Relaunching Titanic: Memory and Marketing in the New Belfast

Relaunching Titanic critically considers the invocation of Titanic heritage in Belfast in contributing to a new ‘post-conflict’ understanding of the city. The authors address how the memory of Titanic is being and should be represented in the place of its origin, from where it was launched into the collective consciousness and unconscious of western civilization.

Relaunching Titanic examines the issues in the context of international debates on the tension between place marketing of cities and other alternative portrayals of memory and meaning in places. Key questions include the extent to which the goals of economic development are congruous with the ‘contemplative city’ and especially the need for mature and creative reflection in the ‘post-conflict’ city, whether development interests have taken precedence over the need for a deeper appreciation of a more nuanced Titanic legacy in the city of Belfast, and what Belfast shares with other places in considering the sacred and profane in memory construction.

While Relaunching Titanic focuses on the conflicted history of Belfast and the Titanic, it will have lessons for planners and scholars of city branding, tourism, and urban re-imaging.

Exhibiting Maritime Histories: Titanic Belfast in the Post-Conflict City

The sinking of the RMS Titanic in 1912 represents one of the most infamous maritime disasters in the history of shipping. Yet despite it entering the public imagination in the decades after its sinking, until recently it has all but been erased from the collective memory of the people of Belfast, the city in which it was built. In a post-conflict context, however, Belfast has begun to re-imagine the role of the ship in the city’s history, most particularly in the re-development of the docklands area and its designation as the Titanic Quarter, and through its landmark project the Titanic Belfast museum. This paper will trace the economic, social and political context from which the Titanic was built, and the role that this played in silencing any very public commemoration of its sinking until after the signing of the Belfast Agreement. The ‘story’ told in the new museum will be analysed from this perspective and will illustrate how the wounds of the Troubles continue to inform the interpretation of the city’s divided past.

Les petits naufragés du "Titanic" / J. Jacquin et A. Fabre ; ouvrage illustré de 65 gravures par G. Dutriac

Collection : Bibliothèque des écoles et des familles

Canada Steamship Lines Ltd. Niagara to the Sea (1923)

Sailing schedule and trip guide for Canada Steamship Lines Limited for the year 1923

Canada Steamship Lines Limited Niagara to the Sea 1917

Sailing schedule and trip guide for Canada Steamship Lines Limited for the year 1917.

Canada Steamship Lines Limited Richelieu and Ontario Division Niagara to the Sea July 1916

Sailing schedule and trip guide for Canada Steamship Lines Limited for July 1916.

Canada Steamship Lines Limited Richelieu (1915)

Sailing schedule and trip guide for Canada Steamship Lines Limited for July 1915.

(Table 2) Production parameters of phytoplankton and some associated parameters in the area of the Titanic Polygon

Studies were carried out mostly in the area of RMS Titanic wreck site (41°44'N, 49°57'W) located above the continental slope and the south of the Grand Banks of Newfoundland. In a period from 18.06 to 24.09.2001 five surveys of production characteristics of surface phytoplankton were conducted over 5-9 days. Mean values of these characteristics obtained during the surveys were 9.2-11.7 mg C/m**3 per day for primary production (C_phs), 0.102-0.188 mg/m**3 for chlorophyll a (C_chls), and 4.44-7.42 mg C/mg chl. a per hour for assimilation number (AN). The main reason for low C_phs variability was a significant inverse relationship (R=-0.66) between AN and C_chls found over the research area. When cold shelf waters dominated in the area (27.07 to 19.08.2001), C_chls values for the slope region (0.125+/-0.031 µg/l) and for the outer shelf (0.130+/-0.040 µg/l) were similar. During strengthening of influence of warmer slope waters within area (from 29.08 to 13.09.2001), C_chls concentration within surface waters of the outer shelf was 0.152+/-0.039 µg/l and exceeded one for the slope region (0.094+/-0.004 µg/l) by factor 1.6. Against the background of low Cchls values, the High values of integral primary production in the water column (510-1010 mg C/m**2 per day) at low C_chls values measured within the area were determined both by high assimilation activity of phytoplankton and by the deep (30-40 m) maximum of primary production. Main reasons for formation of such a maximum were high chlorophyll concentration within the layer of the deep chlorophyll maximum (up to 0.5-2.5 µg/l) and in the relatively high solar irradiance within this layer varying from 1.4 to 8.6% of subsurface PAR.

Zooplankton community within the Titanic Polygon, Northwest Atlantic, summer 2003

In summer 2003 we continued our long-term series of observations over the zooplankton community within the Titanic Polygon (area of the frontal zone of Gulf Stream and the Labrador Current) in the North Atlantic, where interaction of ecosystems of subpolar and warm waters takes place. Depending on hydrological situation occurring in the frontal zone interrelated interannual variations in abundance and biomass of plankton species including Calanus hyperboreus and mesopelagic shrimps of Acanthephyra genus were observed. In different years contribution of two parallel trophic nets passing primarily through the larger and smaller plankters to formation of the community varied. Data on the size structure of population of macroplankton shrimps are presented.