ダルシャイトのおすすめウォーキング＆ハイキングルート

Zum Semersberg s. z.B. https://www.geopark-vulkaneifel.de/eifel/landschaft/aussichtspunkte/eifel-blick-semersberg.html

The Kaiserstein near Mehren in the Volcanic Eifel is a regionally well-known memorial located in the heart of the Lehwald forest and commemorating the first German emperor, Wilhelm I. The monument, a basalt stone, was erected in 1897 and marks a memorial service held on the occasion of the emperor's 100th birthday, although Wilhelm I himself had died nine years earlier in 1888. The inscription on the front of the stone reads: W.I. 1797 - 1897 March 22. This ceremony on March 22, 1897, was a significant event attended by royal foresters, the Mehren War Veterans Association, five schools, and numerous residents of the surrounding villages, underscoring the veneration for the emperor at that time. The Kaiserstein is located in the Lehwald forest, west of the path leading from Darscheid to the Weinfelder Maar, also known as the Totenmaar. Today, it is a cultural monument from the Historicist and Art Nouveau periods and is located within the municipality of Mehren. The memorial is integrated into the region's hiking trails, such as the Biodiversity Trail in Darscheid, and serves as a historical reference point in the volcanic landscape of the Eifel.

Fun fact: when the festivities took place on March 22, 1897, Kaiser Wilhelm had already been dead for nine years. Wilhelm I, whose full name was Wilhelm Friedrich Ludwig of Prussia, had already died in 1888. He had been King of Prussia from 1861 until his death and the first German emperor since the founding of the empire in 1871.

Somewhat unnoticed, surrounded by shrubs and covered in moss, it stands in the heart of the Lehwald forest between Darscheid and Mehren: the Kaiserstein. Many hikers and visitors pass by. Triangular in shape and somewhat forgotten, stands the monument in honor of the first German Emperor, Wilhelm I. It is a basalt stone, erected in 1897 to commemorate the 100th anniversary of the emperor's birth, in the presence of royal forest rangers, the Mehren Veterans Association, five schools, and numerous visitors from the two neighboring towns. The inscription engraved on the gray stone reads: "WI, 1797-1897, March 22."

Unfortunately, the loungers are no longer in the best condition. However, that doesn't detract from the magnificent view of the highest peaks of the West Eifel volcanic field.

Attention: Bridge on the hiking trail no longer exists (December 2023), swampy terrain to the next bridge.

This point does not mark Darscheid as a place, but actually the Darscheider Drees. The Darscheider Drees, the iron-rich sour wine located in the middle of the forest in the immediate vicinity of the Lehbach, has been bubbling out of a newly built fountain since 2014. The Darscheider Drees, which bubbles away in the forest on the outskirts of town, is characterized by its particularly high iron concentration of 46 mg/liter. It contains more iron than all other springs in the Vulkaneifel. This only works because the rising water travels through so many iron-containing rock layers and thus dissolves the iron. The villagers already knew this in the past, because the soursop was caught for the first time in 1870. In 2013, the spring was moved around 100 meters to its current location and redesigned. Enjoy the slightly mineralized, 8 degree cold water when you are in Darscheid.

The Darscheider Drees is the most iron-rich spring in the Vulkaneifel. “How does so much iron get into the water?” one asks, given the iron concentration of 46 milligrams per liter in the water of the Darscheider Drees. Hardly any other source in the Vulkaneifel contains this much iron. The solution to the puzzle: The water rising in the Lower Devonian sedimentary rock moves through iron-containing rock layers and dissolves the iron from them. Since ancient times, many jugs have been filled with the sparkling water on this Drees. The villagers really appreciated the refreshing and wholesome sour water. After the war in 1870/71, the sourling was caught for the first time. Several sources of carbonic acid, which were indicated by reddish soil colors, were led into a well. The water flowed from a stone dome, behind which rose a grotto made of volcanic cinders. When the Drees was redesigned in 2013, the spring outlet was moved to this location. Since then, the Darscheider Drees has appeared in its current form. Source: https://www.geopark-vulkaneifel.de/eifel/landschaft/mineralwasserquelle/darscheider-drees.html