
Cottonwood Canyon State Park, near the campground, looking upstream toward the old Murtha barn and common buildings, the evening sun climbing the worn canyon sides. The Park retained some of the old ranch equipment.
Massive lava flows pushed around the lower John Day and Deschutes rivers over the course of several million years leaving them to find and carve new routes, often next to the very ‘plugs’ that filled their former canyons! Today, deep below the layers of hardened basalt that form the palisades and ramparts projecting out in tiers from the smooth full curves that rise above us, we look through 15 million years of accumulated history. The fine grained basalt shatters and fractures in line with their mineral structure under the forces of water, weather and gravity. Sagebrush and grasses dominate revealing an oddly ‘netted’ pattern across the sloping canyon hillsides, lit by the often harsh sunlight, illuminating some kind of subsurface movement of the thin soils that soften the slopes. The ‘net’ looks as if it had been draped across the land then stretched sideways catching and snagging on what lies beneath in a never the same, but consistent repeating pattern. It shows best when the angle of the sun comes across the pattern, not when it hits it head on or when clouds make it too diffuse. Coarse falls of shattered basalt spill down to the canyon’s bottom always seeking their angle of repose. The sagebrush steppe plant communities cover the surface and in their richness and vigor speak to the soils beneath. Along seeps and drainages cutting verticallly down the canyon’s face, spring lasts weeks longer, and species crowd in that you won’t see other than near the river. The surface botanical palette in this way reveals what lies beneath…if one knows what to look for. Cottonwood Canyon State Park is a great place to observe this. Continue reading