Texas Gulf Coast Faults

Are real faults.  The Earth has broken and rocks on either side of them have 
moved relative to each other.  There are a lot of them.

They are not mud cracks!  A mud crack is a shrinkage phenomenon where the 
surface layer of the mud has contracted as it shrank.  Cooling hot rocks can do 
the same thing and produces columnar jointing seen in igneous rocks (columnar 
basalt as at Fingal�s Cave, the Devil�s Postpile, or Devil�s Tower).  

A fracture or joint is where the rocks are broken but not displaced.  Fracture 
traces are where there is a swarm of fractures closely spaced. Tens or a 
hundred instead of just one.  But still no relative motion across the fracture, 
just an incipient opening. A good place to drill your water well as the yield 
will be better.  If faulting occurs, joints and fracture traces are weaknesses 
in the rock and an actual fault may propagate along a series of fractures.

A fault is where the earth is displaced and there has been relative motion 
across the fault.  It means that there is differential stress on either side 
and movement along the fault releases that stress. It is like bending a stick 
until it finally breaks. The sense of motion can be vertical or lateral, or a 
combination. When the opposite sides of the fault actually move, an earthquake 
occurs. That said, most faults are not the gigantic ones like the San Andreas 
where there has been continued motion of hundreds of miles of displacement over 
millions of years. 

Most faults along the Texas coast are places where adjustment (relatively small 
movements along the faults) has taken place over geologic time as the coast is 
gently raised and lowered, loaded by the accumulation of additional sediment, 
unloaded by erosion, or it is alternatively loaded and unloaded as sea level 
rises and falls.

Drilling and geophysical data show the faults quite well, but they are hard to 
see at the surface.  The surface fault traces are usually places where there is 
slightly more ground moisture and a few more blades of grass per acre.  If you 
look carefully, you can see that!  I remember when I worked for the Texas 
Bureau of Economic Geology we laid out a large mosaic of air photos on the gym 
floor.  If you got up on a step-ladder, you could see the fault and fracture 
traces delineated by slightly greater soil moisture (or something). They were 
shown as subtile lines most probably caused by more grass, lines of better tree 
and shrub growth, and slight alignments of small drainages. It takes subsurface 
data to determine if actual fault displacement has occurred along any given 
line (linement).  We did that exercise to locate possible faults in relation to 
proposed siting of a  nuclear power plant.

That said, these are not locations where there should be great concern.  
However, when the inevitable adjustments of the Earth�s surface occurs, 
breaks will most likely occur again along one of these faults, where it has 
broken before.  There is not much problem for individuals, unless your house 
happens to be on top of one of them when does move.  Not very probable in your 
lifetime, but it could happen -----.  

All things are relative, and driving to a cave is a LOT more dangerous!

DirtDoc

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