The tragedy of the “unsinkable” Titanic
– lost in the cold water of the Atlantic – became part of history and
pop culture, but the story of the main culprit that caused the disaster
is mostly forgotten and only vague descriptions and some photos exists
of the supposed iceberg(s). One famous photography taken from board of the cable ship “Minia“,
one of the first ships to reach the area in search for debris and
bodies, shows a tabular iceberg, an unusual shape for icebergs in the
northern Atlantic. The crew found debris and bodies floating in the
vicinity and the captain assured that this was the only iceberg near the
point of the collision. However most surviving Titanic testimonies
described later the infamous iceberg with a prominent peak or even two.
Fig.1. The moment of the collision according to the sailor Frederick Fleet - one of the two men on duty as lookout in the night of the disaster (after EATON & HAAS 1986).
Fig.2. Journalist Colin Campbell, a passenger of the "Carpathia" - the first ship to approach the scene of the disaster the next morning and save the surviving passengers of the Titanic - described the iceberg for the "New York Tribune" (after EATON & HAAS 1986).
Fig.3.
One of the many icebergs photographed in the morning of April 15, 1912.
The passengers on the ship “Prinz Adalbert”, still unaware of the
disaster of the previous night, reported later to have noted a “red
smear” at the waterline of the white iceberg.
Fig.4. Photography of an iceberg from the cable ship "Minia",
one of the first ships to reach the area in search for debris and
bodies. The crew found debris and bodies floating in the vicinity of the
depicted iceberg and the captain assured that this was the only iceberg
near the scene of the collision (after Titanic & Nautical Resource Center).
Fig.5.
Another iceberg, photographed five days later from board of the German
ship “Bremen”, claimed to be the Titanic iceberg based on the vicinity
to the location of the disaster and the description of the iceberg
according to survivors. An "authentic"
photography of the iceberg that sank theTitanic was worth
a lot of money for the eager press, this also explain why so many photographs of icebergs were taken at the time.
Fig.6. Photography
taken from board of the ship “Birma” of the same iceberg as seen by the
passengers of the “Carpathia” (see also Fig.2.) – the first ship to approach the scene of
the disaster and save the surviving passengers of the Titanic – and
published at the time in the “Daily Sketch”. This iceberg has in fact
some remarkable similarities to the iceberg as described by survivors of
the disaster.
Despite the question if one of the photos shows really the culprit iceberg, the remarkably number of spotted icebergs emphasizes the notion that in 1912 a quite impressive number of these white titans reached such southern latitudes.
Despite the question if one of the photos shows really the culprit iceberg, the remarkably number of spotted icebergs emphasizes the notion that in 1912 a quite impressive number of these white titans reached such southern latitudes.
The icebergs encountered in the North
Atlantic originate mainly from the western coasts of Greenland, where
ice streams deliver large quantities of ice in the fjords which lead to
the Baffin Bay. Every year ten-thousand of small and large pieces of ice drop from the front of the glaciers and are pushed by the West Greenland Current slowly
to northern latitudes, far away from ship routes. Following first the
coast of Greenland this current is diverted by the Canadian coast to the
south, forming the Labrador Current that circumnavigates Newfoundland and delivers the iceberg to the warm Gulf Stream.
A more than 5.000km long journey full of obstacles and incessant
erosion by the sun, the water and the waves. Only estimated 1 to 2% of
large icebergs will, after a period of 1-3 years, reach latitude 45°N,
crossing one of the most important route for ships of the entire
Atlantic Ocean.
Fig.7.
Schematic map of marine currents (blue= cold; red = hot) around
Greenland, probable region of origin (West Greenland) and hypothetical route of the iceberg that hit the Titanic.
Apparently in 1912 icebergs were spotted remarkably often in this region and various hypotheses tried to explain
this “anomaly”. The years before 1912 were characterized by mild
winters in Europe and possibly the northern Atlantic. It was therefore
speculated that the (relative) warm temperatures increased the melting rate and activity of the calving glaciers on Greenland.
Also a strengthened Labrador Current, pushing cold water and icebergs much more to the south, was proposed to explain the ice field that in the cold night 100 years ago forced various ships to stop along the Atlantic route.
Both hypotheses are based on the recorded values of Sea Surface Temperature (see this diagram by the Woods Hole Oceanographic Institution), which show an alternation of a warm and cold period in 1900-1920.
A recent hypothesis – promoted by NG – proposes that an exceptional high tide prevented much of the larger icebergs to run, as normally would happen, on ground along the coasts of Baffin Bay. However considering that this tide occurred just some months before (January 1912) and the average velocity of an iceberg is low (0,7km/h~0,6mph), the Titanic iceberg had to take a straight course to arrive in time for his rendezvous with history – April 14, 1912.
Also a strengthened Labrador Current, pushing cold water and icebergs much more to the south, was proposed to explain the ice field that in the cold night 100 years ago forced various ships to stop along the Atlantic route.
Both hypotheses are based on the recorded values of Sea Surface Temperature (see this diagram by the Woods Hole Oceanographic Institution), which show an alternation of a warm and cold period in 1900-1920.
A recent hypothesis – promoted by NG – proposes that an exceptional high tide prevented much of the larger icebergs to run, as normally would happen, on ground along the coasts of Baffin Bay. However considering that this tide occurred just some months before (January 1912) and the average velocity of an iceberg is low (0,7km/h~0,6mph), the Titanic iceberg had to take a straight course to arrive in time for his rendezvous with history – April 14, 1912.
Based on iceberg counts along the shores
of Labrador and later in the Atlantic, also the year 1912 don’t seem to
be necessarily such an anomalous event, but the disaster raised
considerably the interest (and maybe perception) of the public for
icebergs.
Fig.8. Iceberg counts (estimated before 1912) at 48°N, data compiled from the International Ice Patrol Iceberg Database.
In the days after the disaster bypassing
ships encountered and photographed various icebergs. Some eyewitnesses
claim to have noted red paint on some of them; however there is no
conclusive evidence that one of these spotted white giants is really the
iceberg that sank the Titanic. At least some weeks later the culprit
iceberg, captured by the warm water of the Gulf Stream, melted and
disappeared forever into the Atlantic Ocean.
Bibliography:
EATON, J.P. & HAAS, C.A. (1986): Titanic Triumph and Tragedy. Haynes Publishing: 352
SOUTH, C. et al. (2006): The Iceberg That Sank the Titanic. The Natural World documentary film – BBC
SOUTH, C. et al. (2006): The Iceberg That Sank the Titanic. The Natural World documentary film – BBC
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