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CIHM/ICMH 

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CIHM/ICMH 
Collection  de 
microfiches. 


Canadian  institute  for  Historical  IVIicroreproductions  /  Institut  Canadian  de  microreproductions  historiques 


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Technical  and  Bibliographic  Notes/Notes  techniques  et  bibliographiques 


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0 


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D 


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Ce  document  est  filmd  au  taux  de  reduction  indiqud  ci-dessous. 

10X  14X  18X  22X 


J 


26X 


30X 


12X 


16X 


20X 


24X 


28X 


32X 


The  copy  filmed  here  has  been  reproduced  thanks 
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Library 


L'exemplaire  film*  fut  reproduit  grAce  A  la 
ginirositi  de: 

Siminaire  de  Quebec 
Bibiiothique 


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possible  considering  the  condition  and  legibility 
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other  original  copies  are  filmed  beginning  on  the 
first  page  with  a  printed  or  illustrated  impres- 
sion, and  ending  on  the  last  page  with  a  printed 
or  illustrated  impression. 


The  last  recorded  frame  on  each  microfiche 
shall  contain  the  symbol  ^-^-  (meaning  "CON- 
TINUED"), or  the  symbol  y  (meaning  "END"), 
whichever  applies. 

Maps,  plates,  charts,  etc.,  may  be  filmed  at 
different  reduction  ratios.  Those  too  large  to  be 
entirely  included  in  one  exposure  are  filmed 
beginning  in  the  upper  left  hand  corner,  left  to 
right  and  top  to  bottom,  as  many  frames  as 
required.  The  following  diagrams  illustrate  the 
method: 


Les  images  suivantes  ont  tt^  reproduites  avec  le 
plus  grand  soin,  compte  tenu  de  la  condition  at 
de  la  nettet*  de  i'exempiaire  film«,  et  en 
conformity  avec  les  conditions  du  contrat  de 
fHmage. 

Les  exemplaires  originaux  dont  la  couverture  en 
papier  est  imprimte  sont  filmte  en  commen9ant 
par  le  premier  plat  et  en  terminant  soit  par  la 
dernlire  page  qui  comporte  une  empreinte 
d'impression  ou  d'illustration,  soit  par  le  second 
plat,  selon  le  cas.  Tous  les  autres  exemplaires 
originaux  sont  filmte  en  commenpant  par  la 
premiere  page  qui  comporte  une  empreinte 
d'impression  ou  d'illustration  et  en  terminant  par 
la  derniire  page  qui  comporte  une  telle 
empreinte. 

Un  dee  symboles  sulvants  apparaftra  sur  la 
derniAre  image  de  cheque  microfiche,  selon  le 
cas:  le  symbols  -^>  signifie  "A  SUIVRE",  le 
symbols  V  signifie  "FIN". 

Les  cartea,  planches,  tableaux,  etc.,  peuvent  Atro 
filmte  A  dee  taux  de  rMuction  diff Arsnts. 
Lorsque  le  document  est  trop  grand  pour  Atre 
reproduit  en  un  seul  clichA,  il  est  film*  A  partir 
c<e  I'angie  supArieur  gauche,  de  gauche  A  droite, 
et  de  haut  en  bas,  en  prenant  le  nombre 
d'images  nicessaire.  Les  diagrammes  suivants 
illustrent  la  mithode. 


1 

2 

3 

1 

2 

3 

4 

5 

6 

ir       I 


ABSTRACT  OF  PAPER 


ON 


Deep-sea  Soundings 


AND  TEMPERATURES  IN  THE  GULF  STREAM. 


READ  BEFORK  THE 


AMERICAN  ASSOCUTION   FOR  THE  ADVANCEMENT  OF  SCIENCE,   AT  THE 
MEETING   HELD  AT    MONTREAL,   AUGUST,    1882. 


By  commander  J.   R.  BARTLETT, 
TJ.    S.    NAVY. 


From  the  Pkoceedings  op  the  americak  Association  for  the  Advancement 
OF  Science,  Vol.  XXXI,  Montreal  Meeting. 


PRINTED  AT  THE  SALKM  PRESS. 

SALEM,  MASS. 

