Karlsruhe District
CalwDobelVolzemer Stein
Karlsruhe District
CalwDobelVolzemer Stein
Highlight • Naturmonument
Volzemer Stein
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The Volzemer Stein is a captivating natural monument nestled in the northern Black Forest of Germany, near the municipality of Dobel. Rising to an elevation of 701 metres, this unique site is renowned for its impressive rock formations, often referred to as the "Volzemer Steine." It forms part of the "Grindenschwarzwald und Enzhöhen" natural region, characterized by its distinctive red sandstone ridges and dense forests.
Visitors are consistently drawn to the Volzemer Stein for its remarkable geological features and the…
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4. december 2016
Vandring
•23. februar 2020
Vandring
The quartz-bearing stones of the middle federal sandstone are also called "champanger stones". They are particularly good for making millstones.
•10. juli 2021
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Højdemeter 700 m
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fredag 20. marts
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27 %
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What are the key geological features of the Volzemer Stein?
The Volzemer Stein is primarily composed of Middle Bunter Sandstone, forming a distinctive 'sea of rocks' or blockfield. The main formations are the Großer Volzemer Stein, which is about 100 meters wide and up to 10 meters high, and the Kleiner Volzemer Stein. These rocks contain quartz crystals, causing them to glisten and earning them historical nicknames like 'Kristall-Sandsteine' and 'Champagnersteine'. The area also exhibits a unique microclimate due to the rock formations.
Are there any specific viewpoints or hidden natural features at Volzemer Stein?
While the entire area around the Großer Volzemer Stein offers impressive views of the rock formations themselves, the Kleiner Volzemer Stein is a slightly less prominent but equally interesting feature located a short distance off the main path. Attentive hikers can also spot unfinished millstones and well troughs, remnants from when the durable sandstone was quarried here, adding a historical layer to the natural beauty.
What is the best way to get to Volzemer Stein by public transport?
The Volzemer Stein is situated near Dobel, which can be accessed by bus services. From larger towns like Pforzheim or Bad Herrenalb, you can typically find bus connections to Dobel. From Dobel, the natural monument is accessible via well-marked hiking trails, including the Westweg. It's advisable to check current bus schedules as they can vary seasonally.
Is the Volzemer Stein area suitable for a winter hike or other winter activities?
Yes, the Dobel high plateau where the Volzemer Stein is located is popular for winter activities. While the rock formations themselves are impressive year-round, the area transforms into a destination for cross-country skiing and snowshoeing during winter. Hikers should be prepared for snow and potentially icy conditions on trails during this season.
How long does it typically take to hike around the Volzemer Stein?
The time required to explore the Volzemer Stein depends on your chosen route. Many popular trails, such as sections of the Westweg or the Engel-Weg-Dobel, pass directly through or by the monument. A dedicated exploration of the rock formations themselves might take 30-60 minutes, but combining it with a circular hike in the surrounding forest could easily extend to 2-4 hours or more, depending on the trail length and your pace.
Are there any family-friendly trails or activities specifically designed for children at Volzemer Stein?
Yes, the area is considered family-friendly. The GeoTour Dobel offers an interactive way for families to learn about the geology of the area through engaging tasks and research questions. Additionally, the Annis-Abenteuerweg (Anni's Adventure Trail) is designed with children in mind, providing an enjoyable and educational experience through the forest and past the natural monument.
Are dogs allowed on the trails around Volzemer Stein?
Yes, the trails around Volzemer Stein are generally dog-friendly. Many visitors enjoy bringing their dogs along for walks. However, it's always recommended to keep dogs on a leash, especially in natural monument areas and when encountering other hikers or wildlife. Please also ensure you clean up after your pet.
What is the historical significance of the Volzemer Stein beyond its natural formation?
Before its designation as a natural monument in 1949, the local population utilized the durable Bunter Sandstone of the Volzemer Stein as a quarry. They extracted rock to produce millstones and well troughs. If you look closely, you can still observe unfinished workpieces and blanks for these items scattered in the area, offering a tangible link to the region's past industries.
What kind of terrain and elevation changes can hikers expect on trails around Volzemer Stein?
The terrain around Volzemer Stein involves exploring large sandstone blocks, some up to 10 meters high, so sturdy footwear is recommended for navigating the rocky paths. While the monument itself is at an elevation of around 701 meters, the surrounding trails on the Dobel high plateau generally feature moderate elevation changes, making them accessible for a range of hiking abilities. Expect forest paths, some rocky sections, and well-maintained trails.
Are there any cafes, pubs, or accommodation options near Volzemer Stein?
The Volzemer Stein is located near the municipality of Dobel. In Dobel, you can find various amenities including cafes, restaurants, and guesthouses or hotels for accommodation. It's a popular tourist area, so options are available, especially in the village center. It's a good idea to check opening hours, especially during off-peak seasons.
How crowded does Volzemer Stein get on weekends or during peak season?
As a popular natural monument and a stop on well-known hiking trails like the Westweg, Volzemer Stein can attract a fair number of visitors, especially on pleasant weekends and during peak hiking seasons (spring to autumn). While it might not feel overly crowded due to the expansive nature of the forest, you can expect more people on the main trails and around the rock formations during these times. Arriving earlier in the day can help avoid the busiest periods.