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.
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.
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.
While Peggy was busy photographing wannabe arches, I was concentrating on other landmarks of East Zion National Park.