Here’s the Queen with a bit of decorative hat. There is beauty even in the changes of the seasons, though I am fond of autumn’s color and mildness, and haven’t yet had my fill. I will have to keep autumn’s memory close by being satisfied with the photographs that stay – no matter how wild the weather gets outside.
An Autumn Hang-Up
Autumn is definitely upon us. Everywhere I look there is evidence of summer’s long past retreat and autumn’s complete domination. Two of the trees in my yard are totally bare. Brown, crunchy leaves are spread under their empty branches, and while I find it rather satisfying to stomp through the noisy litter, I’m not too thrilled at the prospect of the raking job that is on the agenda for this week-end – that is, if it doesn’t snow as is predicted.
My red maple is still fully dressed, and lovely. Deep reds at the very top meld into bright reds and then orange-reds towards the bottom of the tree. I’ve been waiting for the sun to shine to take a few photos, but without any luck. It’s raining now, and I haven’t the heart to even check the weather report for tomorrow.
Lots of photographers seem to be attracted to the simple leaf this week. I’ve seen a few outstanding examples. A pair of brown leaves here, and here is another favorite, with a great twist, and then one more product of autumn’s touch, and finally one with a foreign flavor.
How soon until we are all taking photos of that white fluffy stuff? Too soon, I’m thinking. Way too soon.
The Painted Desert – Not Quite What You Expected?
No saguaro or organ pipe cacti or other familiar succulents in this desert. The Painted Desert in northeastern Arizona really isn’t a desert at all – you need to go further west and south for real desert – but is located near short grass plains or desert grasslands. The Painted Desert is barren red Chinle mudstone. Various combinations of minerals provide the different coloration – red is iron oxide and the white is gypsum.
These formations were formed 220 to 225 millions of years ago, and though the rocks are not high, they are approximately 800 feet thick. No drilling for water through this stuff.
Unfortunately, we were traveling through the area in early afternoon. I would have liked to have captured the colors nearer sunset when the reds would reflect deeper colors. It is still an amazing drive, though, through an ancient world that is well preserved. An incredible number of fossils and archeological ruins are found throughout the park.
Not Just Ordinary Rocks
While Arches National Park in northeastern Utah is best known for its hundreds of red rock arches, many rock formations are almost equally as famous. Balanced Rock is one of the more well known, as it is easily seen from the main road in the park.
The uppermost part of Balanced Rock, a strong type of rock called Slick Rock sandstone, rests on a less stable rock known as Dewey Bridge mudstone. Since the mudstone erodes faster than the Slick Rock, top-heavy formations occur with some frequency. Eventually the weaker pedestals will wear away and Balanced Rock will collapse.
At dusk, the red hues of the rock are intensified, and it is quite impossible to drive past the rocks and not stop for a photograph. I would imagine anyone who has ever visited Arches has a photograph similar to this one.
“Good Morning” in the Blue Dawn
Crisp, chilly. I would have been cold if I hadn’t prepared for wintry mornings on the high desert. Everything was frosty, shimmery. Pinks and blues, too – a pastel sort of early morning.