Another braided river meets a gorge: Lamar River, Yellowstone NP
Like the Snake River I posted last week, today I've got another example of a river happily braiding through a wide valley (this time probably glacial, not structural) only to meet an obstacle in the form of topography. I'm looking at the Lamar River on the northeast entrance road to Yellowstone National Park. We're north of the volcanic plateau here and just west of the Absaroka Range, so I think the geology is typical Cordilleran stuff.
One of the things that fascinates me about this example is how short (and steep) the gorge section is (< 3 km, ~100 m elevation drop). Is it a relict of the glacial influence on valley formation? Or is there something structural going on (the Yellowstone geologic map indicates a fault in about the right area)? Food for thought and an excuse to do some field reconnaissance someday maybe. Or you can go there now in Flash Earth.
Images below are a mixture of Google Earth, Flash Earth, and ground photos from my personal collection.
Five-fold fluvial pathology
Pathological Overfitness: The Texas 'Insta-Gorge' Before and After
This flood is getting so much press (e.g., http://www.scientificamerican.com/article.cfm?id=canyon-lake-flood) that I thought that some photos were in order. It was certainly a screamer...and interesting that it spilled into what looks like a minor drainage course in a classic case of pathological overfitness. At first glance, looks like we can learn a bit more about bedrock canyon morphology, etc. Wonder if any real potholes were created in this single event? Does appear that there was some inner-gorge morphology carved out.
Braided river meets mountain gorge: The Snake River escapes Jackson Hole
Though I don't think anything can top Kyle's pathologically misdirected RYNHO, I recently had cause to contemplate a river that everyone has heard of - the Snake River of the northwestern United States. Now, the Snake River has a famous gorge, a famous lava plain, and it's had a famously big flood or two, but the upper reaches of the Snake are pretty scenic too. The Snake originates in Yellowstone National Park and flows through Grand Teton National Park and the Jackson Hole valley. Throughout the broad, flat valley, the Snake is beautifully braided (with some gorgeous terraces too).Then it runs into some mountains - the Wyoming Range - and it runs out of room to braid, becoming constricted into a narrow mountain gorge. Interestingly, after heading south from Yellowstone and through Jackson Hole, the river turns west through the mountains and then quite abruptly turns north towards Idaho's Snake River Plain.
I'd love to know how and why the river started along this path and how intensely the river's course is geologically controlled. I think the gorge is south of the Teton block, and it's possible that it's in an narrow zone that hasn't seen as much uplift as other mountain blocks in the Basin and Range, but I'm just speculating here. If anyone has any good ideas or citations, please drop them in the comments.
The images below are from a mix of Flash Earth (permalink here) and Google Earth. The first is a large scale view of the braided-gorge transition, while the second and third are close-ups of typical braided and gorge reaches, respectively.
Pathological misdirection on the Chulym, River, Russia
Transitions in the Heart of Darkness...the (truly) Mighty Congo
Fluvial Transitions...the June Meme
As a predominantly fluvial geomorphologist, I am particularly intrigued by channel patterns. So for this month, I propose that we focus on finding areas that reveal notably pathological examples of transitions between archetypes of alluvial channel patterns...meandering, braided, and straight.
This is a famous topic in fluvial studies, and was one that was dear to the heart and mind of the late Reds Wolman (see for example USGS professional Paper 282-b). When an alluvial channel adopts a particular planform character, it is an indication of a fundamental change in its discharge, gradient, sediment load, substrate, tectonic environment...or, of cousre, some pathological combination of any of them.
I will start with an amazing and pathological array of channel pattern transitions all crammed into one corner of Tajikistan (note that it is an area draining the edge of a fold and thrust belt). Seriously, this spot is completely wild.
Ahh, right....Tajikistan
Cheers to all geomorphic transitions, fluvial or otherwise.
Baluchistan, Pakistan ((fold-and-thrust belt, structure, mountains))
One final fold-and-thrust belt, for the last day of May. Since no one had yet tackled the Himalayas, I went scooting over there and found this arcuate series of ranges to the west of the main Himalayan front, in the Baluchistan region of northern Pakistan. Apparently, it's called the Sulaiman Range, according to Flash Earth. Lovely differential weathering of folded strata...
Flash Earth link:http://www.flashearth.com/?lat=30.317029&lon=68.721704&z=8.7&r=0&src=msa What's June's theme?
Southern Bolivia, eastern Andean fold and thrust belt
http://www.flashearth.com/?lat=-20.484624&lon=-64.111851&z=9&r=0&src=msa Más "hogbacks," por favor:
http://www.earthscienceworld.org/images/search/results.html?Keyword=Hogbacks