1883. 


i«ki; 


\ 


I 


/Ivihot/eni'fiir   Ih'tht' 

J.  U  Baitlett  .Counuauilei'  U.S.Xavy, 

llydro^^raphfff  to  till-  Hiiriaii  of  Njiviii/ilioii  . 
irti.sJiim/ton.  l),(' . 


Deep-ska  Sounihnos  and  Tempekatuues  ix  the  Gulf  Stream 
OFF  THE  Atlantic  Coast,  taken  xinder  the  untECnoN  of 
THE  U.  S.  Coast  and  Geodetic  Survev.  By  J.  R.  Baut- 
LETT,'  of  LonsiUile,  R.  I. 

[AnSTKACT.] 

I  HAVE  come  to  this  meeting  of  tlie  Association  at  the  kind  re- 
quest of  Mr.  Ililgard,  the  Superintendent  of  the  Coast  and  Geo- 
detic Survey,  to  tell  you  of  the  investigations  made  by  the  steamer 
"  Blake." 

Tlie  hydrographic  party  of  which  I  have  charge,  has  been  in- 
vestigating the  Gulf  Stream  for  the  past  four  j'ears,  the  last  two 
summers  having  been  passed  on  our  immediate  coast.  All  of  you 
have  ideas  or  pet  theories  in  regard  to  this  great  river  of  the  ocean, 
as  Maury  lias  happily  called  it.  Man}'  of  our  greatest  scientists 
have  written  learnedl}'  about  it.  Professor  Bache,  while  he  was 
Superintendent  of  the  Coast  Survey,  caused  extensive  and  sys- 
tematic investigations  to  be  made  of  its  physical  features.  From 
the  data  obtained,  the  Stream  was  assumed  to  start  from  tlie 
Caribbean  sea,  making  the  circuit  of  the  gulf  of  Mexico,  and 
to  issue  with  great  velocity  and  high  temperature  from  the  straits 
of  Florida,  continuing  to  about  latitude  45°N.  It  was  described 
as  a  superficial  stratum  of  warm  water  flowing  over  one  of  cold, 
with  banks  of  cold  water,  and  diviiled  or  bifurcated  into  warm  and 
cold  bands. 

The  bifurcation  was  explained  by  the  presence  of  hills  and  val- 
leys which  were  developed  by  the  soundings,  the  cold  water  being 
said  to  be  in  the  valleys  and  the  warm  water  on  the  elevations. 
As  no  soundings  were  obtained  in  the  strength  of  the  current,  it 
was  supposeil  that  the  stream  ran  over,  if  not  in,  a  great  trough  or 
depression  of  the  sea-bed.  At  tlie  time  the  investigations  were  " 
made  under  the  direction  of  Professor  Bache,  the  means  of  obtain- 
ing the  depth  of  the  sea  were  very  imperfect ;  now  we  have  the 
most  improved  apparatus  anil  soundings  can  be  taken  with  wire  in 
any  current  and  to  any  depth  with  almost  perfect  accuracy. 

The  investigations  made  on  board  the  "Blake"  show  conclu- 
sively that   the   above   assumptions   are  wholly  erroneous.     My 

•  Commandor  U.  S.  Navy. 

0) 


2 


DEEP-SEA   SOUNUINGS  ; 


soumlings  give  no  channel  for  the  Streiiin  to  run  in,  there  are  no 
hills  or  valleys,  and  1  have  never  found  any  bifurcation  or  warm 
and  cold  bands.  The  temperatures  obtained  do  not  show  cold 
water  beneath  the  Stream,  but  a  current  of  warm  water  between 
the  Florida  straits  and  cape  Hatteras  down  to  the  very  bottom. 

As  has  already  been  stated  to  this  Association  by  Mr.  Ililgard, 
the  current  entering  the  gulf  of  Mexico  from  the  Caribbean  sea 
docs  not  make  the  circuit  of  tiie  gulf  as  formerly  supposed,  but 
passes  to  the  noithward  and  eastward  in  the  same  general  trend  as 
the  Yucatan  plateau,  and  thence  to  the  straits  of  Florida. 

