The shift from mountain rock to unending ice was not a gradual blend. It was a razor-straight boundary marked by a line of frozen grey talus.
At four o’clock in the afternoon on Day 120, Kezra Venn took a single long stride across a frost-heaved boulder and set her right boot onto the hard, blue-white crust of permanent alpine firn.
Under the hobnails of her boot, the snow didn’t crunch like fresh valley powder. It squeaked with the dense, glassy pushback of ice that had survived fifty summers of high mountain sun. The air that hit her face was instantly colder, stripped of every trace of resin, soil, and vegetable moisture. He smelled only of pure stone cold and frozen ozone.
She stood on the threshold. She unbuttoned her coat just enough to slip her bonded notebook from its waxed inner pocket.
On the progression page, the list of checked ecologies gleamed in dark, settled ink: 1. Upland Clay & Limestone (Kilnstep) 2. Fiery Ridge Scree (Blackglass) 3. Bitter salt Flats & Basalt (Saltglass) 4. Subalpine Resin Canopy (Hushwood) 5. Montane Underground Basin (Alderfast)
And beneath them, awaiting its final sign-off: 6. High Alpine Cryosphere (Windpit & Spine Crest) — PENDING CIRCUIT
