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- Q7303950 subject Q8487942.
- Q7303950 subject Q8818861.
- Q7303950 abstract "The Red Crag Formation is a series of marine deposits at the base of the Pleistocene in Suffolk and Essex. This material rests on an erosion surface of Cretaceous to Palaeogene rocks. It is a shore deposit, medium to coarse-grained and locally shelly.The most extensive exposure of Red Crag is found at Bawdsey Cliff, the site of which is designated a Site of Special Scientific Interest. Around 2 kilometres (1.2 mi) of Crag from the Gelasian are exposed. Red Crag deposits have been dated from Piacenzian age at Walton-on-the-Naze to Preludhamian age at Sizewell on the basis of microfossils.Crag is a local word for a shelly sand. The Red Crag is generally stained red by ferruginous compounds.".
- Q7303950 wikiPageWikiLink Q1142548.
- Q7303950 wikiPageWikiLink Q12069238.
- Q7303950 wikiPageWikiLink Q1818988.
- Q7303950 wikiPageWikiLink Q2207320.
- Q7303950 wikiPageWikiLink Q23111.
- Q7303950 wikiPageWikiLink Q23240.
- Q7303950 wikiPageWikiLink Q25546.
- Q7303950 wikiPageWikiLink Q422211.
- Q7303950 wikiPageWikiLink Q428579.
- Q7303950 wikiPageWikiLink Q44626.
- Q7303950 wikiPageWikiLink Q514873.
- Q7303950 wikiPageWikiLink Q55810.
- Q7303950 wikiPageWikiLink Q8487942.
- Q7303950 wikiPageWikiLink Q8818861.
- Q7303950 comment "The Red Crag Formation is a series of marine deposits at the base of the Pleistocene in Suffolk and Essex. This material rests on an erosion surface of Cretaceous to Palaeogene rocks. It is a shore deposit, medium to coarse-grained and locally shelly.The most extensive exposure of Red Crag is found at Bawdsey Cliff, the site of which is designated a Site of Special Scientific Interest. Around 2 kilometres (1.2 mi) of Crag from the Gelasian are exposed.".
- Q7303950 label "Red Crag Formation".