The breccia I've seen on the surface in central Texas, including at CWAN, is
usually one of three types:

 

1)      Cemented collapse of a old cave that is now exposed at the surface.
These are scattered randomly throughout the Texas karst.

2)     Breccia along a fault, where chunks of rock broke off as the rock
mass on either side moved against the other side, and then the chunks were
later cemented together. A nice example of such breccia is along the Haby
Crossing Fault behind the volunteer office at Government Canyon State
Natural Area.

3)     Colluvial breccia, where gravity pulled down part of hillside or
cliff and was later cemented together, is much less common and more widely
scattered in Texas.

 

None of these breccias match the broad, extensive, deposits Bruce describes
for the Yucatan. I don't recall seeing those when I was there and would want
to see them in the field before speculating on their origin.

 

George

 

From: Cave Without a Name [mailto:[email protected]] 
Sent: Wednesday, January 27, 2010 9:53 AM
To: [email protected]
Cc: [email protected]
Subject: Re: [Texascavers] breccia

 

That same sort of breccia is on the CWAN property. I doubt that it's the KT
boundry but it is a mystery. If any of you geologists want a sample I'll
show you where it is. I'm pretty sure it's in the upper part of the Lower
Glenrose formation.

 

Mike Burrell

Manager 

Cave Without a Name

----- Original Message ----- 

From: [email protected] 

To: [email protected] 

Sent: Wednesday, January 27, 2010 8:42 AM

Subject: [Texascavers] breccia

 

Mystery rocks? Alien footprints? Pardon me, but it looks like plain old
breccia to me. See:
 
http://geology.about.com/od/rocks/ig/sedrockindex/rocpicbreccia.htm
 
Louise

No question about it being breccia, I just want to know how it happened. How
could such a cake mix slurry of broken chunks get embedded in conventional
limestone then get spread in a thin flat layer across a wide area? The
relative hardness could well be an unrelated issue. 

 

Sleazel


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