The Crag Group is a geological group outcropping in East Anglia, UK and adjacent areas of the North Sea. Its age ranges from approximately 4.4 to 0.478 million years BP, spanning the late Pliocene and early to middle Pleistocene epochs. It comprises a range of marine and estuarine sands, gravels, silts and clays deposited in a relatively shallow-water, tidally-dominated marine embayment on the western margins of the North Sea basin. The sands are characteristically dark green from glauconite but weather bright orange, with haematite 'iron pans' forming. The lithology of the lower part of the Group is almost entirely flint. The highest formation in the Group, the , contains over 10% of far-travelled lithologies, notably quartzite and vein quartz from the Midlands, igneous rocks from Wales,
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| - Crag Group (en)
- Crag (sediment) (nl)
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| - Een crag of schelpenbank is een laag sediment die bestaat uit grind of grof zand en schelpen of schelpfragmenten. Crags worden gevormd in zeer ondiepe mariene omgevingen, bijvoorbeeld zandplaten waar tijdens een storm schelpen en grind ophopen. Vaak liggen ze over erosievlakken. De naam crag komt uit het zuidoosten van Engeland, waar dergelijke lagen met name in de regio East Anglia veel voorkomen. Voorbeelden zijn:
* - Midden-Plioceen
* - Laat-Plioceen
* (Mammiferous Crag) - Plioceen
* (Weybourne Crag) - Vroeg-Pleistoceen (nl)
- The Crag Group is a geological group outcropping in East Anglia, UK and adjacent areas of the North Sea. Its age ranges from approximately 4.4 to 0.478 million years BP, spanning the late Pliocene and early to middle Pleistocene epochs. It comprises a range of marine and estuarine sands, gravels, silts and clays deposited in a relatively shallow-water, tidally-dominated marine embayment on the western margins of the North Sea basin. The sands are characteristically dark green from glauconite but weather bright orange, with haematite 'iron pans' forming. The lithology of the lower part of the Group is almost entirely flint. The highest formation in the Group, the , contains over 10% of far-travelled lithologies, notably quartzite and vein quartz from the Midlands, igneous rocks from Wales, (en)
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| - Coralline, Red, Norwich & Wroxham Crag Formations (en)
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| - Dunwich, Albion Glacigenic, Britannia Catchments & British Coastal Deposits Groups (en)
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| - Red Crag Formation at Bawdsey cliff, Suffolk (en)
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| - The Crag Group is a geological group outcropping in East Anglia, UK and adjacent areas of the North Sea. Its age ranges from approximately 4.4 to 0.478 million years BP, spanning the late Pliocene and early to middle Pleistocene epochs. It comprises a range of marine and estuarine sands, gravels, silts and clays deposited in a relatively shallow-water, tidally-dominated marine embayment on the western margins of the North Sea basin. The sands are characteristically dark green from glauconite but weather bright orange, with haematite 'iron pans' forming. The lithology of the lower part of the Group is almost entirely flint. The highest formation in the Group, the , contains over 10% of far-travelled lithologies, notably quartzite and vein quartz from the Midlands, igneous rocks from Wales, and chert from the Upper Greensand of southeastern England. This exotic rock component was introduced by rivers such as the Bytham River and Proto-Thames. The constituent formations of the Crag Group are the Coralline Crag (mid to late Pliocene); the Red Crag (late Pliocene / early Pleistocene); the Norwich Crag (early Pleistocene) and the (early to Middle Pleistocene). The sedimentary record is incomplete, leading to difficulties in correlating and dating sequences The term Crag was first used in a geological sense by R.C. Taylor in 1823, a word commonly used in Suffolk to designate any shelly sand or gravel. (en)
- Een crag of schelpenbank is een laag sediment die bestaat uit grind of grof zand en schelpen of schelpfragmenten. Crags worden gevormd in zeer ondiepe mariene omgevingen, bijvoorbeeld zandplaten waar tijdens een storm schelpen en grind ophopen. Vaak liggen ze over erosievlakken. De naam crag komt uit het zuidoosten van Engeland, waar dergelijke lagen met name in de regio East Anglia veel voorkomen. Voorbeelden zijn:
* - Midden-Plioceen
* - Laat-Plioceen
* (Mammiferous Crag) - Plioceen
* (Weybourne Crag) - Vroeg-Pleistoceen (nl)
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| - Unconformity with Chalk Group and London Clay Formation (en)
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