Bulletin 1-4
Bulletin 1-4
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In our eReader you can find the full English version of the book. Read Bulletin 1-4 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 Bulletin 1-4
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xlii. This is the natural source for water at Harrisonburg, and in the region along and north of Little River and Catahoula Lake, where in the lowlands flowing water will probably be obtained. There is some probability, as indicated by the Ferriday well, that in the extreme southern part of the parish salt water will be encount- ered. In the central portion, however, no trouble is anticipated.
In the neighboring parishes the Catahoula beds supply the water at Pollock, Alexandria, Boyce, and Zim...merman. If a well does not obtain water in the Catahoula formation, it is believed to be inadvisable to sink deeper.
The next group of water sands occurs about 1,000 feet below the Catahoula (PI. xxxviii, sec. B) in the Cockfield formation.
These have been encountered in wells at Leland, (855) Colfax, (871), 011a (856-857), and Rochelle (881), and in all these cases have yielded unsatisfactory water.
Below the basal Cockfield occur the Sabine sands, and in the northwestern part of the parish, beyond Bayou Funne Louis where the Catahoula sands are not available (Pis.
What to read after Bulletin 1-4?
You can find similar books in the "Read Also" column, or choose other free books by Louisiana Geological Survey to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
xlii. This is the natural source for water at Harrisonburg, and in the region along and north of Little River and Catahoula Lake, where in the lowlands flowing water will probably be obtained. There is some probability, as indicated by the Ferriday well, that in the extreme southern part of the parish salt water will be encount- ered. In the central portion, however, no trouble is anticipated.
In the neighboring parishes the Catahoula beds supply the water at Pollock, Alexandria, Boyce, and Zim...merman. If a well does not obtain water in the Catahoula formation, it is believed to be inadvisable to sink deeper.
The next group of water sands occurs about 1,000 feet below the Catahoula (PI. xxxviii, sec. B) in the Cockfield formation.
These have been encountered in wells at Leland, (855) Colfax, (871), 011a (856-857), and Rochelle (881), and in all these cases have yielded unsatisfactory water.
Below the basal Cockfield occur the Sabine sands, and in the northwestern part of the parish, beyond Bayou Funne Louis where the Catahoula sands are not available (Pis.
What to read after Bulletin 1-4?
You can find similar books in the "Read Also" column, or choose other free books by Louisiana Geological Survey to read onlineMoreLess
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