Javelina

Sedona sits at the southern edge of the Colorado Plateau, where roughly 300 million years of sediment compression produced the red rock formations the region is known for. The color comes from iron oxide — rust, essentially — baked into Schnebly Hill sandstone over hundreds of millions of years. The formations aren't static. They're eroding continuously, shedding material into the creek beds below at a pace slow enough to feel permanent.

The vortexes — four main sites, Cathedral Rock, Bell Rock, Airport Mesa, and Boynton Canyon — are described by locals and visitors as concentrations of energy emanating from the earth. The geology beneath each site shares certain characteristics: layered, fractured stone with high iron and quartz content. Whether that produces anything measurable is contested. What isn't contested is the landscape itself, which has a way of demanding attention that most places don't.

The javelina, Pecari tajacu, has roamed this terrain for millions of years. They're not pigs — they're peccaries, a separate lineage entirely. They move through the desert brush in family groups, unhurried, as though they've correctly assessed that nothing out here is a serious threat to them. They're probably right.