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. ”
