Page:Geology and Mineralogy considered with reference to Natural Theology, 1837, volume 1.djvu/84

 80 and preserved -together with marine shells; such are the Subapennine marine formations, containing the remains of Elephant, Rhinoceros, &c. and the Crag of Norfolk.

Secondly, we have similar remains of terrestrial quadrupeds, mixed, with fresh-water shells, in strata formed during the same epoch, at the bottom of fresh-water lakes and ponds; such as those which occur in the Val D'Arno, and in the small lacustrine deposite at North Cliff, near Market Weighton, in Yorkshire. (See Phil. Mag. 1829, vol. vi. p. 225)

Thirdly, we have remains of the same animals in caverns and fissures of rocks, which formed parts of the dry land during the more recent portions of the same period. Such are the bones collected by Hyæanas, in the caves of Kirkdale, Kent's Hole, Lunel, &c.: and the bones of Bears in caverns of the limestone rocks of central Germany, and the Grotte d'Osse|les, near Besançon. Such also are the bones of the osseous breccia, found in fissures of limestone rocks on the northern shores of the Mediterranean, and in similar fissures of limestone at Plymouth, and in the Mendip Hills in Somerset. These are derived chiefly from herbivore which fell into the fissures before they were partially filled with the detritus of a violent inundation.

Fourthly, we have the same remains contained in deposites of diluvial detritus, dispersed over the surface of formations of all ages.

As I have elsewhere (Reliquiæ Diluvianæ) entered into