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Bloke Plateau

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According to the geographer Anton Melik, the Bloke Plateau is a remnant of a Pliocene peneplain in the middle of the rejuvenated terrain. Poorly permeable karst limestone and Triassic dolomite (in the northern part of the plateau) conditioned the formation of typical surface watercourses (Bloščica Creek and Blatnica Creek), which are bounded by wet grasslands and minerotrophic fens. Lake Bloke (
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The Bloke Plateau measures approximately 15 kilometers (9.3 mi) long and 10 kilometers (6.2 mi) wide. It ranges in elevation between 700 meters (2,300 ft) and 800 meters (2,600 ft). Together with the Rakitna tectonic block, the plateau is delineated by two distinct Dinaric faults.
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Culturally, the Bloke Plateau is known as the place where skiing originated in Slovenia, and a cross-country skiing competition is held there every year. The Bloke Plateau has long been crisscrossed by trade routes connecting the interior of
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The Bloke Plateau is accessible from several directions, especially from the Ljubljana and Littoral directions via the
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The Bloke Plateau was first mentioned in written documents in 1260, and its central settlement of
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Jerić, Marjeta. 2006. Bloška planota in Vidovski hribi. Drago Kladnik (ed.),
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in 1341. The territory was settled in the first millennium BC by the
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Index


Slovene
Slovenia
Inner Carniola
Slovene
Volčje
Lake Cerknica
Slovene
Municipality of Bloke
A1 Freeway
Unec
Cerknica
Ribnica
Sodražica
Cross Cave
Lake Cerknica
Snežnik Castle
Rak Škocjan Park
Nova Vas
Iapydes
Aquileia
Kvarner Gulf
Pannonian Basin
Benete
Carniola
Lower Carniola
Inner Carniola
Croatia
Bloke Plateau on Geopedia

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