Stringers – Second Wave

Second Wave

Tatoosh Island, once a whaling and fishing camp now long abandoned, beckoned with whispers of the ancients, interrupted the horizon. In the shape of a crescent laying diagonally northwest to southeast, the island protected and sheltered a secluded bay known as the Cat’s Paw. Named so not for any particular land formations, but due to the glassine palette of cobalt sea whose surface reflected a pattern of tinfoil creases and blackening shadow on occasion of the breeze preceding a violent storm. A safe haven for those needing it during high seas or sudden marine anomalies.  Private home to puffin, sea otter, seal and grey whale.

Using the island as a compass, continuing one-quarter mile or so due west, a number of subsurface rock formations created an artifact know as the Boneyard. Appropriately named, for at this location death was as likely to occur as fog and the wreckage on the ocean floor spoke clearly of this. Given the right conditions this deadly reef would generate a perfectly formed wave known as Canoes. Breaking left to right, this manifestation would rise and fall with the pulse of the fickle Pacific, an indicator of her heartbeat. And so, flanked by colonnades of tortured Sitka Spruce, watchmen, telling a story of the harsh winds that often battered the coast, Caspar sat, his mind overwhelmed with the images of what he proposed to do.

Twenty four hundred miles to the north, winds approaching hurricane-force toppled trees and assaulted the Alaskan coast from Anchorage to Sitka. Winds measuring seventy-nine miles per hour were measured at a private Sitka airfield where small planes were being tossed about with the chaos of a toddler’s toys. Power-lines dropped haphazardly across homes and cars throughout the city, fishing boats were torn violently from their moorings, tethers of rope and cable snapping with the tension as if they were low-test monofilament. Energy from the fluke summer storm bled to the sea sending a heavy tidal surge southward. High surf warnings were being issued down the continental coast, the most significant pulses to be felt as tremendous swells from British Columbia to Northern Oregon at some point the following day.

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