Hunts Bay Oolite
Stratigraphic range: Holkerian
TypeFormation
Unit ofPembroke Limestone Group, Carboniferous Limestone Supergroup
UnderliesOxwich Head Limestone Formation
OverliesHigh Tor Limestone Formation
Lithology
Primarylimestone
OtherOolite
Location
RegionWales
CountryUnited Kingdom
Type section
Named forHunts Bay, Gower Peninsula

Hunts Bay Oolite is an oolitic Carboniferous limestone geological formation found in the south Wales region. It is named after Hunts Bay on the Gower peninsula, south-south west of Bishopston, where a significant amount of the limestone forms the cliffs there.

Bracelet Bay, eastern Gower, showing beds of Hunts Bay oolite dipping northwards and eastwards.
Steeply dipping beds of Hunts Bay oolite by Mumbles pier, eastern Gower.

Hunts Bay Oolite is a sub-group of the Pembroke Limestone Group which itself is part of the Carboniferous Limestone Supergroup.[1][2][3]

Oolite means 'egg stone': very small grains (up to 2mm) form by accumulating precipitated minerals, usually calcium carbonate. These ooids, created in a warm, tropical environment, are the precursors to the limestone.[4][5]

The Hunts Bay Oolite extends from Pembroke in the West to Monmouth and Chepstow in the East and northwards into the Dowlais Limestone Formation around Merthyr Tydfil. Fossils, such as brachiopods and crinoids associated with a shallow sea environment, can be found in the rock. East of the South Wales Coalfield and in the south east the rock is increasingly dolomitised (where some calcium is replaced by magnesium).[1]

This subgroup was deposited in equatorial seas largely during the Holkerian (British regional) substage of the Viséan stage of the Carboniferous, from 337 to 333.5 million years ago.[6][7]

See also

References

  1. 1 2 British Geological Survey. "Hunts Bay Oolite Subgroup". www.bgs.ac.uk. Retrieved 21 October 2017.
  2. ↑ British Geological Survey. "Pembroke Limestone Group". www.bgs.ac.uk. Retrieved 21 October 2017.
  3. ↑ British Geological Survey. "Carboniferous Limestone Supergroup". www.bgs.ac.uk. Retrieved 18 October 2017.
  4. ↑ "Sedimentology, sea-level history and porosity evolution of the Holkerian (Lower Carboniferous) of Gower". orca.cf.ac.uk. Retrieved 21 October 2017.
  5. ↑ Waters, Colin, ed. (2011). "A revised correlation of Carboniferous rocks in the British Isles: South Wales" (PDF). Geological Society of London: 29–36. Archived from the original on 4 July 2012. Retrieved 21 October 2017.
  6. ↑ Visean, Dinantian, Carboniferous, Wales. "Visean, Dinantian, Carboniferous, Wales". earthwise.bgs.ac.uk. Retrieved 21 October 2017.{{cite web}}: CS1 maint: multiple names: authors list (link)
  7. ↑ BGS Geological timechart. "BGS Geological timechart". www.bgs.ac.uk. Retrieved 21 October 2017.
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.