Report On the Geological Structure of Murphrees Valley And Its Minerals And Ot
Report On the Geological Structure of Murphrees Valley And Its Minerals And Ot
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In our eReader you can find the full English version of the book. Read Report On the Geological Structure of Murphrees Valley And Its Minerals And Ot Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book Report On the Geological Structure of Murphrees Valley And Its Minerals And Ot
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Then its position near the base of the mountasn makes it so accessible as to add greatly to its value. Its position here is a little below its normal place, probably caused by the fault referred to. Half a mile or more farther down the mountain it was seen at a somewhat higher level. There has been a slight downward flexure near the main exposure of the bed, but the amount of it is not great. This bed probably extends for a mile or more up the valley. The shape of the slope or bench above the t...op of the Trenton almost gives assurance of its extension that far. As has been heretofore observed, a bench in the Clin- ton, immediately above the Trenton, may be regarded as indicating the presence of this bed. Should this observation be fully verified, large and extensive bodies of ore will yet be found which are not thought of now, and the value of the Clinton formation will be much increased.
Opposite Village Springs, in the Southern part of Sect. 28, Village Creek cuts through the Red Mountain.
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To quickly assess the difficulty of the text, read a short excerpt:
Then its position near the base of the mountasn makes it so accessible as to add greatly to its value. Its position here is a little below its normal place, probably caused by the fault referred to. Half a mile or more farther down the mountain it was seen at a somewhat higher level. There has been a slight downward flexure near the main exposure of the bed, but the amount of it is not great. This bed probably extends for a mile or more up the valley. The shape of the slope or bench above the t...op of the Trenton almost gives assurance of its extension that far. As has been heretofore observed, a bench in the Clin- ton, immediately above the Trenton, may be regarded as indicating the presence of this bed. Should this observation be fully verified, large and extensive bodies of ore will yet be found which are not thought of now, and the value of the Clinton formation will be much increased.
Opposite Village Springs, in the Southern part of Sect. 28, Village Creek cuts through the Red Mountain.
What to read after Report On the Geological Structure of Murphrees Valley And Its Minerals And Ot?
You can find similar books in the "Read Also" column, or choose other free books by Geological Survey of Alabama to read onlineMoreLess
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