Scientific American Supplement, No. 611, September 17, 1887Various
Science
Scientific American Supplement, No. 611, September 17, 1887
Various
Science -- Periodicals
Although the traces of former volcanic action are evident to the
student of nature, the Rhine with its mild climate and luxuriant
vegetation has covered many marks of the former chaotic state of the
land. Very little of this beauty is seen on the higher and,
therefore, more severe and barren mountains of the Western Eifel,
through which a volcanic fissure runs from the foot of the high
unhospitable Schneifel to Bertrich Baths, near the Moselle. From the
ridge of the Schneifel the traveler from the north has his first
glimpse of the still distant system of volcanoes. The most beautiful
part of this portion of the Eifel is in the neighborhood of Dann and
Manderscheid. Near the former rises a barren mountain with a long
ridge, on each side of which is a deep basin. These are sunken
craters, which now contain lakes, and near these two there is a third,
larger lake, the Maar von Schalkemehren, on the cultivated banks of
which we find a little village. The middle one, the Weinfelder Maar,
is the most interesting for geologists, for there seems to have been
scarcely any change here since the time of the eruption. On the other
side of the mountain lies the Gremundener Maar, the shores of which
are not barren and waste land, like those of the middle lake, but it
is surrounded by a dark wreath of woods whose tops are mirrored in the
crystal water. Farther to the south, near the villages of Gillenfeld
and Meerfeld, there are more lakes.
[Illustration: THE WEINFELDER LAKE ON THE MAUSEBERGE.]
[Illustration: EASTERN DECLIVITY OF MOSENBERGE NEAR MANDERSCHEID.]
The grandest picture of these ancient events is offered by the
Mosenberg, near Manderscheid, a mighty volcano which commands an
extensive view of the country. Two old craters lie on its double top,
one of which has fallen in, forming a short rocky valley, but the
other retains its original regular shape. In the circular funnel,
whose walls consist of masses of lava stone, rests a quiet, black
lake, that looks very mysterious to the wanderer. Only low juniper
bushes grow near the crater, bearing witness to the barrenness of the
land. From the foot of this mountain an immense stream of lava, as
wide and deep as a glacier, broke forth and flowed into the valley,
where the end of the stream is still to be seen in a high, steep wall
of rock.
[Illustration: THE "CHEESE GROTTO" AT BERTRICH BATHS.]
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account