Chapter 68
Subterranean Stress, Breakwater Frequencies, and Mountain Routes
Early Spring of the 18th Year of the Obsidian Tide
As heavy mule trains were rerouted through winding secondary mountain passes to bypass northern refugee blockades, the regions braced for a harsh season where every bushel of grain required armed vigilance.
Ironhollow and Oakhaven
Beneath the high stone vaults of Ironhollow, the relentless rhythmic slamming of blind iron-clad automata continued unabated against the sealed barriers. Obsidian Pact engineering squads rushed additional forged iron braces and high-pressure hydraulic struts against the trembling bulkhead doors, desperately trying to prevent a catastrophic collapse into the upper municipal sectors as the stone framework groaned under the assault.
Simultaneously, with deep ocean floor disruptions echoing along the coast, harbor technicians at Oakhaven Harbor worked frantically along the heavy stone breakwaters. They fine-tuned brass resonance turbines and bled high-pressure steam lines to neutralize low-frequency acoustic vibrations that threatened to shatter the coastal defenses and flood the quays.
The Eastern Valleys
A short distance away across the rugged terrain, as the transition into the new season brought mounting pressures, agricultural administrators in the Eastern Valleys met with independent mule caravan leaders. Facing severe supply bottlenecks and regional unrest, they instituted formalized armed escort rotations and redirected heavy grain shipments through winding secondary mountain passes to bypass turbulent refugee blockades and secure vital winter food supplies.