Geology Q. on Colorado River (Texas)

A. BETTIK

1,000+ Posts
The Colorado river takes a Big Bend from Brownwood to Granite Shoals. Elsewhere it is fairly straight. I am curious why.

I know the Balcones uplift occurred around 10 million years ago. By studying the river basin from Austin to Brownwood you can detect an extreme bias of the river bed towards the eastern edge of the river basin along U.S. 183 of probably 20-50 miles. On the other side, the basin extends more than 100 miles to the west of the river bed with full fledged contributory rivers. The cause of this bias would seem to be the Balcones uplift, which suggests the Colorado River's Big Bend course was set prior to the Balcones Uplift. That is in 10 million years the river basin boundary has altered drastically with a general shift to the west while the river bed course has remained static.

A crude Google topographic survey shows that the area adjacent to the Big Bend of the Colorado is a flat plain occasionally intruded with well advanced erosional cuts from major streams. So how far back in time prior to the Balcones Uplift was the Colorado river course set? And was this Big Bend caused by the remnants of the Llano Uplift that I have seen on some geology maps as having formed islands during prior episodes of limestone deposition in Central Texas?
 
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Sorry, J/K.
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I deserved that. It was worth a shot though, given part of UT borders the Colorado and UT does churn out or employ geologists. I'll rachet up the search elsewhere...
 
Don't give up, the experts will come around. Since this isn't my area of expertise, all I can do is encourage knowledgeable folks to contribute.
 
I am indeed actually curious and am not taking any geology classes. I took the entry level geology class ages ago and couldn't imagine a worse way to learn about geology. Better to use as text the roadside geologist series, especially the Texas volume. Colorado and Arizona are amazing as well.

It's just damned interesting to live on a layer of limestone icing covering the stumps/roots of a dead mountain range with billion year old subduction zone poop (granite) 50-100 miles to the west.

Google Earth out to Marathon to glimpse what Austin terrain might look like were the liimestone icing removed (a lot like parts of Oklahoma and Arkansas maybe) and see if you can see exactly where the Marathon mountain stumps/roots that also run under Austin disappear back into the limestone icing.

It would be a good place for a get away resort with a great view towards several major Texas mountain ranges.

( I know, wise cracks in 3...2...1... )
 
Dammit, it's an interesting question, and I am curious also.

(Don't worry AB, I'll hang around the beer cooler with you even though I don't know the answer either)
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I didn't see this thread until now. This is not really an easy series of questions to address via the interweb, but I'll try later when I have more time (probably Friday).
 
I like rivers
Better than oceans, for we see both sides.
An ocean is forever asking questions
And writing them aloud along the shore
- Edwin Arlington Robinson, Roman Bartholow, Part 111
 

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