It was terrain that lay entirely off any established trail, accessible only by a steeply graded descent through loose rock and sparse vegetation from the ridge above.
On the morning of Thursday, July 2nd, 2026, Dr. Reeve led a team of four investigators into that search zone at 7:00 in the morning, entering from the ridge above and descending the western face in a systematic line search pattern.
The air at that elevation an hour smelled of sulfur, faint but consistent. The planetary exhalation of the geology beneath them, a smell that visitors to the geyser basins found dramatic, but that the park’s long-term staff had learned to notice the way others notice weather as a kind of background information about the state of things below the surface.
The rock here was pale gray riolyte, fractured by thermal stress into slabs and blocks that tilted at irregular angles, creating a series of shelves and depressions that held shadow long after the sun had cleared the ridge to the east.