The  lines  of  soundings  taken  by  the  "Blake"  were  twelve  in 
number,  beginning  at  Jupiter  inlet,  Florida,  and  extending  to 
Currituck,  N.  C.  They  were  run  normal  to  the  general  coast 
line. 

The  soundings  give  very  interesting  data  in  regard  to  the  physi- 
cal featur(!s  of  the  bottom  of  the  ocean  over  which  the  Gulf  Stream 
flows.  Instead  of  a  deep  channel  in  the  course  of  the  Stream,  as 
reported  by  Lieutenants  Maffltt  and  Craven,  and  published  in  the 
Coast  Survey  Reports,  our  later  soundings  with  wire  show  an  ex- 
tensive and  nearly  level  plateau  extending  from  a  point  to  the 
eastward  of  the  Little  Bahama  banks  to  cape  Hatteras.  Off  cape 
Canaveral  this  plateau  is  nearly  200  miles  wide,  and  gradually  con- 
tracts in  width  to  the  northward  until  reaching  Hatteras,  where 
the  depth  is  more  than  1,000  fathoms  within  30  miles  of  shore. 
The  plateau  has  a  general  depth  of  400  fathoms,  suddenly  drop- 
ping oft"  on  its  eastern  edge  to  over  2,000  fathoms. 

The  course  of  the  Gulf  Stream  can  be  traced  by  a  study  of  the 
specimens  of  the  bottom  obtained  ;  on  each  side  of  the  Stream  the 
sounding  cylinder  brought  up  ooze,  but  in  the  strength  of  the  cur- 
rent the  bottom  was  washed  as  bare  of  ooze  and  all  living  things 
as  the  bed  of  a  mountain  torrent.  Instead  of  a  cushion  of  cold 
water  at  the  bottom,  the  temperatures  were  the  same  as  those  found 
at  the  corresponding  deptii  of  400  fathoms  in  the  Windward  pas- 
sage and  in  the  course  of  the  current  through  the  Caribbean  sea  and 
gulf  of  Mexico. 

The  temperature  of  the  surface-water  was  taken  every  mile  on  all 
lines  and  in  no  case  were  there  found  any  warm  or  cold  bands. 
There  was  a  slight  rise  of  temperature  on  entering  the  current,  at 
the  surface,  and  also  a  corresponding  rise  at  the  bottom  in  the 


/ 


rit' 


-V"'.ril«^M>.pgfi.t,<: 


BT   J.    n.    BARTLETT. 


8 


/ 


same  locality.  Tho  surface  temperat.ires  found  in  the  Stream 
were  much  below  those  generally  given  in  published  works  on  the 
subject.  The  average  temperature  in  the  axis  of  the  Stream  rarely 
exceeded  83°F.  in  June  and  July.  On  one  or  two  occasions  the 
thermometer  read  as  high  as  86°,  and  once  89°,  but  it  was  at  high 
noon  in  a  dead  calm.  The  temperature  at  five  fathoms  did  not 
range  above  the  average  of  81^°.  The  surface  temperatures  did 
not  indicate  a  cold  wall  inside  of  the  Stream  ;  the  water  between 
the  one  hundred  fatliom-line  and  the  shore  seemed  to  be  an  overflow 
of  the  Stream,  as  the  temi)eratures  at  five,  ten  and  fifteen  fathoms 
were  nearly  as  high  as  those  found  in  the  Stream. 

Lines  for  series  of  temperatures  from  the  surface  to  the  bottom 
were  run  during  the  past  summer  from  Block  island  to  the  Bermudas, 
and  thence  to  liatteras.  The  isothermals  show  the  Labrador 
current  until  nearing  the  Stream,  when  they  descend  gradually 
and  in  the  stream  itself  abruptly,  to  their  greatest  depths.  Instead 
of  the  warm  stream-water  thinning  away  as  it  was  reported  to  do 
when  spread  out,  it  was  not  much  over  fifty  miles  in  width  at  the 
time  of  our  crossing,  as  shown  by  the  current  and  high  surface 
temperatures.  The  temperatures  below  the  surface  were  much 
higher  than  at  the  same  depths  off'  the  coast. 

