Recumbent Fold - Crackington Haven (S3)

At the base of the cliff at Pencannow Point on the north side of Crackington Haven.
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.
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Crackington Haven is to the north of Boscastle in Section / Gallery 3
Ref:
2785
Date:
2016-02-02 00:00:00.0
Location:
SX 1404 9674
Photographer:

Recumbent Fold - Crackington Haven (S3)

At the base of the cliff at Pencannow Point on the north side of Crackington Haven.
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.
---------------------
Crackington Haven is to the north of Boscastle in Section / Gallery 3
Ref:
2785
Date:
2016-02-02 00:00:00.0
Location:
SX 1404 9674
Photographer: