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PUBLISHED BY THE NETHERLANDS MARITIME INSTITUTE
ROUND THE HORN
OR THROUGHMAGELL4N,
An Extreme Case of Voyage Planning
Report Number R 109
17 MEl 1979
PiOject Number: SNAV 089
This report was prepared by:
C. Glansdorp, M..Sc.,P.Ri.N.
G H Goldsteen, B.Sc.
P. A. Kluytenaar
-.
ROUND THE HORN
OR THROUGH MAGELLAN
An Extreme Case of VOyage Planning
TABLE OF CONTENTS
Page
ABSTRACT i
INTRODUCTION . . ... . . .. iii
CONCLUSIONS AND RECOMMENDATIONS v
VOYAGE PLANNING . . . . f
...
I I 1 Terms of Reference - . - 1 .1.2 GeneraiPhilosophy ... . . ..... .
....
. . 3VOYAGE ENVIRONNT .
8 2.1General ...
. . . .. ....
8 2.2 I1éteorological Data a 8 2.3 Oceanographic Data . a . . .. .. . . . a 9 2.4 Geographic Data...
....
1!POSITION FIXING IN MAGELLAN STRAIT 15
SPECIFIC VESSEL CHARACTERISTICS 16
4.1 Theoretically Required Pathwi4th 16
4.2 Determination of Distance to New Course. . .
.. . 16
5 COMPARISON OF ROUTE ALTERNATIVES 19
6.. TIME SCHEDULES OF THEPASSAGE THROUGH MAGELLAN STRAIT 22
THE AREAS OF CONSTRAINT AND THEIR NAVIGATION
MANPOWER REQUIREMENTS
EPILOGUE .
. . 23
24
TABLE OF bNTETS (contiiued)
APPENDICES
1. VOYAGE PLANNING
1.1 Description of the Route through Magellan Strait 1.2 Influence of Tide on Available Pathwidth
1.3 Descriptio of the ROute round Cape Horn
2 VOYAGE ENVIRONMENT
2.2 Meteorological Data
2.3 Oceanographic Data
2.4 Geographic Data
POSITION 'IXING IN MAGELLAN STRArr 3.1 Methods Employed
3.2 Accuacies at Specific Position 1n Magellan Strait
SPECIFIC VESSEL CHARACTERISTICS
4.1 theoetically Required Pathwidth.
4.2 Determination of Distance to New Course
CONPARISON OF ROUTE ALTERNATIVES
5.1 -The Inside Route Voyage Duration
5.2 Diffrence in Route Lengths
5.3 TimeLoss Rounding Cape. Horn
5.4 Conclusions
TIE SCIED1JLES OF THE PASSAGE THROUGH MAGELLAN STRAIT
THE AREAS OF CONSTRAINT ANI) THEIR NAVIGATION
7. 1 The Passage through Pri-mera Angostura and past Bano Trit6n
7..2 The assage from abreast o Pta. Pasaj.a to Isia Beware
7.3 Rquirements of Ship-basedPlanning
7 4 Worked Example of the Passage of Bajo Satflite and the 10 Fathom Patch
MANPOWER REQUIREMENTS WHEN PASSING THROUGH MAGELLAN. STRAIT LIST OF REFERENCES
1.1 1.2 1.3 1.4 1.5 2.1 2.2 2.3 2.5 2.6 3.1 4.1 4.2 4.3 4.4 4o5 4 ..6 4.7 4.8 4.9 4.10
TABLE OF CONTENTS (continued)
EXHIBITS
Block Diagram of Voyage Planning
Required Skill versus Time during a Voyage Pilot chart of the North Atlantic (Area ).
Pilot Chart of the South Atlantic (Area 50)
Variations in the Voyage Duration Base4 on a Ship Speed
of 15 Knots
Track of ss TULA at the Entrance .df EstrechO de Magillanes
Position of Grounding of ss METtJLA Daily Predictions fOr Puerto MOfltt
Daily Predictions for Bãha Santiago and Baha Felipe
Projected 'id'El CUrVe of 10 FthOm Patth, Januay 19th, 1975 Projected Tidal CurVe of 10 Fathom Patch, Jaivary 1st, 1975 Available Pathwidth and Depth along Magellan Strait
Extreme Limits of Icebergs
Mean Northerly limit of Icébetgs
Ship Draughts and Survey Danger Line Climatic Table - Grupo EvangelIstas Climatic Table .- Pta. Arenas
Climatic Table - Pta. Dungeness Parallel Index 'tedhnique
Increase of Required Pathwidth. Due to Crosswind/Current Ratio Available Pathwidth/Theoretically Requfred Pathwidthl Current Côntant: Drift Angle
Track during a Course Change Manoeuvre Distance tO New Course
Headitig- versus Time during aCourse Change Manoeuvre
Rudder Angle versus Time during a Course Change Manoeuvre
Schematized RUdder Angle foi
Calculation--Rate of Turn versus Time during a Course Change ;noeuvre:
Deviation of-f
TABLE OF CONTENTS (cOntinued)
4.11 Course Deviation at Cheek Time
4.12 Distance to New Course
4.13 Total Time for Completion of Course Change
4.14 Time at which Swing should be Checked
15 Course DeviatiOn at Check Time
4.16 Distance to NE COurse
4.17 Total Time for Completion of Course Change
4.18 Of f-Track Deviation
4.19 Results of Zigzag Tests.- ss METULA
4.20 Results of Zigzag Tests - ss NETULA
4.2.1 Results: of Spiral ests - ss T1.A
5.1 Average:Wind Distribution for Area 2 and Area.50
5.2 Time Los for. Different Wave Height
5.3 Relation between Median Wave. Period and Significant
Wave Height - Area' 2 and Area 50 5.4 Speed Loss versus Wave Height
5.5 Time Loss Distribution
5.6 Direction, Constariy and Ayerage Speed of Predominant
Current in Winter (July.). . . .
5.7 Pilot. Chart of the NorthAtlantic (Area. 2)'.- Decémbér
5.8 Pilot Chart of the NOrth Atlantic (Area. 2).- January
5.9 Pilot Chart of the North Atlantic: (Afea 2) .ebruary
10 . Pilot. Chart. of the South .Atl'ritjc (Area '50.) Winter.
5.11 "PilOt. Chart: of the. South Atlantic (Area 50) -' Spring'
5. 12 Pilot Chart of the South Atlant.i "(Area '50)
Sier
5.13. Pilot Chart of the, Sout1 Atlantic: (Area 50) Autumn'
1 Tidal Stréa. Rates accordirg to..BA and Chilean Cha.rt
6.2 Tidal S,reäm.Rate's according .to the Pilot
6.3 Tidal InforiatiOtz .'acco'ding to .ChiI'ear. Tide Tables, 1975
6.4': Daily Prediction.s, Standard Pors ' .
6.5 Daily Predictions, Secondary Ports .. .. ."
6.7 Times of Sunset, Sunrise and Civil Twilight during 1974
6.8 Sche4ule of Passage during Spring-Tides, Januaty 1, 1975
6.9 Schedule of Passage during Neap-Tides, Jafluary 19,. 1975
7. 1 Worked Example of Passage of Bajo Satlite and 10 Fathom Patch
7.2 Worked Example of Passage through Paso Tortuos.o
8.1 Examples Of Duty Division
Area Map
This report discusses the planning of a voyage by a VLCC through
relatively unknown waters. It points out the navigation and
manoeuvring requirements in as far as they differ from routine practice or are considered to be unfamiliar to the average navigator and owner's fleet management department.
A detailed comparison is made of the route through Magellan Strait (Estrecho de Magallanes) and the alternative route
round Cape Horn (Cabo de Hornos). Upon completion of the desk
planning for these two voyages, it became clear that the nature of the route through Magellan Strait requires that the voyage be planned in the greatest detail, both by the owner's fleet management and the master of the ship, to ensure a safe passage. To be certain whether or not a passage is "safe" one needs to have on board an elaboration of the manoeuvring characteristics, obtained from sea trials, which can be used in predicting the
ship's track during course changes. Unfortunately this
inform-ation is usually not available on board. Also in some sections
of the Strait the accuracy with which a ship can be positioned might be insufficient to ensure that it is within its channel. At present only visual bearings and radar observations can be
used.
