Paleoanthropological and genetic evidence points to two primary dispersal corridors used by Homo sapiens migrating out of Africa:
Groups moved from the Horn of Africa across the Bab-el-Mandeb strait (lower sea levels created a land bridge) along the southern coast of the Arabian Peninsula—through modern-day Yemen and Oman. From there, they spread rapidly along the coastlines of the Indian Ocean, reaching the Indian subcontinent, Southeast Asia, and eventually Australasia (Australia and New Guinea) by at least 50,000–65,000 years ago. This route favored marine resources and warmer climates.
Another wave crossed the Sinai Peninsula into the Levant (modern Israel, Palestine, Jordan, Lebanon, Syria). From this gateway, populations fanned out into the interior of Eurasia—north into Anatolia and Europe, and east into Central Asia. This corridor was likely used earlier (perhaps 100,000+ years ago) but saw major expansion later, around 45,000–50,000 years ago.
Both routes were shaped by climate fluctuations: "Green Sahara" periods opened corridors; glacial lows exposed land bridges (like the Bering Land Bridge later). Access to freshwater, coastal shellfish, and game determined the pace and direction of movement.