Europe Geography

Europe has no single defining landform — it's better understood as a set of bands running roughly north to south. The North European Plain, the continent's most densely populated region, stretches from western France through Germany and Poland into Russia, with little elevation change across enormous distances. South of it, a belt of central uplands rises into the Alps, Europe's highest and most extensive mountain range, running through France, Switzerland, Italy, and Austria, with the Pyrenees forming a second, smaller barrier between France and Spain.

To the north, the Scandinavian Peninsula is shaped by glaciation rather than tectonics — fjords, thin soils, and exposed granite rather than plains. To the east, the Ural Mountains are the conventional line where Europe is considered to end and Asia begins — a political and cultural boundary more than a dramatic physical one.

Water shapes Europe as much as elevation does. The Rhine and Danube are the continent's two major rivers, both historically central to trade and settlement, and Europe's coastline is unusually long relative to its land area — few points on the continent sit far from the sea, which has shaped everything from climate to where its major cities were built.