There are not enough navigation aids to assist the helmsman in
steering (accurately).
A large number of radar beacons (RACONS) should be installed. Charts are either unreliable or not sufficiently detailed.
From the meteorological point of view the route round Cape Horn
is not as bad as is generally believed. There is, however, not
conditions during the year and hence the. associated wave heights, direction and period.
This route certainly seems to be a feasible alternative to the Strait passage, which in the case Of such a large ship demands
from its officers constant ãt:téntion and precision over a
prolonged period of time. Besides this, they are: continuously
eposed to nterous submerged hazards, both charted and uncharted, tidal currents of up to 8 knots, the dangers of little searoom and general uncertainty about ay details.
This report was Tprimarily intended as an examp] of the extremely
detailed voyage planning which should be dOne by the owner's fleet.management and not as a source of ififOratiôn onthe
Cape Horn and Magell4n Strait area.
However, the information given and the recOendations made in this report have become more important now that independent
tanker owners have proposed sending tankers, coming from Val4ez,
Alaska and carrying crude oil to the eastern regions of the USA, roimd.Cape Horn or through Magellan Strait instead of through
INTRODUCTION
This report was commissioned by the Directorate of Shipping to
the Netherlands Maritime Institute a a. follow-up tO the results
of the investigation by thE Admiralty Court of the Netherlands
(Raad voor de Scheepvaart) in connection with the grounding of
the VLCC TULA on 9 August, 1974 and the subsequent analysis of this grounding by Captain A. Wepster, Head of the Navigation
Research Centre, NMI. An abstract of the. relevant facts of the
voyage is contained in the Epilogue, page 25.
This report is concerned with the dek planning of a voyage of a VLCC through an area which is relatively unknown, to see what is
involved in such planning on the part of both the ship owner's fleet management and the master of the ship., although most
emphasis has been laid on the planning required from the fleet
management. It also specifies what information is necessary
and whether or not this information is available on board.
This type of planning is normally performed in a rather general manner but sldom or never in as much detail as is shown in
this report. It was felt that the TULA case provided a
perfect example of poor ship-
an4
shore-base4 planningcon-tributing significantly to the grounding. Tb appreciate the
circumstances which created the need for this report it is recomeflded that the above investigation and analysis be
re-viewed by the reader.
Each chapter of the present report suarizes a particular
area of the planning as indicated by its title. The similarly
named appendices show the planning down to the smallest detail including information derived from the South American Pilot1, charts and other information sources as required for the
plan-- iv
fling of each subject area. For example, more detailed
inform-ation on Chapter 2, section :2.2 is contained in Appendix 2,
section 2.2. Reference numbers used in the text correspond
CONCLUSIONS.. 'AND RE.CONDATIONS
QMuch has been written about vyage planning..' .The available
literature covers almost it:s'entire -range in so far 'as.the
voyages are of. a routine nàture No single. publication
however, covers' the entire 'range of !'routineh' 'voyage planning
but only a specific part Of it. Therefore it is our opinion
that a. guide is:'needed -which .cofers all -aspects of voyage planning, fro the general. directives 'which" should. be, fol:
-lowed to the very Ipecial techniques (of- which some arC
-mentioned in this, report) to -e used.. ,
In this .report', a description is given of planning Of a very
particular.nature, namelythe passage of. a very largevessel.
on a difficult 'and rarely used' shipping route.
It is' hoped that after reading this report it wi-il be clear
that such a case goesbeyond normal planning, procedures'.' It
cannot be assumed. beforehand that the passage can be afely
made. Much of the necessary information is not readily
available. In fact even after our (detailed) piannin; was
completed it still appeared impossible to get more than a,
general notion about whether or not the risks for either
passage are acceptable. To quantify the risk factor mOre
data as well as further development
of the methodology in-
-volved, in the planning are needed.
To improve this "risk notion" one could look for other areas on the globe with comparable conditions, but for which more
vi
It appeared necessary to develop new thethOds to reduce the.
risks as much as posSible in case the route through Magellan
Strait is chosan. Otie of those methods was the way in. which
the "distance to new course" is determined. Whn there is little searoom available, it is important that elaborations of the ship's manoeuvring characteristics are available on board to assist the master in determining the distance to new
coUrse.. Until now this information was not available..
It also appeared that the normal complement of navigation officers is insufficient for a safe passage through Magellan
Strait. Th:is reinforces the need fot flexibility in the
number of (navigation) officers dependiflg on the' roite.
As will be c'lear from this report, even for the planning of a
normal passage a great many publications are needed to obtain
the necessary information. Planning would be much easier and
there would be less risk of omitting valuable details if the
information were condensed into one publication., per specific
area. This publication should cona,jn.such details as:
- chart information
- winds and currents
- outer dangers
coastal features '
navigational marks (includitig ight towers, buoys, Special
characteiS tics) anchorages
tidal information
radio beacons, radio stations (coastal, port and pilot) wit-h
- v
- major ports: directions, iandarks, navaids, depths,
limitations, restrictions, p.iOtage facilities, regulations.
The information should be well indexed and easily accessible so as to avoid lengthy study to get a particular item
This has been introduced in the revised Sailing Directions of
the USA, Much of' the above-mentioned information, such as:
- radiO beacons, radio stations (frequencies and broadcasting times)
- port entry procedures, quarantine pOcedures, area procedures
routing schemes
- search and rescue information
- checklists fOr passage planning
- distance tãblès
could be presented in a chart, thus further facilitating passage
planning and execution.
Publication of such charts has just been started by J.D, Potter Ltd.,
® Finally, we hope to have been succeSsful in pointing out the need for a careful approach in which nothing is left to chance
and all possible resources are utilised when planning passages
VOYAGE PLANNING
1.1 Terms Of Referetice
The analysis of the. unfortunate grounding of the VLCC METULA on Bajo Satlite near the t4e5teth. exit of the First Narrows
has undoubtedly shown that in the area of planning,
improve-ment is, to say the. least, desirable. The work here presented
ende ours to show what voyage planning means in a case where
both technological and hurn capacities in navigation are
stretched t. their limit. One thing is quite obvious, i.e.:
When aaftty margins decrease, care
- should increase.
This rule. applies to all-, concerned, both decision makers ashore as well as the staff on board.A somewhat unique aspec.t of this particular case is constituted by. the fact that although Magellan $trait is not strictly
with-in pilotage seaters, pilots can be Qbawith-ined an4 with-in the case of the TUIA. were. actually used.
The question then aise of
how much responsibility tests with oners and masters for
proper' planning for transits-undet pilotage. The answer t
this question cannot be simple and unambiguous, unless
sticks to a purely legalistic viewpoint. - The..master, being
ultimately responsible, will consequently be responsible for
the entire planning from departure berth to arrival berth, including pilotage waters.
However, it must be borne in mind that circumstances can and do differ, depending on the vessel size, the area to be
navi-gated, familiarity with. the area, etc. The nature of the
managerial circstances must also be taken to: consideration when comparing practical possibilities versus legal obligations
on the One hand and generally established practice on the other.
The case in hand, the planning of a passage of a loaded VLCC
through Magellan Strait, is a very special one. The specific
circumstances are:
a) a rarely frequented, difficult fairway in a climatologically
uhfavouràbie area
a very large vessel with difficult handling characteristics
pilots with no previous ecperience o
the hdling
characteristics of such vessels
a flexible fleet allOcatiOn system whereby vessels and.
their árews can be é-rOutCd at very short notice.
