Monkstone Point folds 2
Monkstone beach view to Gower 2
Monkstone beach view to Gower 3
Tenby from coastal path 1
Tenby from coastal path 2
Waterwynch fields from coastal path
St Govan's Chapel 1
St Govan's Chapel 2
St Govans Chapel 3
View to St Govans Head
View west from Mewsford Point
Bullslaughter Bay folds
Bullslaughter Bay
Bullslaughter Bay folds 2
Bullslaughter Bay caves
Bullslaughter Bay panorama
Elegug Stacks
View to Lundy Island from Elegug Stacks
Green Bridge of Wales
Tenby North Sands chevron fold couplet
Tenby North Sands chevron fold couplet panorama
Tenby North Sands chevron fold couplet structural…
Tenby skyscape
Monkstone beach view to Gower 1
Overturned bedding at Trevayne Point
Tenby from Trevayne Point beach
Trevayne Point anticline
Lodge Valley beach
Lodge Valley waterfall 4
Lodge Valley waterfall 3
Lodge Valley waterfall 2
Lodge Valley waterfall 1
Lodge Valley bedding plane descent to beach 4
Lodge Valley bedding plane descent 3
Lodge Valley bedding plane descent 2
Lodge Valley bedding plane descent 1
Suilven from Glencanisp Grid Ref NC 109 219 view S…
Suilven from Grid Ref NC 1180 2218 view SE
River Inver at Grid Ref NC 1157 2344 view NW
River Inver at Grid Ref NC 1157 2344 view ENE
Start of path to Glencanisp at Grid Ref NC 1156 23…
River Inver at Grid Ref NC 0987 2320
Ben Stack: view north-east towards Arkle
Ben Stack: view north over knock and lochan from C…
Ben Stack: view west to Eddrachillis Bay (2)
1/500 • f/5.6 • 15.0 mm • ISO 400 •
Canon EOS 600D
EF-S15-85mm f/3.5-5.6 IS USM
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Monkstone Point folds 1
Coastal traverse and geology from Waterwynch to Saundersfoot, Pembrokeshire
At Monkstone Point, grey, channel-fill sandstones of the Namurian age 'Millstone Grit Series' have been folded into a complex anticline with subsidiary folds, thrusts, and bedding plane slips which accommodate the 'space problem' in the core of the main anticline.
These sandstones are probably the equivalent of the prominent overturned sandstone ribs at Trevayne Point at the south end of Monkstone Bay.
At Monkstone Point, grey, channel-fill sandstones of the Namurian age 'Millstone Grit Series' have been folded into a complex anticline with subsidiary folds, thrusts, and bedding plane slips which accommodate the 'space problem' in the core of the main anticline.
These sandstones are probably the equivalent of the prominent overturned sandstone ribs at Trevayne Point at the south end of Monkstone Bay.
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