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Pieniny Spiskie

Pieniny Spiskie often called Hombarki, are situated in southern Poland, in the Central Carpathians, the lowest part of the Pieniny. Administrative terms, almost all Pieniny Spiskie located in an area municipality Łapsze Low, outside the Pieniny National ParkOnly a small patch of north-east (Green Rocks) was included in the area of the park.

Lie between the Dunajec River and the watershed between the Kramnicą Białki a Obłazowa. The length of the whole band is 14 km, width of 3-4 km, the relative height of the Reservoir is 350 m Czorsztyn Zar. The highest peak is 879 m. The heat main part of the Pieniny Spišské creates the parallel to the shaft from Niedzica Dursztyn, which in turn makes the climaxes: Cisówka 777 m, 725 m Mountain dyes, Zar, 879 m, 782 m Gajna rock, 733 m Mountain Jurgowska, Pine Top 748 m. In the middle of its length, this shaft is divided Pass span. Topografowie stand still Cisówek group divided into several small valleys and ridges domed tops. In addition, there is still a few small hills and rocks, including They are: Hombark niedzicki and Łapszański, Bald Hill 739 m, rocks Dursztyńskie, Kramnica, Green Rocks. In scientific studies Spiskie Pieniny are still divided into different sub-units. And so, for example, distinguishes between the lock Skalice Spiskie Niedzica a Dursztyn Skalice Nowy Targ and the Dursztyn after Szaflary and Old Clever.

By the local population these mountains were called Hombarkami and this is probably the name of German origin. In the area of Pieniny is a lot of geographical names of German origin, at some point in our history, many feel was the German settlement.Kazimierz Sosnowski introduced Pieniny niedzicki name, but did not catch on. On the German and Austrian charts figured wrong name Branisko range. Pieniny Spiskie name only introduced after World War II and it is not logical, because does not include the Slovak part of the Pieniny lying in the Spis region.

The peaks are small relative height, but the topography is quite varied. Main Ridge in the vicinity of Caloris Basin is a rocky, narrow and steep. Slopes are cut by valleys and flowing streams of the bottom in some places are bare trough carved in the rock. Detail the geology of the area developed after 1951 Chris Birkenmajer. He highlighted a series of Branisko, Pieniny and czorsztyńską. Pieniny Spiskie are built of limestone immersed in the Carpathian flysch. Supreme Caloris Basin shaft is made of hard limestone and radiolarytów rogowcowych. The area is heavily irrigated, there is here about 130 sources, mostly at an altitude of 500-700 m above sea level Entire Pieniny Spiskie are in the Dunajec basin. Streams are mainly the course of Meridian and fed rampart, Łapszankę, or directly Niedziczankę Czorsztyn tank. Slopes are covered with forest, gentler used for agricultural purposes.

In terms of historical and ethnographic, this area is part of the Spis region. It is inhabited by people of Polish origin Spisz and Slovak. Survived much wooden monuments of folk architecture, and a few wooden churches belonging to the leading sites around the Polish sub-Tatra region. There are numerous roadside shrines. The most famous monument of the region is located on the eastern edge of the Pieniny Castle Spišské Niedzica.

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