It is our belief that tmder the above-mentioned operational
conditions, full .repOh5ibilitfotvOyáe planning rests with
the nagementwhO, f Or êcoiOmicreaOn want tO undertake the
assage. Only thanagethent is in pOition to' obtain all the
relévantdàtãànd, oh the basis of théè data, tO assess
"risk
rus ecOnofrdc benfit
If this asSessment leadS to-the Onc1usion that the 'passage is
feasible, thésters of th
vssèls "ordered" to eeóute theoperation should:
be briefed very carefully
-be instructed to supply feedback information based on
practical experience in the area concerned. This feedback
information should be carefully analysed and where necessary
be used to improve and update the planning or, at the other
-. 3'
The full responsibility for planning a voyage of 'a loaded VL through Magellan Strait rests with the owners, suppárted by their masters, because of the extraordinary conditions
encount-eredon such a passage. The Netherlands Maritime institute
carried out a voyage planning exercise based on the above
conclusion. The. result of this.exercise is cOntained in this
report.
I±i order 'to be able to evaluate the TULA case against the
required planning activity, the data used are those which were available prior 'to the time when it was decided to negotiate
Magellan Strait with VLCCs. We hope that this planning ecample
of a very unique and difficult passage will be a valuable con-tribution which will assist future voyage planners in their Wor[(.
1 .2 General Phi losophy
Before going into any specific detail it will be advantageous
to first define what is meant by voyage 'planning. Examples of
it can be found in:
- Aditiralty Manual
of
Navigation9, Chap.ter V, pages 121-155- Dutton's Navigation and Piiotihg28, 13th editidn, Chapters
11 and 12
18)
- Shell s Guidelines to Navigation
- The Use of Radar 'at Sea24, Chapter 8 pages 112-129
- "Guide to the Planning and Conduct Of
Passagès"2',
'Mex XII
Exhibit 1 gives a general outi]ne of how to approach the rather
complex process of voyage platining.
Exhibit I : Block Diagram. pf. Voyage Plannjng.
REQUIREMENTS F
-4-VOYAGE PLANNING VOYAGE ENVIRONMENT BEHAVIOURAL CHARACTERISTICS NAVIGATION & SAFETY EQUIPMENT METHODS AND WORKLOAD SHIP Feedback ReportingH
E)CUTION QUALITY QUANTITY E)ERIENCE CREW*In this context, referring to the population as seen from the ship, i.e. including both surrounding traffic and coastal populations.
This block diagram indicates that there are 10 major areas of
consideration. Four ãteás. deal with -the- particuiars of the
vOyage and three deal
with
the technical. particulars of thevessel intended for the voyage. Analysis of these seven areas
will first of all have to be provide an answer tp. the question:
"Is the plannd voyage possible: Xes or
METEOROLOGICAL
OENOGRAPHIC
GEOGRAPHICAL
-5=
If the answer is No, a more suitable sh ip will. have to ..be fod or the rOute will have to be abandoned.
If the answer is Yes, the analysis will have to be pursued in
detail in order to establish:
the ;ethods and .edürE fôf safe navigation
the workload involv4 in safe navigation.
In the final stage en investigation should be made o whether
the three crewing elements match and 2 above or whether
additionalquality, quantity or experience is required.
This planning philosophy is equally valid for. both shore
staff-and ship staff. The shore staff, however, will generally.
con-centrate, on the possibility of the voyge as an açceptab1erik while the
hip staff will, on the other hand, cocrae on
its safe execution and on minimising the risk element
It is obvious that voyages con emplated in new, unknown areas with new types of vessels demand most planning attention.
Rout1ine voyages on regular routes.will soon develpp routine
operting.proçedures.. The executionpf such routjne proeedu;es
should however be meticulous and precise.
One of ithe main objectives in voyage p1aning will alway be
the identification of "areas of constraint", 1 e areas of
exceptional risk demanding more than normal attention, skill and experience This identification process for a voyage such as the one in question, is graphically displayed in Exhibit 2 over-leaf. .
Sill Level
Exhibit-'2: Required Skill versus T1me during:"j
-Vbya'e;'-- 6' -Vbya'e;'--. Normal Available Skill keuired' Skill
Ehibit' 2' indicates that there are two arèá bf the voyage"
under consideration
which
reui're additional skill beyond what is normally available on board." (Skill 'is to be interpretedas the totality of quality, quantity and experience depicted
in Exhibit I under "crew".) "These areaEàrC 1 undér pilotage,
and2A,
astal; FOr 'area 1' the'additionàlskillrequirèmentis mebr the' pilot. krea 2A" is what 'cOuld be called' an area
of ãtticula± cOtraint which hãs'tO be thoroughly itivesi-gated in order to determine th'e methds And workload Involved in safe navigation and the manpower needed to meet these
requirements. In an area such as 2A, it is notknown whether'
the skill 'requirement will' be met by'thepilot: in thecase of Magellan Strait', itis even most unlikely since at the time for
whi'ththe 'planning i this" report is carried out, 'no' VLCs had
been in the area.' 'Therefore one could be' certain that the available pilots had no experience with VLCCs in this specific'
area. Little was known regarding the ships on which they did build up their experience and whether or not they would have
T-ime
2 4 2
Coastal :' Land
I Coastal
3 fall 2 2A 3
P Ocean Coastal Ocean
had up-to-date knowledge of advanced equithéntTIiis:togetherL with the very probable language barrier leads to the conclusion
that a Magellan Strait pilot should be used for his local
know-ledge only. Ship handling and navigation should remain under
the exclusive control of the master and his off iëer;.:.;
This report will deal in detail with a passage which involves
two 'such are'as of onst.raint;!. '.The purposei of this 'is..to 4emon St.ràte: the extent and complexity of the prObFems that:. canari.se
insuch'caSe's.H:.'
-"..'--
...Planning 'of..standard. procedi1rs,!. although just:.s. neceêsary, is len exact'ing and. can eas.ily'be' .dsdUced fron:.non-standard
prOcedutes:b'y a process of
.el.ii.natioñ...-
; _7...,,...2. - VQYAGE ENVIRONMENT
2.1 General
The specific case under consideration is a VLCC voyage from
the Persian (Arabian') Gulf to Quintero Bay on the acific Coast
of Chile. The planning is concentrated on the passage from
the South-Atlantic to the South P,aci'.c The question is
whether to go round, Cape Horn, or through Magellan .,,Strait. To
answer it, a Very thorough investigation of' 'the circumstances
of'. both possibilities is required.
2.2 Meteoroloica1 Data
In order to make a satisfactory choice between 'the two route alternatives, a detailed review of climate and weather conditions
for both routes is needed. Due attention should be paid to the
occurrence of icebergs and pack ice as a potential danger to
navigation. Contrary to North Atlantic conditiOns, there is
no ice patrol and, due to the very small amount of ocean traffic
in this area, there is also a very limited amount of recent infOrmation on ice conditions during the different seasons.
For that reason we have not only used sources of recent
infotma-tion such as:
- the South American Pilot1) further referred to' as the. Pilot
the Pilot Gharts3
but have alsoinves,tigated sources dating b4c1c,o sailing shlp
an4 pre-Panama
Caxl.-4ay
ti
this area was more frequentlytraversed 'by men and ships co1etely'depen4eit or wealet
conditions. The best söurqe proved to be:
DaS. Segelhandbuch f.ir den Atlantischen Ozean4.,
b4s4 On
observations from 1868 to 1908.
Detailed meteorolQgical- descriptions
i4
data ?re prpvi4ed irAppet.dix 2.2. :.
As is wel.i known, the weather can be clas.sifie4 as unfavourabie in many aspects such as wind-fOrce, temperature, precipitation.
and visibility. This is.trüe of, both routes. The Mgel1a1
Strait 'ill obviously offer some shelter fom the devastating
powers of the ocean, but this advantage will -have ..to.be care-fully weighed against the dangers to navigation which will be
encountered there. ., ,. .