The  ordinary  temperature  at  the  bottom  off'  Savannah  and 
Charleston  in  400  fathoms  was  45°.  In  the  Stream  between 
Block  island  and  the  Bermudas  it  was  as  high  as  55°  at  400 
fathoms.  The  isothermals  remained  at  almost  the  same  depth  to 
the  southward,  as  in  the  Stream,  on  the  entire  line  to  the  Ber- 
mudas. Just  north  of  the  Stream  the  temperature  at  400  fathoms 
was  394°  and  40°.  At  a  point  well  in  tlie  Lal)rador  current  away 
from  the  Stream,  the  temperature  at  400  fathoms  was  38J-°. 

From  the  Bermudas  to  liatteras  the  isothermals  were  at  the  same 
depths  as  were  found  south  of  the  Stream  on  the  previous  line, 
but  when  in  the  current  off'  liatteras,  where  the  Stream  trends  to 
the  eastward,  they  rose  to  the  same  depth  as  oflT  Charleston  and 
Savannah  on  the  plateau. 

These  temperatures  below  the  surface  seem  to  suggest  that  the 
Labrador  current  underruns  the  Stream  at  Hatteras,  but  at  no 
other  point.  It  probably  keeps  its  natural  boundary  or  western 
wall  along  the  1,000  fathom  curve,  and  thus  follows  around  the 
plateau  towards  the  equator.     No  definite  conclusion  can  be  drawn 


tit: 


4  I)EKr-8EA    SOUNDINOS  ;    BY   J.    R.    BAHTLKTT. 

from  the  datn  obtainod  thus  fur;  but  we  have  at  least  a  clear 
field  to  work  upon  in  the  future,  in  regard  to  temperatures  and 
currents,  and  tiio  contour  of  tlio  bottom  as  far  as  Ilatteras  is  well 
portra^x'd. 

Tables  are  appended  giving  the  depths,  etc.,  found  on  the  several 
lines. 


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Cii.  H. 

I'M  III. 

riii.i./.          iM.i.iu. 

I'lll.  112. 

I'lll.  Ill, 

I'hl.OI 

.... 

KO- 

KU" 

no- 

Kl- 

«• 

nil- 

»{' 

Kir             mr 

w 

w* 

»ir 

.... 

f.ic 

41)* 

*IV 

421' 

42r 

ill' 

41' 

44*                          41* 

4,1' 

4.1* 

w 

.... 

N.  X  K  »■» 

N.XR.2..1 

N.  X  K.  2.B 

N.XK.3.» 

N.  X  i:.  2-1 

N.  X  r.  1. 

N.  X  K.  n. 

NXK.l,         N.Xf:.2.« 

N.  !,.» 

,           N.l, 

0 

"1 

"1 

41 

41 

1 

M 

^l 

LINK  1).     tlliiM  HIIOIll'',, 

:il          1             .1                       41 

i.ATm;i)K 

41 

m'  If.V  N,  TO  LAT.  m" 
SI                        °i 

l.H 

■J  7 

42 

■.'2.1 

21 1 

:ill 

.T-? 

11.1 

4ai                      4.17 

4111 

411 

414 

nik.  81.. 

llik.  Ml. 

Cn.  H.,  brk.  .i^li. 

Cri.  8.,  Iirk.  9h. 

Kill',  .s. 

Co.  H. 

Cii. 

Co. 

i'o.                     Co, 

III. 

Co. 

Co. 

(HI- 

«!• 

»r 

IB' 

M" 

*'h 

DHJ* 

mil' 

Ml"                    HI* 

nr 

SI* 

HI' 

TO* 

(Ill- 

r,.ii- 

1:1' 

111 

41' 

4I\* 

1.1  i- 

4ni'                40' 

4,V 

in* 

41' 

V.  W.  1. 

N. \V.  1.1 

N.W.  I..1 

n 

N.  X  W.  1. 
11 

N.  N.  w.  a. 
41 

N,  N.  W.  :l. 
4 

N.  N.  W.  .1. 
41 

N,  N.W.II,    '     N   N   \V.;l, 

M    W    tL'    '1 

N,  N.  IV.  11. 
Fl.,\.,  TO  I..1 

"1 

{., ........ 

mi 

■INK  K.     l.|;iiM  ST.  .lOII.N'H  lllVI'.lt 

4»                        4                          .11 

T.  Mil"  ild 
'H 

58 

17 

111 

iin 

'2T1 

:ill 

37,1 

411 

4110                       4nO                         IMI 

407 

41.1 

.... 

