
The Atacama Desert in Chile
Photo Credit: © Dr. Benedikt Ritter-Prinz
Scientific Frontline: Extended "At a Glance" Summary: Atacama Desert Hyperaridity
The Core Concept: The hyperarid core of the Atacama Desert in Chile established its extreme dryness approximately 45 million years ago. This establishes it as one of the longest continuously dry terrestrial environments on Earth.
Key Distinction/Mechanism: Unlike temperate regions where precipitation drives continuous erosion and sediment transport, hyperarid regions experience less than two millimeters of annual rainfall. This severe water limitation results in extraordinarily slow surface processes, effectively preserving the landscape over geological timescales.
Origin/History: Previous scientific consensus placed the onset of Atacama Desert aridity in the Early to Mid-Miocene (10 to 20 million years ago). Recent analysis pushes this timeline back by 20 million years, indicating that extreme aridity was established shortly after the global cooling that followed the Early Eocene Climate Optimum (EECO).
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