“A geologic age before, the runoff from Alakan Glacier high up in the Quilak Mountains chewed through a granite ridge to form a narrow canyon fifteen miles long. A millennium before, a massive earthquake exacerbated a fault in the ridge. Half of it cracked and slid off to the southwest. It left behind a V-shaped wedge between the confluence of two watercourses, which would one day be named Gruening River on the south side and Cataract Creek on the north. The tip of the vee pointed due west. The ...surface of the wedge was flat and topped with a thick slice of verdant soil raised a hundred feet in the air by the earthquake. That earthquake had also fractured a way to the surface through the granite uplift for an underground spring. The spring’s outflow trickled down the south face of the wedge, over time carving a channel for a little stream too steep to support a salmon run and too shallow to be good for anything but watering the blueberry bushes that grew thickly along its sides. In spring, this slope was first to thaw, snow and ice giving way to a fairyland of wildflowers, the brash orange and yellow florets of western columbine, the shy blue of forget-me-nots, the noxious brown blooms of chocolate lilies, the elegant pink paintbrush, and the dignified purple monkshood.MoreLessRead More Read Less
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