If you read my previous article published in the National Parks Traveler, then you’ll know how I prepared for my photography trip to Crater Lake National Park during the Coronavirus pandemic. My latest article published by the Traveler is about the photography you can achieve within this park.
To read my photo article, click on the image above.
It is possible to take a safe and enjoyable trip into a national park, if you prepare and use some precautions. I returned alive and well (it’s been 14 days since my return) to write how I did it and what I saw at Crater Lake National Park in Oregon.
To read the story published in the National Parks Traveler, click on the image above.
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.
According to the NPS, Sheep Rock (that pointy-peaked mountain), in the Sheep Rock Unit of John Day Fossil Beds National Monument, gets its name from the bighorn sheep that once populated its slopes. At the top of Sheep Rock is the Picture Gorge Basalt. That brown line across the middle part of the mountain is the Picture Gorge Ignimbrite (pumice and volcanic tuff). This ignimbrite makes a nice marker bed by which geologists can place and date geologic events. The green soils you see in the second image are colored by the mineral celadonite. Celadonite comes from the French word for “sea green.”
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!
It’s Fun Fact Friday! Here’s some interesting facts for you if you happen to visit John Day Fossil Beds National Monument in Oregon.
In the first photo, that’s the first hill you’ll see that will get your attention as you drive past the sign welcoming you to the Painted Hills Unit. The top of this hill is capped with a volcanic tuff called the Picture Gorge Ignimbrite. This tuff is 28.7 MILLION years old.
The other images show other sides to this same hill as you drive further along the gravel road into the Painted Hills Unit. The red and tan soils are called paleosols, and the red paleosols are indicative of a warmer, wet, tropical to subtropical climate, while the tan soils represent a cooler, drier, more temperate climate.
Those blue-ish shadowed mountains in the background of a couple of the images are the Sutton Mountains.
All images on these posts are the exclusive property of Rebecca L. Latson and Where The Trails Take You Photography. Please respect my copyright and do not use these images on Pinterest, Facebook, Tumblr, Instagram, Snapchat or any other business, personal or social website, blog site, or other media without my written permission. Thank you.
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