With regard to.the, ice conditions, it is considered that thet is no' appreciable difference 'in favour of oneor the othei
roUte. Both routes ar already with..n the ice limits before
the point of divergence is reached (see xhibits 2 1 and 2 2
in Appendix 2). -Bbth routes cross the area with the heaviest'
ice concentration Only a much more northerly route could keep
vessels out of the area where .they are endangered by ice. ,,
-2.3
Qceanoayhic Data
Sea-conditions and-swell data were. also obtained from the sources
10
-and Lumb. However, for the same reason mentioned under 2.2,
i.e. low traffic density, the number of observations appeared to be too small to provide reliable predictions regarding
encounter frequencies. This is necessary to estimate the
con-sequences on ship motions of expected wave conditions, both with regard to speed loss and the probability of structural
damage.
In view of the lack of sufficient observations, we followed a method developed by Professor Warren C. Thompson of the naval postgraduate school in Monterey, California and which was used for a thesis by Edward M.A. Perera in forecasting climatological
wave data for Colombo, Ceylon. The method is based on the
assumption that in the first approximation the wave systems of two open ocean areas can be considered statistically equivalent
if the weather systems for these areas are similar.
Consequently, for the purpose of ship motion analysis, we have used the data for area 2 of Hogben and Lumb (eastern part of
the North Atlantic) as an equivalent area for the period
December to February inclusive. According to the Pilot Charts3,
the frequency as well as the wind velocity (wind-force) distri-bution of westerly winds are sufficiently similar, and the fetch is also large enough to give rise to a wave pattern equivalent to that of area 50 with which we are actually
con-cerned (see also Exhibits 3 and 4).
This same heading should also include dita on currents and tidal streams which are especially important for the passage through
Magellan Strait. Details will be found in Appendix 2.3.
The final results will be used to make a time comparison of the
route round Cape Horn, which involves -delays due to the encounter
.2.4 raphic Data;
-Ej
.In order to obtain an impression Of the area- tob navigated,
a careful study of the relevant Admiralty Piloit.., List of
Lights, the charts, and other literature is necessary. It is
advisable to use as far as posible material published by the
cotmtry having jurisdiction in the area. Language barriers
may uifortunately sometimes prevent this.
Great attention should be paid to the cautions, warnings and
navigation advice provided by these sources. They are to be
incorporated in the. overall planning of the route. The route
itself should be drain on the charts which will be used for
the actual navigation Of the area. Dangers should be specially.
marked and highlighted, including relevant danger bearings. Courses and, bearings should be recorded on the. chart in three
0 0
digits from 000 to 359
Due attention is to
be
paid to the availability of shore-basednavigation systems and similar navaids and their local accuracy,
i.e. their accuracy along the intended route. (See Chapter 3
and ts appropriate appendix for further information Ton
posi-tioning.)
In this context it must be mentioned that great care should also be taken tO assure the charts' reliability, especially
- -1 1. -.
distance, iththe.routethrpug1 Magellan Strai, which ::V9.veS
delays due to waiting times sincethe passagepf the,First: Narrows is dependent on the tides and should pe.ferabiy be made
in. 4.ghç.
;i:.12
-in the case unde± ão
ideàtibi whre the vCsei is
of-extreme size (seeAppendix2a4)i
Finally, it hould be noted that the. sailing directions in
the Pilot are based on information provided by the sailing
ships of the middle to late 19th century. Naturally these
directions were suited to the ships of that era, which were. small comparêd to those of today, powered by sail instead Of reliable diesel or steam engines, withou.t radio aids to navi-gation and also without weather information from shore-based meteorological institutes.
Uvsrpoal GLAND LONDON outhempton '050° .0300W 020°W / -> ' 01o,w
I95O . LIsard P&nt 2rw
92ON .00,w
/ )/
'
d Ouesa&liI'''I
-Int-Nereire 0 ire FRANCE 0000 1 Oostei Dunkerque Bouogn. B 0tj
0 rt (-A,_flrrcMR
San JuIin Santa Cruz Punta Aren Rio Grande gall. Stro g tidal . oc r f,-om t Strait ofto Id. los (s4os
d,n a MairelS 8it :
Is Di
tanley= =--= = --= =-- ==-- = =--= = --==
1=
15
-3. POSITION FIXING IN MAGELLAN STRAIT.
The available pathwidth in some sections iS very small,
there-f öre the demands on the accuracy and reliability othere-f the position
fixes in Magellan Strait are high. Since no other suitable
rádiö navigation systems ae available and because'o the need
for continuous position informtion in the areaS of coüstraint
(see Appendix 7), rãdat plays'- an important role in navigatiOn of the Strait.
Firstly, two independent displays are needed: oe fOr the
pilot(s) and one for the ship's own navigation team! Secondly,
both radars should be in optimal condition. Any malfunctioning
detected before entcring the Strait which could influence
accuracy and/or reliability should be répairèd before entry,
otherwise the passage should be cancelled. The same applies to
the gyrocompass, compass repeaters and azimuth circles, because
visual compass bearings, form the secondary position fixing
method (in someparts even the primary position fixing method)
throughout th passage (see Appendix 7). Emphasis should be
placed on-using t19e tiq4 ijçh.pptimise
tbe
accuracy andreliability of pqsitiQn fixing (s-'Appendix3.1).
As mentioned above, the available pathwidth is very small at
some locations. It is necessary to get an idea of what part
of this available pathwidth is "claimed" by theinaccuracy
of the position fixing Therefore we have computed the 957
probability contours of those position' fixes which were
obtained by the nest favourable methods in the thore difficult
part of the passage, from the FirSt Narrows o-Cabo Quod
16
-4.
SPECIFIC VESSEL CHARACTERISTICS4.1 Theoreticai1y RequiredPathwidth
The theoretically required patn4dth is computed in Appendix
4 1,
which also ixplains that an additional safety margin shOuld be added to this value to arrive at the actuallyrequired pathwidth. This safety ma±gin should provide for:.
- weather conditions
ififluene of ëur±nt
- turning of the ship
- fairway characteristics
reliability of the charts
Since the influence of currentS and the reliability of the
chartsre unknow,it is impossible to quantify the êxáct
safetyrgin
However, it- was cpnsidered useful to compute the. theoretically reqüi±éd pathwidth bècauSè the ratiO between available pathwidtfi and theoretically required pathwidth will still give an idea of where the areas of ëonstraint are.4.2
Determination Of Distance to Nè CourseThe available pathwi4th -iS very sthall at some parts of the
- 17
cause,:an unwanted'off-traek deviation, some investigation was.' done into the way in. which coUrse changes are usually -handled.
It appeared that at present this depends greatly on the ecperi-ence of. the master 'or máte. .It should be noted that the..ship
manoeuvring simulator training courses give no help other than the opportunity 'to gain some. experience. -' The only "niethodical"
approach to course changing seemsto be the of the.
distance to newcourSe (the distance between the.point where
rudder should be given:and the intersection point of. the
'origina1-trckthidthe new track) from the ship's'"turning circle data't. In practice, use of this method is hardly possible because on most merchant vessels the available
turning circle data are restricted to large angles of helm;
these data were determined tO get more insight into the turning capability during mergencies.. FUrthermore, this thod only
provides information about the istance to new course,.
but'-does not indicate when, where .and how much couitter-rudder
should be given to check the turning motion when approaching
the new course to be steered. Although it appeared that the
effect of counter-rudder on the distance to new course is raher small providing it is applied in time, larger Off-track
deviations result when counter-rudder is applied too laite (see Appendix 4.2).
Therefore, the method given in Appendix 4.2 was developed to assist masters and officers, particularly those with little
experience. The aim of this method is, not to provide more
accurate values for the distance to new course than are pro-vided by the "turning circle" method, but to allow an "edu-cated guess" to be made regarding the execution of a course change manoeuvre by providing checking times, corresponding
18
-We hope thàt.this method will be helpful in the navigation
procedure traIning on simulators, as well aS on board ship.
