Statistic
Data Chilean Navy
1.- General Information.
This island
is the southernmost of the Hermite Group and particularly known by the
famous Cape that has its name.
The
soil of Hornos Island consists mainly of peat, and some granitic areas
which makes it possible to reach the peak of Cape Horn, which is erected
at 425 meters of height. It
must be taken into account that the climbing is difficult and it requires
4 hours to reach the top.
2.- Lighthouses.
At the south of the island, there is a lighthouse which was constructed in
1962. Its main characteristics are: white beam sent every 12 seconds, 40
meters of height, 17 miles of geographic range, visible at 249° to 080°,
equipped with a RACON.
At the Espolon promontory, in the SE of such island,
the MONUMENTAL CABO DE HORNOS lighthouse is located which was built in
1991. Its main
characteristics are: a white beam every 5 seconds, 57 meters high, 20
miles of geographic range, visible from 127° to 056°.
This lighthouse is fitted with
a RACON.
3.- Requirements of the Chilean Pilot.
Ships that are headed to Cape Horn with the intention of disembarking
passengers should do so with Chilean Pilots on board. There is an anchoring berth - called Caleta León - located
NE of the Monumental Lighthouse, at 800 meters from the lighthouse.
There is a landing place along the same coast for small crafts and
a ladder that allows to go up to the Lookout and Signal Post permanently
manned by personnel of the Chilean Navy, whose main mission is to maintain
the lighthouses on, exercise Naval Control of Shipping in the area and
issue meteorological bulletins every three hours.
4.- Cape Horn’s Current.
The current that flows through the South of the islands located South of
Tierra del Fuego is known as the Cape Horn current and flows to the East
side reaching the meridian of the Diego Ramirez islands.
From this point, this current takes a more inclined direction to
the NE to the Strait of Le Maire and the Estados island, and finally comes
to join the Falkland or Malvinas current.
The strength of the Cape Horn current varies and is
frequently influenced by the prevailing winds.
From observations made in 1910 and in 1927, it was concluded that
this current reaches up to 22 miles per day.
5.- Tidal Currents.
The tidal wave that moves
from the Pacific Ocean rounds Cape Horn and heads to the Atlantic in the
area included between the Falkland islands and the continent.
In the Strait of Le Maire, the tide is produced very
close to high or low tide time in Buen Suceso Bay. The flux current heads to the North and the ebb tide to the
South reaching a speed of 1 to 3 knots.
6.- Presence of
Icebergs.
It is rare to see icebergs in
Cape Horn. However, it is
common to find them in the austral Atlantic Ocean.
They occasionally emerge at the latitude of the Cape and even
further North along the Eastern Patagonian coast eventually reaching
latitude 38°S.
7.- Meteorological
Statistic Data.
According
to statistic information provided by the Meteorological Service of the
Chilean Navy for the period of 1982 - 1999 (19 years), the records provide
the following yearly average values for the Lookout and Signals Post
corresponding to Horn Island
| Average
barometric pressure of the period |
995,14
H.P.A. |
| Average
temperature of the period |
5,3° Celsius |
| Maximum temperature of the
period |
20,5°
Celsius
(Feb. 1996) |
| Minimum
temperature of the period |
-
14,5° Celsius (June
1992) |
| Average
relative humidity of the period |
86.4
% |
| Average
wind direction of the period |
264° |
| Average
maximum intensity of the period |
84
knots |
| Maximum
intensity registered of the period |
119
knots
(Aug. 1995) |
| Precipitation (annual average
of the period) |
697,5
mm. |
| Precipitation of the most
rainy year |
1263.2 (1990) |
8.- Weather.
All explorers and hydrographers that have studied the austral zone, agree
in establishing that spring is the season in which the most violent storms
take place, while wintertime is relatively calm. The average speed of the
wind in spring is actually greater than in winter and its dominant
direction corresponds to the 3° and 4°quadrants. During a year, the
winds of these quadrants have a 75% prevalence.
This
fact, nowadays statistically proved, had already been noticed by Captains
Philip Parker King and Robert Fitz Roy when stating in the "Sailing
Directions for South America of the year 1850" that: "The winds
of the west prevail during major part of the year", referring to the
Cape Horn area, and furthermore indicating that: "the months of
August, September, October and November are the worst of all in rounding
Cape Horn", adding that: "the best weather is shown in March,
April, May and June, in spite of the fact that daylight is shorter and the
average temperatures very low, they it is the best period for vessels to
round the Cape in west direction. Even
more, the presence of the east wind in these months is more frequent.
The best months to undergo the crossing from the
Pacific to the Atlantic, through Cape Horn, are during the months of
December and January. As it
is an easy and short crossing, there is no need for a previous
planification at the time it is performed.
As
an anecdotal fact, it is necessary to state that the crossing that broke a
record in the time to cross Cape Horn from East to West belongs to the
sailboat SUSANNA in 1905, which took 99 days – from the end
of August to the end of November of the aforementioned year.
The opposite record, the fastest one, was established by the
frigate "PRIWALL" in 1938 during the first week of November.
This event becomes an exception to what is previously mentioned
referring to the worst months in crossing the Cape from East to West.