f

■M

-

*

mt-

■A*

» * ■

t#

/'C-

£

<?// L-

-/

c*~

7

/

♦

V

/

Cflentlichen Arbeit*

Vr'iiiotfr^

d©t

%

•K«-

f .4

-

,

-5

l?

•*S

f

'h

S.

* %.y

*

'

%

• V

I

Biblioteka Politechniki Krakowskiej

100000301043

3?Z^3/■

(S

Zs

£Ay3vA^;

pA

/    z*'"    ,

/?•' AA& ^■c&LfrrtA?”'<&?*'

CS Cj/

3: cZArtA fL&&z<r&4,

<* ■

cA&y <sA

/ /^    / fO

~ L? iZ&AAzsL' lAp-A-t^-

/ .--■

<z%'    e$, P,~t~ s&aS7    ,_    —

a^Z&P-Z^⁷. p02**^

p3rt3pz^<yj0/    *-#

" ts? Aptc <pz*/yze^?A3~

077- AA A^-~*>*

* ^ ' /

Af3zaAApA-₁

Jt

C&rz&z

~ Sfs£?$.

A/Z.*. ■£<? Jf.

•ss®s^

Cffentlichea Albeit*!

<r

<oa,\ K

e

TIDE TABLES

FOR

CHARLOTTETOWN, PICTOU

AND

ST. PAUL ISLAND, C.B.

FOR THE YEAR 1905-

With Tidal Differences for Northumberland strait, the sonth-western side of the Gulf of St. Lawrence, the north coast of Prince Edward island, and Cabot strait.

Issued by the Tidal and Current Survey in the Department of Marine and Fisheries of the Dominion of Canada.

(Eighth year of Issue.)

OTTAWA:

GOVERNMENT PRINTING BUREAU. 1904.

il 12149 e s-ntfri

05

V

TIDE TABLES

FOR

CHARLOTTETOWN, PICTOU

AND

ST. PAUL ISLAND, C.B.

FOR THE YEAR 1905.

With Tidal Differences for Northumberland strait, the south-western side of the Gulf of St. Lawrence, the north coast of Prince Edward island, and Cabot strait.

Issued by the Tidal and Current Survey in the Department of Marine and Fisheries of the Dominion of Canada.

(Eighth year of Issue.)

OTTAWA:

GOVERNMENT PRINTING BUREAU. 1904.

%

!>

&

3

TIDE TABLES

FOR

CHARLOTTETOWN, PICTOU AND ST. PAUL ISLAND-

•, '*•

These Tide Tables are issued by the Tidal Survey, in the Department of Marine and Fisheries of the Dominion of Canada. They are based upon direct observation of the tide, obtained by means of self-registering tide gauges, erected at eleven localities in the south-western portion of the Gulf of St. Lawrence, and in Cabot strait. It has thus been ascertained that these tides can best be deduced from St. Paul island, which is one of the principal tidal stations, commanding the main entrance by which the tides enter the Gulf from the Atlantic. For this purpose, a division is required into two regions as follows :—

I.    The open Gulf Co\st.—Including the northern part of the coast of New Brunswick, and the north coast of Prince Edward island. The tides on these coasts can be referred directly to St. Paul island, provided that the difference in time is taken as earlier, or forthe preceeding tide. Otherwise, the difference in the time of the tide varies so widely as to be practically valueless. There are few localities where the rise of the tide is more than five feet at springs and three feet at neaps.

The tides on both sides of Cabot strait, are also referred directly to St. Paul island.

II.    Northumberland Strait.—The tide after passing through Cabot strait, enters Northumberland strait at its eastern end, and proceeds westward. It attains its greatest range at Charlottetown, where it amounts to ten feet. At the western end of the strait, from Shediac to Richibucto, owing to tidal interference, the amount of rise and fall is usually very slight; and the time of the tide is correspondingly uncertain.

The tide throughout this region is characterized by a marked diurnal inequality. This feature of the tide is under the influence of the declination of the moon ; and the alternations in the time-intervals and the height are in accord with its upper and lower transits. This diurnal inequality becomes more pronounced as the tide proceeds along Northumberland strait. It has therefore been found advisable to take Pictou as a secondary port of reference in the middle of the strait itself; as the inequality in the tide in the two directions, can thus be better distributed.

Method of Calculation.—The Tide Tables for St. Paul island itself, are based upon a continuous tidal record during four complete years, obtained in 1895-96, 1898, 1899 and 1900. This record has been reduced by the latest methods of analysis; and from the tidal constants thus obtained, the tide tables are calculated in the Nautical Almanac office, London.

