ドリーニーボブルのおすすめ登山＆山歩きルート

definitely worth it 😃

The rock formations are located on the border between the Czech Republic and Poland. They are called "Svinské kameny" in Czech, "Trzy Świnki" in Polish, and "Sausteine" in German.

It's really boiling there :)

The Snow Pits (Polish: Śnieżne Kotły) in the Giant Mountains are an impressive natural wonder that delights both hikers and nature lovers. They consist of two glacial cirques, the Great Snow Pit (Wielki Kocioł Śnieżny) and the Small Snow Pit (Mały Kocioł Śnieżny), located at an altitude of approximately 1,200 to 1,300 meters. These steep and deep rock faces were formed by glaciers and provide a breathtaking backdrop. The walls of the Snow Pits drop almost vertically to a height of up to 100 meters, making them one of the most spectacular places in the Giant Mountains. Rare flora and fauna: Due to the special microclimate, plant species normally found only in arctic regions thrive here. On the ridge above the Snow Pits stands the historic Snow Pit Hut (Polish: Schronisko na Śnieżnych Kotłach), a building that formerly served as a meteorological station.

The Pig Stones, in Polish Trzy Świnki and in Czech Svinské kameny, are a distinctive granite rock formation in the western part of the Silesian Ridge of the Giant Mountains, on the border between Poland and the Czech Republic. The Pig Stones are located in the immediate vicinity of the ridge path, about 400 meters northwest of the Twarożnik (Cheese Cliff). A green marked hiking trail leads from there to the Horse Headstones (Końskie Łby) and around the Reifträger Peak. The rock formation was created by natural weathering processes of the granite, which took place over millions of years and created the characteristic shapes of the Pig Stones. The name "Pig Stones" derives from the rocks' resemblance to three pigs lying next to each other. There are various local legends that explain the formation and naming of the rock formation. The Pig Stones offer impressive views of the surrounding landscape and are a worthwhile destination for hikes in the Giant Mountains.

Ostrzyca Proboszczowicka is the highest peak of the Kaczawskie Foothills. In reality, it is a volcanic neck, a fragment of a volcano chimney that was active about 20-25 million years ago, prepared by erosion. The elevation, rising to a height of 501 m above sea level above the flat area, is made of basanite, a volcanic rock poor in silica. In the top part, you can admire the largest rock fields in the Sudetes and a columnar joint occurring in basanites.

A beautiful waterfall and a great hiking trail along the river - in season it's worth getting there early to get a parking space and some peace and quiet. There's an entrance fee for the hiking trail!

Beautiful rock formation right on the ridge path, but reminds me more of a camel.