Deposits of the same age, found on the flanks of the Pyrenees, contain also a great number of shells common to the Paris and London areas, and three or four species only which are common to the cretaceous formation. The calcareous division consists often of a compact crystalline marble, full of nummulites (see fig. 189.), shells of the class _Foraminifera_. [Illustration: Fig. 189. _Nummulites_. Peyrehorade, Pyrenees. _a._ external surface of one of the nummulites, of which longitudinal sections are seen in the limestone. _b._ transverse section of same.] The nummulitic limestone of the Alps is often of great thickness, and is immediately covered by another series of strata of dark-coloured slates, marls, and fucoidal sandstones, to the whole of which the provincial name of "flysch" has been given in parts of Switzerland. The researches of Sir Roderick Murchison in the Alps in 1847 enable us to refer the whole of these beds to the Eocene period, and it seems probable that they most nearly coincide in age with the Lower Eocene. They enter into the disturbed and loftiest portions of the Alpine chain, to the elevation of which they enable us therefore to assign a comparatively modern date. The nummulitic formation, with its characteristic fossils, plays a far more conspicuous part than any other tertiary group in the solid framework of the earth's crust, whether in Europe, Asia, or Africa. It often attains a thickness of many thousand feet, and extends from the Alps to the Apennines. It is found in the Carpathians, and in full force in the north of Africa, as, for example, in Algeria and Morocco. It has also been traced from Egypt into Asia Minor, and across Persia by Bagdad to the mouths of the Indus. It occurs not only in Cutch, but in the mountain ranges which separate Scinde from Persia, and which form the passes leading to Caboul; and it has been followed still farther eastward into India. Some members of this lower tertiary formation in the central Alps, including even the superior strata called _flysch_, have been converted into crystalline rocks, and changed into saccharoid marble, quartz, rock, and mica-schist.[206-A] EOCENE STRATA IN THE UNITED STATES.