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in comparison to other Eifel maars; only in two places are there greater accumulations of tuff; the rest of the surrounding area is covered only by a thin layer. Either most of the tuffs have already been removed, or the eruption produced very little tuff.
59:. The floor of the maar is in the shape of an elongated oval and is about 700×500 metres in size, its upper boundary has a diameter of about 1,300 × 1,050 metres. This makes the Mosbrucher Maar the third largest of the maars in the western
137:. The long-term renaturalisation measure is embedded in the overall project "Restoration and conservation of hillside bogs, raised bogs and intermediate bogs and their adjacent habitats in the Hunsrück and the Eifel", with the
106:- there are still remains of Roman facilities on the Hochkelberg - the remaining water was impounded to create a fish pond. In 1838, water was drained from the pond so that the western outlying areas could be used as
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EU LIFE+ Natur
Projekt "Wiederherstellung und Erhalt von Hang-, Hoch und Zwischenmooren sowie angrenzenden Lebensräumen im Hunsrück und der Eifel."
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studies, the crater was formed about 11,000 years ago by a volcanic eruption. In the area around the maar there are very few volcanic
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as the project sponsor. Visitors to the maar are guided by carefully laid-out gangplanks in order to protect the maar from damage.
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ceased, water collected in the maar basin and a very shallow maar lake was formed. Because of its low water level it
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The bog has created an excellent habitat for rare plants and animals. In 1980, the
Mosbrucher Weiher was declared a
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In the 20th century, the 6-metre-thick peat layer of the lake was harvested in order to produce
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relatively quickly and, after a few thousand years, became
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stream flows past and close to the
Mosbrucher Weiher.
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133:. It was the 100th nature reserve in the state of
39:east of the municipal boundary of the village of
121:for heating. Peat cutting ceased in the 1950s.
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162:(pdf; 127 kB). Description of the project.
139:Stiftung Natur und Umwelt Rheinland-Pfalz
250:Nature reserves in Rhineland-Palatinate
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199:Article in the Daun local yearbook
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110:. Today, it forms meadowland and
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221:50.260931°N 6.952013°E
175:Wilhelm Meyer (1986),
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20:The Mosbrucher Weiher
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135:Rhineland-Palatinate
226:50.260931; 6.952013
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245:Maars of the Eifel
177:Geologie der Eifel
28:, also called the
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89:volcanic activity
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108:arable land
104:Roman times
55:, a former
53:Hochkelberg
45:Vulkaneifel
239:Categories
209:50°15′39″N
169:Literature
145:References
212:6°57′07″E
93:silted up
34:silted up
41:Mosbruch
57:volcano
49:Germany
32:, is a
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87:After
71:Origin
65:Üßbach
81:tuffs
61:Eifel
181:ISBN
157:pdf
119:peat
37:maar
24:The
97:bog
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