휘플러에서 가장 멋진 20개의 천연기념물
천연기념물을 방문하여 휘플러의 아름다운 풍경을 만나보세요. 휘플러에 있는 20
개의 천연기념물과 상세 정보를 살펴본 후에 방문하고 싶은 천연기념물을 다음 모험 계획에 추가해보세요!
마지막 업데이트: 5월 28, 2026
옛 글란탈 철도 노선
하이라이트 • 자전거 도로
The Glantalbahn is a non-electrified and now largely disused railway line that runs largely in Rhineland-Palatinate and to a small extent in Saarland, mainly along the river Glan. It was built at the turn of the 19th and 20th centuries, primarily for strategic reasons. The Glan-Münchweiler - Altenglan section was built in 1868 as part of the Landstuhl - Kusel railway line. In 1896 and 1897, the Lauterecken - Odernheim - Staudernheim section followed, initially as a continuation of the Lautertalbahn opened in 1883. The other sections Homburg - Glan-Münchweiler, Altenglan - Lauterecken and Odernheim - Bad Münster were opened in 1904. In Odernheim, the railway line split into the branch to Staudernheim, which had existed since 1897, and the branch to Bad Münster.
Due to the sparse population in the region, traffic was rather low except during the two world wars, when the route was of strategic importance. After the Second World War, the second track was gradually dismantled. From 1961 to 1986, passenger traffic was discontinued on large parts of the railway line. Since 1996, the line has been closed with the exception of the Glan-Münchweiler - Altenglan section, which is part of the connection from Landstuhl to Kusel. The Glantalbahn has been dismantled between Waldmohr and Glan-Münchweiler and between Odernheim and Bad Münster. Since the beginning of 2000, a draisine rental company has been offering draisines for self-drivers on the Altenglan - Staudernheim section.
Source: de.wikipedia.org/wiki/Glantalbahn
Information about the Glan-Blies cycle path: de.wikipedia.org/wiki/Glan-Blies-Radweg
Glan-Blies cycle path website: glan-blies-weg.de
Due to the sparse population in the region, traffic was rather low except during the two world wars, when the route was of strategic importance. After the Second World War, the second track was gradually dismantled. From 1961 to 1986, passenger traffic was discontinued on large parts of the railway line. Since 1996, the line has been closed with the exception of the Glan-Münchweiler - Altenglan section, which is part of the connection from Landstuhl to Kusel. The Glantalbahn has been dismantled between Waldmohr and Glan-Münchweiler and between Odernheim and Bad Münster. Since the beginning of 2000, a draisine rental company has been offering draisines for self-drivers on the Altenglan - Staudernheim section.
Source: de.wikipedia.org/wiki/Glantalbahn
Information about the Glan-Blies cycle path: de.wikipedia.org/wiki/Glan-Blies-Radweg
Glan-Blies cycle path website: glan-blies-weg.de
번역자 Google •
팁에 의해
글란강의 에르데스바허 제방
하이라이트 • 강
If you deviate 20 meters from the route, you stand on the Glanbrücke and have a wonderful view of the Erdesbacher weir.
번역자 Google •
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무료 회원 가입
헬러베르크 채석장 – 역사적인 마노 채굴지
하이라이트 • 역사적 장소
𝑯𝒊𝒔𝒕𝒐𝒓𝒊𝒔𝒄𝒉𝒆𝒓 𝑨𝒄𝒉𝒂𝒕𝒂𝒃𝒃𝒂𝒖
Agate mining in the Freisen and Oberkirchen area was first documented in the 14th century. The banded chalcedony was initially sold to agate cutters in Freiburg and Venice, before their own loops were made in Idar and Oberstein (documented from 1520). According to a document from 1853, "the agate stone-rich Freisen and Oberkirchen were the main places where the agate loops get the raw stones". Agates were collected in fields or broken from the rock. Not only on Weiselberg, where pingen and tunnels are still in today Terrain are visible, agate mining is historically documented in Freisen. Poverty in the early 19th century drove many into emigration. Oberkirchen emigrants discovered Brazilian agates, which they had delivered to their old homeland from 1834. The Idar-Oberstein grinding industry experienced an economic one Soon the number of water loops had increased from 31 in 1827 to over 150 in 1867. Since deliveries from Brazil did not always work smoothly, farmers and craftsmen found work and bread again in local agate mining Agate diggers not rich, but helped them through times of dire need When the rough stones from overseas became more reliable around 1870, the 500-year-old mining in Oberkirchen and Freisen ended. Source: Text information board
𝑺𝒕𝒆𝒊𝒏𝒃𝒓𝒖𝒄𝒉 𝑯𝒆𝒍𝒍𝒆𝒓𝒃𝒆𝒓𝒈
