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The Eastern Steppe is a vast grassland in Eurasia, characterized by a harsh climate with extreme seasonal temperature variations, being higher, colder, and drier than its western counterpart. This region, stretching from the Altai Mountains to the Greater Khingan Range, includes Mongolia and surrounding areas. Despite the arid conditions, sparse grass grows, supported by seasonal rainfall and snowmelt from higher elevations.1

The Eastern Steppe's climate and geography historically prompted nomadic peoples to migrate, often southward towards Manchuria and northern China, or westward towards the more hospitable Western Steppe. This region's environment, while challenging, allowed for irrigated cultivation along streams and supported a complementary economy of pastoralists and oasis dwellers.21

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