Co.  Ilk.  s. 

(  .1. 

C.I.  s. 

Co.  n. 

Co.  1. 

<.i.                       C.I.                        Co. 

Co.  M. 

Co.  «, 

ft!" 

W 

!i;r 

Mi- 

Kll 

lu- 

K\' 

M' 

M'                        H21' 

1-21' 

Ii-2i* 

Ml- 

!■«• 

i»;i' 

ir 

ir.l- 

l:l- 

ll* 

u- 

41* 

41-                        41* 

4I1' 

4.11* 

iV 

N.  N.  K.  2.7 

N.  N.  K.2.7 

N.N.  E.  2.7 

N.N.  K,2.7 

N.  N.  H,  2.7 

N.N.  K.3.7 

N.  N.  K.  2.7 

N.  N.  K,  2.7        N.  N.  B.  'J. 7 

N.|K.  I.'JJI 

N,u:.  I.2S 

N,|K.  1. 

»l 

"1 

nj 

.11 

0 

OJ 

0 

■11 

LINE  i:    l'UO.M  TYIIKI':  IIO.IDH, 

H        1           »1         1           f.1 

liA.,  Tl)  LAT 

f'l 

'11 

Jl 

40 

:il 

.V, 

1« 

21  Mi 

2li1 

■20.1 

'jra 

:i20 

;uii 

3^18 

:iii.i 

<i. 

ii. 

s.  Ink.  .-ill. 

Ilk.,  wli..  (i. 

.... 

I'll. 

.... 

Cii. 

Co. 

Co. 

C.I, 

Co. 

Co, 

SOi 

Hll- 

KU- 

m- 

Hi* 

W 

M' 

m* 

Kl* 

Kl* 

l>l\- 

T0\- 

liV 

n7 

mi' 

.vr 

US- 

111' 

im* 

4-H- 

.HI* 

.11' 

Ml* 

nij' 

0 

N.  N.  K.  1. 

N.  N.  v..  1. 

N.N,  K.  1. 

N.  N.  K.  1. 

N.N.  K.  1. 

N.  N.  |.:.2.1 

N.N.  h:.2.4 

N.l.., 

N.  I..1 

N.  I..1 

N,  I..1 

N.  1..1 

Dirlam-ebctwcfii  j*ouiuliiii{-,      is 

DeiiUi  In  fatUomw !     10 

Clianu'terof  boUom .... 

Siirrano  teiiiponilnt'u 

Doltiini  teinp(ii'iitun> i    •  •  ■  • 

Current i    ••-• 

Distance  liftrtd'ii  -xiuiiiIhik^j      I.'i 

DL'ptli  ill  faitiom^ J'» 

Clianu-tur  uf  Imltom 

Snrfaci,'  teinpcraliiri' 

Boltoin  tL'iiii'uratun' 

Current ■■•• 

Diiitaiinc  lietwflen  iouinliiiys'      11 

Depth  ill  fiU  limns 10 

CImracter  ff  hott(tiii 

Surfaro  ((.'tnpeiatiire.. 
Bottom  leiiipiiraiiiie... 
Current 


t 


DHtaiice  liPtwi'Pii  hiHtndinir-j 

Depth  in  fathoms j 

Character  of  bottom ^ 

Surfaea  temperatun- 

Bottom  temperature j 

Current 1 


17 
1.1 


I5i 
17 


20i 
19 
Cri.  yl.  S.lik.r 
Hi' 

N.  i:.  0.  i. 

i"l 

ID 

Brk.  Sh. 


H    I 


Distanno  between  .soui 

I>'pth  infalhoniK 

Character  of  bottom... 
flurl'acc!  temperatiiio.i 
Bottom  tompi-raturL'.. 
(-'urreiit 


-Unj.- 


71 

111 

11 

30 

:r 

701- 

::l' 

wr 

i:.s.K.2/. 