The main mining period in the Becker am Hellerberg quarry was closely linked to the construction of the motorway (A62), which reached the Freisen area in 1972. At the end of construction in 1981, the quarry also closed. The last blast was in 1980. In the quarry, several lava flows are exposed, which are separated by almond stone zones and volcanic loose masses. In the bladder cavities of the almond stone structure, duct agates and drusen with zeolite and goethite, smoky quartz and amethyst have developed. To this day, mineral collectors from near and far are looking for the stone treasures. During the construction of the motorway in the 1970s, the entire range of great agates and druses was found in Freisen. Even after that, every major construction site lured stone seekers out. In addition to a few other localities, they found what they were looking for on Füsselberg and Freisener Höhe. Source: Text information board
Agate mining in the Freisen and Oberkirchen area was first documented in the 14th century. The banded chalcedony was initially sold to agate cutters in Freiburg and Venice, before their own loops were made in Idar and Oberstein (documented from 1520). According to a document from 1853, "the agate stone-rich Freisen and Oberkirchen were the main places where the agate loops get the raw stones". Agates were collected in fields or broken from the rock. Not only on Weiselberg, where pingen and tunnels are still in today Terrain are visible, agate mining is historically documented in Freisen. Poverty in the early 19th century drove many into emigration. Oberkirchen emigrants discovered Brazilian agates, which they had delivered to their old homeland from 1834. The Idar-Oberstein grinding industry experienced an economic one Soon the number of water loops had increased from 31 in 1827 to over 150 in 1867. Since deliveries from Brazil did not always work smoothly, farmers and craftsmen found work and bread again in local agate mining Agate diggers not rich, but helped them through times of dire need When the rough stones from overseas became more reliable around 1870, the 500-year-old mining in Oberkirchen and Freisen ended. Source: Text information board
𝑺𝒕𝒆𝒊𝒏𝒃𝒓𝒖𝒄𝒉 𝑯𝒆𝒍𝒍𝒆𝒓𝒃𝒆𝒓𝒈
The main mining period in the Becker am Hellerberg quarry was closely linked to the construction of the motorway (A62), which reached the Freisen area in 1972. At the end of construction in 1981, the quarry also closed. The last blast was in 1980. In the quarry, several lava flows are exposed, which are separated by almond stone zones and volcanic loose masses. In the bladder cavities of the almond stone structure, duct agates and drusen with zeolite and goethite, smoky quartz and amethyst have developed. To this day, mineral collectors from near and far are looking for the stone treasures. During the construction of the motorway in the 1970s, the entire range of great agates and druses was found in Freisen. Even after that, every major construction site lured stone seekers out. In addition to a few other localities, they found what they were looking for on Füsselberg and Freisener Höhe. Source: Text information board
번역자 Google •
팁에 의해
Achatweg의 바살트 로즈(안데사이트 구체)
하이라이트 • 자연 기념물
𝑾𝒖𝒏𝒅𝒆𝒓𝒘𝒆𝒓𝒌 𝒅𝒆𝒓 𝑬𝒓𝒅𝒈𝒆𝒔𝒄𝒉𝒊𝒄𝒉𝒕𝒆 - 𝑲𝒖𝒈𝒆𝒍 𝒎𝒊𝒕 𝑺𝒄𝒉𝒂𝒍𝒆𝒏𝒃𝒂𝒖
Like a broken sphere made of concentric shells, a strange phenomenon has developed in the andesite rock of the Hellerberg. On the "Achatweg" in the quarry walls further outcrops with similar semicircular shapes can be discovered, although none is as impressive to look at as this one. The shape popularly known as the "Basalt Rose" raises questions, especially one. How did it come about? A special process of desquamation, which can occur in igneous rocks when the pressure is released, must first be considered as the cause of the phenomenon: the so-called exfoliation. Pressure relief occurs, for example, when the rock masses lying on top of it are removed by erosion or valley formation and the previously compressed rock underneath is freed from the load or the lateral pressure. This causes the exposed rock to expand somewhat, in the direction of the decreasing pressure. Fissures and fissures form parallel to the surface of the land, creating an onion skin-like appearance. Transverse stresses create additional cracks. Weathering can then model the shell formation even more concisely. Source: Text information board
𝐿𝑎𝑣𝑎𝑠𝑡𝑟𝑜𝑚, 𝐼𝑛𝑡𝑟𝑢𝑠𝑖𝑜𝑛 𝑜𝑑𝑒𝑟 𝑁𝑒𝑏𝑒𝑛𝑘𝑟𝑎𝑡𝑒𝑟?
