Karawanks in the context of "Jesenice"

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⭐ Core Definition: Karawanks

The Karawanks or Karavankas or Karavanks (Slovene: Karavanke; German: Karawanken, German pronunciation: [kaʁaˈvaŋkŋ̍] ) are a mountain range of the Southern Limestone Alps on the border between Slovenia to the south and Austria to the north. With a total length of 120 kilometres (75 mi) in an east–west direction, the Karawanks chain is one of the longest ranges in Europe. It is traversed by important trade routes and has a great tourist significance. Geographically and geologically, it is divided into the higher Western Karawanks and the lower-lying Eastern Karawanks. It is traversed by the Periadriatic Seam, separating the Apulian tectonic plate from the Eurasian Plate.

Near the summit of the Dreiländereck (1,508 m) is the tripoint of the three countries: Austria, Italy and Slovenia.

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👉 Karawanks in the context of Jesenice

Jesenice (Slovene: [jɛsɛˈnìːtsɛ] , German: Aßling) is the tenth-largest town in Slovenia, located in the traditional province of Upper Carniola. It is the seat of the Municipality of Jesenice spanning the southern side of the Karawanks, along Slovenia's border with Austria to the north. Renowned as a mining town, its ironworks and metallurgy industries being the driving force of the town's historical development.

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Karawanks in the context of Mountain chain

A mountain chain is a row of high mountain summits, a linear sequence of interconnected or related mountains, or a contiguous ridge of mountains within a larger mountain range. The term is also used for elongated fold mountains with several parallel chains ("chain mountains").

While in mountain ranges, the term mountain chain is common, in hill ranges a sequence of hills tends to be referred to a ridge or hill chain.

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Karawanks in the context of Upper Sava Valley

The Upper Sava Valley (Slovene: Zgornjesavska dolina) is an alpine valley in the Upper Carniola region of Slovenia. The Sava Dolinka River flows along it. It begins in Rateče at an elevation of 870 m and ends at Moste at 560 m. It is the geographical border between the Julian Alps and the Karawanks. It was created on a tectonic fault that runs down the middle of the valley. Its geomorphological forms are a result of the actions of the river and glaciers. A number of smaller valleys lead into it from both sides.

The largest settlements in the valley are Kranjska Gora and Jesenice. Some of the traditional and modern settlements are located on active alluvial fans that may cause a threat of the modelled torrents and debris flows.

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