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DITRstocks

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DITRstocks

Re: DITRstocks post# 16182

Friday, 01/25/2013 12:09:59 PM

Friday, January 25, 2013 12:09:59 PM

Post# of 18597
$USGT Metamorphism has not altered the geologic structure of the original sedimentary beds. The contact between hornfels and quartzite is sharp, striking 10°NNE and dipping 20°NW. The contact zone is discernible on satellite images and is shown on the geologic map.
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