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Bashkir Anticlinorium
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Bashkir Anticlinorium

geological feature, Russia
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Learn about this topic in these articles:

  • Ural Mountains
    Ural Mountains
    / Geology

    
west of it, is the Bashkir Anticlinorium. Both are composed of layers (sometimes four miles thick) of ancient metamorphic (heat-altered) rocks—gneisses (metamorphic rocks separable into thin plates), quartzites, and schists—that are between 570 and 395 million years old.

    Read More

    
west of it, is the Bashkir Anticlinorium. Both are composed of layers (sometimes four miles thick) of ancient metamorphic (heat-altered) rocks—gneisses (metamorphic rocks separable into thin plates), quartzites, and schists—that are between 570 and 395 million years old.

    Read More