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Świętokrzyskie Mountains
The Świętokrzyskie Mountains (Polish: Góry Świętokrzyskie, IPA: [ˈɡurɨ ɕfjɛntɔˈkʂɨskʲɛ] ⓘ), often anglicized to Holy Cross Mountains, are a mountain range in central Poland, near the city of Kielce.
The mountain range comprises several lesser ranges, the highest of which is Łysogóry (literally "Bald Mountains").
The two highest peaks are Łysica, 614 m (2014.44 ft), and Łysa Góra, 594 m (1948.81 ft).
Together with the Jura Krakowsko-Częstochowska and some other regions, the mountains form a region called the Lesser-Poland Upland (Wyżyna Małopolska). Geologically speaking, the Holy Cross Mountains possess also a margin which extends further than the mountains themselves; the Owadów–Brzezinki palaeontological site is situated in the margin of the Holy Cross Mountains, but not in the mountains themselves.
They cover an area of 1684 km2 (650 mi2).
The approximate location is 50°53′N 20°55′E / 50.883°N 20.917°E.
The Świętokrzyskie Mountains are one of the oldest mountain ranges in Europe.[citation needed] They were formed during the Caledonian orogeny of the Silurian period and then rejuvenated in the Hercynian orogeny of the Late Carboniferous period.
The region was once on the southern coast of the ancient supercontinent of Laurasia. The oldest known evidence of tetrapods comes from 395-million-year old fossil footprints found in Zachełmie. The rocks were formed from a marine tidal flat or lagoon.
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Świętokrzyskie Mountains
The Świętokrzyskie Mountains (Polish: Góry Świętokrzyskie, IPA: [ˈɡurɨ ɕfjɛntɔˈkʂɨskʲɛ] ⓘ), often anglicized to Holy Cross Mountains, are a mountain range in central Poland, near the city of Kielce.
The mountain range comprises several lesser ranges, the highest of which is Łysogóry (literally "Bald Mountains").
The two highest peaks are Łysica, 614 m (2014.44 ft), and Łysa Góra, 594 m (1948.81 ft).
Together with the Jura Krakowsko-Częstochowska and some other regions, the mountains form a region called the Lesser-Poland Upland (Wyżyna Małopolska). Geologically speaking, the Holy Cross Mountains possess also a margin which extends further than the mountains themselves; the Owadów–Brzezinki palaeontological site is situated in the margin of the Holy Cross Mountains, but not in the mountains themselves.
They cover an area of 1684 km2 (650 mi2).
The approximate location is 50°53′N 20°55′E / 50.883°N 20.917°E.
The Świętokrzyskie Mountains are one of the oldest mountain ranges in Europe.[citation needed] They were formed during the Caledonian orogeny of the Silurian period and then rejuvenated in the Hercynian orogeny of the Late Carboniferous period.
The region was once on the southern coast of the ancient supercontinent of Laurasia. The oldest known evidence of tetrapods comes from 395-million-year old fossil footprints found in Zachełmie. The rocks were formed from a marine tidal flat or lagoon.