May, 1960 COMMENTS ON THE MAPPING EXPERIMENT 169
NS Fic. 2. Physiographical divisions
3 NN 3 of the map area. 1. Alluvial
marine deposits, clay. Nearly
plan, some shallow gullies. 2.
Rock-knob rounded by the
glaciers of the ice age. 3. Till,
ground moraine with very detail-
ed surface. Rather difficult to
plot where general inclination
is small. 4. Valley in the till area
flowing into the Bonnechere
valley near the town area. There
the valley has carved into the
bedrock. 5. Gravel pits. 6. Town
area.
FIrsT- AND SECOND-ORDER PLOTTING
The comparison between anaglyphic and non-anaglyphic plotters is an essential
part of the experiment. One can perform this comparison from elevation readings at
control points, and this was very well organized by the National Research Council.
The figures submitted by the participants doubtless give a good indication of the
efficiency of both types of plotters.
Besides numerical results the topographic and cartographic task involves the repre-
sentation of the landscape by contour lines and planimetry, including boundary lines
of forest, fields, etc. Here it is much more difficult to assess the quality of plots from
the two types of plotters. The quantitative evaluation of the plots by the National
Research Council was very valuable. But only the combination of qualitative and
quantitative data with the time spent in plotting will lead to conclusions on the efficiency
of the plotters used and the economic aspects. One can also draw some conclusions
regarding the skill of the operators at the instruments. Obviously the result is influ-
enced by many factors. For a future experiment these factors should be separated as
far as possible. Special specifications could then be prepared for first-, second- and
perhaps also for third-order plotting. All experimental work must be based on identical
photographs. In addition, a physiographical description of the test area should be
supplied to define the desired contents cf the plotting for different-order instruments.
The contents for the first-order plotting can be defined most easily. The alti-
metric and planimetric presentation must include all details of the terrain, with the
exception of unimportant features that may be excluded in view of the mapping scale.
The contours should be drawn with the greatest possible accuracy.
Checking first-order plots is relatively simple because the map is supposed to be
an exact replica of the terrain. For the evaluation of the quality of plots, precise plots
of selected check areas produced from photographs taken from a lower altitude or
from direct field survey are used.
For second-order plotting, naturally, lesser accuracy and completeness are allowed.
It would be important to specify both the details that could be omitted and those that
must be represented. This applies also to the generalization of contour lines.
Checking second-order plots is considerably more difficult because some omissions
and generalizations cannot be marked as errors. They are necessary if the typical and
essential forms only are to be shown. Figure 3 shows two contourings of the same area
but of different quality. The second-order contour lines give fewer details. For
instance, the structures on the side walls of the rock-knob are omitted, but the typical