Recumbent Fold - Crackington Haven

On the north side of Crackington Haven, at the base of the cliff at Pencannow Point .
Bands of pale sandstones and grey shales have been deformed to form isoclinal recumbent folds at the end of the Carboniferous Period during the Variscan Orogeny.
Ref:
2785
Date:
2016-02-02 00:00:00.0
Location:
SX 1404 9674
Photographer:

Recumbent Fold - Crackington Haven

On the north side of Crackington Haven, at the base of the cliff at Pencannow Point .
Bands of pale sandstones and grey shales have been deformed to form isoclinal recumbent folds at the end of the Carboniferous Period during the Variscan Orogeny.
Ref:
2785
Date:
2016-02-02 00:00:00.0
Location:
SX 1404 9674
Photographer: