Anticline - 2
In geology, an anticline is a fold that is convex up and has its oldest beds at its core. Anticlines are usually recognized by a sequence of rock layers that are progressively older toward the center of the fold. Now that you know what a geologic anticline, -----is let's look at some.
Anticline near Pinedale, Wyoming
Pinedale, Wyoming is a booming natural gas area. Hydrocarbons are known to get trapped in anticlines where the overlaying strats are not permeable. Of course the natural gas is trapped by anticlines deep underground.
This anticline is in Alberta, Canadia in the Rocky Mountains
This looks to be a classic anticline to me.
This Anticline is presented in a strata of sedimentary rock
This is a beautifully formed anticline
Anticlines are recognized by a sequence of rock layers that are progressively older toward the center of the fold.
This is a classic anticline
Click here for more Anticlines
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Mike & Joyce Hendrix
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