バウムホルダ周辺の山頂は、フンスリュック山地とノルトプファルツ丘陵の間に位置し、探検のための高所を提供します。この地域は、自然の美しさ、歴史的重要性、そしてレクリエーションの機会を特徴としています。バウムホルダ自体の標高は466メートルで、最高点は540メートルに達します。これらの場所は、訪問者に景色の良い眺めとユニークな特徴を提供します。
最終更新日: 4月 19, 2026
ハイライト • 歴史的な場所
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ハイライト • 山頂
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ハイライト • 展望台
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ハイライト • 山頂
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This is where it starts to hurt on the Juwel CTF ;-)
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The Potzberg, known as the "King of Westrich", is a wooded hill, 562 m above sea level, in the North Palatinate Uplands in Rhineland-Palatinate. (Source: Wikipedia)
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At the Nahekopf, hikers can enjoy a sheltered picnic area and a beautiful view of parts of the military training area and the Kaiserallee. Information panels detail a Celtic-Roman excavation that took place on the mountain plateau in 2015. Source: https://www.outdooractive.com/de/poi/nahe/nahekopf/52969627/
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There is no direct view from the 506 m above sea level Ballenberg summit (also called Ballenhubel), but the vegetation opens up along the path from time to time and allows a view over the Hunsrück hills.
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𝗔𝘂𝘀𝘀𝗶𝗰𝗵𝘁 𝗮𝘂𝗳 𝗱𝗲𝗻 𝗣𝗼𝘁𝘇𝗯𝗲𝗿𝗴 The Potzberg is a 562m high wooded mountain in the North Palatinate Uplands and is nicknamed "King of Westrich". Today the Potzberg wildlife park, the Potzberg tower, a military tower and a hotel are located on the summit. The Potzbergturm is a 53.5m high viewing and transmission tower. Originally, a 18.5m high radio antenna on the platform completed the structure. The radio programs of what was then Südwestfunk were broadcast from here until the 1990s. The approx. 30ha large area of the wildlife park offers, favored by its altitude, an indescribable panorama of the North Palatinate mountains, with a visibility of more than 30km. Source: text information board
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Highest point in the vicinity. A few moderately interesting trails lead towards Georg Weierbach.
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𝗡𝗮𝗵𝗲𝗸𝗼𝗽𝗳 On the Nahekopf there was a Celtic fortification measuring approximately 300m x 300m from the Late La Tène period (5th and 1st century BC). This is an era of the later pre-Roman Iron Age in large parts of Central Europe. The La Tène culture is considered "Celtic" primarily due to ancient textual sources. Parts of the massive circular wall, the probable location of the gate, and traces of settlement were archaeologically recorded in 2008. On the Celtic foundations, the Romans built a fortification, which, based on finds, was dated to the mid-3rd to 4th century. It is a reconstruction of the Roman gate system, unique in the region on the left bank of the Rhine, and the creation of an avenue of the most important Roman emperors. A space for cultural events is also planned. Source: Text information board
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𝐒𝐭𝐞𝐢𝐧𝐞𝐫𝐧𝐞 𝐌𝐞𝐞𝐫 From a geological point of view, the »Steinernes Meer« is a heap of scree made from weathered material from the Weiselberg. From a geological point of view, this sea of rocks at the foot of the mountain is a work of the Ice Age. The last ice age only ended around 10,000 years ago. Magma rising underground got stuck under the earth's surface and solidified into mostly pentagonal column formations, quite typical of slowly cooling basalt rock. Over the course of millions of years, the surrounding softer sedimentary rock was removed by erosion. In geology, the very hard rock, which shines deep black when cut and is reminiscent of a starry sky with its bright feldspar particles, has been given the name »Weiselbergite«. The frost change climate during this geological epoch caused extreme weathering and erosion processes that were able to separate the blocks and columns weighing several tons from the rock structure. Not least because of the extreme daily temperature fluctuations, the steep southern slope of the Weiselberg with the typical vertical basalt columns offered the best conditions for the formation of the Felsenmeer. The boulders collected on the mountainside and have since been exposed to weathering. Covered with mosses, the »Steinernes Meer« repeatedly gave rise to eerie legends: Whether wild cyclopes played with it or the remains of an enchanted castle are left to the imagination of the observer. The Romans were already digging for agates on the surface of the Weiselberg. From the 15th century, when only little was to be found above ground and a veritable agate boom began, the agate seekers went deep. Some tunnels buried today bear witness to this. After the war there were concrete considerations to dismantle the Weiselberg as a quarry. This was prevented by the designation as a nature reserve in October 1950. In earlier times, the minerals of this region such as agate, chalcedony, jasper and petrified wood were processed in the gemstone metropolis of Idar-Oberstein. 3000 of these precious stones can be viewed in the Mineralogical Museum in the old school in Oberkirchen (0 68 55/332) and in the Mineral Museum (2000 exhibits) in Freisen (0 68 55/13 25). In the Gemstone Dorado in Freisen, treasure hunters can search for gemstones themselves. (0 68 55/1849 31) Source: Text information board
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これらのガイドでさらに素晴らしい頂上を見てみましょうバウムホルダーでの:
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