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- Q22004645 subject Q15712705.
- Q22004645 subject Q6582734.
- Q22004645 abstract "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.".
- Q22004645 wikiPageWikiLink Q1008765.
- Q22004645 wikiPageWikiLink Q105006.
- Q22004645 wikiPageWikiLink Q1125.
- Q22004645 wikiPageWikiLink Q15712705.
- Q22004645 wikiPageWikiLink Q17151027.
- Q22004645 wikiPageWikiLink Q171917.
- Q22004645 wikiPageWikiLink Q178272.
- Q22004645 wikiPageWikiLink Q2203651.
- Q22004645 wikiPageWikiLink Q2976542.
- Q22004645 wikiPageWikiLink Q33666.
- Q22004645 wikiPageWikiLink Q37559.
- Q22004645 wikiPageWikiLink Q4867740.
- Q22004645 wikiPageWikiLink Q5134437.
- Q22004645 wikiPageWikiLink Q647290.
- Q22004645 wikiPageWikiLink Q6582734.
- Q22004645 comment "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.".
- Q22004645 label "Waulsortian mudmound".