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- Q15144302 subject Q8487942.
- Q15144302 subject Q8818861.
- Q15144302 abstract "The Norwich Crag Formation is a series of marine deposits at the base of the Pleistocene Series in East Anglia in eastern England. It includes both sands and clays e.g. the Chillesford Clay and the Easton Bavents Clay which overlie the Red Crag Formation. The Norwich Crag is itself overlain by the Wroxham Crag Formation.The part of the Norwich crag assigned to the Antian warm stage contains fossils of zebra-like horse and southern elephant, and the cooler Baventian shows little change,with zebra-like horse, southern elephant, Euctenoceros (a deer) and Mimomys (a vole).Undifferentiated Norwich Crag has yielded clawless otter, fallow and other deer, and gazelles, beaver and most spectacularly, sabre tooth tiger,Norwich Crag is closely related to the Cromerian interglacial stage (a relatively shorter period of temperate climate change) approximately midway during the Pleistocene epoch,coming at the end of the Quaternary period.".
- Q15144302 wikiPageWikiLink Q1140849.
- Q15144302 wikiPageWikiLink Q1291566.
- Q15144302 wikiPageWikiLink Q159857.
- Q15144302 wikiPageWikiLink Q188717.
- Q15144302 wikiPageWikiLink Q190858.
- Q15144302 wikiPageWikiLink Q21.
- Q15144302 wikiPageWikiLink Q25546.
- Q15144302 wikiPageWikiLink Q47542.
- Q15144302 wikiPageWikiLink Q580631.
- Q15144302 wikiPageWikiLink Q7239178.
- Q15144302 wikiPageWikiLink Q7303950.
- Q15144302 wikiPageWikiLink Q8487942.
- Q15144302 wikiPageWikiLink Q8818861.
- Q15144302 comment "The Norwich Crag Formation is a series of marine deposits at the base of the Pleistocene Series in East Anglia in eastern England. It includes both sands and clays e.g. the Chillesford Clay and the Easton Bavents Clay which overlie the Red Crag Formation.".
- Q15144302 label "Norwich Crag Formation".