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What (who) is Uralian - definition

THE LONG SERIES OF LINEAR DEFORMATION AND MOUNTAIN BUILDING EVENTS THAT RAISED THE URAL MOUNTAINS

Uralian orogenic belt; Uralian Orogenic Belt; Ural orogeny; Ural Orogeny; Uralides; Uralian orogen; Uralide orogeny

Uralian

MOUNTAIN RANGE IN RUSSIA

Ural mountain range; Uralskiy Khrebet; Urals; The Urals; Ural'skiy Khrebet; Ural Soviet; Uralskiye; Ural Mountain; Ural mountain; Ural Mountains (Russia); Ural Mountains Region, Russia (Federation); Ural Mountains Region, Russia; Ural Mountains Region; Ural Mountains Region (Russia); Ural Mountain Range; Uralsky Khrebet; Middle Urals; Trans-Urals; Uralian; Uralskiye gory; The Ural Mountains; Ural mountains; Fauna of the Ural Mountains; The Ural mountains; Geology of the Ural Mountains

·adj ·Alt. of Uralic.

Uralian orogeny

The Uralian orogeny refers to the long series of linear deformation and mountain building events that raised the Ural Mountains, starting in the Late Carboniferous and Permian periods of the Palaeozoic Era, 323–299 and 299–251 million years ago (Mya) respectively, and ending with the last series of continental collisions in Triassic to early Jurassic times.

https://en.wikipedia.org/wiki/Uralian_orogeny

Main Uralian Fault

IN THE URAL MOUNTAINS OF RUSSIA

The Main Uralian Fault (MUF) runs north–south through the middle of the Ural Mountains for over 2,000 km. It separates both Europe from Asia and the three, or four, western megazones of the Urals from the three eastern megazones: namely the Pre-Uralian Foredeep, West Uralian, and the Central Uralian to the west, and the Tagil-Magnitogorskian, East Uralian, and Transuralian to the east.

https://en.wikipedia.org/wiki/Main_Uralian_Fault

Wikipedia

Uralian orogeny

The Uralian orogeny refers to the long series of linear deformation and mountain building events that raised the Ural Mountains, starting in the Late Carboniferous and Permian periods of the Palaeozoic Era, c. 323–299 and 299–251 million years ago (Mya) respectively, and ending with the last series of continental collisions in Triassic to early Jurassic times.

The region affected by the orogeny, the Uralian orogenic belt or the Uralides, is usually thought of as the boundary between Europe and Asia. It extends from the Aral Sea to Novaya Zemlya, and it includes in addition to the Ural Mountains, the Pay-Khoy Ridge of northwest Russia and the Mugodzhar Hills of northwest Kazakhstan. Its total length is about 3,500 kilometres (2,200 mi), of which the Ural Mountains are about 2,500 km (1,600 mi).

At the latitude of the Middle-Urals Ring Structure (c. 56° N, between Perm and Ufa) the Ural mountains have an eastward-convex bend. It has been proposed that the Precambrian Middle-Urals Ring Structure caused a disturbance in the orogeny leading to the formation the bend.

https://en.wikipedia.org/wiki/Uralian orogeny