It should be stressed, 'hOwever., that "incorrect course changing"
is only oneOf the possible causes of off-track deviations. It
is possible that "correct course. changing" could have caused
certain groundings to occur eariir. For example, the effect
of the error which was the actual cause of such ground-ings could have been counteracted by the effec.t of "incorrect course
changing". This of course should- not justify "incorrect course
ch*nging". ..-
-Finally1 it should be made clear that. the calculations htch
provide the information shown in Exhibits 4..9 - 4.16. will,
because -of their complexity, normally to be dOne by -the
shore-based organization. This again stresses the need .fO±
19
-5. COMPARISON OF ROUTE ALTERNATIVES
As already mentioned, the two route alternatives are through Magellan Strait and round Cape Hon. The following is a comparison of both routes.
.Meteorological Conditions (see Appendix 2.2):
On both routes vety rough weather can be encoutered. In
Magellan Strait, rough weather means mainly squalls with or
withOut bad visibility. When rounding Cape. Horn it means
gales with the possibility of leavy headseas. .
Available Pa.thvi4th (see Appendix 4):
In Magellan Strait, the available pathwidth is sometimes very
sll, especially in. relation to the accuracy of the available
position fixing methods. When-rounding Cape Horn suffi,çient
searoom is available. .
Position Fixing (see Appendix 3)
In Magellan Strait, position fixing is meinly done by means of
.radar and visual, bearings. The- accuracy requirents are.
times very high, because of the little available pathwidth.
When rounding Cape Horn, position fixing is mainly done by means f radar and astro-navigation if the ship is not fitted with SATNAV. It is very possible, however, that the-navigation haS to be baSed entirely on radar observations and dead reckoning,
- 20 =
Required Pathwidth (see Aèndix 4)'.:
The required pathwidths in the areas of consttaint in Magellan
Strait, as computed in Appendix 4, already come very close to the values of the available pathwidths. . Moreover, as
mentioned in the same appendix anxtra safety mergin should.
be added to, the values of the theoretically required pathwidth
to find the, actually required pathwidth. The value of this
safety mergin is not known,'.but owing to the extraordinary
conditions in Magellan Strait, it is a distinct possibility
that." in some places the pathwidth required for safe navigat-ion
might excee4. the available pathwidth.
Voyage. Duration (see'Appen4ix-5):.
As shown below, on average there will be no difference between
the two routes. It.'should, however, be stressed again that
the values in Appendix 5 and the table below are mean values.
The actual values for both the route round Cape Horn and
through Magellan Strait cOuld .tay weli.i.ider those, mentioned
or exceed them.
Exhibit 5:
Variations in th VoyagtigiiBad.on.a
ShIP.speed of '1.5 'c,ots
- Magellan Strait .. Cape Hori
Mean delay owing to .
recoendation in the Pilot
' ..
+lOhr 34mm
Tim loss due tq longer:
'route distance + 6hr 36mm
ilean shorter passage time
owihg tofdlIow,ing current 51mm
Mean' time loss due to
headwaves + 2hr 00mm
Longer.passage time owing to speed adjustment in
areas of consträiht.
.
i- 58mm
Time. loss due to countercurrent
H
+ 2hr OOmi,n
Longer passage tithe Owing
to delay in boarding of
pilots unknown
Time loss due to voluntary
speed reduction uiiknown
Total extra voyage
duration 10hr 40mm
Total extra voyage
21
-Cost:
On the basis of time there is no computable cost difference
other than a possible slight difference in fuel consumption.
Therefore the only cost difference that can be mentioned with any degree of certainty and accuracy is a difference in pilotage and hospital dues amounting to something in the order of
US$102,000 in favour of the Cape Horn route. However, it is
possible that part of these dues may still have to be paid when rounding Cape Horn, because a call is made at a Chilean port.
.22
-6. TIME SCHEDULES OF THE PASSAGE THROUGH MAGELLAN STRAIT
When planning the passage it is necessary to prepare a time
schedule which should start on the intended day and time of arrival at the entrance of the Strait and take into account
the recoendations of. the Pilot concerning the t.me of passage
of the First Narrows. It
IS
also necessary tO:prepare asimi,-lar schedule starting one day later in case Idiate passage
upon arrival is for some .reason not possible.
There are several reasons for preparing a. time schedule. One
of these reasonS is the need to have a duty divisiOn in order
that sufficient manpower be available when needed. Another
reason is the need to know which section will be traversed
during daylight conditions, and which during night conditions.
This may be iortant in determining the position fixing
methods to be used. A diagram with the times of sunset,
sun-rise and civil twilight for the area wil,l be of help here.
The times for 1974 are given in Appendix 6, Exhibit 6.7. In
the same appendix two examples of time schedules are given:
one for a passage during spring-tides and the other during
neap-tides. The time difference between the two is about
half an hour. This is because of the considerable difference
between the rate of the tidal stream during spring-tides and neap-t ides.
23
-7. TUE AREAS OF CONSTRAINT AND THEIR NVIGATJC)N
In planning, it is necessary tä detèrine where the areas of
conStraint are, aSpecial
Should: be given to thernFrom the description of the passage in the PilOt (see Appendi-ceS I and 2) and from the iat-iO of available pathwidth tO
theoet-iëall teuired pathwidth (see Appendix 4 1), it is
clear that there are two areaS of constraint: -
-a-) from abreast of Banco Di-recc-i6n as far as BancO Thit6n
b) from abreast of Pta. Pasaja as far as Isla Beware.
In Appendix 7, these two areas are further subdivided into
different iections, each having its own particular
diffi-culties. Furthermore, a navigation plan and the menpower
requirements are given for each section. One section, namely
the passage. of Bajo Satlite and the 10 fathom patch, haS been
p.anned in detail as it should be done on boar4 ship, and this
is accompanied by the notes which should be written in the bridge
note book and those whih should be inserted on the chart. In reality of course it is necessary to plan the whole passage in
the same detail.
The fleet nagement should plan a passage, such as the one
through Magellan Strait, in-the Same depthof detail as the
navigation plan given in this report. Firstly, this will enable
the nagemént to asSess the degree of difficulty of the passage;
secondly, it enables them to decide on the npower requirements,
8. QWI
Qj$ENTS
When rounding C4pe Horn no additional offloer is required, as
the passage is in fact normal coastal navigation.
However, from the descript-io of the navigation in the areas of
constraint (see Appendix 7), it becomes clear that when passing through Magellan Strait an additional deck officer is needed to allow the captain to asume fui1 responsibil:ity fQr super. vision of the navigation. The need for an additional officer is
also emphasized in the duty diVisipnexamples in Appendix .8,
where it becomes c1er that, depending on th time of entering
the Strait,. t may be very difficult to provide officers who
are fit for duty when needed. Obviously the planning must
be basfd ona capable and well integrated team of officers. Attention should also be paid to the duty division Of the helmsmen, as well as to the refresher training oi these men
during the voyage before the passage.
25
-EPILOGUE
This section concerns the grounding of the loaded VLCC METIJLA (104,378 gross tons, 206,719 tons dwt, drawing 58' 06" fwd,
62' 06" aft) while on passage from Ras Tanura (Saudi Arabia)
to Quintero Bay in Chile. The cargo consisted of 190,415 tons
of crude oil.
The accident occurred at 2216 local time in the First Narrows of Magellan Strait (Admiralty charts 1336 and 1337). At that time the weather was fine and clear, wind westerly, force 3. During the transit of the Narrows the current was ebbing north easterly at a rate of 6 knots and was decreasing in strength. Shortly after the grounding the current started to flood.
Two radars (3 and 10cm with interswitching facilities) and an echo sounder were in operation throughout the whole period
concerned and were functioning properly. Both radar displays
were constantly used by the two Chilean pilots who checked the position of the ship by taking radar ranges and bearings and plotting them on their own Chilean chart 1137. The third mate,
who was 00W, regularly took visual bearings of shore lights and plotted them on the Admiralty chart; later, at the request of the pilots, he moved to the port wing compass repeater and sang out - via walkie-talkie - the bearings of Pta. Mendez Lt. The
master - an ex-pilot in one of the Persian Gulf ports, with experience of all types of tankers, and who had also followed a VLCC course on a ship-handling simulator - checked the navi-gation of his ship on both the Admiralty chart and the Chilean chart. An experienced sailor was on the wheel.