Wi 

l.l 

File.  ^-y.  3. 
8:il' 
70' 


2 

en 


7 

.12 

li.  .sh. 

t'O' 

on* 
S.  K.  1.3. 

lilj 
20 

Cr».  s, 
H' 

oi:!' 

0 

10 

30 


N.E.X-"*.  1.73 


DHtuiice  liL'twoen  iiouit'iiii;:.- 

Depth  in  fnlhoins 

Clmr.ir.tor  "f  Ijottom j 

Surface  tpinperntiiii' 

n'lttomteii'iiPMituri' 

Curii'iil 


'■■i  1 

101 

10     1 

10         1 

7:1* 

70" 

71'/ 

.181- 

-.U'  0..1M 

w.0.,1. 

Ul.ill.iii 

wl' 
111' 


lo'i 

21 

ru...  ,<, 


1 

142 


3t 
■iii 


7 

70 

Wli.  l.k.  ril..s. 


s.  \v.  o.r,       i     .■*.«•.  0.1 


21 
Van,  gy,  S. 

Si' 
(Ml' 
0 


81* 

611' 

N,  E.  X1.73 

I.IXE  K 

21 

427 

Uloli.  0. 

81' 

40- 

K.  N.K.2.i 

U 

21 


7 
111 

BO.  S. 

bill' 

51' 

.S.E,1J 

n 
.11 

.s.  o.,  Uik,  .Sh. 
SI' 

0:1' 
0 


421' 
S.  K.XN.l 
I'lJdM  C 

n 

I.'.:  I 

I, I. III.  o/.. 
Kl* 

;i71* 
i:..N  K.2. 

n 


»1 

217 


4 

123 

Co. 
81* 
52" 
0 

4] 

lU 

8-21* 
M' 
0 


2] 

210 


41 

l.Kl 

811* 
4J* 

N.w.xiv.o.; 


HI* 
41' 


7 


,.  J  N.  3.2 


I.IXK  fi.     I''l;(iM  CAIT,  HUMAN,  S.  I'.,  [(I  I, AT.  !I0°  fill'  >'.,  \.i 


■II 

2'<l 
C.I.  8, 
8.2' 
41* 
K,  a  N,  3.2 


:>1 


431 
E.  1  N.  3.'3 


■'1 
.ll'j 

Co.  It. 
8,11' 

4n- 

K.  J  X,  3.: 


31  I  3J 

311  3.1.1 

I  u.  U.  Co.  It. 

83' 


I.V 
K.  1  S  3  2 


401' 
E,  I  N.  .1. 


LI.NK  II.     I'ltOM  .SlIOUK,  I.AITnDi:  :1;1'  ;i8'  \,  Tl)  LAT,  ill' 


224 
S.  C„ 


H  oj 

2;,i  3ia 

Kill'.  K,  Cii.  It. 

811"  81* 

,N.  IV. X  "'0,7.1  JN.  W.X"'.  o  7.1  N.  W.  X  "'.o  r.  N.  E.  ]  E. 


182 

\Vli..lik.  S. 

801* 


377 
Co, 

Kr 

421* 
N.E.JE.  1.7 


«1 
303 
Co, 
831* 

3^1* 


OJ 


e:i* 
40' 


S  EXH  IE.3.3  N.EXE.  I  I 


I.IXK  1.    I'Uk.M  CAl'l';  I'KMl,  Tl)  LAT.  It'"  05'  X.,  J.UXd 


X.  E.  1  E, 
.WE  IIATI 


31 
120 

8-2' 

N.  W,X  W, 

0| 

li:ii 
lil.'li.  .,/.. 


2l>'.l 


8^ 

431'  I  43- 

N.W.XM'.2.|    N.E.iN.2. 


2.73 
KliAS 


1 1:,'^ 
i;ioii.  oz. 

81* 

37',- 
E.  .s.  i:,2..' 

4 

31 

a.,  lok..>i|i. 

701* 


371* 
K.  1  K.  2.73 
■m  LAT. 

