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File:Devonian coral-stromatoporoid reefal limestone.jpg

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Deutsch: Polierte Abbaufront im auflässigen Unica-Bruch in Villmar, Hessen. Die Wand besteht aus einem devonischen Riffkalk („Lahnmarmor“) des östlichen Rheinischen Schiefergebirges. Bei den hellgrauen „Flecken“ handelt es sich um Stromatoporen, kalkschwammähnliche Fossilien, deren lagiger Aufbau relativ gut erkennbar ist.
English: Polished quarry wall in the abandoned Unica limestone quarry in the town of Villmar, Hesse, Germany. The wall consists of Devonian reefal limestone (“Lahnmarmor”, i.e. “River Lahn Marble”) of the eastern Rhenish Massif. The light gray “patches” represent stromatoporoids which are fossils similar to calcareous sponges. Their layered structure is fairly visible in the image.
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Author Fritz Geller-Grimm
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Camera location50° 23′ 39.5″ N, 8° 11′ 03.5″ E  Heading=337.5° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo

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7 July 2007

coordinates of the point of view

50°23'39.502"N, 8°11'3.502"E

heading: 337.5 degree

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Date/TimeThumbnailDimensionsUserComment
current15:52, 31 December 2008Thumbnail for version as of 15:52, 31 December 20081,200 × 798 (1 MB)Dysmachus{{Information| |Description= {{de|Lahnmarmor, Steinbruch Unica A, Villmar, Hessen, Deutschland}} |Source=Own work |Date=2007-07-07 |Author=Fritz Geller-Grimm |Permission={{self|cc-by-sa-3.0}} |other_versions=- }} Category:Villmar

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