Poprad Landscape Park
A wooded valley on the Slovak border where mineral springs made a line of spa towns, and where the river runs north.
Saved in this browser only - no account, nothing sent anywhere. See your map
The Poprad is unusual: it rises in Slovakia on the southern side of the Tatras and then cuts north through the Carpathian ridge into Poland, which is the wrong way for a river in this region and gives the valley its shape - a wooded gorge with the border running through it and a railway threading along the bank. The park covers about fifty thousand hectares of that country, mostly beech and fir, and what made the valley prosperous is underground: carbonated mineral waters come up along faults here in quantity, and the spa towns of Krynica, Muszyna, Zegiestow and Piwniczna were built on them from the nineteenth century, with pump rooms, promenades and wooden villas. Several springs are free to drink from and the waters are heavily mineralised and taste of it. Walking is on gentle wooded ridges. The Lemko villages of the valley have wooden churches, several of them UNESCO-listed in the wider group.
What you actually see
- A river running north - the Poprad cutting through the Carpathian ridge the wrong way.
- Carbonated springs - mineral waters rising along faults, free to drink at the pump rooms.
- Nineteenth-century spas - Krynica, Muszyna and Zegiestow with villas and promenades.
- Lemko wooden churches - in the valley villages, several UNESCO-listed.
When to go
May to October. Two days.
Honest expectations
The mineral waters are strongly flavoured and not to everyone's taste. Spa towns are busy in summer and prices rise. Walking here is gentle rather than dramatic. Some wooden churches are locked and need a keyholder.
Nearby
Krynica-Zdroj is east; Nowy Sacz is north down the valley.
What to pack for Poprad Landscape Park
Chosen from what this place is for. Tap a kit for the full checklist.
Opening times, ticket prices and seasonal closures change - check the official source before you go: official site.