the
80
t
due to
any
such insufficient form
of protection for along Section A, where
no rubble exists the same hard and uncorroded surface underlies the
An additional then deposit of silt. An
and
interesting piece of evidence of
the filiress of this ground for foun -
I think be gathered
dations
may from the boulders
Shingle
of
the similar
le and clay beach along Bel- cher's Bay at the western extremilyy
the Prays; these
of
ing
above the
AAL
seen
project-
ground.
ound at
d at low tide
scour around.
without the signs of them usual in the softer sands 4- and travelling shingles of other shores in the shape of the hollows and pools which the waves scoop around them.
Though
Though a less likely contingency it.
was not found wither at the four places where the wall
was pulled down
for inspection that the lower had been pushed out by back pressure noticeable dif
LUTLA
there
any very
stone and another
ference between one in the inward pitch of
the
footings.
As the undisturbed level of the lower!
original wall attests the its foundations beneath
courses of integrity of
the
the me
as well as
any
other feature.
--
کمر
are here:
photographs hos
8, 9 and 10 given of the places left standing
*-----་
after the lyphoon intermediates to those which were pulled down for examina tion, special attention being called to the ugly and irregular coping masonry which must not be taken
Ax