A painted view in the Painted Hills in John Day Fossil Beds National Monument, Oregon. Rainfall from a passing storm brought out the colors of this natural wonder.
After the rain in the Painted Hills of eastern Oregon, the colors stand out in bold contrast. I live an hour and a half away from these strange geological features and patiently wait for the storms of fall to arrive.
The first image shows the view from the road to the Overlook parking area. The hills are located within the John Day Fossil Beds National Monument.
Though I’ve been here several times, I’d never hiked the 1/2 mile Painted Hills Overlook Trail. The easy trail leads you past this dramatic scene. Wow!
Here’s a closer view.
These hills are on the south side of the trail.
There are four short, easy trails and a more moderate longer trail a short distance away.
This photo shows part of the Painted Cove Trail after the rain.Continue reading
Steep knife-edged mountains arose from the plains centuries ago. Over time, torrential rains wore them down into rounded hills. Though plants tried to take root on their soil, none survived.
The Wise One summoned the artists of her tribe. She asked them to paint the hills in sacred colors. Pale green colors, from crushed sagebrush leaves and golden rabbitbrush blossoms, and black and red, from sumac trees, filled their brushes. The artisans painted the hills with broad brushstrokes and veiled the skies with delicate dabs of white.
It is easy to see why the Painted Hills are designated as one of Oregon’s Seven Wonders. The Painted Hills Unit of the John Day Fossil Beds National Monument , located nine miles northwest of Mitchell, Oregon, is 3,132 acres in size.
If you visit the Painted Hills after rainstorms move through the area, the colors will look more intense from the recent moisture. The colors are striking no matter what season it is. It is like looking at a parfait of luscious layers spread out before you. The deep crimson and black layers at the base of the hills contrast with the sandy browns and golds of upper layers.Continue reading