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Fig. 2 Mapscale vs. contour interval
T "1:31 Vv1T1 T
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Fig. 3 Mapscale vs. production rates
—
A number of explanations can be offered for the large spreads evident in all
three graphs. In the first instance, these ratios are also influenced by other
parameters. As an example, the ratio between mapscale and contour interval is
obviously also a function of the terrain slope. It is therefore clear that a
much larger sample is required if the effects of the various influencing para-
meters are to be isolated. Furthermore, and this applies particularly to the
production rates, a number of the figures extracted from the enquiry are
questionable and require further verification.
In conclusion, these large spreads are certainly indicative of the urgent
necessity to develop and implement systematic procedures for planning photo-
grammetric projects since, to give an example, the variation in photo scales
for a given map scale by more than a factor 4 cannot only be justified by the
various uses of a particular map scale.
Acknowledgement
I am greatly indebted to Mr. J. Kure who collected and ordered the material
included in this report and who also had a considerable role in preparing the
final draft.
A.J. van der Weele
T scale
NTI sc