The Tide Tables for Pictou are computed from the St. Paul island tables, by means of two series of variable differences in the time of the tide, based upon observations in 1896, 1897 and 1901. The two series are for high water and low water respectively ; and the differences vary in accordance with the declination of the moon, and alternate with its upper and lower transits. The variation in the range of the moon’s declination in the 19-year period, is also allowed for by a modification in the series of differences used.

The Tide Tables for Charlottetown are computed from the Pictou tables, by means of the average difference in the time of high water and low water, as found from simultaneous observations at the two places in the summer seasons of 1896, 1901 and 1903.

Tidal Differences.—The differences given in the following table, enable the time of the tide to be known in these regions, so far as reliable information is available. In addition to Pictou and Charlottetown, observations with self-registering tide gauges have now been secured at Lower Neguac, Alberton, St. Peters, Neil harbour, Sydney, Port aux Basques, Souris, Cape Tormentine and Summer-side. These have afforded simultaneous comparisons with St. Paul island and Pictou. The differences given for the remaining places, which lie between these, are obtained from careful comparison with the Establishments in the Admiralty list.

WITH PICTOU TIDE TABLES.

For Northumberland Strait.

WITH ST. PAUL ISLAND TIDE TABLES.

For the South-western side of the Gulf of St. Lawrence, the north coast of P.E. I. and Cabot Strait.

For the time of H. W. in Atlantic Standard time, apply the following ditlerences to the time given in the St. Paul island Tide Tables

For the time of the tide in Atlantic Standard time, apply the following differences to the time given in the Pictou Tide Tables :—

Locality.

For II. W.

Locality.

For H. W.

For L. W.

H. M.

H. M.

H. M.

Lower Neguac, and the entrance to Mira-michi bay.................................

Alberton, P.E.I............................

Richmond bay; within the entrance.......

Grand Rustico ; at the Lighthouse........

St. Peters ; at the entrance to the bay......

Neil harbour, C.B........................

Sydney.....................................

Port aux Basques, Newfoundland..........

Subt. 3 21 “    2    33

“ 2 2G “ 2 31 “ 2 10 “    0    19

“    0    25

Add. 0 17

Note.—The south-east coast of Cape Breton-island, and the eastern angle of Newfoundland, are referred to Halifax. (See Halifax Tide Tables.)

Souris...........

Port Hood........

Cape Bear.......

Cape George.....

Pictou............

Tatamagouche ..

Pugwash .........

Charlottetown ... Cape Tormentine

Bay Yerte .......

Summerside.....

Subt. 1 17 “ 1 02 “ 0 57 “    0    45

“ 0 00

Subt. 1 15

“ 0 00

Add 0 04 ...........

“ 0 36 ...........

“ 0 38 Add 0 50 “    0 23

“ 0 27 “    0 50 Add 1 15

“ 0 43

Ocrrent in Northumberland Strait.—It has now been ascertained that the current in this strait like the tide itself, is primarily governed by the declination of the moon. From observations taken on the north side of Pictou island, it appears that the difference in time between the turn of the current in the strait, and High and Low Water at Pictou is not constant; but that the difference may vary from its average amount by nearly two hours, earlier or later. This variation alternates with the upper and lower transits of the moon, at times when the moon’s declination has a high value, north or south of the equator. Further, as this variation recurs in the period of the nodal or declination month, which is over-run by the synodic month in which the moon’s phases recur, it is sometimes the spring tides which are affected, and sometimes the neap tides. It is for these reasons that the turn of the current in the strait has the appearance of so great irregularity, which is usually attributed to the wind. The observations secured are not yet sufficiently extended, however, to enable rules to be given with precision; but the laws governing the current are more fully explained in the Tidal Survey reports.

Wm. P. Anderson

Chief Engineer.

W. Bell Dawson,

Engineer in Charge of Tidal Survey.

MAY.

Da te.

Day.

High Water.

Low Water.

Morning

After’n

Morning

After n

Moon.

Date.

Sa.

hXSC FH rH Ot

wtstatstctststotste

O®09^Oi&<^QStSM

* 3^ g p ^ a**® ? 3 ^ g    ?! 3 3

■ • • * • • • • * • • • • * • • • •

Sa.

H. M.

9 01 9 45 10 23

10    54

11    24 11 53

0 24 1 0L

H. M.

23    13 23 49

12 23

H. M.

9    37 10 49

H.

