Gl
|
’
«
*
Bere on tho averasto.
activity
a
«|
-
a
7 ne
In other worcs,
whieh dis apravontly moving im
st
“44a
dhe
op
ans
-
“4
“
fas
tnozss is
aw!
this
~
as
tho current Stroama,
4%
4
“4
i
viceosnrone
oO A ee
Some
a
war
oo
4
we
8
te
t.
ast
Lon
eye wyen Be
nag
G2
it at losst- has made the
tuzgn
into
the
Javanese
curroat,
but
Gl
.
it has not yat reonened the United Svat.
DR. DIORA
roy
.
«
.
:
Shank you
very
mush,
he
Those
tg
,
a
two poesentarioenas
ara now Goen for cdiscevssacn,
BX. LEVDBSNG:
DR. HARLEY:
Was there any inddcaticn of the cepth?
fo an semoewhat ef a srade avsut that.
Covdencat thet ws had,
With this
ov almest any acscsuntiag Gandrmmont, our
acccuatensers Were very nich,
dust env standard Coviation to
counting alene may have been as hich es 2550.
terns of large numbers
of those (indicating).
FF am spoaking in
If you take a
Jong proltilo andaverare tint cut, you roaline that thet coos
not do much and you will got a fadriy nice falloff with a
logosriphic cetivity, aad you got scovt of a tail, and this is
cowa at a vory low activity where you would get one of those
averages Wnich is quite deiinite.
In other words, I belicsve there is semo activity betwvoon
the thermocline and boloy tho osdduary mised laver,
rathor lew and only twice
660 meters,
It is
Gid wo mako moasurenents mucn below
Below 6609 meters covn--and thove
are several cascs
of several bottles--the activity was newtliciblic, but 600 maters
was d3finitely below ths thernocline.
FROU THE FLOOR:
wouldn't bo below th
££ contft know the Pacizic very well,
Y
rmanent tharmeslina,
ft