Manual of Terreohmetry
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In our eReader you can find the full English version of the book. Read Manual of Terreohmetry 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 Manual of Terreohmetry
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, may be less than 50 feet, or it may be as much as 400 or 500 feet, or over, depending on the conditions of depth to the ore and whether or not it is desirable to make any determinations 83 with regard to the character of the ledge itself, as is further explained in sections 5 and 6.
The lines m n, op, etc. , should be laid out, as near as may be at right angles to the strike of the ledge, and should be straight lines, not curves, for the reason, as illustrated in fig. 9, that the current does... not traverse the shortest distance between the points of contact as A and m, but travels by the line of least resistance. In other words, from any point of contact not in the ledge, as m, the current traverses country rock to the ledge by the shortest route, thence along the ledge to the other point of contact, as A.
As the distance of the contact from the ledge, as mB, is successively shortened or lengthened by moving the contact in either direction along line m n, as from m to o or from o to m, the length of earth section traversed by the current is successively decreased or increased by the dis- tance m o, and the resistance is also decreased or increased, but in a greater ratio than that of distance, for the reason that points o, m, etc.
What to read after Manual of Terreohmetry?
You can find similar books in the "Read Also" column, or choose other free books by Ethan Scheidler to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
, may be less than 50 feet, or it may be as much as 400 or 500 feet, or over, depending on the conditions of depth to the ore and whether or not it is desirable to make any determinations 83 with regard to the character of the ledge itself, as is further explained in sections 5 and 6.
The lines m n, op, etc. , should be laid out, as near as may be at right angles to the strike of the ledge, and should be straight lines, not curves, for the reason, as illustrated in fig. 9, that the current does... not traverse the shortest distance between the points of contact as A and m, but travels by the line of least resistance. In other words, from any point of contact not in the ledge, as m, the current traverses country rock to the ledge by the shortest route, thence along the ledge to the other point of contact, as A.
As the distance of the contact from the ledge, as mB, is successively shortened or lengthened by moving the contact in either direction along line m n, as from m to o or from o to m, the length of earth section traversed by the current is successively decreased or increased by the dis- tance m o, and the resistance is also decreased or increased, but in a greater ratio than that of distance, for the reason that points o, m, etc.
What to read after Manual of Terreohmetry?
You can find similar books in the "Read Also" column, or choose other free books by Ethan Scheidler to read onlineMoreLess
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