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The Czech Republic is a landlocked country in Central Europe.It is bordered by Germany to the west, Austria to the south, Slovakia to the east and Poland to the north. It consists mostly of low hills and plateaus surrounded along the borders by low mountains.
Satellite image of Europe by night 1916 physical map of Europe Topography of Europe. Some geographical texts refer to a Eurasian continent given that Europe is not surrounded by sea and its southeastern border has always been variously defined for centuries. In terms of shape, Europe is a collection of connected peninsulas and nearby
Pre-Triassic development of the Czech West Carphathians is related to the Brunovistulian. The pre-Devonian basement and the sedimentary cover of the Brunovistulian underlie the Mesozoic and Cenozoic formations in the West Carpathians.
The Czech Republic, [c] [12] also known as Czechia, [d] [13] and historically known as Bohemia, [14] is a landlocked country in Central Europe.The country is bordered by Austria to the south, Germany to the west, Poland to the northeast, and Slovakia to the southeast. [15]
Czech Republic geography-related lists (3 C, 8 P) B. Bohemia (18 C, 27 P) Borders of the Czech Republic (6 C, 4 P) C. Czech Silesia (2 C, 26 P) E. Ecoregions of the ...
Mountains and hills of the Czech Republic (4 C, 102 P) R. Rock formations of the Czech Republic (16 P) S. Sinkholes of the Czech Republic (2 P) V. Valleys of the ...
The corresponding watershed tripoint with a marker for symbolic "roof of Europe" (50°9'27"N 16°47'27"E) is located at Czech-Polish border on Mt. Klepáč near Dolní Morava in Králický Sněžník Mountains. The catchment area of the Elbe down to Czech-German border in Hřensko/Schöna covers 51,394 square kilometres (19,843 sq mi). This ...
It is a large massif stretching over most of the Czech Republic, eastern Germany, southern Poland and northern Austria. The massif encompasses a number of mittelgebirges and consists of crystalline rocks, which are older than the Permian (more than 300 million years old) and therefore deformed during the Variscan Orogeny .