'  1 
l,-,i;o 
<;i.iii.  iiz. 

811' 

371' 

E.  X  N  3. 


:ll 
104 

KJ-.  S. 

821' 

471* 

N.  IV.XW.'J. 

m 

2010 
I. lull.  111!. 


N,  E.  IR.  2.75 

Xo"  2V  N.,  LO.Sd.  74'  »)'  W, 


31 


81" 

43* 

N.  E.  1  N.  ■J. 


Ml* 

10* 

NX.  E..'). 


II 

280 
Ilk.,«h.S. 

841- 

4.1* 
N.  N,  E.  3. 


310 

Ilk.,  wh.f 

81* 

44* 

N.N.K.S, 


LiNi: ,(.    n;(iM  CAi'i;  i.uuKuur,  .n.  v.,  to  i.ai'.  :ii»  iW  \.,  i.c 


I 


iloh. .,/.,  (:i..ii. ../.. 

40*  13*  ....  12*  3:i*  38*  .'In-  j  371*  37* 

S.  \V.0.3  S    \V.0,3  .■<.  W.0  3       I       S.W.O.  5  S.  W.0.3  8.  W.  0.3  .S.  W.  0.3      |       .S.  IV.  0.3  .i^.  W   11.3       I  .'<.W.  0.3 

ii:;  lu'iii,:;  mi'a>uri'il  IVoiii  Uio  shiii'i'.     Tlir  lUiIni'vliitjini-s  IVoni  rliorofti'r  i>i  imttiiin  'av  :  I'li.'..  Itiir ;  hk.,  hhirk;  yy..  firt'y;  ivli..  ■ 
Tlii^  llrst  line  A  w.as  rtiii  .Iiiiio  Ist,  iiiid  tiny  wen.'  i.'oiitliiiii'il  to  tlio  mirtliwanl  diiilii;,'  ,Iiiiie  iiml  July,     The  lilies  were  run  iliiriiiij  doy  iiinl  iiiylit,  Imt  we  cro.'.wil  ihc  oU'eiiiii  in  liio  .loyllnn-.     A,<  iiieutliiiicil  in  llie  I'ssii) 


[(■.no 

i;iiiii.  112. 

811* 

.■171* 

E.  4. 

'2! 
.3.10 
Cllll).  iiz. 


i 

1013 

Uliili.  <.z. 

81* 

371* 

E.  1. 

21 

077 
I.Joli.  nz. 

70* 

38* 
8.  W.  0.3 


u 

1027 
(iloh,  oz. 

81* 

37" 
E.  3. 


11 

I7.V1 
liliih,nz. 
831* 
301* 
E.3 


LINK  L.     |-|;0.M  Cl'ldtl'l  UCK,  V.  (',   ri(  LAi'.  :ili°  \i'  N.,  LO 


43 


5 


1003 
Iji.ili. 


1103 

i;ioi..oz. 

7111* 


J,',,,.],. The  dlstuiice  lieUvi'i'ii  souiiiliii^'8  :iii'  ^-ivon  in  iiiiiilirol  niili'S,  lliu  llrst,  - 


illlWNHpHIW'*'y" 


•HOM   MITIKH  INI.KT,  H.A.,  T(»  (  I  IIIHII  «  K,  N.  (' .  IIY  TIIK  (OAST  AND  OKODKTIC  MrRVKY  KTK.  "I»I<AKK,"  COMMVNnKIt  .1. 

1:11  iM.i;i',  Ki.A.,  ID  MiiMiMiv  iiO(  i>,  i.irTi.i;  ii\y  \\i.\  msKs 


».  IIAIlTr.KTT,  V.  H.  N. 


I  V,ir 

IKUK,  I.AI'II'I'DK  JT"  07'  K.  T"  I.AT.  IIT'  Jl',  I,ON«l.  TT"  il;i'  W. 


1 

.11 

n 

«l 

41 

4J 

» 

M 

<l 

II 

41 

M 

A 

H 

H 

n 

HI 

>.., 

.... 

mi 

«ip7 

4;i 

4-..1 

Wll 

Mil 

M7 

W„l 

M 

Tt^U 

hki 

ni- 1 

mil 

IllHI 

mil 

nil 

,it. 