15

15

16

16

17

17

18

19

19

20

21

22

23

12 07

0 54

8    10 9 00 9 59

11 09

1    03

2    01

12

13

14

15

16

16

17

18

19

19

20

21

22

23

12

13

14

©©GC-^SbCT^WtSI-¹

M V4 M M M

Sii 4- 09 to M

wwtotototctototstotatSMMM

H©®X<t©CA4i>WtOM©©X*^

Day.

High Water.

Low Water.

Morning

After’n

Morning After’n

Moon.

MM    M-¹ M S-¹    ffl

OOOGOSSO^WWWHCOHCOOO).

H. M.

22    26 23 15

POtO*'‘©PosOGO-'JOiCSO'tOIrf^^OStO.*¹'

H. M.

15 11

21    59 23 09

OHHN

JUNE.

JULY.

Tli.

W M M W tv M

*S M M M

ooocm

ti

tv tv tv

«-ui;

is ® x a © Ot 9* M 01 0* M

So®»QO<)®OI|f».C>5biPHOHOO®^

bo bo bo a co oo bw •

4^0b02 oc go .

23    07 23 54

iH(MM'!#eS®t'i»C5©-H5IeO’te5CO pH pH pH pH pH pH

QO'INaOIit'OSWMMHO

20    16 21 18 22 11

0 55

1    56

2    49

OOtOM'ICSOli^ieMtiHOOOO®?’

H. M.

22    52

23    31

toaxi'ioiatiiWMRitih'OO

EoOffltCCDKiKiootOl^MbiHO

0 57 2 06 3 06 3 54

g2S££^S5S8feSS2^S85S8££S££££8SiS8£P*

AUGUST.

Date.

Day.

High

Low

Morning

After’n Morning

After’n

©tXM©S'*-WWM

M.

24

09

H. M.

23 51

M M

00 -J

UUliKIGliKiGliMHXw

0 29 1 08

6    57 8 02 9 00 9 50

10    38

11    24 0 25 0 57 1 24

9    23 10 16 11 08

23    17 23 52

12 08

0 14

H. M.

17 14

Kp I Moon.

| Date.

Day.

High Water.

Low Water.

M M M M M M M

s ti » M i; « c “ x -l S f «• M (V -

M M

GO -I

o«ce*ieeu^ci9EiMoe

Morning

H: m. 0 02 0 39 1 17

11    14 11 56

0 20 0 49 1 14

11    07 11 53

After n Morning

After n

Moon.

H. M.

15    24 1G 34 17 54 •19 17

20    23

21    20 22 09

22    47

23    21 23 51

22    16 23 56 23 35

0 51

H. M.

18 14

17    13 17 55

OCTOBER.

NOVEMBER.

eac*s9?*"M(« m

M M M

OStCH

M M I—

© OT £•

iy (JO G O

|H i-i pH 01

CGCQt3t3i£*SK>K>iCK>tO

jjOOHNIMW^tDNKaOHH 'OOOrtHNWIOtONWOOH

0 12

h'OtDOO'IffllC!r

0 52

OOiOtOHWg h-i M tO GO F

18    18 18 59

)OHMM

0®8S*I

COK>*S*S*S*S*9*Si«*S C ; * -1 5 1' - « N. -

0 25 0 54

0 25

H. M.

23    11 23 47 13 10 13 52

H. M.

h. m. i

21    56 | <$ 23 09

12 57 f 14 01 |

14    55 -

15    45 I

32 ©

16

JANUARY.

FEBRUARY.

Date.

Day.

High Water.

Low Water.

Morning! After’n

Morning

After’n

Moon.

Date.

Day.

'High Water.

Low Water.

Morning

After n

Morning

After n

Moon.

5S0C*1®5<5-5O15m

h. M.

H. H.

“    y_

03 5> 5. 53 «5 — ©

M M GC -l

G0C015151515151515t51515M M©©GCM03 5ai^S015M©©

0 31 1 18 2 07

0 36

4    57 6 16 7 31

11    46 0 37

H. M.

12 59

®GC*3©S!T#i*SQ15M

H, M.

8    37

9    25 10 09

10    49

11    25 11 58

0)

H-¹ I—¹ O

0 36

H. M.

16    16 17 21

^T-HC<ico-<tiTfiioinsot~t^coaoo5©

1 11 2 09

H. M. 14 01

0)

MARCH.

APRIL.