It is questionable whether the phenomenon can already be adequately explained by the pressure relief. As is so often the case in nature, different processes overlap here too. It is obvious, especially in the case of an old volcanic landscape like the Hellerberg, that stress cracks were created while a flowing body of igneous melt was cooling, which later led to a platy-shelled secretion under pressure changes. The shape cut in the outcrop could originally have emerged from a small lava flow or an underground melt, an intrusion, perhaps also from a volcanic secondary crater. Source: Text information board
Like a broken sphere made of concentric shells, a strange phenomenon has developed in the andesite rock of the Hellerberg. On the "Achatweg" in the quarry walls further outcrops with similar semicircular shapes can be discovered, although none is as impressive to look at as this one. The shape popularly known as the "Basalt Rose" raises questions, especially one. How did it come about? A special process of desquamation, which can occur in igneous rocks when the pressure is released, must first be considered as the cause of the phenomenon: the so-called exfoliation. Pressure relief occurs, for example, when the rock masses lying on top of it are removed by erosion or valley formation and the previously compressed rock underneath is freed from the load or the lateral pressure. This causes the exposed rock to expand somewhat, in the direction of the decreasing pressure. Fissures and fissures form parallel to the surface of the land, creating an onion skin-like appearance. Transverse stresses create additional cracks. Weathering can then model the shell formation even more concisely. Source: Text information board
𝐿𝑎𝑣𝑎𝑠𝑡𝑟𝑜𝑚, 𝐼𝑛𝑡𝑟𝑢𝑠𝑖𝑜𝑛 𝑜𝑑𝑒𝑟 𝑁𝑒𝑏𝑒𝑛𝑘𝑟𝑎𝑡𝑒𝑟?
It is questionable whether the phenomenon can already be adequately explained by the pressure relief. As is so often the case in nature, different processes overlap here too. It is obvious, especially in the case of an old volcanic landscape like the Hellerberg, that stress cracks were created while a flowing body of igneous melt was cooling, which later led to a platy-shelled secretion under pressure changes. The shape cut in the outcrop could originally have emerged from a small lava flow or an underground melt, an intrusion, perhaps also from a volcanic secondary crater. Source: Text information board
번역자 Google •
팁에 의해
켈트족 고분 (할슈타트 시대)
하이라이트 • 역사적 장소
A barrow or burial mound (Latin tumulus, plural tumuli; Greek τύμβος tymbos) is an elongated, round or oval pile of earth. Inside there are tombs or other prehistoric monuments. The graves can be body burials (possibly in a tree coffin), urn graves or scattered corpse burns. The mounds can have built-in components, e.g. B. from concentric circles, buildings (burial mounds of Trappendal), stone burial chambers or stone boxes.
번역자 Google •
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커뮤니티 팁
Great rock formations. However, I wouldn't go too close, as rocks can still break off and fall down.
번역: Google•
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Dirk Rüger
6월 1, 2025, Celtic Burial Mound (circa 450 BC)
⚰️ A silent witness to the past: This moss-covered burial mound dates back to around 400 BC – presumably of Celtic origin. The small plaque seems almost inconspicuous, but if you look closely, you'll sense the specialness of this place. Mystical. Timeless. Touching. 📍 Tip: 🪨 Slow down a few steps here – this place has more depth than meets the eye.
번역: Google•
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📍 Agate Trail Freisen Right on the edge of the quarry stands a simple bench – overlooking what was once an active mining site. Today, silence reigns here. The contrast between the rugged rock faces and the tranquility of the moment makes this place special. Ideal for a short rest – with a panoramic view of space and time. 💡 Tip: A beautiful spot for a second breakfast, a deep photo, or simply for reflection. Those who sit here tend to stay a little longer.
번역: Google•
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Eike
7월 19, 2024, Erdesbacher Wehr am Glan
You can sit by the water and relax. Perfect way to cool down in summer 😉
번역: Google•
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Seba
3월 11, 2024, Hellerberg Quarry – Historic Agate Mining Site
Very interesting former agate quarry.
번역: Google•
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쇠넨베르크-퀴벨베르크그리스발트모어던츠바일러난츠디에슈바일러브뤼켄(팔츠)뵈르스본슈타인바흐 암 글란크로텔바흐Herschweiler-Pettersheim옴바흐글란-뮌히바일러라이히바일러프론호펜헨슈탈디트와일러울프슈타인노이키르헨 암 포츠베르크힌츠바일러Kreimbach-Kaulbach콘켄브라이텐바흐로셀베르그레바일러오버스타우펜바흐라스와일러베데스바흐마첸바흐글란브뤼켄장크트 줄리안울멧다임베르그반베겐아슈바흐Föckelberg알텐글란퀴른바흐/팔츠에르데스바흐셸바일러웰히바일러네르츠바일러탈리히텐베르크페펠바흐러츠바일러 암 글란알베센셀첸바흐헤렌-술츠바흐오베랄벤부본Theisbergstegen니데랄벤운터예켄바흐에치베르그쾨르본덴바일러-프론바흐에바일러에스바일러니더스타우펜바흐보젠바흐엘츠바일러호르슈바흐오버바일러 임 탈오펜바흐-훈트하임렐스버그헤퍼스와일러루스와일러블라바흐러츠바일러 안 데어 라우터하쉬바흐 암 레미기우스베르크람멜스바흐헤르히바일러하우스바일러호프슈테텐누스바흐메르츠와일러아이뇰렌오버바일러-티펜바흐라우터레켄그룸바흐비스바일러라이폴츠키르헨론바일러오덴바흐호에뇰렌긴즈와일러하인젠하우젠메다르크로넨베르크아덴바흐
