NK0630 : Recumbent Fold

taken 7 years ago, 3 km from Collieston, Aberdeenshire, Great Britain

Recumbent Fold
Recumbent Fold
This is a wider view of the fold in NK0630 : Devil's Study.

"A prominent westward closing recumbent syncline occurs in thick-bedded, partly gritty, psammitic greywackes and cordierite schists. The axial plane spaced cleavage (spacing c 0.5 cm) is uniformly developed across this profile." [Dr J R Mendum in 'Excursion Guide to the Geology of the Aberdeen Area', Scottish Academic Press, Edinburgh, 1987, Page 168, Excursion 13, Locality 4]

Psammite is metamorphosed sandstone and schist is metamorphosed mudstone. If you are mystified by 'axial plane spaced cleavage', see NK0630 : Axial Planar Cleavage.

See also NK0630 : More of the Recumbent Fold and NK0630 : Still More of the Recumbent Fold.
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NK0630, 12 images   (more nearby )
Photographer
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Date Taken
Friday, 2 July, 2010   (more nearby)
Submitted
Sunday, 4 July, 2010
Category
Geological feature   (more nearby)
Subject Location
OSGB36: geotagged! NK 060 309 [100m precision]
WGS84: 57:22.1223N 1:54.0736W
Camera Location
OSGB36: geotagged! NK 060 309
View Direction
NORTH (about 0 degrees)
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Image classification(about): Geograph
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