AFFLEUREMENT DE QUARTZITES DE SIERCK-LES-BAINS
SIERCK LES BAINS
Die Quarzitaufschlüsse in der Gemeinde Sierck-les-Bains erstrecken sich über 10 Hektar im Tal des Baches Montenach zwischen der Mühle von Sulzen und der Kapelle von Marienfloss. Das geologische Interesse an den Taunusquarziten liegt im sehr hohen Alter dieser geologischen Formation aus Eruptivgestein, die aus dem Devon (Primärzeitalter) stammt. Das Vorhandensein von Silikatgestein in einem Kalksteingebiet ermöglicht das Blühen seltener säureliebender Pflanzen. Ein Entdeckungspfad führt durch das Gelände. Vier Lehrtafeln vermitteln die Lebensräume, die Sie durchqueren.
©Emmanuel Stourm 2020 Licence Open Data
57480 SIERCK LES BAINS
Langues parlées à lʾaccueil :
Deutsch
Animaux acceptés :
JA
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