🇵🇱 Wakacje w Polsce - Iwonicz Zdrój 2025. Ciekawe miejsca do odkrycia na Podkarpaciu.

Iwonicz, one of the oldest spa towns in Poland, is located in the Iwonka stream valley. The first mention of the healing properties of the local springs comes from Wojciech Oczko's "Cieplice" published in 1578, a book by Stefan Batory's court physician Wojciech Oczko. In the 17th century, the "miraculous" properties of the Iwonicz waters were known throughout the country. Prominent physicians treating royal families took an interest in them. Its history dates back to the 14th century. The first known owners of Iwonicz were members of the Iwanicki family. The Załuscki family, who became owners of the village in 1799, contributed significantly to the development of Iwonicz and were also the founders of the spa. In the second half of the 19th century, an eclectic manor house was built as the family residence. The exploitation of oil deposits in the late 19th century contributed to the development of the town. The interwar period brought further development to Iwonicz, driven by the spa's operations and increased oil production. After World War II and the confiscation of the property from the Załuski family, the palace fell into disrepair. The postwar period saw the rapid development of the entire spa, with numerous sanatoriums established, a significant expansion of the treatment options, and the expansion of the sports and recreational infrastructure (swimming pool, ski jumps, tennis courts, walking trails, etc.). Recording: June 2025 Music: YouTube Audio Library All recordings and the film were produced by me. Unauthorized use is prohibited. The film is copyrighted and belongs to the website Mro.Channel.pl All recordings and the film are produced by me. Unauthorized use is not allowed The video is protected by copyright and belongs to the Mro.Channel.pl website The "Olza" rock face, rising in the Wisłok Valley (near Rudawka Rymanowska), is the largest outcrop of menilite schists in the Polish Carpathians. The Olza face is named after Polish geologist Stanisław Dżułyński. The cliff is over 30 meters high. The outcrop was formed by deep erosion following a river change. The characteristic, layered rock formation was created by the deposition of gravels, sands, and clays in the deep Tethys Ocean in the Lower Oligocene, approximately 35 million years ago. In winter, icefalls form on the high rocks. Since 2022, this has been the site of the Olza Nature Reserve. The tree stand on the summit, with a high degree of natural species composition, has also been protected; These are mainly fertile Carpathian beech forests. The Wisłok River, flowing over the rocky bottom, adds to the picturesque wall's charm. It creates small but spectacular cascades here.