호프슈테텐-바이어스바흐‬에서 가장 멋진 ‪5‬개의 산 정상

로마 스타일의 아름다운 산장, 꽤 괜찮음

비극적인 역사적 사건을 기리기 위해 언덕에 자리한 추모 십자가. 잠시 멈춰 서서 성찰하게 하는 장소로, 자연과 역사, 인간의 운명이 얼마나 밀접하게 연결되어 있는지를 상기시켜 줍니다.

It is a memorial to an unpunished murder that occurred deep in the forest around 285 years ago. A large wooden cross stands on the base of the so-called Tirolerstein, located in the heart of the Hunsrück-Hochwald National Park and directly on the border between the Birkenfeld and Trier-Saarburg districts. A seating area in front of it invites you to take a break in the greenery. Since the former chapel in the nearby Neuhütten district of Muhl was converted into the National Park Church a few years ago, and since then, star hikes have been held there, the Tirolerstein has also been a place where believers occasionally hold services.

A memorial to a murdered Tyrolean trader.

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/

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

𝑴𝒊𝒏𝒆𝒓𝒂𝒍𝒐𝒈𝒊𝒆 𝒅𝒆𝒔 𝑾𝒆𝒊𝒔𝒆𝒍𝒃𝒆𝒓𝒈𝒆𝒔 The mineralogical peculiarities of the Weiselberg, which are also addressed in the saga, are the rock and the gemstones that occur in it. The rock of the 571 meter high Weiselberg was named in 1887 by the famous mineralogist Rosenbusch with the local name Weiselbergit. The deep black, shiny rock (pitchstone consists of over 60% glass mass (non-crystallized silica) to impose a comparison with a starry night sky Source: Text information board 𝐴𝑐ℎ𝑎𝑡𝑣𝑜𝑟𝑘𝑜𝑚𝑚𝑒𝑛 In the middle of the last century, a mining activity that had been going on since the 15th century for grindable quartz varieties ended on Weiselberg, the most colorful of which is agate, which is still highly valued today. In addition to the banded agate, the Weiselberg also supplied the translucent chalcedony and the transparent jasper. To this day there is no generally accepted theory about the origin of agate. The published theories are just as diverse and varied as the agates themselves. The main evidence of the agate digging, which lasted more than four centuries, are four buried tunnels and the agate penguins that look like bomb craters, which can still be seen on the surface today, especially on the poor northern slope of the Weiselberg. The most famous gemstone "the setting sun" can be viewed along with 1500 other exhibits in the mineralogical museum in the old school in Oberkirchen. Source: Text information board

𝐆𝐞𝐨𝐥𝐨𝐠𝐢𝐞 𝐝𝐞𝐬 𝐖𝐞𝐢𝐬𝐞𝐥𝐛𝐞𝐫𝐠 Weiselbergite is an igneous hardling. 𝑀𝑎𝑔𝑚𝑎: Greek: dough; glowing material of the earth's interior 𝐿𝑎𝑣𝑎: Magma reached the surface of the earth in the course of volcanism Magmatites are the result of the solidification of magma or lava. In terms of geological history, Weiselbergite was formed by volcanism in the Permian period about 260 million years ago. The time of the Carboniferous 340 million years ago, in which, as is well known, the Saarland coal was formed, lies before the Permian period. The first reptiles, from which the mammals and thus also humans descended, dated matt only about a hundred million years after the Permian period. The Weiselberg consists of a single type of rock and is divided into columns of different sizes and directions of incidence. These "columnar rock formations" often occur in volcanic rocks. So-called contraction fissures were responsible for the creation of the mostly pentagonal rock pillars that make up the entire mountain. These are shrinkage fissures that have arisen during the cooling process by reducing the volume of the solidifying lava. The Weiselberg is the remnant of what was once a much larger igneous “plug”. For about 70 million years (beginning of the erosion, after the uplift of the south-west German area out of the chalk sea) it has been constantly exposed to the ravages of time, which freed it bit by bit from the covering and enveloping softer sedimentary rocks. Source: Text information board