58 U \i:ini: i U x \ OF 8T. ANDREWS. 



only uses to which some of the other molluaks are applied are 

 in the amateur manufacture of ornaments, such as shell pin- 

 cushions from various univalves and bivalves, bracelets from 

 Nassa incrassata and Trochus cinerarias, after the latter has 

 had its nacreous layer exposed by an acid. 



The rock-boring shell-fish are five in number, though only 

 one exercises any great influence on the disintegration of the 

 rocks — viz. Pkolas crispata, which often swarms in the shale 

 and sandstone, and takes the place of the P/iolas dactyl us of 

 the chalk rocks of the south. Pholas Candida occurs too rarely 

 to require special mention in this respect ; and the same may 

 bo said of Sa.ricara rtti/osa. The excavations of PateUa rnl- 

 (jata and Chiton fascicular is in sandstone show that no special 

 boring-organ is necessary for this purpose. The latter species 

 sometimes scoops out considerable cavities in sandstone, in 

 which it reposes. The only wood-borer is Xylophaga dorsal 'is. 

 In taking, under this head, a general survey of the boring 

 forms, it is found that they belong to at least three invertebrate 

 subkingdoms, viz. the Protozoa, Mollusca, and Annulosa. In 

 the first are boring sponges ; in the second, Bryozoa and various 

 mollusks; in the third, sea-urchins, gephyreans, annelids, and 

 cirri pedes. 



The sponges appear to bore only into calcareous substances, 

 such as shells and limestone. The Bryozoa perforate shells ; 

 the mollusks proper, limestone, sandstone, aluminous shale, 

 gneiss and other rocks, wood, wax, shells, &c. ; the annelids 

 tunnel shells and rocks of various kinds; the sea-urchins cal- 

 careous rocks, gneiss, granite, and other rocks ; the gephyreans 

 and eirripedes shells and limestone. Good opportunities are 

 afforded at St. Andrews for studying the boring-action of the 

 mollusks and annelids. Pholas crispata and Leucodore ciliata 

 are equally abundant, and must exercise as much influence 

 on the disintegration of the sandstone and shale between tide- 

 marks as the boring sponges amongst the shells in deep water; 

 while, Patella, Chiton, Saxicava, and Dodecaceria are also 

 frequent. 



The theories which have been promulgated to explain the 

 mode by which these various creatures perforate materials so 

 diverse may be ranged round two great centres, viz. the 



