Many different causes likely contributed to the fall of the Roman Empire, in the various stages of that phenomenon. But new research has identified a significant factor that may have pushed things past the final tipping point, sealing the Empire’s fate and guaranteeing its status as historical memory. Fresh geological findings from Iceland suggest that a dramatic cooling event known as the Late Antique Little Ice Age (LALIA), associated with a notable global temperature drop, likely played a much larger role in the fall of the Roman Empire than previously understood. For years, scholars have speculated that shifts in Earth's climate may have weakened the once-mighty Roman Empire, leaving it vulnerable to external threats, economic trouble, and internal conflict. Now
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