Caves around Beratzhausen offer a diverse range of geological formations and historical sites within the Upper Palatinate region. The area features natural karst caves formed by water dissolving limestone, alongside unique cave dwellings and historical cave structures. These natural landmarks provide insights into both geological processes and human history, with some formations dating back to the Jurassic period. The landscape around Beratzhausen is characterized by its limestone cliffs and river valleys, providing ideal conditions for cave development.
Last updated: June 27, 2026
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The Höhlenburg Loch > a geotope The Höhlenburg Loch is one of only two cave castles in Bavaria (the second is in Stein an der Traun in Upper Bavaria). The lower, flatter part of the castle complex lies in slab dolomites belonging to the Velburg Horizon. The steep wall, at the base of which the (residential) caves appear, is formed by mass dolomites of the Middle Franconian Alb Formation. Bavarian State Office for the Environment (LfU). https://www.umweltatlas.bayern.de/standortauskunft/rest/reporting/sb_geotope/generate?additionallayerfieldvalue=375A026
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Beautiful rock formations in the forest
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Beautiful view back over the Vils
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Rock formations are now majestically visible in March. They soon disappear into the sea of leaves and are then almost invisible again—unfortunately!
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Loch Castle Ruins Loch Castle was probably built by the Rammelsteiners, the lords of a nearby estate. They were first mentioned in the 12th century and were ministerials of the burgraves of Regensburg and later of the Bavarian dukes. Their castle in Loch was probably only built after 1300 to protect an iron hammer mill in the Laber Valley. A "Hugo vom Loch" is mentioned in a fief book of the Regensburg monastery of St. Emmeram at this time. Jakob Rammelsteiner vom Loch was district judge in Sulzbach in 1388 and court master to the Duke of Ingolstadt, Ludwig the Bearded, in 1413. His descendants Dietrich and Wolfgang took part in the knights' revolts of the Böckler and Löwler, but this did not cause any lasting damage to the family. After 1500, the lords of the castle also gained control of the Schönhofen and Eichhofen castles. When the last Rammelsteiner Sebastian died in 1556, the complex passed to his nephew Wolf Heinrich Sauerzapf in 1573 after long inheritance disputes. The Sauerzapf - a very successful family of hammer lords - gave up their seat in 1625 at the latest and resided in Schönhofen. In 1714, the last Sauerzapf Christoph bequeathed Loch Castle, already in ruins, to the Carthusian monastery of Prüll in Regensburg. The former Loch Castle, although it remained historically insignificant, offers many interesting features. The shape of the cave castle is extremely rare. The entrance was in the north, where a moat, still clearly visible today, separates the castle terrace. A gatehouse with a drawbridge can be clearly seen in the 1718 depiction, as can the residential buildings, which lean against the steep wall in the east in front of several cave rooms. At the southern end of the terrace stands the well-preserved keep, which is 23 meters high. It has 2 m thick walls, a toilet bay and large windows on the top floor. The structural design of the keep, which was built from roughly hewn rubble stone and was designed to be relatively comfortable with large windows and a toilet bay, clearly points to the 14th century. Clearly visible remains of built-in features have been preserved in the largest cave. It is surprising that such an uncomfortable and defensively unfavourable location was chosen for a castle in the late Middle Ages. It was extremely vulnerable to attack from the plateau above. The reason for the choice of location was probably solely the nearby hammer mill. Source: Excerpts from www.burgenseite.de
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ATTENTION: On the Etterzhausen JURA🦕Steig ascent to the robber's cave, a very special person, compared to whom even real robbers appear to be honorable merchants, has made nasty mistakes: 3 flats in 6 months, always in the same place, and today, while patching, he discovered a fresh thumbtack. See picture #82. Time to upgrade to tubeless! Always a flat ride! 🍀🚴🏿♂️😀
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Great trail again today, especially in combination with a detour to the plateau and subsequent technical downhill S2-S3.
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The castle is best seen from Eichhofen, as entering is forbidden and not possible due to the fence
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The region around Beratzhausen features natural karst caves, which are formed by water slowly dissolving limestone. You can also find unique historical cave dwellings and rare cave castles, showcasing both geological processes and human history.
The Robber's Cave is notable for its historical significance, potentially used by Celts and later as a strategic hideout due to its view of the Naab river. Another fascinating site is the House without a Roof (Kallmünz), a cave dwelling that has been inhabited for centuries, with records dating back to 1707.
Yes, the Osterhöhle (Easter Cave) is a prominent show cave in the region. It features extensive passages, dome-like expansions, and rich dripstone formations, including stalactites, stalagmites, and sinter basins. Guided tours are available, and visitors are provided with flashlights to explore its geological wonders.
The Robber's Cave is publicly accessible with no entry fees or specific opening times, making it a good option for families. It's a large cave hall where you can explore cracks and cavities. For the Osterhöhle, guided tours are about 30 minutes, which can be suitable for families, and flashlights are provided for an engaging experience.
The Osterhöhle is typically open from Easter until October. It closes during winter months (November to March) as it serves as a retreat for bats. For publicly accessible caves like the Robber's Cave, you can visit year-round, but be mindful of weather conditions, especially in winter.
Many caves, like the Osterhöhle, are karst caves known for their diverse dripstone formations (stalactites and stalagmites), sinter basins, and even small underground lakes. The Robber's Cave, formed during the Jurassic period, showcases how water slowly dissolved limestone to create large cave halls.
The House without a Roof (Kallmünz) is a unique example of a still-used cave dwelling. Built into a natural dolomite rock cave, its opening is enclosed by a plastered wall with a door and windows. While you cannot enter the house itself, a board at the entrance provides explanations about its fascinating history and structure.
The region offers various outdoor activities. You can find numerous road cycling routes, running trails, and MTB trails around Beratzhausen. Many caves, like the Robber's Cave, are located along hiking paths such as the Jurasteig trail, making them ideal stops during a longer tour.
Yes, the Loch Cave Castle Ruins are an extremely rare example of a cave castle. Here, two natural caves in the slope were connected and walled to create living quarters within the rock. Please note that the site is currently closed and cannot be visited.
For caves like the Robber's Cave, a flashlight is highly recommended to explore the interior. Inside the Osterhöhle, the temperature is a cool 9 degrees Celsius, so bringing an extra layer of clothing is advisable even in summer. Comfortable shoes are also recommended for exploring the terrain around the caves.
Visitors appreciate the diverse geological formations and the historical insights offered by the caves. The publicly accessible nature of some caves, like the Robber's Cave, allows for easy exploration. The unique blend of natural beauty and human history, from ancient uses to cave dwellings, makes the region's caves a captivating experience.
Near the Osterhöhle, you can find a rustic Waldschänke (forest tavern) with a beer garden, offering local specialties. For other caves, especially those in more natural settings, it's advisable to check for nearby towns like Kallmünz, which offers amenities such as cafes and restaurants, or Beratzhausen itself for broader options.


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