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- Bala_Series abstract "In geology, the Bala Series is a group of dark slates and sandstones with beds of limestone which occurs in the neighborhood of Bala, Gwynedd, in north Wales.It was first described by Adam Sedgwick, who considered it to be the upper part of his Cambrian System. The series is now placed at the top of the Ordovician System, above the Llandeilo beds. The Bala limestone is from 20 to 40 ft (12 m). thick, and is recognizable over most of North Wales; it is regarded as the equivalent of the Coniston Limestone of the Lake District. The series in the type area consists of the Hirnant limestone, a thin inconstant bed, which is separated by 1,400 ft (430 m). of slates from the Bala limestone, below this are more slates and volcanic rocks. The latter are represented by large contemporaneous deposits of tuff and felsitic lava which in the Snowdon District are several thousand feet thick.In South Wales the Bala Series contains the following beds in descending order: the Trinucleus seticornis beds (Slade beds, Redhill shales and Sholeshook limestone), the Robeston Wathen beds, and the Dicranograplus shales. The typical graptolites are, in the upper part, Dicellograptus anceps and D. complanatus; in the lower part, Pleurograptus linearis and Dicranograptus clingani. In Shropshire this series is represented by the Caradoc and Chirbury Series; in southern Scotland by the Hartfell and, Ardmilian Series, and by similar rocks in Ireland.".
- Bala_Series wikiPageID "2929388".
- Bala_Series wikiPageLength "1902".
- Bala_Series wikiPageOutDegree "18".
- Bala_Series wikiPageRevisionID "701951393".
- Bala_Series wikiPageWikiLink Adam_Sedgwick.
- Bala_Series wikiPageWikiLink Bala,_Gwynedd.
- Bala_Series wikiPageWikiLink Cambrian.
- Bala_Series wikiPageWikiLink Caradoc_Series.
- Bala_Series wikiPageWikiLink Category:Geology_of_Wales.
- Bala_Series wikiPageWikiLink Category:Stratigraphy_of_the_United_Kingdom.
- Bala_Series wikiPageWikiLink Coniston_Limestone.
- Bala_Series wikiPageWikiLink Geology.
- Bala_Series wikiPageWikiLink Graptolithina.
- Bala_Series wikiPageWikiLink Hirnant_Limestone.
- Bala_Series wikiPageWikiLink Limestone.
- Bala_Series wikiPageWikiLink Llandeilo_beds.
- Bala_Series wikiPageWikiLink Ordovician.
- Bala_Series wikiPageWikiLink Sandstone.
- Bala_Series wikiPageWikiLink Slate.
- Bala_Series wikiPageWikiLink Stratum.
- Bala_Series wikiPageWikiLink Wales.
- Bala_Series wikiPageWikiLinkText "Bala Series".
- Bala_Series wikiPageWikiLinkText "Bala".
- Bala_Series volume "3".
- Bala_Series wikiPageUsesTemplate Template:Convert.
- Bala_Series wikiPageUsesTemplate Template:EB1911.
- Bala_Series wikiPageUsesTemplate Template:Reflist.
- Bala_Series wikiPageUsesTemplate Template:Regional-geology-stub.
- Bala_Series wikiPageUsesTemplate Template:Update-EB.
- Bala_Series wikiPageUsesTemplate Template:Use_British_English.
- Bala_Series wikiPageUsesTemplate Template:Use_dmy_dates.
- Bala_Series wstitle "Bala Series".
- Bala_Series subject Category:Geology_of_Wales.
- Bala_Series subject Category:Stratigraphy_of_the_United_Kingdom.
- Bala_Series hypernym Group.
- Bala_Series type Band.
- Bala_Series comment "In geology, the Bala Series is a group of dark slates and sandstones with beds of limestone which occurs in the neighborhood of Bala, Gwynedd, in north Wales.It was first described by Adam Sedgwick, who considered it to be the upper part of his Cambrian System. The series is now placed at the top of the Ordovician System, above the Llandeilo beds. The Bala limestone is from 20 to 40 ft (12 m).".
- Bala_Series label "Bala Series".
- Bala_Series sameAs Q4849696.
- Bala_Series sameAs Balaserien.
- Bala_Series sameAs m.08dbcq.
- Bala_Series sameAs Q4849696.
- Bala_Series wasDerivedFrom Bala_Series?oldid=701951393.
- Bala_Series isPrimaryTopicOf Bala_Series.