The Preparation of Illustrations for Reports of the United States Geological Survey: With Brief Descriptions of Processes of ReproductionRidgway, John L.
Science
The Preparation of Illustrations for Reports of the United States Geological Survey: With Brief Descriptions of Processes of Reproduction
Ridgway, John L.
Illustration of books
The draftsman should determine in advance the reduction for each
drawing or for each group of drawings, in order that he may use the
same size of letters or the same kinds of type for the lettering on a
series of drawings that require the same reduction. The reduction
should preferably be marked in fractions (as "1/2 off," "1/4 off" or
"reduce 1/2," "reduce 1/4"), and the choice of the same reduction for
a group of drawings will not only insure greater uniformity in the
drafting and in the reproduction but will permit the drawings to be
reproduced more economically, for the engraver can photograph them in
groups instead of each one separately.
The draftsman should therefore note and consider (1) the special
features shown in the author's originals; (2) whether or not these
features have been plainly indicated and whether the originals are
complete; (3) the size of the printed page of the volume in which the
illustrations will appear and the reduction required for each drawing;
and (4) the process by which each drawing should be reproduced. If an
original is of doubtful or uncertain interpretation or appears to be
incomplete the draftsman should confer with the author of the paper if
he is within reach or should bring the matter to the attention of the
chief of the branch; otherwise he may waste much time in making the
drawing.
PREPARATION OF MAPS.
PROJECTION.
The base maps furnished by authors (see pp. 13-14) are prepared in
many different ways and in different degrees of refinement and of
crudity, but the work of redrawing them for reproduction involves
well-established and generally uniform principles. All maps except
those of very extensive areas should be based on a map projection
which will show with a minimum of distortion the effect of the
curvature of the earth. The polyconic projection (see fig. 5) is used
for most Government maps. In this projection the central meridian is
a straight vertical line, and each parallel of latitude is developed
independently of the others. The mathematical elements of map
projection are given in tables published by the Geological Survey[6]
and the Coast and Geodetic Survey.[7] Figure 5, however, illustrates
the mechanical or constructional features of the polyconic projection
and if used in connection with the published tables will probably be
a sufficient guide for projecting a map on any desired scale.
[Footnote 6: Gannett, S. S., Geographic tables and formulas, 4th ed.:
U. S. Geol. Survey Bull. 650, 1916. See also Gannett, Henry, Manual of
topographic methods: U. S. Geol. Survey Bull. 307, pp. 85-86, 1906.]
[Footnote 7: Methods and results: Tables for the projection of maps
and polyconic development; Appendix No. 6, Report for 1884; Tables for
a polyconic projection of maps, based upon Clarke's reference spheroid
of 1886; 3d ed., 1910.]
[Illustration: Figure 5.--Diagram illustrating method of projecting a
map.]
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