The Mariana crust-sink fault at minus twenty-five thousand meters was a jagged, lightless deep gap of boiling liquid dark rock, crushed earth-shaking plates, and white-hot stone salt water.
Here, at the boundary where the Pacific oceanic crust was forced beneath the Eurasian land-wide shelf, the physical pressure exceeded two hundred and fifty tons of pressure. The water didn’t behave like normal fluid. It was hyper-dense, soaked with dissolved quartz dust, iron sulfide, and overload steam that vented from jagged hot-water chimneys at four hundred degrees.
Two of the Thalassic World-Eater Kraken’s master tentacles—each nearly three hundred yards in width, thick as fiery mountain ridges and coated in miles of linked black hard shell armor—dropped into the deep pit.
They coiled around the exposed edge of the Pacific land-wide plate with the slow, crushing inevitability of a world-size vice.
The suction cups lining the tentacles were eighty feet across, their internal rings of living steel teeth churning into the ancient dark rock bedrock like heavy-duty bucket-wheel excavators. With every flex of the Kraken’s massive high-pressure musculature, the land-wide shelf groaned in painful protest.
Inside Titus’s command module, the artificial gravity compensators shrieked as the entire fourteen-ton living bathysphere was buffeted by the rising blast waves.
