Lützelsoon with Devil's Rock
Five larger mountain ridges can be distinguished from each other in the Hunsrück: The Hochwald,
to the West of the Erbeskopf (816m) is the highest German mountain West of the Rhine; the
approximately 30km long quarzite ridge of the Idarwald forest with the Idarkopf (746m); the
Lützelsoon with the Womrather Höhe (597m); the south-eastern Soonwald forest formed by three
parallel mountain ridges, the highest point of which is the Ellerspring (657m); and the Binger
forest with the Salzkopf (628m).
Three hundred million years ago, at the end of the Carbon Age, the Devon layers of the Hunsrück
were squeezed together by a massive pressure directed from southeast to northwest. The subsequent
folding and creation of landmasses resulted in the Variscian mountain range (Northern range).
Together with the current Hochwald forest-, Idarwald forest-, and Soonwald forest ranges a high
altitude mountain range developed that eroded over millions of years. Very hard quarzite resisted
the erosion in some places better than other stone types, and was therefore "dug" up. One of
these quarzite pieces is the Teufelsfels (natural monument, translated: Devil's rock),
which (like the
Berger Wacken) lies on the Lützelsoon (568m) like a massive chunk
(="de dick Steen"). Above the tree tops an observation tower reveals a fantastic 360 degree view
over the villages Bruschied, Schneppenbach and over
Hikers can best reach the Teufelsfels via the parking lot near Hennweiler village.