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re: Now Closed: I'll answer any question you have about ROCKS!

Posted on 7/10/14 at 3:10 pm to
Posted by Pectus
Internet
Member since Apr 2010
67302 posts
Posted on 7/10/14 at 3:10 pm to
quote:

Here at the foot of Pikes Peak there is a lot of what's known as Pikes Peak granite. It is a pinkish granite due to it containing a lot of potassium feldspar minerals. Sometimes I see big chunks of PP granite that have alternating layers of pink granite and dark gray granite. So my question is that given that granite is composed of magma that cooled slowly, what causes the striations or layers in these rocks?



Ooh! That's actually gneiss!

I know what you're talking about because I've seen it.

That gneiss is older than the Pikes Peak Granite. That gneiss is all along the walls of Royal Gorge.

This post was edited on 7/10/14 at 3:12 pm
Posted by Rouge
Floston Paradise
Member since Oct 2004
136867 posts
Posted on 7/10/14 at 3:12 pm to
quote:

Royal Gorge
and we now have a name for TigerHoney's vagina
Posted by MountainTiger
The foot of Mt. Belzoni
Member since Dec 2008
14672 posts
Posted on 7/10/14 at 3:18 pm to
The banding is fairly thick, not in thin layers like I've seen in gneissic banding. I've seen bands that were from 1 to maybe 5-6 inches thick.

I'm not sure the Pikes Peak batholith goes that far south but maybe it does. Or it could be a different but similar batholith.

PP granite is approx. 1 billion years old. Not that that has anything to do with anything, I just find that fact interesting.
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