The Interpretation of Topographic Maps (Classic Reprint)

Rollin D. Salisbury

ISBN 10: 1332018319 / ISBN 13: 9781332018314

Published by Forgotten Books Apr 2018, 2018

About this Item

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Bibliographic Details

• Title: The Interpretation of Topographic Maps (Classic Reprint)
• Publisher: Forgotten Books Apr 2018
• Publication Date: 2018
• Language: English
• ISBN 10: 1332018319
• ISBN 13: 9781332018314
• Binding: Taschenbuch
• Condition: Neu
• Dimensions: 229W x 152H x 25D millimeters 229 millimeters width by 152 millimeters height by 25 millimeters depth
• Weight: 1342 grams

About this title

Synopsis

Excerpt from The Interpretation of Topographic Maps

The features shown on topographic maps may, for convenience, be classed in three groups (1) Water, including seas, lakes, ponds, rivers and other streams, canals, swamps, etc.; (2) relief, including mountains, hills, valleys, cliffs, etc.; (3) culture, i. E., works of man, such as towns, cities, roads, railroads, boundaries, etc. The conventional signs used for these features are grouped on P1. II. Variations appear in some maps of early dates.

All water features are shown in blue, the smaller streams and canals in full blue lines, and the larger streams, lakes, and the sea by blue water lining. Certain streams, however, which flow during only a part of the year, their beds being dry at other times, are shown, not by full lines, but by lines of dots and dashes. Ponds which are dry during a part of the year are shown by oblique parallel lines. Salt-water marshes are shown by horizontal ruling interspersed with tufts of blue, and fresh-water marshes and swamps by blue tufts with broken horizontal lines.

Relief is shown by contour lines in brown. Each contour passes through points which have the same altitude. One who follows a contour on the ground will go neither uphill nor downhill, but on a level. By the use of contours not only are the shapes of the plains, hills, and mountains shown, but also their elevations. The line of the seacoast itself is a contour line, the datum or zero of elevation being mean sea level. The contour line at, say, 20 feet above sea level is the line that would be the seacoast if the sea were to rise or the land to sink 20 feet. Such a line runs back up the valleys and forward around the points of hills and spurs. On a gentle slope this contour line is far from the present coast line; on a steep slope it is near the coast. Thus a succession of these contour lines far apart on the map indicates a gentle slope; if close together, a steep slope; and if the contours run together in one line, as if each were vertically under the one above it, they indicate a cliff. In many parts of the country are depressions or hollows with no outlets. The contours, of course, surround these, just as they surround hills. The small hollows known as sinks are usually indicated by hachures, or short dashes, on the inside of the curve.

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