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How did the Green River flow "uphill" for about 100 miles?

Glenn MacGrady

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Many canoeists have paddled the Green River, which is the Colorado's largest tributary. We have trip reports of the Green on this site. But did you know there is:

". . . an American mystery which has baffled geologists for a century and a half: How did a river carve a path through a mountain in one of the country's most iconic landscapes? Scientists have long sought an answer to this question of how the Green River, the largest tributary of the Colorado River, managed to create a 700-meter-deep canyon through Utah's 4km-high Uinta Mountains instead of simply flowing around them. The question is particularly confounding because, while the Uinta Mountains are 50 million years old, the Green River has been following this route for less than 8 million years."

New research suggests this can be explained by ""lithospheric dripping" of the Uinta Mountains. I don't quite understand this, but it seems to posit that entire mountain ranges can bounce down and then back up.


Then, of course, there's the theory that the entire Colorado River once flowed in the other direction.


Wouldn't it be simpler if rivers and mountains (and lakes, of course) would stay in their "natural" state?
 
I've been getting into geology over the last few months and have heard some about this. I don't think there remains much question of how it carved a path through the mountains rather than going around them. Multiple very high mountain ranges were created in that area and after millions of years of erosion the valleys had filled in and buried what remained of the mountains, leaving an essentially flat landscape. More millions of years later the area began to be uplifted and what were broad and slow moving rivers with little elevation change began to flow faster and stronger. As the landscape continued to be uplifted the rivers continued removing more and more of the accumulated debris as they dug deeper channels. Eventually they reached the buried mountains and began to cut vertically down through them. Over more millions of years we ended up with what we have now: The buried mountains have been mostly excavated and now rivers run straight through them.

When mountain ranges are created they are obviously very heavy and they can cause the mantle to slump and the area can lose elevation. As they become more and more eroded the mantle can begin to rise back to "normal" levels and cause the area to uplift. Other forces can cause uplift as well. I believe this is also happening in the Canadian shield. The land had dropped under the weight of the glaciers and it's still rebounding after the glacier melt.

TLDR: The rivers didn't punch through the mountains, they wore through from the top down at a time when the mountains already existed but were buried in debris.

Alan
 
I don't think there remains much question of how it carved a path through the mountains rather than going around them. Multiple very high mountain ranges were created in that area and after millions of years of erosion the valleys had filled in and buried what remained of the mountains, leaving an essentially flat landscape.

Alan, I recall you are watching some geology courses, but I believe the phenomenon you are describing—mountains that silted over with debris and hence became flat land—is one of the theories that the brand new (February 2026) "lithospheric drip" hypothesis rejects. As the author of the study says in the Phys.org journal I first linked (italics mine):

"This is a long paper, because we wanted not just to lay out the case for a lithospheric drip creating the route of the Green River but also to acknowledge some previous theories. The evidence we've collected strongly contradicts the idea that the river predated the mountains, or that sediment deposits might have built up enough for the river to overtop the range, or that erosion from the south of the mountains captured the Green River."

The hypothesized geological phenomenon seems to be solely a subsidence of the surface (mountains) caused by a heavy mineralized "drip" in the crust below the mountain root, followed by rebound of the surface (mountains) when the crustal drip breaks off, rather than having anything to do with erosion or silting of the original Uinta Mountain range.
 
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