Shrinkage

Definition and stakes

William O. Crosby,  Common Minerals and Rocks

“ Contraction joints or shrinkage cracks.—That many cracks in rocks are due to shrinkage, there can be no doubt. The shrinkage may result from the drying of sedimentary rocks; but more generally from the cooling of eruptive rocks. Every one has noticed in warm weather, the cracks in layers of mud or clay on the shore, or where pools of water have dried up; and we have already seen that these sun-cracks are often preserved in the hard rocks. They have certain characteristic features by which they may be distinguished from the joints of the first class. ”
Source: Gutenberg

C. W. D. Boxall, Henry Adams, F. W. Loasby,  Cassells' Carpentry and Joinery (1907)

“ Radially, or in the direction of the medullary rays, the shrinkage is only slight, as shown by the board f, Fig. 126. If the log is whole, the shrinkage causes shakes and wind-cracks; if cut up into planks or quartering, the shrinkage is determined by the position of the annual rings, and, with care, shakes are not caused. The wood curls or bends breadthwise, with the edges turning on the side which is farthest away from the heart. This is illustrated at e, g, and h, Fig. 126. This circumstance must always be considered in fixing timber in position. ”
Source: Wikisource

William Noyes,  Wood and Forest

“ If the bark is left on and evaporation hindered, the splits will not open so wide.
There is still another effect of shrinkage. If, immediately after felling, a log is sawn in two lengthwise, the radial splitting may be largely avoided, but the flat sides will tend to become convex, as in Fig. 39. This is explained by the fact that circumferential shrinkage is greater than radial shrinkage.
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Source: Gutenberg

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