The Uralian orogeny refers to the long series of geological events that raised the Ural Mountains starting in the Late Carboniferous and Permian periods of the Palaeozoic Era, ca. 318-299 and 299-251 Mya, and ending with the last series of continental collisions in Triassic-early Jurassic times. In terms of plate tectonics and continental drift, the Uralian resulted from a southwestern movement of the Siberian Plate, catching a smaller landmass, Kazakhstania, between it and the nearly completely assembled supercontinent, Pangaea. The mountains rose as the edge of Kazakhstania rode over the European plate. This event was the last stage in the assembly of Pangaea. The Ural Mountains (Russian: УраÌльÑкие гоÌры = УраÌл) also known simply as the Urals and as the Riphean Mountains in Greco-Roman antiquity, is a mountain range that runs roughly north and south through western Russia. ... The Carboniferous is a major division of the geologic timescale that extends from the end of the Devonian period, about 340 million years ago (mya), to the beginning of the Permian period, about 280 mya. ... The Permian is a geologic period that extends from about 280 to 248 million years before the present (mya). ... The Palaeozoic is a major division of the geologic timescale, one of four geologic eras. ... Plate tectonics (from the Greek word for one who constructs, τεκτων, tekton) is a theory of geology developed to explain the phenomenon of continental drift, and is currently the theory accepted by the vast majority of scientists working in this area. ... Portrayal of shifting continents The concept of continental drift was first proposed by Alfred Wagner. ... Map of Pangaea Pangaea (Greek for all lands) is the supercontinent that existed during the Paleozoic and Mesozoic eras, before the process of plate tectonics separated the component continents. ...
Orogeny (Greek for "mountain generating") is the process of mountain building, and may be studied as a tectonic structural event, as a geographical event and a chronological event, in that orogenic events cause distinctive structural phenomena and related tectonic activity, affect certain regions of rocks and crust and happen within a time frame.
Orogenic events occur solely as a result of the processes of plate tectonics; the problems which were investigated and resolved by the study of orogenesis contributed greatly to the theory of plate tectonics, coupled with study of flora and fauna, geography and mid ocean ridges in the 1950s and 1960s.
It was, in the context of orogeny, contested hotly by proponents of vertical movements in the crust (similar to tephrotectonics), or convection within the asthenosphere or mantle (geology).
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