In all ways but one our scrutiny of the planet is confined to such view
as we might get of it from the car of a balloon poised above it in
space; from which disadvantage-point we should see the surface only as
a map spread out below us, a matter of but two dimensions. The
exception consists in the observation of what are called projections;
irregularities visible when the disk is gibbous upon that edge of the
planet where the light fades off. Striking phenomena in themselves they
are of particular value for what may be deduced from them. For by them
we are afforded our only opportunity of gaining knowledge of the
surface other than in plan and thus of determining between peak,
plateau, or plain that to a bird’s-eye view alike lie flattened out to
one dead level.
It might at first be thought that our best chance of noting any
elevations or depressions of the Martian surface lay in catching that
surface in profile, by scanning the bright edge of it which stands
sharp-cut against the sky and is called the limb. For this is
practically what we do on earth when we mark a mountain against the
horizon and measure its height by triangulation. Unfortunately the
method fails in the case of Mars because of the great distance we are
away. Unless the planet were distinctly more generously equipped than
the earth in the matter of mountains, nothing could be hoped from so
forthright an envisaging. So relatively insignificant to the size of
its globe is the relief of the earth’s surface that an orange skin
would seem grossly rough by comparison. The same proves true for Mars.
With the greatest magnification we can produce, the Martian limb still
appears perfectly smooth.
Public-domain text, read in full here on John Shaqi.
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