Note: As you read this, Peggy and I are in Amsterdam at the beginning of a Rhine River cruise between Amsterdam and Basel. I’ve been scheduling posts ahead of time so I can maintain a more regular presence on WordPress than I have been able to for the past several months. My goal for now is once a week on Fridays. At this rate, I already have enough material on the Southwest national parks we visited in April and May to keep going for three months. LOL. I may never catch up.
Checkerboard Mesa is the dominant geological feature of the eastern section of Zion National Park. (Photo by Peggy Mekemson.)
Rudyard Kipling said it:” East is East and West Is West, and never the twain shall meet.” That’s not true of Zion National Park, of course, but the eastern section of the Park will provide you with a significantly different experience than you have down in the Canyon or the western sections of Zion. Checkerboard Mesa shown above is the primary example. We can thank ancient sand dunes laid down in an early-Jurassic-era, Sahara-size desert that covered significant portions of what is now Nevada, Arizona, Utah, and Colorado 190 million years ago. The horizontal lines are caused by what is known as cross-bedding of the dunes. The vertical lines are caused by breaks in the cross bedding caused by freezing and thawing. It was thought that the results resembled a checker board, thus the name. Peggy and I found the mesa a fun subject for photography.
I moved back to provide a broader perspective on the Mesa using pine trees for framing.Peggy added a photo of the massive chunk of Navajo Sandstone reaching toward the sky. It’s quite a scroll down. Grin. (Photo by Peggy Mekemson.)If you are driving up from Zion Canyon, this will be your first view of Checkerboard Mesa.We were both interested in the cross-bedding. Peggy took this interesting side view.(Photo by Peggy Mekemson.)This was the view looking a bit farther north of Peggy’s photo.This was the view looking south.
If you have been in Zion and either entered or left by the east entrance/exit, you know there is much more to East Zion National Park than Checkerboard Mesa. One thing that fascinated Peggy was the alcoves that may eventually lead to towering arches such as those found in Arches National Park.
Looking toward the top of a Navajo sandstone mountain, you can see how the ridge coming down the front is eroding from both sides. This may eventually lead to an arch. (Photo by Peggy Mekemson.)This provides a straight on view of the alcove on the right of the ridge. Note how deep the alcove is. (Photo by Peggy Mekemson.)Another alcove. Alcoves and arches are created when a harder capstone is on top of a softer stone that erodes more rapidly. (Photo by Peggy Mekemson.)And another alcove photographed by Peggy. Had there been more, I am sure that she would have photographed them as well! (Photograph by Peggy Mekemson.)
While Peggy was busy photographing wannabe arches, I was concentrating on other landmarks of East Zion National Park.
I found this landmark rather impressive.I wondered about the huge chunk of rock that left behind a bright red scar in this landmark. The other side is one of the alcoves that Peggy photographed. Another prominent Mesa standing out like the prow of an ocean liner.A mesa on a mesa. Peggy was impressed with its color. (Photo by Peggy Mekemson.)I’ll close today with this interesting photo that Peggy took of shrubs and small trees growing on cross-bedded sandstone. I thought, ‘Wow, this would make one heck of a challenging puzzle!’ (Photo by Peggy Mekemson.)