The following is one of the lessons that I have learned from who knows where: When you see something interesting in the background, find something else interesting in the foreground to add to it. The red hills in eastern Oregon caught my eye. I am intrigued by sagebrush. One plus one equals three. I can still smell the wonderful aroma of sage as I look at this image.
This image of Oregon’s Painted Hills was taken from the main overlook. The overall scene was immense and beautiful. However, the bright mid-day sun made the image look flat. As I was surveying other images of the Painted Hills, I came across several dramatic images of the hills in late afternoon/early evening sun. I took the challenge to see if I could get close as I post-processed the image. Using a variety of adjustment layers and masks, I came up with the following image.
Driving up to Oregon’s Painted Hills, I saw this pastoral scene and stopped to capture the feeling. It was “high noon” and the sun was bright, but I still wanted to give it a try. To recreate the feeling I had, I processed the image in Topaz’s Impression and added a little texture in Photoshop. Who say’s you can’t make good images in bright noon day sun!
I have heard many people comment on the beauty of the Painted Hills of NE Oregon. Being from central Washington, I had never taken the 2-3 hour drive to see them. So on a recent trip to central Oregon, I thought I would go exploring. My purpose was more of a scouting trip than specifically to take images. I was there mid day on a very bright warm summer day. Even in this bright light, the colors of the hills radiated out. I look forward to coming back during the late afternoon sunlight.
Painted Hills is one of the three units of the John Day Fossil Beds National Monument, located in Wheeler County, Oregon. It totals 3,132 acres (1,267 ha) and is located 9 miles (14 km) northwest of Mitchell, Oregon. The Painted Hills are listed as one of the Seven Wonders of Oregon. Painted Hills is named after the colorful layers of its hills corresponding to various geological eras, formed when the area was an ancient river floodplain.
The black soil is lignite that was vegetative matter that grew along the floodplain. The grey coloring is mudstone, siltstone, and shale. The red coloring is laterite soil that formed by floodplain deposits when the area was warm and humid.[