What then are we to understand by the term "neutral" as applied to the
Panama Canal in war time? I suppose the meaning to be that if there be a
war to which the United States is not a party, the Canal will be used by
belligerents in exactly the same way as was the Suez Canal, _e.g._, in
the Russo-Japanese War, and that the Government of the United States has
pledged itself to see that such neutrality is preserved. But if there be
a war in which the United States is a party, the circumstances of
fortification and operation by the United States in fact render it
impossible for the other belligerent to use the Canal, and are
intended[3] to have that effect. This being so, the United States is
preparing to defend the Canal from attack. Thus it is important to the
proper understanding of the undertaking on which the United States
Government has embarked that we should clearly realise that the Canal is
only neutral in a restricted sense.
The commercial status of the Canal, however, is similar to that of Suez,
in that by Article III., § 1, of the Hay-Pauncefote treaty, "The Canal
shall be free and open[4] to the vessels ... of all nations ... on terms
of entire equality, so that there shall be no discrimination against any
such nation, or its citizens or subjects, in respect of the conditions
or charges of traffic, or otherwise."
[3] See Report of Canal Commission, 1897, p. 168.
[4] In Article XVIII. of the treaty with Panama this clause is cited,
with the addition "and the entrances to the Canal."
CHAPTER II
ON THE CANAL AS IT IS TO BE
BETWEEN Colon and Panama the American Isthmus is about 36 miles across
as the crow flies, and is therefore nearly, though not quite, at its
narrowest. In this portion of its sinuous course both coasts trend north
of east and Panama lies nearly south-east of Colon. The Isthmus in
general is a very confused mass of hills and mountains. It is crossed by
no transverse trench (such as sometimes occurs in mountainous regions),
neither by the trough provided by down-folded strata, nor the rift
valley produced by fracture and foundering of rock. A low-level
transverse can only be found by following up the course of a river,
crossing the divide, and following the course of another river
downwards to the other ocean. From the vicinity of Colon, by following
up the valley of the River Chagres, we are led in precisely the required
direction, _i.e._, directly towards the Pacific, for nearly two-thirds
of the way. The distance from the head of Limon Bay, following the
curves of the valley, is 26 miles to this place, Obispo, and for the
greater part of the distance the river flows in a broad valley of deep
alluvial deposits.
[Illustration: FRENCH DREDGER LAID UP.]
[Illustration: FRENCH TRUCKS PARTLY COVERED WITH FOREST GROWTH]
Public-domain text, read in full here on John Shaqi.
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