Columnar jointing

Definition and stakes

Various,  Encyclopaedia Britannica, 11th Edition…

“ Compression-joints are generally associated with the more intense movements which have involved shearing, minor-faulting and slaty cleavage. A minor cause of tension-jointing is shrinkage, due either to cooling or to desiccation. The most striking type of jointing is that produced by the cooling of igneous rocks, whereby a regularly columnar structure is developed, often called basaltic structure, such as is found at the Giant’s Causeway. This structure is described in connexion with modern volcanic rocks, but it is met with in igneous rocks of all ages. ”
Source: Gutenberg

Charles Sherwood Robinson,  Geology of Devils Tower National Monument…

“ At the base of the tower, below the bench, the rock is massive and jointing, poorly developed. Here the joints form large irregularly shaped blocks rather than columns.
Columnar joints form as the result of contraction within a rock mass. In igneous rock the contraction is the result of cooling; that is, the cold solidified rock requires less volume than the same rock when molten. As a rock cools it contracts, and the resulting tension is in a plane parallel to the cooling surface.
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Source: Gutenberg

Portrait of Thomas C. Chamberlin Thomas C. Chamberlin,  Geology (1906)

“ If the axis of a fold is not horizontal, that is, if it “plunges,” as it commonly does, a second set of joints roughly perpendicular to the first will be developed. If the uplift be dome-shaped and sufficient to develop joints, they will radiate from the center. It is true that joints affect regions where the rocks have not been folded, and where they have been deformed but little, but deformation to some extent is well-nigh universal.
Fig. 416.—Jointing in granite. The surface of the rock is a joint plane.
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Source: Gutenberg

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