Geological Dating Places Yonaguni’s Bedrock in the Miocene Epoch

The stone beneath this ‘ruin’ formed millions of years before humans.

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The Miocene epoch saw significant tectonic shifts that shaped many modern island arcs in East Asia.

The sandstone composing the Yonaguni Monument dates to the Miocene epoch, roughly 5 to 23 million years ago. This geological age far predates human existence, confirming that the base material is entirely natural. The debate does not concern the rock’s origin but whether humans modified its surfaces. Miocene sandstones often display pronounced bedding and joint systems. These structural weaknesses create planes along which blocks separate cleanly. Understanding the rock’s deep-time origin reframes the site as part of a much older geological narrative. Any human involvement would represent modification of ancient bedrock rather than construction from quarried blocks.

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The time-scale shock is profound. The stone itself formed when early apes had not yet evolved into humans. Millions of years of tectonic compression prepared the fractures now visible underwater. If humans later shaped these fractures, they worked atop a foundation forged in prehistoric oceans. The monument thus compresses geological deep time and potential human agency into a single structure.

This intersection of epochs highlights how archaeology often depends on geological context. Natural processes create canvases that humans may later modify. Yonaguni embodies that layered timeline, spanning from Miocene sedimentation to modern diving expeditions. The sheer temporal depth intensifies its mystique within forbidden archaeology discourse.

Source

Encyclopaedia Britannica

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