192 CARTES A PETITES ECHELLES, DISCUSSION
Je donne la parole au Colonel Thompson pour
la méthode utilisée au Canada.
Mr J. I. THomPson: This problem is not only
a fascinating one but it is one in which we in
Canada are directly engaged. My comments are
based upon our experience over a number of
years combined with my wishful thinking of
what we would like to do if we were start-
ing again. This type of reconnaissance map
should be considered strictly from the user's
point of view, and not from what we as photo-
grammetrists would like to produce. Our users
have told us that they wish to be able to use this
map on the ground in exploration and in the air
from light aircraft. They have no desire for high,
absolute accuracy, either in the vertical or the
horizontal. They wish for accurate, relative
shapes again on both horizontal and vertical
features. They have agreed that their need is
met by our choice of a publication scale of
1 : 250,000, with form lining at 100' intervals
in areas of low relief and 500' in mountainous
areas. Except in exceptional cases, they will not
require any further information until a larger
scale of the order of 1 : 50,000, or larger, is
requested. However, they do stipulate that they
want these maps now and not in generations to
come. A conservative estimate of our produc-
tion in Canada this year, in this particular field
of mapping, is approximately 300,000 square
miles. That is approximately one million square
kilometres, and we anticipate having to meet this
yearly target for at least five years to come.
In reality, one of the basic factors in our con-
sideration of our procedure has been that our
methods in all phases will lend themselves to a
simple and efficient procedure which will allow
us to use our limited resources of trained per-
sonnel to the greatest advantage. In actual fact,
our tests have indicated that the average mean
error in absolute horizontal position does not
exceed 150 metres, approximately six-tenths of
a millimetre at publication scale; and the error in
the vertical values on which our form lining is
based does not exceed 50' to 60', approximately
20 metres.
Were we to re-fly our basic cover — un-
fortunately it is now done or virtually complete
— we would call for a minimum of photography
taken with a superwide angle lens in areas of
low relief, and the wide angle lens in areas of
high relief, with a flight altitude of approximate-
ly 30,000 feet.
To effect economy, we would require that
radar altimetry would be carried out simulta-
neously with the vertical photography and would
be keyed to it. In Canada, because of the nature
of the land, we would use the helicopter and
light aircraft to support Tellurometer operations
in the field to establish horizontal control. It
would be run in a grid pattern in which the grid
dimensions would be approximately 150 miles.
Vertical control, to which the radar altimetry
would be tied, would be run by instrumental
levels using water transfer procedures on the
vast number of bodies of water that we have.
These level lines would be transferred to our
photographic flights at minimum intervals of
150 miles and maxima extending to 250 miles.
Form lining would be carried out on the pho-
tographs by skilled field topographers, based
on the height deduced from the radar altimetry
coupled with the basic natural drainage pattern.
Their instruments would be simple conventional
universal stereoscope, and possibly the parallax
bar on occasions. In the areas of difficult relief,
the Multiplex and lower orders of plotters would
be used. The information on the photographs
would be transferred to the compilation man
equipped with such simple transfer devices as
the Sketchmaster or the Stereoscope.
In the past, in Canada, we have used shoran
to a tremendous amount, but economically we
have now dropped this method. However, in
areas where aerial navigation is extremely diffi-
cult, if not impossible, shoran could be used to
its best advantage to provide a most effective
means of navigation, as well as to provide
horizontal control. This, coupled with simulta-
neous radar altimetry, keyed to photography,
would provide you with all your supplementary
horizontal and vertical control.
Monsieur M. BAUSSART: Je vais vous rappe-
ler briévement la méthode qui a été adoptée par
l'Institut Géographique National pour la solu-
tion des mémes problémes. Cette méthode per-
met de déterminer directement les altitudes des
quatre points nécessaires pour l'orientation de
chacun des modéles. Je ne l'exposerai pas car
elle a fait l'objet d'une communication à la
Commission IV. Je ferai à son propos unique-
ment quelques remarques.
Son principe consiste, une fois la couverture
normale exécutée, à utiliser un émetteur-récep-
teur aéroporté et à faire des enregistrements de
profil le long des zones communes aux bandes
longitudinales, ainsi que le long de certains
axes transversaux. L'originalité de cette méthode
consiste en deux choses: d'abord l'enregistre-
ment des profils ne se fait plus en méme temps
que la prise de vue, mais tout à fait séparément
et à une altitude plus basse — d'autre part et
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