1S15151S1515151515MMM

50 W 15 M C SO

~ia2O!#.03tCh-‘®!^HJ©CD‘®GC~l©5O!C0t>St3M©©!— MOOCDJOCO^l®

tl* Ox 03 M‘OOMbiCHWOIH‘t003 03l-‘0>m®l-‘hfx®©fc50*t5>tx©MI--lB F-‘fc5©4xU!C30xC3t5rfxatOl&3 00 00©©G0O!tfx®©,(x©C0Cn0x<aa333HX.r'

H. M.

12 18

16    43 18 00 19 11

H. M.

0 13 1 26 2 21 3 09

H. M.

21    55 21 58

23 22

23    39 23 54 13 19

®GC*l035a£.S0i5M

M M M M M M M

05 t- CO IS M ©

15 M M M © © 00-1

50151515151515151515

OS0CC<$055i>5>S015H

Sa.

'■

n.

Tu.

\V.

TJ».

F.

Sa.

M.

Tu.

W.

Til.

F.

Sa.

M.

Til.

W.

Tli.

F.

Sa.

M.

Tu.

W.

Til.

F.

Sa.

^©©©OO-l^IOi^OJtOh-'Oot^MOOOCDQO?'

H. M. 20 11 21 03

21    49

22    30

23    06 23 41

WtOh^l—‘OOO-^Oi^COCOfcOtO OCOOiHCUOWGOCNCOC'.OO

H. M. 14 10

SC'.OJ^WbJHH©

12 00

21    49 23 03

12    47

13    39

MAY.

JUNE.

Date.

Day.

High

Low Water.

!Morning

After’n ) Morning

After’n

Moon.

Date.

Day.

High Water. Low 1 Morning j After’n Morning

After’n

Moon.

M M M i*5 M ©

©©©•^©CX^CO

^•©©COMffiSJx^W^M

oo-<j©©ot4^WMi-‘©©®®®aooo-q©at^o:toi-‘©®®®®

® CO 00

H. M.

11 24

H. M.

9    43 10 58

0 41

9    38 10 53

M t* M M M M

r. i. — ii <c — c © x ..» © i' ~ ii ii —

H. M.

8    48

9    20 9 51

10 24 10 59 0 29

9    05 9 45

H. M.

21    44

22    25

23    05 23 46

24

0 18 1 09 1 55

Q3K>tSK>K>*£iOiOK>»«K>M

©«tim®;i#.wisHS8

03

38

23    11 23 55

20

01

26

10

56

24

07

H. M.

9    58 11 04

0 05 1 06 1 59

H. M. 15 04

14    00 14 42

is5s^

JULY.

AUGUST.

^ 00 05 O

WWt0*SK>***SKIi®te*e»0

HO®»^©Sl||iWHH©

®®®co-a'<i®®>£-'Wt£>rJ®®©

ge?2gg£85&ISJg!SSS:££&§S82885Si!i2SgS88g8£?!

H. M.

22 09

22    48

23    27

gSKISSSgSSSgSS

O GO -<! Ci OT 4^- 4^ 00 fcS • '

MOOiOiOHtC^ObO^S

cot—

•OiOn PC H H

GOOO-^CJOtil^pJC/JtObS!-¹©®

0 47

0 07 1 16 2 16 3 04

Til.

©®GO^CSO'tf.OJI..Sti>t-¹l-‘©®t7‘®®<®00-<IC30t>£-OitOI-‘(-¹©

OtW®®Ol®l^-U)OChJOO^I®4iC!II-*OT^^I^O!VSOT®CO®®01i4^®l—

H. II.

23 08 23 46

12 06

23    09 23 42

12 08

II. M.

H. M.

21    54 23 07

0 45

16    03 16 44

Tidal Differences for Northumberland strait are given on page 4.

Date.

Day.

High Water.

Morning

After’n

Low Water.

Morning j After’n

Moon.

Date.

Day.

High Water.

Low Water.

Morning After’n Morning After’n

Moon.

©00-^©5)!|^WiCM

HOOOO^IOsOlWMMHHOOMHOOaiCONOlrfkOSMtOMO' M®

H. M. 23 56 12 06

23    08 23 37

12 28 13 06

H. M.

9    04 10 16 11 37

0 01

9    34 10 48

H. M.

0 29

12 57 14 01

0)

jH

M©oGCM©0!^wiCH-o®oc-?e5»!if!.

