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As the surface of the calcareo- argillaceous plain of Pampean formation, on the northern side of the wide valley of the Colorado, stands at about the same height with the mortar- like cemented gravel capping the sandstone on the southern side, it is probable, considering the apparent equability of the subterranean movements along this side of America, that this gravel of the Rio Negro and the upper beds of the Pampean formation northward of the Colorado, are of nearly contemporaneous origin, and that the calcareous matter has been derived from the same source.

The strata in this space consist, in general, of sand-stone, coal, lime-stone or marble, iron-stone, and marl or argillaceous strata, with strata of analogous bodies, and the various compositions of these.

The soil of the Mamelles, like almost all that of the middle of the Peninsula, which appears to lie upon argillaceous lava, in a state of decomposition, is much better. There are even to be found, here and there, some spots that are very fertile; this is the arable land of the inhabitants.

Upper Lias, argillaceous, with Ammonites striatulus. FOREIGN. Keuper beds of Germany. Cassian or Hallstadt beds, with rich marine fauna. BRITISH. Wanting. FOREIGN. Muschelkalk of Germany. BRITISH. Bunter or Lower New Red sandstone of Lancashire and Cheshire. FOREIGN. Bunter-sandstein of Germany. BRITISH. Upper Permian of St. Bees' Head, Cumberland. FOREIGN. Dark-coloured shales of Thuringia.

Here the river formed a cataract of about two feet, falling over some argillaceous ironstone: and as the waters glittered in the moonlight I listened with awe to the unwonted murmur of this mysterious stream which poured through the heart of a desert, by its single channel, that element so essential to the existence of all animals. June 11.

They cover nearly half the island, and near its centre, at Castrogiovanni, reach an elevation of 3000 feet. They consist principally of two divisions, the upper calcareous and the lower argillaceous, both of which may be seen at Syracuse, Girgenti, and Castrogiovanni.

It was then observed that, in places where the secondary formations are unaltered, the uppermost consist of common Apennine limestone with nodules of flint, below which are shales, and at the base of all, argillaceous and siliceous sandstones. In the limestone fossils are frequent, but very rare in the underlying shale and sandstone.

Here numerous proofs are seen of submarine eruptions, by which the argillaceous and sandy strata were invaded and cut through, and tufaceous breccias formed. Inclosed in these breccias are many angular and hardened fragments of laminated clay in different states of alteration by heat, and intermixed with volcanic sands. View of the Isle of Cyclops, in the Bay of Trezza.

Here is the same induration of sandstone by means of fusion, that in the argillaceous strata has produced jasper. But oblique veins of jasper are represented as traversing these last strata; now this is a fact which is not conceivable in any other way, than by the injection or transfusion of the fluid jasper among those masses of indurated strata.

Box-tree flats, of more or less extent, were intercepted by abrupt barren craggy hills composed of sandstone, which seemed to rest on layers of argillaceous rock. The latter was generally observed at the foot of the hills and in the bed of the river; it had in most places been worn by the action of water.