.... 

^, 

r.i. «. 

(ii.lt. 

I'l.i.  i». 

I'l.l.  114, 

I'M.  «t. 

rill  o>. 

I'lil.  iia. 

Mil.  111. 

I'm.  IX. 

I'lil.Oi. 

I'lil.  IK. 

I'lil    IK. 

I'lil.OI 

l-til.  III. 

l-lil.iK. 

.in. 

.... 

»r 

»!• 

;j* 

7ir 

:v 

7il- 

7lf 

TH- 

7H* 

;»• 

711- 

I- 

•,f 

7II" 

771' 

Tn- 

to* 

.... 

Ji- 

41" 

«l' 

44J' 

44" 

41- 

4ir 

4ii- 

4n- 

Ki' 

iWl- 

••lil" 

DO* 

3B» 

no- 

au- 

•  ••• 

.... 

..1 

ll 

«.  (1.11 

( ; 

Mniiihtrly, , , , ,  „ , 

.... 

nuK,  i.ArnuiiK  aH»  w  n.  to 

I,AT.»  SN"  41'  N.,  t.ONCI.  THo  Ti'  W. 

.........) 

"" 

1 

*\ 

•11 

'11 

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10 

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I'l 

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,,,, 

.... 

.... 

.... 

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4M 

ll'4l 

4''l 

4:» 

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CM 

•  ••• 

.... 

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I'ltl.  112. 

w 

I'l.l.Ml, 

Hi* 

4.r 

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Ml' 

l'l'l.n<. 
HI- 

Till.  ni. 
711" 
4I1- 

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Til" 
411- 

I'lil.  IK. 
71H 
4J' 

I'lil.OI. 

711* 
41* 

.... 

.... 

.... 

.... 

.... 

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t          N.l, 

0 

II 

H.x  >:..». 

H.XW.  1. 

M.  H.  >V,  l.J 

,.,, 

,,,, 

.... 

.... 

>iii;,  i.ATiiiDK  m'  a:.'  N.  to  lat.  an'  n:"  n.,  lono.  tip  'm'  w. 

i 

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H 

I'l 

11 

11 

0 

III 

10 

101 

I'l 

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0 

I'l 

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4111 

411 

411 

4.M 

411 

4IH 

4.MI 

4117 

470 

1117 

4IM 

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lit, 

C.i. 

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I'll,  iia. 

■■III.  "1. 

I'lll.lK. 

I'lil.  III. 

I'M.  IK. 

1'lil.ni. 

I'M.  III. 

I'M.  IK. 

I'M.  III. 

rill.  01. 

rill.  III. 

rill.  01. 

rill.  01 

"!• 

SI* 

Kf 

(tr 

111- 

wil- 

Sir 

mi- 

Wll- 

M- 

n- 

M* 

mi- 

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m- 

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471- 

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411* 

411- 

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471- 

411- 

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V.  \.  U'.;l. 

( 

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0 

II 

0 

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0 

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T.  Jill"  ;«)'  N.,  LONIJ.  TIP  H'  W. 

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0 

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1 

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I'l.l.  i.«. 

rill.  III. 

I'Ul.i./. 

I'lil.  IK. 

I'M    IK. 

I'M.  IK. 

I'M    IK. 

I'lil,  IK. 

I'lil.  IK. 

rill.  IK. 

fill.  IK. 

rill.  III. 

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(►.•I- 

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8.'i- 

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K.'l* 

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Kll- 

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w 

nil- 

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47" 

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0 

TYIJKl'.  IIOADS,   CiA.,  TO  LAT.  iKI"  :.V  N.,  l.ONCJ,  77"  Oil'  W. 

1 

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to. 

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riii.ii/.. 

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Ill  ill  ilii-  iliijiliiii'.     A.<  iiioiiiiiiiii.'il  ill  III!'  I'ssiiy.  till'  (lii-rcUim  of  llii-  ciiii-i-ii  huh  vci-j-  iiiiicli  liilliiciu-cd  by  dircctlDii  iiiiil  foi-ce  (if  the  wliiil,  .1.  u,  1). 


