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The postglacial lakes have long since been filled in, and glacial outwash masks the weakly developed meltwater valley channels.
Baltic Coastal Plain stretches across northern Poland from Germany to Russia, forming a low-lying region built of various sediments.
It is largely occupied by the ancient province of Pomerania (Pomorze), the name of which means “along the sea.” The scarcely indented Baltic coastline was formed by wave action after the retreat of the ice sheet and the raising of sea levels.
Katowice is the largest centre, and the region is closely linked with that around Kraków (Cracow).
The Little Poland Uplands protect the Little Poland Lowlands, in which Kraków lies, from the colder air of the north.
To the north the Staropolski (“Old Polish”) Basin, situated in the foothills of the Świętokrzyskie Mountains, has a long history of industrial production.
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The Pomeranian (Pomorska) Bay in the west and the Vistula (Wisła) River forms a large delta.
Sandbars, on which the winds have created large dunes, line much of the coast, separating the coastal lakes and lagoons from the sea.
In the southern part of the country, by contrast, older and more diverse geologic formations are exposed.
The mountainous arc of the Carpathians, dating from the mountain-building Paleogene and Neogene periods (from about 65 to 2.6 million years ago), dominates the topography.
The third zone consists of the central lowlands, whose minimal relief was created by streams issuing from the retreating glaciers.Tags: Adult Dating, affair dating, sex dating