DUNAJEC RIVER AND PIENINY MOUNTAINSDUNAJEC RIVER AND PIENINY MOUNTAINS

Gimnazjum nr 1 im. Jana Pawła IIGimnazjum nr 1 im. Jana Pawła II

DUNAJEC RIVER IN SPRINGDUNAJEC RIVER IN SPRING

ABOUT DUNAJEC RIVERABOUT DUNAJEC RIVER

The Dunajec is a river running through southern Poland. It is the right tributary of the Vistula River. It begins in Nowy Targ at the junction of two short mountain rivers, Czarny Dunajec and Biały Dunajec (Black and White Dunajec). Dunajec forms a border between Poland and Slovakia for 27 kilometers in the Pieniny Środkowe (Slovak: Centrálne Pieniny) range, east of the Czorsztyn reservoir. It is the only river taking waters from the Slovak territory to the Baltic Sea.

The Dunajec is a river running through southern Poland. It is the right tributary of the Vistula River. It begins in Nowy Targ at the junction of two short mountain rivers, Czarny Dunajec and Biały Dunajec (Black and White Dunajec). Dunajec forms a border between Poland and Slovakia for 27 kilometers in the Pieniny Środkowe (Slovak: Centrálne Pieniny) range, east of the Czorsztyn reservoir. It is the only river taking waters from the Slovak territory to the Baltic Sea.

DUNAJEC RIVER IN SUMMERDUNAJEC RIVER IN SUMMER

ABOUT DUNAJEC RIVERABOUT DUNAJEC RIVER

The Dunajec is 274 kilometers long, running through southern Poland for 247 kilometers, which makes it Poland's fourteenth longest river. It has a basin area of 6,804 square kilometres (4,852 in Poland, and 1,952 in Slovakia). On the Slovak/Polish border, it flows through the Zamagurie region, with attractions such as the Dunajec River Gorge, the Trzy Korony massif with a 500 metres (1,600 ft) precipice, Červený Kláštor, and two Pieniny castles in Czorsztyn and Niedzica.

The Dunajec is 274 kilometers long, running through southern Poland for 247 kilometers, which makes it Poland's fourteenth longest river. It has a basin area of 6,804 square kilometres (4,852 in Poland, and 1,952 in Slovakia). On the Slovak/Polish border, it flows through the Zamagurie region, with attractions such as the Dunajec River Gorge, the Trzy Korony massif with a 500 metres (1,600 ft) precipice, Červený Kláštor, and two Pieniny castles in Czorsztyn and Niedzica.

HOW DOES THE RIVER FLOW?HOW DOES THE RIVER FLOW?

PIENINY MOUNTAINS IN SUMMERPIENINY MOUNTAINS IN SUMMER

ABOUT PIENINY MOUNTAINSABOUT PIENINY MOUNTAINS

Pieniny is a mountain range in the south of Poland and the north of Slovakia.

The Pieniny mountain range is divided into three parts – Pieniny Spiskie (Slovak: Spišské Pieniny) and Pieniny Właściwe (Slovak: Centrálne Pieniny) in Poland; and, Malé Pieniny (English: Lesser or Little Pieniny; Polish: Małe Pieniny) in Poland and Slovakia. The Pieniny mountains consist mainly of the limestone and dolomite rock strata. The most famous peak, Trzy Korony (Three Crowns), is 982 meters high. It is also the summit of the Three Crowns Massif. Pieniny’s highest peak – Wysoka (Polish); Vysoké Skalky (Slovak) – reaches 1,050 meters above sea level.

Pieniny is a mountain range in the south of Poland and the north of Slovakia.

The Pieniny mountain range is divided into three parts – Pieniny Spiskie (Slovak: Spišské Pieniny) and Pieniny Właściwe (Slovak: Centrálne Pieniny) in Poland; and, Malé Pieniny (English: Lesser or Little Pieniny; Polish: Małe Pieniny) in Poland and Slovakia. The Pieniny mountains consist mainly of the limestone and dolomite rock strata. The most famous peak, Trzy Korony (Three Crowns), is 982 meters high. It is also the summit of the Three Crowns Massif. Pieniny’s highest peak – Wysoka (Polish); Vysoké Skalky (Slovak) – reaches 1,050 meters above sea level.

PIENINY IN AUTUMN PIENINY IN AUTUMN

ABOUT PIENINY MOUNTAINSABOUT PIENINY MOUNTAINS

Pieniny mountains formed at the bottom of the sea in several geological epochs. They were folded and raised in Upper Cretaceous. At the beginning of the Paleogene geologic period a second wave of tectonic movements took place causing a further shift. The third wave of movements during the Paleogene and Neogene resulted in a more complex tectonic structure. At the same time erosion resulted in stripping of the outer mantle rocks and further modeling of terrain. Peaks were built from weather resistant Jurassic rocks, mainly limestone.

Pieniny mountains formed at the bottom of the sea in several geological epochs. They were folded and raised in Upper Cretaceous. At the beginning of the Paleogene geologic period a second wave of tectonic movements took place causing a further shift. The third wave of movements during the Paleogene and Neogene resulted in a more complex tectonic structure. At the same time erosion resulted in stripping of the outer mantle rocks and further modeling of terrain. Peaks were built from weather resistant Jurassic rocks, mainly limestone.

THE THREE CROWNS IN PIENINY MOUNTAINSTHE THREE CROWNS IN PIENINY MOUNTAINS

THANK YOU VERY MUCH FOR YOUR ATTENTION

THANK YOU VERY MUCH FOR YOUR ATTENTION