Loss of the Steamship "Titanic"Great Britain. Court to investigate loss of steamship "Titanic"
History
Loss of the Steamship "Titanic"
Great Britain. Court to investigate loss of steamship "Titanic"
Shipwrecks; Titanic (Steamship)
An examination of the North Atlantic route chart shows that this track
passes about 25 miles south (that is outside) of the edge of the area
marked "field ice between March and July," but from 100 to 300 miles to
the northward (that is inside) of the dotted line on the chart marked,
"Icebergs have been seen within this line in April, May, and June."
That is to say, assuming the areas indicated to be based on the
experience of many years, this track might be taken as passing clear of
field ice under the usual conditions of that time of year, but well
inside the area in which icebergs might be seen.
It is instructive here to remark that had the "turning point" been in
longitude 45° W. and latitude 38° N., that is some 240 miles to the
south-eastward, the total distance of the passage would only have been
increased by about 220 miles, or some 10 hours' steaming for a 22-knot
ship. This is the route which was provisionally decided on by the great
trans-Atlantic companies subsequent to the _Titanic_ disaster.
It must not be supposed that the lane routes referred to had never been
changed before. Owing to the presence of ice in 1903, 1904, and 1905
from about early in April to mid-June or early in July, westward-bound
vessels crossed the meridian of 47° W. in latitude 41° N., that is 60
miles further south than the then accepted track.
The publications known as "Sailing Directions," compiled by the
hydrographic office at the Admiralty, indicate the caution which it is
necessary to use in regions where ice is likely to be found.
The following is an extract from one of these books, named "United
States Pilot (East Coast)," Part I (second edition, 1909, p. 34),
referring to the ocean passages of the large trans-Atlantic mail and
passenger steamers:
To these vessels one of the chief dangers in crossing the Atlantic
lies in the probability of encountering masses of ice, both in the
form of bergs and of extensive fields of solid compact ice,
released at the breaking up of winter in the Arctic regions, and
drifted down by the Labrador current across their direct route. Ice
is more likely to be encountered in this route between April and
August, both months inclusive, than at other times, although
icebergs have been seen at all seasons northward of the parallel of
43° N., but not often so far south after August.
Public-domain text, read in full here on John Shaqi.
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