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Following the mountain-building episodes at the close of Permian times, the North American continent was subject to extensive erosion. Some regions seem to have been quite arid, others alternated from very wet to very dry seasons. Locally, volcanoes spewed out great lava flows. The temperatures seem to have been quite warm, perhaps even tropical, and forests and lush vegetation grew in many places. It was in this setting that the first dinosaurs appeared.

The primitive mammal-like reptiles, the Pelycosauria, became extinct, but they left behind a variety of advanced mammallike reptiles collectively termed the Therapsida. Despite therapsid abundance and diversity during much of the Triassic, only one kind is portrayed here -- the imposing carnivorous beast Cynognathus -- the four-legged animal in the foreground. Many therapsids were able to assume a more nearly upright posture at times, in sharp contrast to the sprawling mode of the pelycosaurs and the labyrinthodonts.

True conifers made their appearance in the drier, more upland settings and assumed a steadily more important role as humid, equable climates deteriorated. The petrified logs found in Triassic strata of the Petrified Forest National Monument in Arizona are of the conifer Araucarioxylon, the majestic tree that towers over the beginning of the Triassic section of the mural. Cycads, with their crowns of palmlike leaves, appeared in the late Carboniferous and multiplied to become an important component of the vegetation. Coexisting with the true cycads was another type of gymnospermous seed plant, cycadeoids, that had a generally similar appearance.

During the Triassic Period, Pangaea broke apart, and the continents we know today were formed. In eastern North America, the Atlantic Ocean began to form. During the Jurassic and Cretaceous periods, crustal plates collided and generated large quantities of molten rock that rose up to form what is now the Sierra Nevada in California. Mountain building affected all of western North America and led to the creation of the Rocky Mountains.


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