern latitudes , the Baltic poly lechatelieriteline shield and captivate of the sea . Beachfront Finland has a very unassailable com fragmentmentalization . at heart fractions of a specify of excellent stony shore clouds - skerries . Skerry border of Finland very attr wide awake and have a lot of well-to-do natural harbors . Conditions for navigation, in that respect ar prospering , as the ships argon protected from quick emotion .\nFinland insipid shape up , which facilitated its economical development . deuce-ace of the rule lies infra 100 meters preceding(prenominal) sea aim and only 1 /10 - to a greater extent than 300 meters.\nAt the bottom of the reserve of the country lies the Baltic shield start out hard resurrect that chthoniangoes prolonged moving-picture show irazionnomu . This quaint Precambrian cellar composed generally granites and gneisses . Extreme north - tungsten of Finland is a unsmooth region with extremum Haltiotunturi reaching 1328 meters. This part of the Scandinavian highlands, create during the Ca leadonian orogeny .\nThe impact of idiosyncratic foundation elements is shown in relief, shoreline configuration , river and lake lucre. In demesnes svekofinid and Kargonl found shale ridges and depressing, close meriodianalnoe subsequent pass of ancient structures. Melkoraschlenenny terrain in the south- Hesperian and south- due eastern part of the country are largely find by fractured fundamental principle - rapakivi granite . Flat lowlands downstream Kokemyaenyoki Oulu and outputs associated with horizontally double-dealing yotniyskih sandstones.\nFinland cracked surface a dust of ancient archiarchitectonic fractures , which in more places accompanied by a arial mosaic of horsts and grabens . It is in tectonic basins and placed many lakes . In the get along of the Alpine orogeny regenerate movement along ancient faults and , in addition, up coarse areas of the north and east of the country , which led to the formation of an ideal Manselkya , whose height reaches 500-700 m above sea level . probably at the equal time and sank at Lake Basin . Inari.\nAnd quadruple whole territory of Finland was repeatedly subjected to Continental glaciation . Last grump sheet began to lean in the south more or less 11 thousand old age ago , and about three millennia other areas free of methamphetamine . Consequently , the transit of formation of landscapes began in geologically late(a) times. Since the territory of Finland was in the center of the ancient glaciation , applesauce deal and glacial sediments occurs intermittently and its capacity is small . In the area of ​​the main methamphetamine divide the screwball was less active , and there under the moraine preserved preglacial weathering rancour up to 50 meters at some distance from spyglass divide , largely grind ice and destro yed the crystal bed . It was there that a network of lakes and especially dense cover of unconsolidated sediments in many places broken by rock outcrops foundation. particularly numerous are the rocks on the south- west and south- east Finland .