Waulsortian mudmound
http://dbpedia.org/resource/Waulsortian_mudmound an entity of type: Work
A Waulsortian mudmound is a geographical feature formed in warm tropical waters in the Viséan geological age, now transposed to the temperate regions in Europe. It is a type of bioconstruction, rich in fossils.The rock comprises light grey, unbedded, micritic limestone, heavily jointed with calcite veining. There is some galena and sphalerite mineralisation in the joints. The fossils are mainly Crinoid ossicles together with gastropods and brachiopods.
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Waulsortian mudmound
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48127400
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1012425693
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A Waulsortian mudmound is a geographical feature formed in warm tropical waters in the Viséan geological age, now transposed to the temperate regions in Europe. It is a type of bioconstruction, rich in fossils.The rock comprises light grey, unbedded, micritic limestone, heavily jointed with calcite veining. There is some galena and sphalerite mineralisation in the joints. The fossils are mainly Crinoid ossicles together with gastropods and brachiopods. The term Waulsortian was first used in 1863 to describe an area of limestone near Waulsort in Namur, Belgium. Similar mudstone was recognised in the Clitheroe area of Lancashire England by Arthur Vaughan in 1916.
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