アルテンシュタイクの天然記念物・トップ20

via the Felsensteig you come to the Stubenfelsen and can then cross it

Like most raised bogs, the bogs on the Kaltenbronn were formed at the end of the last ice age more than 10,000 years ago. The melting of massive ice sheets created depressions where water could not drain away. The high rainfall that prevails on the Kaltenbronn caused the landscape to become swampy. This allowed lush vegetation to develop on the nutrient-poor sandstone subsoil. Dying plants, whose plant remains did not completely decompose in the oversaturated soil, were overgrown by new plants. This process caused a thick layer of peat to develop over the course of thousands of years. The plants gradually lost contact with the groundwater-bearing soil layers due to the peat layer and could no longer be supplied with sufficient nutrient-rich water. The nutrient-poor rainwater led to a change in the existing vegetation, in which only undemanding plants such as cotton grass, cranberry, rosemary heath, round-leaved sundew and the few-flowered sedge could survive. In drier places, heather, cloudberry, crowberry and leaf mosses also occur. Source: https://www.schwarzwald-informationen.de/wildsee-hornsee-kaltenbronn.html

The Kaltenbronn high moor with the two lakes is worth seeing. You should definitely take your time.

The Stubenfelsen is a mighty group of rocks consisting of several large rocks. The rocks are stratigraphically placed in the upper scree horizon of the Middle Buntsandstein. The rocks show overhangs and cave-like niches. Very good cross bedding cycles have been developed on the walls. Source: https://www.touren-schwarzwald.info/de/punkt/naturdenkmal/stubenfelsen/7901961/

Please take the exit in good time!

Very nice environment here!

Nice hike but please, please put on non-slip shoes.

Very nice, adventurous hike through this gorge with its small waterfalls ... surefootedness absolutely necessary