Vietnam or Thailand ? Vote for the TOP Country of the Week !

Updated: May 21, 2025


The meridian altitude of the fifth day has to be looked for where ocean-life, with its sauria and innumerable animals, gave its impress to organic life on earth, and the air was filled with inhabitants: geology calls such a time the secondary period of trias, Iura, and chalk.

And, knowing that reptiles that walked upon their hind legs and shared many of the anatomical characters of birds did once exist, it becomes a very important question whether the tracks in the Trias of Massachusetts, to which I referred some time ago, and which formerly used to be unhesitatingly ascribed to birds may not all have been made by Ornithoscelidan reptiles; and whether, if we could obtain the skeletons of the animals which made these tracks, we should not find in them the actual steps of the evolutional process by which reptiles gave rise to birds.

The lava-sheets have since undergone extensive denudation, and are intersected by valleys and depressions eroded down through them into the sandstone floor beneath; and though the precise geological period at which they were extruded must remain in doubt, it appears probable that they may be referred to that of the Trias. Green. "On the Geology of the Cape Colony," Quart. Jour. Geol.

As the Orthoceras had never been met with in the marine Muschelkalk, much surprise was naturally felt that seven or eight species of the genus should appear in the Hallstadt beds, assuming these last to belong to the Upper Trias.

Ceratites nodosus, Schloth. Muschelkalk, Germany. The next member of the Trias in Germany, the Muschelkalk, which underlies the Keuper before described, consists chiefly of a compact greyish limestone, but includes beds of dolomite in many places, together with gypsum and rock-salt. This limestone, a formation wholly unrepresented in England, abounds in fossil shells, as the name implies.

Revolutions have failed to shake it; persecution has not broken it; it has gained strength in blood and tears, and we may believe, after thirteen centuries of trial, that the Roman faith will disappear from Ireland only with the name of Patrick and the last Irishman." He edited only two volumes: the first under the title of "Trias thaumaturga " containing the various lives of St. Patrick, St.

We know that the dry land of the Trias absolutely teemed with reptiles of all groups except Pterodactyles, Snakes, and perhaps Tortoises; there is every probability that true Birds existed, and Mammalia certainly did. Of the inhabitants of the Permian dry land, on the contrary, all that have left a record are a few lizards.

The two mammals of the Trias, also, appear to belong to Australian groups. Every one is aware of the many curious points of resemblance between the marine fauna of the European Mesozoic rocks and that which now exists in Australia.

So that, at the present time, the Labyrinthodont Fauna of the Carboniferous rocks is more extensive and diversified than that of the Trias, while its chief types, so far as osteology enables us to judge, are quite as highly organized.

In Wurtemberg there are two bone-beds, namely, that containing the Microlestes, which has just been described, which constitutes, as we have seen, the uppermost member of the Trias, and another of still greater extent, and still more rich in the remains of fish and reptiles, which is of older date, intervening between the Keuper and Muschelkalk.

Word Of The Day

potsdamsche

Others Looking