Redcar Mudstone Formation Explained

Redcar Mudstone Formation
Period:Hettangian
Age:Hettangian-Pliensbachian
~
Type:Geological formation
Prilithology:Mudstone, siltstone
Otherlithology:Sandstone, limestone
Unitof:Lias Group
Underlies:Staithes Sandstone Formation
Overlies:Lilstock Formation
Thickness:up to 283m (928feet)
Coordinates:54.6°N -1.1°W
Paleocoordinates:41.1°N 2.3°W
Region:North Yorkshire
Extent:Cleveland Basin
Namedfor:Redcar

The Redcar Mudstone Formation is a geological formation in North Yorkshire, England. Part of the Lias Group, it was deposited in the Hettangian to Pliensbachian stages of the Early Jurassic. The lithology consists of fissile mudstones and siltstones, with the lower part having thin beds of limestone and the upper part having thin beds of sandstone.[1] The Redcar Mudstone Formation at Wine Haven, Robin Hood's Bay, Yorkshire contains the Global Boundary Stratotype Section and Point (GSSP) for the base of the Pliensbachian.[2]

Further reading

Notes and References

  1. Web site: Redcar Mudstone Formation. British Geological Survey. BGS Lexicon of Named Rock Units. 10 August 2018.
  2. Meister. Christian. Aberhan. Martin. Blau. Joachim. Dommergues. Jean-Louis. Feist-Burkhardt. Susanne. Hailwood. Ernie A.. Hart. Malcom. Hesselbo. Stephen P.. Hounslow. Mark W.. Hylton. Mark. Morton. Nicol. 2006-06-01. The Global Boundary Stratotype Section and Point (GSSP) for the base of the Pliensbachian Stage (Lower Jurassic), Wine Haven, Yorkshire, UK. Episodes. 29. 2. 93–106. 10.18814/epiiugs/2006/v29i2/003. 0705-3797. free.