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Above the sandy bed d-f, the stratum c is somewhat disturbed, while the next bed, b, is much less so, and a not at all; yet all these beds, c, b, and a, must have undergone an equal amount of pressure with d, the points a and g having approximated as much towards each other as have d and f.
The chief result has obviously been due to the bending; but, in proof of elongation, it will be observed that the thickness of the bed d-f is now about four times greater in those parts lying in the main direction of the flexures than in a plane perpendicular to them; and the same bed exhibits cleavage planes in the direction of the greatest movement, although they are much fewer than in the slaty strata above and below.
Vertical section of slate rock in the cliffs near Ilfracombe, North Devon. Scale one inch to one foot. Fine-grained slates, the stratification being shown partly by lighter or darker colours, and partly by different degrees of fineness in the grain. d, f. Subsequently Mr. The points d and f in the stratum d-f must have been originally four times as far apart as they are now.
We're stuck here, and " I did not wait to hear what he wished to say further, but neutralized and collapsed him with the other aboriginals. The portatron apologized for having caused me inconvenience; but of course it was not its fault, so I did not neutralize it. Using it for d-f, I quickly located the culprit, Foraminifera 9-Hart Bailey's Beam, nearby.
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