|

2nd Gallery: Geology of southern tip of Hook Head and Templeton Bay - Paleozoic Section of Hook Head, South West Coast of Co Wexford, Eire
Second Page Introduction
This is the second page which links to a gallery of diagrams and photographs that illustrate the geology of the Paleozoic rocks that outcrop on Hook Head in South West County Wexford. The photographs were taken by Christopher Kendall on a field trip lead by Peter Haughton and Ian Somerville of the University College of Dublin of Ireland. If you wish to read an introduction to the Geology of Hook Head click on the highlighted words to left.
The photographs occur in same order the outcrops of Hook Head were visited on this trip and the stops immediately below are from Hook Head to Templeton Beach.
Hook Head Lower Carboniferous shelf slope carbonates
This f irst stop is located on the southwestern end of Hook Head adjacent to the lighthouse. The Lower Carboniferous shelf slope carbonates are largely formed of bioclastic packstones to wackestones. The rocks are highly bioturbated exhibiting a Cruziana Ichnofacies. Bedding planes appear to be current or wave driven erosion surfaces. Sediment surfaces are often coated by fenestral bryozoans. There abundant crinoidal remains and other echinoidea fossils. Corals and brachiopods are common too. Small monoclinal like Variscan folds are common.
Hook Head Lower Carboniferous dolomitized carbonate grainstones
This stop is located on the west side of Hook Head around half a mile from the lighthouse. The dolomites are largely grainstones. The rocks are highly crossed bedded with some bioturbation exhibiting a Scolithos Ichnofacies, suggesting a nearshore beach or barrier facies. Bedding planes are often draped by finer sediment.
Templetown Bay on west side of Hook Head
Late Cambrian contact with overthrust and/or unconformable Devonian. Late Cambrian Cambrian Booley Bay Formation is formed of thin bedded fine quartz sands, silts and shales that show small scale slumping and current ripples within sharply defined continuous beds. They show some evidence of Variscan structural deformation, including tight folding. The Devonian grades from low angle cross beds of conglomerate and coarse sands, to more steeply inclined cross bedded sands with gravels floating in this matrix.
 |
Page 2 of 4 |
 |
 |
Page 2 of 4 |
 |
|