The next time you visit a place that has some elevation difference, take a moment to observe the other differences due to that elevation difference. For instance, notice the differences in these images here? The lowland forest interior, captured at the entrance to Westside Road in Mount Rainier National Park, looks deep and dark and is filled with lush vegetation like ferns and devils club along with dead logs and moss on parts of the trees. Sunlight makes its way into the forest in spots. Whereas the forest along Trail of Shadows in the Longmire Historic District looks – well – clearer, with more space in between the trees, less moss, and a clearer forest floor. Yes, there’s vegetation there, too, but as you can see, not quite as thick. In part because it’s not quite as wet as it is in the lowland forest, plus the difference in elevation between the Nisqually entrance and Longmire creates a difference in temperatures, too. Observation is key to getting nice photos, rather than just a grabshot.
Yahoo! The Great American Outdoors Act has been passed! So, now what? How will that $1.3 billion a year over the next 5 years be spent, and who gets the money? Remember, there are 419 units in the National Park System.
The National Parks Traveler has an interesting article asking that very question. Go check it out.
To read the article, click on the image above.
As for that image, I had arrived at the Crater Lake Lodge area around 4:00 a.m. and realized it was too cloudy to get any pre-dawn star shots. So, I sat in the car for awhile before finally venturing out to find the steps leading to the overlook, then setting up my tripod and camera for Blue Hour, sunrise, and after-sunrise shots.
I used my Sony Alpha 7R IV camera and 16-35mm lens for this shot.
I love geology. I went to school to study it. So when I travel, I like to read about the geology of the places I visit and the roads I travel. In hindsight, I wish, now, that I’d have bought and looked through the Roadside Geology of Oregon, by Marli B. Miller *before* rather than after I’d driven to John Day Fossil Beds National Monument. At least, then, I would have been able to follow the mile markers and understood what I was seeing.
Anyway, I’d stopped here because I happened to turn my head to look at the scenery right when my car was passing by these awesomly-colored outcroppings. Turns out, my inner geology radar must have been working intuitively. What you see here is called an angular “unconformity.” An angular unconformity is – in easy terms – when you see tilted beds (the green and reddish outcropping of beds) overlain by straight beds (the red-brown lines of columnar basalts you see above. It shows there is a gap in the geologic time record. So, if you are following a series of formations along a geographic distance, you might suddenly see that one formation or sediment layer of that formation is totally missing from the order of deposition, and all you see is this contact line dividing angular tilting beds from straight layers above. Any of this make sense? If not, then just admire the pretty landscape.
This image was captured using my new Sony Alpha a7r IV and 24-105mm lens. I am loving this camera!
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