26
-During his stay in Capetown the master had received detailed reports from two other masters from his Company who had already navigated their ships through Magellan Strait on a similar
voyage to Qiintero Bay. TheSe reports had been thoroughly
studied and circulated among deck and engineering officers.
Six das before arfivä. the ter Sent a telgram to the
agents in Valparaiso, Statitig hil ETA at the pilot station
(Baha. PoSesi6n, see Exhibit 6) as 1000 local time. This
specified time was, according to the master,, a very import-aüt factor because 'it would allOw the vSSsèl tO pass through Prirnéra Angostura during daytime So 'that shàIlowS -' covered with seaweed - could easily 'be de'teôted, and also to pàs
Bajo Satglite (see Exhibit 7) with a rising tide almost at
High Water. ' ' H
-The material facts leading up to this accident tete as follows
(all times lOëal): '
.0849: AbOut eightmiles frOth the pilot st4tion.
Rèdeivëd a telegram ith a request to anchor at'
-BahIãPoseSi6n, and alt there for thE two pilOts
-' ' who were expected to arrive at -1900 in an
east--bound' vESSel'
0900-1900: 0ing-to the.strong current (5 khots), the mastEr
dcided- gainstanchoting and instead resolved to keep the Shiptinderway by steaming up and down thE
bay. 'Regiiiarcoi''uniëation with thE-maSter in the
othervessel-wastháintainEd in order to establish a tim&and-a place for embarcation.
-1920: Both ptlots-embaticed-havingbeen transferred from
the other vëssël b means of a' Chilean Naval tender.
27
-o receive
e
pilots, rporte4: to th m4ster, via a wàlkié-taikie, that the pilots had no Objection whatsoever tO navigating in the dark and that pilqtage could be started withoutdelay.
Position: South of. Banco Narrow (see Exhibit 6).
1930: Full
sea
Sp4 ($0 rpm, 14 knots by log).1930-2130: Slow progress over the ground (6 knots) owing to
very strong counter-current (ebbing).
During 4iscuss ions with the ,piiots the master learnt that their experience with large vessels did not extend to. Ships oyer 100,OQQ tons.
At 2110 the pilots took up their positions at the
displays,
aking, 'be.rings att.d ranges withthe vajable range markers. Meanwhile, the master, having ,a good look at the new Chilean
chart provided by: the pilots, iloticed a 14m/15m
shliqw patch on it.. To idefltify this shoal on
the ship's working qIar-t he
anfeed its
lati-t.ude an4 .longitude frorn the Chilean chart to
Admiralty. chart 1337. The result was that the
patch fell apparently exactly on the reco ended track shown on the Admiralty chart (in fact, this
patch is correctly shown on the,
ialty cart
sot1 of, the'recoiended track, see: Exhibit 7).
The master later,noticed that there was a
dis-crepancy of about 6 cables between the, grid
systems qf the two charts5 but the 4iscovey was nevertheless upsetting.. He fel.t thathe could not
rely further On the. Admiralty chart. He had also
lost valuable time in checking the navigation carr:ied out by the' pilots.
2130: Entered Primera Angostura.. Pta. Delgada abeam a.t a
distance of 1.2 miles. Course 225°.
28
-2208: 3rd Mate took station at the port wing compass
repeater and sang out the bearing of Pta. Mendez: 063.5°.
2210: No change in the bearing of Pta. Mendez: 063.5°. Radar bearings taken by one of the pilots gave a position slightly to starboard of the recommended
track on the Chilean chart.
2212: No change in the bearing of Pta. Mendez: 063.5°. Radar bearings taken by the pilots gave a pos-ition further to starboard of the recommended track. Pilots gave order to alter course to 2420. 2214: Ship started to turn to 2400.
No change in the bearing of Pta. Mendez. As the master now sensed that something was going wrong
he ordered the wheel to port. At about the same
time he looked over a pilot's shoulder into one of the radar displays and noticed that the near-est coast was just a little more than a mile away. 2216: While the master was transferring this distance
to the chart, the ship ran aground. Stop engines.
As a result of the grounding considerable leakage from the f
or-ward and bunker tanks took place. Two days later, on the flood
tide the ship swung round from 2300 to 1850 damaging more tanks
and flooding the engine room. The overall damage was enormous.
47 days later, after pumping out about 90,000 tons of oil, the ship came afloat, was towed away and later sold for scrap. No personal injuries were incurred.
At a subsequent investigation it was found that the master was partly responsible for the accident although there was no doubt
that a great deal of the blame can be attached to the actions of
Cerro Oireccidn Pta. elgada 2130 Pilots on board 1920 1900
Se'Orawing
No.7 69°W..-J
0800 07.00 68030WSOUTH ATLANTIC
OCEAN
C.Virgenes.Pta Dungeness
.%--0800
5220S
52°30 8 rt tn!62°308
52!358
SOundings...a..J.
- ... ...
in fathoms
-.fathom
tErn) This -8.(14m/
-...,,.
... . ..patd, it hôwñ
as 52i6"3S,
coPra5pOnti. / .-Position of Grounthnq at 22 16
I/
/
. Racon .ii
I
22 i,"
-$3/1
/2'o
-I/..
4_,i.-'
/
\
\
Pta. Satélité -, b\,
Satelite Bank,ç,#'
\..
,';1;#1:;A
on the chilean c/1rt 7137
69°46'.9W which apparently
--
-
t
-. I-/
-- : 69°50W89°40W
1. VOYAGE PLANNING
1. 1 Description of. the Routé. through MagellanStrai.
(from the Pilot)
Anchorages:
SW of Pta. Dungeness:
Bahia Posesi6h:
Puerto Sara:
Rada de Pta. Arenas:
Further west there are
Descri2tionof Navation Points:
C. VIrgenes:
C. Virgenes. Lt.:
Between C. Virgenes an Pta. Dungeness:
Pta. Dungeness:
exposed to wind and tidal streams; bottom: mud and sand.
exposed to stong tidal streams and S winds;, good holding grqund. exposed to tidal streams; bottom: sandy.
sheltered from W winds;
bottom: mud, sand and in some places rock.
no iuitable anchorages.
height 41m; marked by white cliffs
forming the seaward termination of a. range of hills of moderate
eleya-don; radar conspicuous at about 25m.
white,- metal framework light er,
central colu with black bands,
26m in height; a red brick dwelling at the base of the tower.
a conspicuous white house iith red
roof; 2. cables .N a 41m high st.
the extremity of a low spit of
gravel and sand, 3'n S of the foot
pf a. range of hills (see view, chart 1336).
APPENDIX,
-APPENDIX I Page _2 Pta. Dun.geness Lt.: Cerro Dirección: C. Direcci6n Lt.: C. Orange: C. Orange Lt.: Pta. Delgada:
situated on the point;. round metal tower 25m high, painted red with white bands; a beacon (pyramidal, red with white bands, 16m high)
close to and E of the tower.
Pta. Wreck: . . conspicuous flare.
C. EspIritu Santo: a steep white cliff, 58m high,
difficult to distinguish except from the Strait.'
C. Espiritu Santo Lt.: meta) frawork tower, white with
orange bands, concrete base, 7m
high.
C. Posesi6n: ' bold and sheer headland, 112m high;
from a distance of 15 to 20 miles E. the cape appears as an island (see
view,, chart 1336).
C. 'PoseSi6n Lt.: urn high, white square masonry tower, 6 cables WNW of the suit of the. cape.
68rn high, appears as island, together
with anOther hill S of it, when apprqached fr, the E (see view1
chart 1336).
round metal tOwer, red with 'hité bands,, 2m high, on the summit; a 'beacon (pyramidal, red with white
bánd, red globe toprnark, 16rn high)
close NW of the light tower.
sharply pointed conical and sandy hill, 41m high, unmistakable, app-roached from the E, a white patch
will be seen on its E side. rnetal framework tower, aluminium colour, lOrn high, on the summit;
Some brilliantly lit oil derricks
are SSW of the light toer.
