Teaching Earth Sciences - Earth Science Teachers' Association
Teaching Earth Sciences - Earth Science Teachers' Association
Teaching Earth Sciences - Earth Science Teachers' Association
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Figure 5 Plunge refers to the dip of the fold axis. In a non-plunging fold, it is<br />
horizontal.<br />
Figure 3 A symmetric fold has limbs of equal length: the fold axes are<br />
perpendicular to the enveloping surface. In an asymmetric fold, the limbs are<br />
unequal, and the axial planes are oblique to the enveloping surface.<br />
Figure 4 Fold attitude is defined by the orientation of the axial plane and the<br />
younging directions of the limbs.<br />
Figure 6 The inter-limb angle of a non-plunging fold can be calculated by<br />
subtracting the sum of the dips of the two limbs from 180˚.<br />
described as ‘upright’. In 4b, the axial plane has moved<br />
away from the upright, but the younging direction in both<br />
limbs is upwards – the fold is therefore said to be ‘inclined’.<br />
4c shows a fold in which the axial plane is so inclined that<br />
the younging direction in one limb is now downwards,<br />
allowing the fold to be defined as ‘overturned’. In 4d,<br />
the axial plane is more or less horizontal and the fold is<br />
‘recumbent’. It is the inclined fold that is most frequently<br />
mis-identified as asymmetric.<br />
Plunge refers to the inclination of the fold axis: a plunging<br />
fold has an inclined axis (Figure 5b); if the axis is horizontal,<br />
the fold is described as non-plunging (Figure 5a). The<br />
attitude of the axial plane is irrelevant.<br />
The inter-limb angle, as the name implies, is the angle<br />
between the limbs. In a non-plunging fold, it can be<br />
calculated by adding together the dips of the two limbs,<br />
and subtracting them from 180˚: the remainder is the interlimb<br />
angle, as shown in Figure 6. This gives 5 categories of<br />
fold (Figure 7):<br />
• gentle folds have an inter-limb angle of<br />
120˚ – 180˚.<br />
• open folds, in which the inter-limb angle is<br />
70˚ – 120˚.<br />
Figure 7 Five categories of fold can be recognised based in inter-limb angles.<br />
• close folds with an inter-limb angle of 30˚ – 70˚.<br />
• tight, in which the onter-limb angle is less than 30˚<br />
• isoclinal (literally, “equal dip”) if the limbs are<br />
approximately parallel.<br />
In some systems of classification, the ‘gentle’ and ‘open’<br />
categories are merged, as are the ‘closed’ and ‘tight’<br />
for inter-limb angles greater than, and less than 90˚<br />
respectively.<br />
Figure 8 illustrates the difference between cylindrical folds,<br />
which are persistent and have straight hinge lines (8a), and<br />
non-cylindrical folds, which are impersistent (8b).<br />
www.esta-uk.net Vol 35 No 1 2010 <strong>Teaching</strong> <strong>Earth</strong> <strong><strong>Science</strong>s</strong> 53