II. M.

11 57 0 09 0 46

0 21 0 50

8    26 9 22

10 12 11 01 11 49

O tH O

rH r-i

1-^5000-5 05050!®

1 06 2 02

5    01 5 45

NOVEMBER.

DECEMBER.

SooScoSo^coShScoo^Im

JOOH1MCC10«CNX0050HH(M 5    HHHH

0 22 1 04 1 59

H. M.

22    28 23 04 23 42 13 14

H. M.

11    44 0 15 1 16 2 02

9    41 10 53

H. M.

21    46 23 01

0 40

M M M M 1-1 M M

#W#.63»MC

HHM

© oo

fj)

W W tv tw to tv iC i* i-i I* t& iw M © ©CCM©O!^03i«M©

H. M.

0 25

11    28 12 09

0 01 0 50 1 49

6    56 8 06 9 08

10 01

0 14 1 04

H. M. 14 02

H. M.

7 07

H. M.

22    20 23 32

18    20 19 03 19 49

FEBRUARY.

Date.

M M M 5C GC <1

w w ic    k <i to ic ii

MO«GCMOSOx#.MtOMC

• • • ••• • • • • • •••

High

Morning

H. M.

0 36

0 04

H. M.

11    14 11 46

0 30 1 21 2 24 3' 42

8    21 9 01 9 40

10 18

Low Water.

After’n Morning After’n

H. M.

H. M. 11 06

0 44

H. M.

23 45 12 08 13 03

20    06 21 08 22 18 23 27

12 18

Moon.

Date.

Day.

High Water.

Low

Morning

After’n

Morning

After’n

Moon.

H. M.

7 03

0 12 0 56

0 48 1 50

3    05

4    25

H. M.

14    50 16 00

H. M.

0 23 1 18 2 07

8    45 10 00

W^^CfWG0C0O4*-Oa5OO4^tOP

MARCH.

APRIL.

H. M.

23    06 23 45

12 20

H. M.

11 14 0 07 1 02

8    58 10 20 11 39

0 21

9    32 10 50

H. M.

12 18 13 13

19    48 21 00 22 20 23 25 12 00

10

li

12

13

14

15

16

20

21

22

23

24

25

26

28

29

30

• • • • • • ••• ••••• •

H. M.

11    10 0 21 1 18 2 20

H. M.

H. M.

0 40 1 23

8    40 10 02 11 14

0 55

7    50 9 00

10 20 11 28

H. M.

23    55 12 20

. 13 15 14 00

23    52 12 20

MAY.

Date.

Day.

High

Morning

After’n

Low Water.

After n

Moon.

Date.

Day.

High Water.

Low Water.

Morning

After’n

Morning After’n

Moon.

M M GO -4

OJOiOl^WWHOOOOCO! GO-1 OOl^05WMOrJOO^>OlGO<J<Ja5?’

H. M.

19 13

23    10 23 58

12 08

OHOH(N(MCC^^lO^NCOaiOH • ® HH    rH rH •

H. M.

13 02

©x<4aeo(>u)«M

M M M M M M M

© tii rf- W tv V- ©

M M M

© at> *4

WtStStStiWtOtOtStStO

©©GCv|©Snrf.WtSM©

H. M. 7 14

11    08 0 28 1 21 2 18

9    07 9 48

10 30 11 14 0 27 1 09

H. M. 20 10

22    21 23 04 23 46

12 00

18    10 19 06 19 54

t‘o:oooc5Si®<ie-ooo3U>i-‘i-**

WMMOOlOKU^OMOIHg

MOOI^tDMOOlOIOOlOOlS"

0 53

0 40

0)

JULY.

AUGUST.

M M h- H M M M

#W^M(4MOO»»lffiS'it‘Mt4N

8a.

» N> W W i*

U5 © X © © pH

HCJCiOl^WWHHOHOOOOOCOSOJOl^WtiHOOOOOaJCON?

H. M.

23    15 23 50

H. M.

9    54 11 04

©Qe<»©S^4*W*aM

tObLHHHMMMMM OOOCONCJOD^ WW

O’HW^OiWOOOtO

Ol^OOOJWWOOCW

0 32 1 28

0 57 1 45

M M M M M M M

ao<^w($He

WC0*9i0K>*SK>K>K>*S*S

M©©ae«4®Cnrf-Wt«>-*

C©5Oa0~3-qaiOlWti>l-‘l-‘©

SSBSSgS&SSi^KgSSigggggSSSSSgSgSggg.*

H. M.

OHH rH rH rH

GOODSOSOiH-WWMOO

12 28

23    12 23 43

bOtOMMHMHMPHM HHO^OCOSOl^ WW

WWW

rffcssasssassssggssggssssssss

OHOHHINOOCO^iOlOCNNXOH rH rH    rH rH

H. M.

15 05

21    48 23 05

0 36

1    25

2    09 2 52

MHMI—‘MtOWbOMMMMMHMMHHMH Wtd WtOOOOGOODNOiOOiOi^ WtC

Date.

