Recumbent Folds - Little Strand (S3)

The cliffs at 'Little Strand' are thinly interbedded sandstones and shales , part of the Upper Carboniferous age Crackington Formation.
The Sedimentary rock layers were deformed , over a period of 80 -100 million years , during the Variscan Orogeny (mountain building period ) .
Complex folding at this location with Crumpled recumbent chevron folds .
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Location - South of Crackington Haven and Cambeak - Section 3
Ref:
722
Date:
2014-12-25 00:00:00.0
Location:
SX 1293.9600
Photographer:

Recumbent Folds - Little Strand (S3)

The cliffs at 'Little Strand' are thinly interbedded sandstones and shales , part of the Upper Carboniferous age Crackington Formation.
The Sedimentary rock layers were deformed , over a period of 80 -100 million years , during the Variscan Orogeny (mountain building period ) .
Complex folding at this location with Crumpled recumbent chevron folds .
------------------
Location - South of Crackington Haven and Cambeak - Section 3
Ref:
722
Date:
2014-12-25 00:00:00.0
Location:
SX 1293.9600
Photographer: