In our recent post we demonstrated the consensus that the Devensian ice at the western edge of the vale of Glamorgan lay approximately in the position of Porthcawl. The geological map shows this rather clearly -- we can see assorted deposits (note particularly the till patches shown in blue and the sands and gravels shown in pink) between the northern edge of the town and the M4 motorway. These patchy deposits are overlain by extensive blown sands -- including the Kenfig Burrows and the links golf course of Royal Porthcawl and Pyle and Kenfig Golf Club. It looks to me as if Devensian till underlies at least a part of the town and the coast to the NW -- so it would come as no surprise if fresh till exposures are to be seen along the coast between Nash Point and Margam Burrows.
How much do we know about Stonehenge? Less than we think. And what has Stonehenge got to do with the Ice Age? More than we might think. This blog is mostly devoted to the problems of where the Stonehenge bluestones came from, and how they got from their source areas to the monument. Now and then I will muse on related Stonehenge topics which have an Ice Age dimension...
THE BOOK
Some of the ideas discussed in this blog are published in my new book called "The Stonehenge Bluestones" -- available by post and through good bookshops everywhere. Bad bookshops might not have it....
To order, click HERE
Some of the ideas discussed in this blog are published in my new book called "The Stonehenge Bluestones" -- available by post and through good bookshops everywhere. Bad bookshops might not have it....
To order, click HERE
Saturday, 3 October 2020
A Devensian ice edge at Porthcawl?
In our recent post we demonstrated the consensus that the Devensian ice at the western edge of the vale of Glamorgan lay approximately in the position of Porthcawl. The geological map shows this rather clearly -- we can see assorted deposits (note particularly the till patches shown in blue and the sands and gravels shown in pink) between the northern edge of the town and the M4 motorway. These patchy deposits are overlain by extensive blown sands -- including the Kenfig Burrows and the links golf course of Royal Porthcawl and Pyle and Kenfig Golf Club. It looks to me as if Devensian till underlies at least a part of the town and the coast to the NW -- so it would come as no surprise if fresh till exposures are to be seen along the coast between Nash Point and Margam Burrows.
Subscribe to:
Post Comments (Atom)
No comments:
Post a Comment