'identified by the light tower on it ànd'the' small settlement in its vicinity.
APP .NDIX '1
Page
Pta. Delgada Lt.: round tal tower, white with orange
bands, lZm,'in height, on the point;
white house with orangeroofand a ' mast nearby; a prominent flare near
the Light tower, approaching from the E the flare obscUres the light.
Sometimes two leading lights are shown for the lighthouse tender.
Cerro Angulo (Angle Hill): 31m high, very prominent, same
appearance as C Orange, no
light-house on it. Pta. Mendez Lt.:' Morro Nuiez: Pta. Barrancã: Bajo Satlit'e: Pta. Baxa:
on the highest cliff, on theS side
of the'narrows (elevation 28w); rotd
metal tower, red with white bands, 2m in height.
2 miles SWOf Pta. Delgada,
con-spicuous triangular, cliff, 22w
high..
Pta. Satlite Lt.:. '- red metal framework tower', 5w. in
height, situated on the point
identified by its lOw cliffs, which are the only ones in the vicinity (see view, chart 1337); a.'beacon: (metal pyramid, red, two white cylin-drical cases topmark, lOm in height)
stands on the point at an elevation
of 16w.
covered by a red sector of' Pa'. 'Delgada
Lt. between the bearings 039 and
0
044 ; SE edge of the shoal s steep
to but is reported to be extending; it is marked by kelp, which may be run der from half flood to half ebb.
when approaching from the W' it- iS
the fourth cliff from the S, mile
NE of 'the point.
Pta.. BaxaLt. '
' a round, metal light tOwer, 3m in height.
C. Gregori'o: sandy and terminates in a small, 4m
APPENDIX I Page 4
PuertO Sara: oil terminal and oil storage tanks.
Puerto Sara Lt.: Cerro Cono Lt.::. Pta. Grãcia: I.Sta Nagdalena: I. StaMagdalena .Lt.:. I.. Contraniaestra: Pta. Gente: Pta. Arenosa:
on a wooden post at the head of the
pier,- lOm elevation.
round metal tower, red with white
bands, 3m in height on suit of
CerroCono, a.distinctive hill,
41m high.
53m high, cliffy (see view 35 in
Pilot).
C. San Simon: highest cliff on S side of Segunda
Angostura, 64tn high.
Monte Agudo: remarkable conical peak, a good mark
until C. San Simon can be seen.
Segunda Angosttira Lt.; 4. miles SE of Pta. Gracia; white
concrete tower, 5m in height.
C. San Vicente Lt.: - square, white concrte tower, 3m in
= height, Situated mile NE of the W
extremity of C. San Vicente (56m
high).
I. Sta Nrta: sheer cliffs, elevation 19m, flat
suimnit, slopes slightly to the E. 40m high at its W end, whete it rises vertically from the sea.
white, circi ar metal tower, 13m in
height; dwelling close by.
15m high; light frorn round concrete
tower, 6m in height. Light is weak
and easily confused with the light-buoys S and E of the island.
22m high.
projection of low land, consisting
of sand and gravel covered with grass and bushes; 4 illuminated, very prominent radio masts, 4 cables WNW-of- Pta.. Arenosa (see chart 1337).
Nuela Prà.t. Lt.
(Pta. Arenas):
Pta. Sta Anna:
Pta.. Sta Anna Lt.:
C. Froward:
C. Ho11and: C. Sàii Isidrb:
C. San Isido Lt.:
Pta. Joaquin:
metal pedestal, 6m in height, at-the
head of the pier. Two conspicuous,
'illuminated radio masts, 3 cables NIE Of Muela Prat (see chart 1281). extremity of narrow. promontory, can
be recognized by a large clt of
trees.
square, white concrete tower, 5m in height, 2 cables WNW of the point.
small peninsula, 1 cable wide, which
joins a low but prominent rounded
hillock (21m high and covered with trees.) to the inland.
white,, circular concrete tower, 8m in height, with red-roofed, white
dwelling close to and NWofit, on
the cape.
a. hillock on it, difficult to
dis-tingui'h from the surromding land
on approach fron N, but prominent when aeen from off C. Froward (see
view, chart 1281).
rises abruptly to an elevation of 359m (see view, chart 1281 and views 36 and 37 in Pilot).
C. Froard Lt..: white concrete colui, 3m in height,
situated on the cape.
steep, bold and prominent, consiSts of a detached ridge parallel to the
shore, 4 miles long, 342m high; the
seaward side has precipitous cliffs, with densely wooded ledges (see view, chart 1284 and view 38 in Pilot)'.
APPENDIX I Page 5
C. Gallant: 25rn high, massive and steep, prominent
from the E (see view 40 in Pilot).
I. Rupert. Lt.: white, circular metal columo, 2m high,
island.-APPENDIX 1 Page 6 Roca Anson: Roca Crooked: C. Crosstide: C. Quod: C. Falso Quod:
C. NOt&:
C. Hunter: 275m high and steep.
I. Shelter:. -prominent with well defined summit,
116m high, steep to and covered with vegetation.
massive and cliffy with deep water
close round it.
'240m high, projects. well' into the
Strait, urimistakable from the E as
it appears to have a cut in. its'
su=it.
when approaching from the W at 'night or in thick weather C. Quod can be
distinguished from C. Falso Quod by
Ite. Beware close to and W of it. very remarkable sheer mass of' rock,
119m high, extremity of small peninsula.
Ite. Cohorti Lt.: round metel tower, white with re4
bands,. on concrete base, 8m in height, situated on 6m high islet.
Moat
of
the coast be1,een Cabo Gallant and Canal Jerónirno isfringed with kelp and should not be approached closer than 3 cables.
The hazards of Pw2ta Pasaja are reported to project further
into the Strait than is indicated on the chart.
depth -5.2m over it, the kelp on this
rock Shows only 'at lack water because
it is pulled under by 'the tidal streams
(see view B chart 887). C. CrosStide
should be neared to avoid it. The S
extremity of I. Borja Grande in line
with the cut in the suit of C. Quod,
bearing 277°, leads S of Roca AnsOn.
depth less than 2m over it6 marked
by kelp. The bearing O61. of the
sUmmits of I. Borja Grande and I. Borja Chica in line leads. 2 cables
SE gf it. Ite. Beware bearing
295 and open to C. Quod leads SW'
C. Cooper Key: C. Cooper IceyLt.: C. Monday: Pta. Havannah: C. Upright: C. Parker: I. Westminster Hall: Bajo Magallanes: Bah'a Felix Lt.:
C. Cortado:
C. Pilar:-. round
jfl
shape, not easy to recognise from W except by its light; from E it. shows as a very prominent steepheadland, and in clear weather after
rounding C. Quod, 29 miles ESE, appears as the end of Paso Largd. circular metal column, red with white
bands, 2m in height, situated on the cape (see chart .1105).
bold headland; the cape is formed by
the flat suit of a ridge and
des-cends vertically to the sea; 247m high. sloping projection of bare white
rocks.
flat topped, square faced headland. the termination of. a long sloping ridge with three symetrical
sugar-loaf hills on it, one behind the other above the S hill which is hOrn high; only prominent from E.
precipitous and of granite, 342m
high, remarkable appearance (see view 50 in PilOt).
rocky bank, depth 19.8m over it, steep to, a heavy sea rises on the bank during strong W gales.
round metal tower, white with re,d
bands,. 14m in height..
60m 'high sheer, steep to, unmista-kable from either side.
the sides of the cape are Sheer. and
cliffy; it, is backed by two tmtains
which form a high and remarkable
pronntory. Viewed. from the E, the cape appears to have one double' peaked
suit; the W peak is shaped like 'a
tower and rises, to an elevation of 552rn from the shore W of the cape;
the part of the cape facing the Strait presents a low rounded hill, while its W side shows considerable erosion by the sea.
