n a scientific
t nothing of
it and iden-
ey.
rance of any
CS,
y is not jus-
| quality can
nguage very
ictionary he
terpretation
erial photo-
Imost daily.
rs should be
ery interest-
cople astray.
)0,000 aerial
ation is still
intelligence
cult science.
hink I have
ear what is
an show me
ette stub in
ven position
nber X, the
onan Doyle
ey does not
fferences in
in shade of
d so much
d wind; the
et up rules.
nature has
f centuries,
terpretation
by photo-
thus make
"wn techni-
my opinion
inbelievable
ay will one
Fig. 1. Portion of a vertical
aerial photo mosaic, scale 1/
50,000, showing Dutch territo-
ry in which soils exhibit varia-
ble resistance to erosion. Com-
pare with fig. 2.
Fig. 2. Same area as fig. 1, on
which density of dots indicates
degree to which soil resisted the
working of the water, formed
barriers or cliffs, or consisted
of dunes built up by water or
wind. Areas containing few or
no dots are those in which
water caused erosion of thc
soil, forming of rivers, lakes or
moors, and in some cases, des-
truction of rivers.
Of course, such a publication will meet with objections. As Prof. Scher-
merhorn once said: *Be careful; after you have been dead for many years,
people will still curse you because you told them things they did not like to
hear.”
However, this should not prevent us from making progress. I should like
to illustrate my methods with some slides, showing parts of the Dutch territory
colored in red and blue on black maps scale 1 : 50.000.
Blue means that the aerial photographs show that in a given period water
did its work there: erosion of the soil, forming of rivers, lakes or moors,
destruction of rivers.
Red means that the photographs show that this soil resisted the working
of the water, formed barriers or cliffs, or consisted of dunes, built up by water
or wind. The red/blue map given as an annex, shows clearly the great impor-
tance of the mapping of these features; a single photograph only gives a slight
impression of what happened.
Eprror’s NOTE: Because of difficulties involved in the reproduction of Mr.
von Drabbe's maps in color it has been necessary to substitute annotated pho-
tography instead. It is recognized and regretted that the effectiveness of his
illustrative material is thereby somewhat diminished.