No weather data
0.0 /5
Number of ratings: 0
Address: Pitoniówka 12 , Kościelisko
We cordially invite you to relax in Gora Hawira, where in a nice, family atmosphere you can spend time and relax from the hustle and bustle of the big city. We offer warmly furnished 2,3,4-bed rooms with bathrooms equipped with RTV equipment. We offer a Jacuzzi, sauna, billiard room, fireplace room, conference and cinema room and observation deck.
No results
Szymoszkowa Glade is a ski station, whose undeniable advantage is the beautiful views of the Tatra Mountains. Two cable cars are available for skiers and snowboarders. A large six-person train running to the top of...
It is located on the top of Gubałówka, 60m from the top station of the PKL funicular railway in Zakopane. An ideal place for active holidays throughout the year. Is one of the largest rope parks in Poland. It has 7...
The valley probably provides the most attractions from all Tatra valleys. The valley tour begins in the town of Kir. It is a general valley, it stretches from the foot of the Tatra Mountains to their ridge. It is about...
The total length of the Kościeliski Stream within the Tatra Mountains is about 8.5 km. Because a significant part of the rocks flowing over the stream is susceptible to karst processes, it has definitely less inflows...
Szymoszkowa Glade is a ski station, whose undeniable advantage is the beautiful views of the Tatra Mountains. Two cable cars are available for skiers and snowboarders. A large six-person train running to the top of...
It is located on the top of Gubałówka, 60m from the top station of the PKL funicular railway in Zakopane. An ideal place for active holidays throughout the year. Is one of the largest rope parks in Poland. It has 7...
The valley probably provides the most attractions from all Tatra valleys. The valley tour begins in the town of Kir. It is a general valley, it stretches from the foot of the Tatra Mountains to their ridge. It is about...
The total length of the Kościeliski Stream within the Tatra Mountains is about 8.5 km. Because a significant part of the rocks flowing over the stream is susceptible to karst processes, it has definitely less inflows...