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Geological Formation

Podhale

Structural and Tectonic Formations

Podhale, sometimes called the Polish Highlands, is the southernmost region of Poland, lying in the foothills of the Tatra Mountains within the Carpathians in Lesser Poland Voivodeship. It is the best known Goral ethnic territory, home to extensive peat bogs and alluvial fans, and includes the towns of Nowy Targ, its historic capital, Zakopane and Czarny Dunajec. The region keeps a living regional dialect and folk culture distinct from other Polish traditions. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

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Caused By

Erosion, Processes

Wikidata P31 formation-type mapped to formative process Erosion via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Podhale

In Discipline

Wikidata P31 formation-type mapped to discipline Geomorphology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Podhale
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Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Podhale
Sources
Podhale (Wikipedia)
Lead section
Quote, Lead section
Podhale (Polish pronunciation: [pɔtˈxalɛ] ; Podhale dialect: Podhole lit. 'below the mountain pastures'), sometimes referred to as the Polish Highlands, is Poland's southernmost region.
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Wikidata: Podhale
Wikidata Q115155, class allow-list match (w-wdresolver-0926)View the Source
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