105
Will May, the latter
levil from beny
May
A
low
till October. The
extraordinary disparity between them
is due to the land locked shape
of
tion
the harbour, to the driving
of
the monsoons
and
A ë
to the
a
penning up of the ebb waters in ..
their endeavour
dead
at
against
constructed a
to excaper eastwards
the winds throught channel as the Ly-
Prev. There is but litelo
doubh also that the
great freshe
water current of the Canton Stever
under certame Conditions steams the
progress of the flow which
through the harbour and
passes.
abulo
interesting
natural
producing
these peculiar tidal phenomma_ suffice it briefly
the N.E. mov
Joon
to
suy
that de
they combine
exert a damming influence
during
گر هم مرح
the waters in the Starbour, while the
5.W monsoon).
site tendency
gevee
what
for
has
directly oppor
The figure below.
convenience has
not been pepeated in the drawings
and Neap
sit the ordinary Spring tide levels
of
High Water
both monsoons.
Ordinary Springs N. E. Monsoon!
DO
Neaps N.E. DS
De
Springs S.W. DO
De
Neaps S.W. De
*M 'N "M *M
against it at right angles.
éla
would be out of place hereto
enter into the various
and
interest
ing
Low Water
Ordinary Neaps N. E. Monsoon
De
Spring's N. E.
DY
མྨཾ, དྷུགནཡ ཎཱཔུསྶ ཡ
Neaps S. w.
DI
De
De Spring's 5. W.
*
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