_ _    _ _____  ___   __                       
 __      _(_) | _(_)___ / ( _ ) / /_   ___ ___  _ __ ___  
 \ \ /\ / / | |/ / | |_ \ / _ \| '_ \ / __/ _ \| '_ ` _ \ 
  \ V  V /| |   <| |___) | (_) | (_) | (_| (_) | | | | | |
   \_/\_/ |_|_|\_\_|____/ \___/ \___(_)___\___/|_| |_| |_|

Volgo–Uralia

In today's world, Volgo–Uralia has become a topic of great relevance and interest to a wide variety of people. Whether due to its impact on society, its relevance in the professional field, or its importance in history, Volgo–Uralia is a topic that does not leave anyone indifferent. Its influence extends globally, affecting different cultures and contexts in different ways. In this article, we will explore the different facets of Volgo–Uralia, analyzing its importance and impact on various aspects of daily life.

Volgo–Uralia is a crustal segment that, together with the Sarmatian Craton and the Fennoscandian Craton, makes up the East European Craton. Volgo–Uralia is the easternmost of the three segments and borders the Sarmatian Craton to the southwest along the Pachelma aulacogen and the Fennoscandian Craton to the northwest along the Volhyn–Central Russian aulacogen.

References

  1. ^ Gorbatschev, Roland; Bogdanova, Svetlana (December 1993). "Frontiers in the Baltic Shield". Precambrian Research. 64 (1–4). Elsevier Science Publishers B.V.: 3–21. Bibcode:1993PreR...64....3G. doi:10.1016/0301-9268(93)90066-B. ISSN 0301-9268. Retrieved 22 September 2015.