Day.

High Water.

Low Water.

Morning After’n Morning After’n

Moon.

Date.

Day.

High Water.

Morning After’n

Low

Morning

After’n

Moon.

F.

8a.

H. M.

9 45

10    32

11    22

1TI.

Tn.

W.

Til.

F.

8a.

M.

Tu.

YV.

Til.

tOiOtOMMMMM

«M©»»^SStn

F.

8a.

M.

Tu.

YV.

Tli.

0 26 1 16

8    26 9 05 9 42

10 18

10    54

11    32

© <v (0 (0 K Iv (C fi © ® X -I © O' iC

F.

8a.

OT.

Tu.

YV.

Tli.

F.

8a.

tOOOGONCIOTMMPOO

MOlOHHMOlMWifcO

C10ff.WCiCOCltOCW05

gSggSSSSgEgg'SSgggggggggtiPfeSStiSgKF:

H. M.

8    57 10 18 11 38

H. M.

10    23

11    12 12 05

WWHMOHOCDOO^lOSOlOlrfi'-^WWtOMO

15    04 15 46

M -• M M M M M

atniHWKIHS

tw M M M © © X -1

M©®X-l©0'^WiOM

S:OONCfl'^¹o®GcceoH

CCC0Q0--lC50l^b0MO

e«8gifc85&88S&Sfcg8!gS8S8g;£g?s:£&Sgsgs;gK

H. M. 4 01

9    50 11 07

OHH(MfCW^^nCCCSCCOH

rH r-i

0 43

g88S8Sg585ggSSg!gg8g!jgg;g,gSg5gfefeS85*

NOVEMBER.

DECEMBER.

H. M.

11 55

— M — M — M —

# S' it* MiSM O

t- 00 © O 91

rtrtrt«««

W $S *S K> M tS tO M © © X *1 ffi O' #. W

HOOfflOOSOSOlifiMM®’ 5 t* ® ®

® QO CC —1 ® ® Ot cc to ►—¹ ®

S8feg^8SS£J2gSS£g5gS£8B88 88825888 «

H. M.

CH^05tatiM-‘®M®®00-q050li^.>^.Cl5C>5fcS

8Eg82SS8£S:S£8g?;2S£;Sggg&

£££££££: g8E2££i$tS£S;&;££:££58BSgS£iSP £82883^; 2S85fegS88!Sg£88g88fe5i5gSf«

H. M. 12 28

£8gS2gg£££;SKE£S8l8g>2gg^S££J55SESg?]

8fc5Sg5g5;8§SgS%fcg%gsggfeS£jgg£3gggsagB

CJOt^^WMMOOMO®135 0SOIif.^Mt5M

£888852&88££8S!8g£Sg28&SS2gggS2g<2gg8*

KOOCONnO!®

OOH

H. M.

18 05

(MCCCO^^lOCCNCOCOHN

HHHHrinHHHHHtNJLM

3)

ft

»

%

\,v>:    '

..

Biblioteka Politechniki Krakowskiej

Biblioteka Politechniki Krakowskiej

7YDZIALY

11-353587

BIBLI

100000317766

I

Biblioteka Politechniki Krakowskiej

Biblioteka Politechniki Krakowskiej

ll

L. inw..

MI-18440

Biblioteka Politechniki Krakowskiej

ru, Czapskicl

11-353586

'00000317767

10G00G3G1G43

Biblioteka Politechniki Krakowskiej

Biblioteka Politechniki Krakowskiej

II-353585 100000317768

t.

BiOlioteka Politechniki Krakowskiej

Biblioteka Politechniki Krakowskiej

II-353584 100000317769

Biblioteka Politechniki Krakowskiej

Biblioteka Politechniki Krakowskiej

Ufa

11-353583

Biblioteka Politechniki Krakowskiej

Biblioteka Politechniki Krakowskiej

11-353582 100000317771

Biblioteka Politechniki Krakowskiej

Biblioteka Politechniki Krakowskiej

11-353581 100000317772