uszyca

navigate by keyword : nature reflection tree autumn river leaf morning lake landscape water wilderness mountain forest plant sunlight flower reservoir pond quarry kamyki uszyca silesian voivodeship gluszyca this turquoise located altitude 585 above sea level hidden among rust colored eastern slopes ostoja massif suche mountains covered trees former melaphyre melafir rock characterized durability hardness abrasion resistance making ideal material example railway ballast mining works rna carried germans during after war closed exploitation area completed excavation flooded overgrown pines spruces beeches

PTTK shelter andrzejowka on the three valleys pass in the suche mountains Royalty Free Stock Photo
viewing platform on the small maly gomolnik suche mountains Royalty Free Stock Photo
viewing platform on the small maly gomolnik suche mountains Royalty Free Stock Photo
foggy landscape of Lower Silesia, the gluszyca area Royalty Free Stock Photo
foggy landscape of Lower Silesia, the gluszyca area Royalty Free Stock Photo
   
   
morning at the quarry kamyki, gluszyca, silesian voivodeship
foggy landscape of Lower Silesia, the gluszyca area Royalty Free Stock Photo
old quarry kamyki , gluszyca, lower silesian voivodeship Royalty Free Stock Photo
   
   
old quarry kamyki , gluszyca, lower silesian voivodeship Royalty Free Stock Photo
old quarry kamyki , gluszyca, lower silesian voivodeship Royalty Free Stock Photo
old quarry kamyki , gluszyca, lower silesian voivodeship Royalty Free Stock Photo
This turquoise reservoir, located at an altitude of 585 m above sea level, hidden among the rust-colored eastern slopes of the Ostoja massif in the Suche Mountains, covered with trees, is a former melaphyre quarry. Melafir is a rock characterized by durability, hardness and abrasion resistance, making it an ideal material used, for example, as railway ballast. Mining works in G?uszyca Górna were carried out by the Germans during and after the war. The quarry in G?uszyca has been closed since the 1970s. After the exploitation of the area was completed, the excavation was flooded with water. Over time, the slopes were overgrown with pines, spruces and beeches.


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