Coralline Crag Formation

The Coralline Crag Formation is a geological formation in England. It is a series of marine deposits found near the North Sea coast of Suffolk and characterised by bryozoan and mollusc debris. The deposit, whose onshore occurrence is mainly restricted to the area around Aldeburgh and Orford,^[1][2] is a series of bioclastic calcarenites and silty sands with shell debris, deposited during a short-lived warm period at the start of the Pliocene Epoch of the Neogene Period.^[3] Small areas of the rock formation are found in locations such as Boyton and Tattingstone to the south of Orford as well as offshore at Sizewell.^[4]

Coralline Crag Formation
Stratigraphic range: Pliocene PreꞒ Ꞓ O S D C P T J K Pg N ↓
Coralline Crag Formation exposed in Suffolk, England.
Type	Formation
Unit of	Crag Group
Underlies	Norwich Crag Formation
Overlies	Thames Group (unconformity)
Thickness	Up to 25 metres
Lithology
Primary	Sand
Location
Region	England
Country	United Kingdom
Extent	Suffolk

Crag is a local word for a shelly sand. Coralline Crag has sometimes been used historically in the Suffolk coast area for building and a number of quarries exist.^[2] The tower of St Peter's Church in Chillesford is one of only two built using the rock.^[2]

• 
  A map, published in 1898, showing the extent of Coralline Crag rocks in Suffolk
• 
  Quarried block of Coralline Crag, containing bryozoan fossils, in the wall of St Peter's church in Chillesford in Suffolk
• 
  Fossils from the Coralline Crag. From Chatwin (1954).^[5]

See also

• Earth sciences portal
• England portal
• Paleontology portal

• Geology of Suffolk
• List of fossiliferous stratigraphic units in England