Map reading
G. H. C. Dale
Paperback
(RareBooksClub.com, May 21, 2012)
This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1921 Excerpt: ...at X, and E. and W. through point A, from its present scale of 4 inches to the mile to TfTSTTo--(Sides of squares:1.) (4) Continue the line East through C. Assuming the present V.I. to be 100 feet and the height of the centre of the triangular patch of ground to be 436 feet, interpolate contours at 25 feet V.I. in that portion of the map North of this line and West of a line N. and S. through point D. (See Map 8.) CHAPTER IV. GRADIENTS. FINDING GRADIENTS. The figure at the head of this chapter must be familiar to everyone, as the sign placed alongside railway tracks to show the rise or fall of the ground in certain distances. The right-hand arm indicates that the land between that point and the next sign rises 1 foot in every 40 feet, and that on the left it drops 1 foot in every 50 feet. This " 1 in 40" and " 1 in 50" is called the gradient of the ground, and in map-reading is usually expressed as a fraction thus: or The numerator is the "rise" or the "fall," and the denominator is the "distance" in which the ground rises or falls one foot. Fin. 46 a. If a light railway were running up the hill (Fig. 35) from A to C, you would have to plant a post at A and another at B. 89 The distances are not the same, hence the gradients will not be the same. Now the rise from A to B and the rise from B to O are technically known as V.l.'s, and the distance from A to B and that from B to C are known as the H.E.'s. So it appears that the gradient, as a fraction, may also be expressed by placing the V.I. over the H.E. and reducing until the fraction shows 1 foot over the corresponding distance in feet..,,.. Rise or Fall V.L..,. Thus the gradient is, or, (in feet). Distance H.E. N.B.--The H.E. in a gradient must always be e...