APPENDIX I Page 7
APPENDIX I
Páge8
Peones Lanchäs Espaoles:
séverãl small but steep islets. loseto C Pilar, the largest, an enormous detached rock, 93m high, is clearly
seen as a prominent detached islet
from E Shoal water is reported to
lie. 2 miles NW of C. Pilar.
Grupo E ngelista.s Lt.: a white, circular granite tower, I Im
Reconended Track_throuNa.11an Strait
Course of groundtrack Theoretical position of
tobe followed: course.changes:
course 235° till 52°-49'S 068°-0O'W
o
320 Pta. Dungeness 000 6.lnm
290° Cerro Direcci6n Lt. 267° 14. 8nm
267° Cerro Direci6n Lt. 267? 6.7
225° Pta. Mendez Lt. 135° 1.Onm
218° Pta. Satlite Lt. 008° - 2.lnrn
246° Pta. Sat1ite Lt. 052° - 7.2
o 0
229 C. Gregorio 275 I0.5nm
0
257 C. San Vicente abeam
1760 I. Sà Magdalèna Lt. 2780
- 43
210 Pta. Arenas 270
192° Cape I mile SW of C. San ISidro abeam
234° C. Froward Lt. abeam
293° I. WoOd 270° - 2.lnm
312°. Pta. Pasaja abeam
315° Pta. Rowe abeam
- 0
--27-2 C. Quod abeam 0.8nm
302
Nother
spur of I. Spider-abeam 0.9rm305° Cape 2nm, S of Cooper Key. Lt. (southern
side of the Strait) abeam I.lnm
318° I. Centinela Lt. abeam 2.5nm
297° NW cape of Pta. Felix abeam 3.5nm
309° Roca Qutpost (Grupo Westminster)
abeam 4.5nrn
288°
APPENDIX 1 Page 9
APPENDIX I Page 10
Available Pathwidth in Maé1iTah-Sttait
Abreast of:
.. -.Available pathwidth (nm)>2..0im,
Pta. Dungeness Pta. Daniels Pilot Station Plumper Michorage Pta. .Anegada Pta. Delgada. Pta.. Mendez Pta. Satglite
Bajo Satlite
10 Fathom Patch Banco Trit6n Banco Nuevo C. Gallant Rocas Rupert Pta. Pasaja C. Middleton I.. Cohorn Lt. Roca AnsOn Roca Crooked I. Beware I. Spider' C. NOtch' C. Hunter I. Shelter C. .Pilar 1.8 1.6 1.6.. 1.5 0.8 1.700
1.5 i.b.'. 0.6 1.0 i.'0 0.7 0.8 1.2 1.5 1.4 1.5 .0000
1.2. Influence of Tide.on Available Pathwidth.
The
vicinity of the 10 fathom patch, 6.7nm SW of Pta. Satlite, is apparently the oniy part of the recoéndéd track through Magellan Strait, where the available pathwith is small butwhere the risiig of the tifle bight
gie a
Significant increasein available pathwidth.
-7) . .
-In the Chilean Tide Tables details are given for Bahia Santiago
and Baha Felipe which are immediately north and south of the
10 fathom patch, respectively. It is assumed that the average
of the tidal information for Bah!a Santiago and Bahia Felipe would provide the values for the vicinity of the 10 fathom patch. The tidal curves fot BahIa Santiago and Baha Felipe are found by interpolation, in Table III of the Chilean Tide Tables and
the daily predictions. The fact that Table II. has to serve for
both standard
a'4.
secondary port of the tidetable may, however,justify some doubts
as
'o is accuracy.
E,thibit 1. 1: Daily Predictions for Puerto NOtt
Standard port, January 1st, 1975 (springtide):
APPENDIX I
Page 11
-Time Of HWand LW Heights above Gha Datum
03.36 6.86m
10.00 0.52m
16.08
APPENDIX I
Pagi 12 -:
Exhibit 1.2: Daily Predictions for BahaSantiagd atidBàhiaFelipe
Secondary ports (see Exhibit .5):
Conclusion
Addihg the values .of bpth curves (see Exhibits 1.3 änd-14 to the
charted depths near th 10 fathO patch will Shd that the patch
Of about 8 fàthoE of it cannot be pasCd over at an
tié Of
the tide. However, if the passage through Primetà AngOstura
made at the time recoended in the Pilot, the 10 fathom patch wil.l be passed ábüt 2 hoüs before .HW inBaMa Santiago and
Baha Felipe. Consequently the charted 12 fathom depth On the
portside of the recoended track and iediately after the
10 fathom patch, which at low water would be the port limitof the available path, will be increased by 1.7 respectively 1.9 fathoms to about 14 fathoms actual water depth, which provides enough under-keel clearance not to be a problem at
either spring-tide or neap-tide.
Bahia Santiago BahIa Felipe
Time of HW and LW Heights above Chart Dat
Times of HW and LW Heights above
art Dati - --23.51 (31/12) 06.15 (01/01) 1.2.23 18.26 4.62m 0.03m 3.86m 0.58m 23.51 (31/12). H 06.15 (01/01) :12.23 18.26 5.98m 1.04m 5.22rn ].59m
1.3 Description of the Route round Cape Horn
(from the Pilot)
Generally speaking, the coast of Tierra del Fuego, including the islands lying off it, has not been well surveyed and the
available charts are of very small scale. However, 10 to 20
miles from the land the depths vary from 110 to 365m, the bottom
being sand almost everywhere. Not until within about six miles
of the coast does the bottom become irregular with rocks rising
to or nearly to the surface.
Description of Navigation Points:
I. de los Estados:
APPENDIX I Page 13
mountainous, with its peaks covered
with stiow almost all year round.
Everywhere the coast consists of rocky
cliffs, from 60 to lOOm high. When
passing E of the island care should be taken because the NW-going current
sets strongly towards the island. Vessels are advised to stay at least
10 miles E of the island because of
the very dangerous overfalls, caused by a tidal stream of up to 5 knots
against the wind, of f the E extremity of the island.
Cabo de Hornos (Cape Horn): seen from a distance there is nothing very striking in the appearance of
I. Hornos. Nearby it is more
remark-able, showing high black cliffs to
the S. The Cape rises to an elevation
of 405m (see view, chart 1373).
Cabo de Hornos Lt.: truncated conical wooden tower, 4m
high, on Cabo de Hornos.
Is. Barneveldt: 99m high, nearly I mile long, with
APPENDIX .1
Page 14
I. Deceit:
Is. Hermite:
Is. Ildefonso:
Cerro, Cathedral de York:
Rocas Cabrestante:
Rocas Philips:
I. Treble:
C. Castlereagh:
I. Noir:
44Om high. When seen -from the E,
its outline is not' unlike'that of
I. Bartholo, the largest of Is. Diego Ramirez.. A detached group of pinnacle rocks lies 3 miles off the
SE extremity of the island (see view, hart 1373 and view 14' in the Pilot).
slopes gadually W from the rugge4
heights in its E part.
185m high. Supposed to be the top
of a narrow submerged. utain range.
Vessels can pass derately close to
them, according, to the Pilot. In
1969 the islands wüe reported to lie
3 miles farther S than charted.
Cauti,,on: there
i8
a.4ifferenc
beeen the charted positions on
the various charts.
resembles the building of that narne 'The island of which it is a part
(I. Waterman) is very hjg1.
the st seaward termination of Is.
Christmas.. It is 6m high with
breakers 2nm seaward of it. The Pilot reco=ends that it be given a berth
Of at least 5 miles.
very low and, dangerous, should be given a wide berth.
the largest of a small group of
islets and rocks off the SW end of i.Londbnderry. The islet has 3 'peaks, and is visible from a
con-siderable distance.
the SW .ettemity of I. Stewart. It
is high an4 remarkable (see view 15
'in Pilot).
-183m high; extends , piles W to C.
'Noir,. rocky pinnacle resembling a tower or belfry at the, extremity of a low point (see view 16 in Pilot).