As I mentioned in my last post, Kim and I snuck away for a short vacation in the mountains last week. It was a great trip, but now I’m catching up on all the work that was waiting for me when I got home. Since I’m a little pressed for time, I figured I’d just share a bunch more vacation photos instead of writing a long pithy post on prairie ecology.
When I go to the mountains, I usually try to get up above tree line as much as possible. Hiking trails that just pass through dense stands of evergreens doesn’t do much for me. I want to feel the big open space that I like so much about prairies.
However, I found this year that my objection to hiking wooded trails doesn’t apply to autumn hikes through stands of quaking aspen. WOW, that’s a great experience. Of course, I still enjoyed getting up and out of the trees too, but since we were too late for most wildflowers, the aspen provided a lot of the color in the landscape. Kim and I are already planning our return visit next fall.
I hope you enjoy these photos. I’ll try to get back to prairie photos and topics for my next post.
I’ve seen ruffed grouse in the Black Hills. I also thought what you photographed was a ruffed grouse. As I told you before, the reason I like your blog is I’m always learning new things.
The sedimentary rock layers you showed (heavy cobbles overlying fine shale) are typical of flood event deposits. That’s flood with a small “f”. We’ve got similar formations here in the East along the Delaware River on the PA side. There are alternating bands of pebbles grading from large to small to mud deposits and then repeating. These are interpreted as being remains of heavy flooding where high energy/high volume water swept through an area, depositing the larger stones as the water lost momentum, followed by smaller stones and so forth until just mud was dropped. I realize the deposits in your photo appear to be reversed from this order, but it may be that the sediments have been flipped here or there are pebbly layers underneath that shale layer that are as yet unexposed.
Many thanks for sharing your experience! Your photos are beautiful and inspiring! Reading your post made me feel like I took a vacation. Also made me want to plan a trip for next fall. Interesting to read that you snapped a smart phone photo but you carried a big camera gear. Those little phones are so handy. Looking forward to reading your next blog!
Glad you got to visit the western Colorado mountains during fall color season. Bill and I were actually in the same vicinity (we concentrated on Kebler Pass and Owl Creek Pass — near Ridgway) over the past weekend. We never miss it (or crane migration in Nebraska) because it is nature at its most glorious. Of course the fabulous weather with the cerulean skies certainly helped. And Ice Lake — where does that blue come from?
Thanks for sharing! Adding to my list of places to visit. Always look forward to your posts, you have yet to disappoint.
You should make posters of some of these pictures to use for a fund raiser — they are stunning.
Looks like an awesome trail. I think your grouse was a Dusky Grouse though. Ruffeds don’t regularly occur in Colorado.
Yeah, you’re right. I didn’t even know they existed, so didn’t consider that as an option. Joel Jorgensen said the same thing. Thanks!
I’ve seen ruffed grouse in the Black Hills. I also thought what you photographed was a ruffed grouse. As I told you before, the reason I like your blog is I’m always learning new things.
Great pictures! Simply breathtaking!
The sedimentary rock layers you showed (heavy cobbles overlying fine shale) are typical of flood event deposits. That’s flood with a small “f”. We’ve got similar formations here in the East along the Delaware River on the PA side. There are alternating bands of pebbles grading from large to small to mud deposits and then repeating. These are interpreted as being remains of heavy flooding where high energy/high volume water swept through an area, depositing the larger stones as the water lost momentum, followed by smaller stones and so forth until just mud was dropped. I realize the deposits in your photo appear to be reversed from this order, but it may be that the sediments have been flipped here or there are pebbly layers underneath that shale layer that are as yet unexposed.
Many thanks for sharing your experience! Your photos are beautiful and inspiring! Reading your post made me feel like I took a vacation. Also made me want to plan a trip for next fall. Interesting to read that you snapped a smart phone photo but you carried a big camera gear. Those little phones are so handy. Looking forward to reading your next blog!
Chris:
Glad you got to visit the western Colorado mountains during fall color season. Bill and I were actually in the same vicinity (we concentrated on Kebler Pass and Owl Creek Pass — near Ridgway) over the past weekend. We never miss it (or crane migration in Nebraska) because it is nature at its most glorious. Of course the fabulous weather with the cerulean skies certainly helped. And Ice Lake — where does that blue come from?
Katie Stevens Moab, Utah ________________________________
Hi Chris, your flowers at teh lake are Helenium hoopsii or sneezeweed.
Thanks Mike!