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The new method, however, offers new opportunities not
only for obtaining the elevation data required for mapping but also
for charting the planimetry and determining the scale. This very
significant fact also opens up new possibilities for aerotriangulatiol
and it would appear that the synthesis of the aerotriangulation metho
and the radar profile method might provide the long sought solution t:
the problem of the provision of control points for detailed mapping o!
a small or intermediate scale.
Obviously the radar profile offers an immediate solution
to a great many of the technical problems connected with topography
and it is unfortunate that they cannot all be dealt with in this
brief outline.
A further significant fact about the airborne profile
recorder method is that it permits in actual operation a very elastic
relationship between the altitude at which the photographs are taken
and the profile flights flown, thus achieving a high degree of
economy in photogrammetric mapping.
As I mentioned earlier, the radar profile method has
already developed beyond the initial stages and is now being used,
as well as other methods, to overcome many of the problems encountere:
in map production. This does not mean, however, that its development
is by any means complete. On the contrary, a number of projects now
in hand are aimed at the improvement and perfection both of the instr
ments used and the procedures followed, and the active participation
of photogrammetrists in this work will be indispensable if our growin,
hopes for the radar method are to be fulfilled.