From marginality to resurgence: the case of the Irish islands

Abstract: The islands off the coast of Ireland declined after the Irish famine of the 1840s. The number inhabited and the size of the population on those that remain populated both fell dramatically, faring worse collectively than the Irish mainland to which they were marginal in every sense. The reasons for this decline are examined. In the early 20th Century there are some signs of resurgence. The article considers that this might be put down to the efforts of islanders themselves, coupled with state and European Union support. There is an interest in and regard for the islands associated with their being seen as repositories of Irish culture and heritage. This has had positive benefits regarding the attitude of the state agencies and also for tourism, which is an important factor in many contemporary island economies. In fact, some of the resurgence as measured by population totals can be put down to people having holiday cottages on the islands rather than an increase in the size of traditional communities.

Postcolonialism and islands: introduction

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Postcolonial Culture on Dependent Islands

This article first considers the significance of historical experience in academic studies, including postcolonial studies, concluding with Jane M. Jacobs that “the structures of power that gave rise to empire live on in a more disorganised fashion.” They live on in an organized way, too, in that many islands remain in a colonial relationship, being simultaneously colonial and postcolonial, although having tended “to slip the net of postcolonial theorising.” The article attempts to help fill this gap, especially through consideration of Brian Rourke’s ideas on cultural imposition applied to dependent islands and through investigation of why some islands have not progressed to independence. Case study detail is presented, especially for Bermuda and the Falkland Islands.

Revised age estimate of the Mjauvotn tephra A on the Faroe Islands based on Bayesian modelling of C-14 dates from two lake sequences

Tephra horizons are potentially perfect time markers for dating and cross-correlation among diverse Holocene palaeoenvironmental records such as ice cores and marine and terrestrial sequences, but we need to trust their age. Here we present a new age estimate of the Holocene Mjauvotn tephra A using accelerator mass spectrometry C-14 dates from two lakes on the Faroe Islands. With Bayesian age modelling it is dated to 6668-6533 cal. a BP (68.2% confidence interval) - significantly older and better constrained than the previous age. Copyright (C) 2010 John Wiley & Sons, Ltd.

Evaluation of effective groundwater recharge of freshwater lens in small islands by the combined modeling of geoelectrical data and water heads

In small islands, a freshwater lens can develop due to the recharge induced by rain. Magnitude and spatial distribution of this recharge control the elevation of freshwater and the depth of its interface with salt water. Therefore, the study of lens morphology gives useful information on both the recharge and water uptake due to evapotranspiration by vegetation. Electrical resistivity tomography was applied on a small coral reef island, giving relevant information on the lens structure. Variable density groundwater flow models were then applied to simulate freshwater behavior. Cross validation of the geoelectrical model and the groundwater model showed that recharge exceeds water uptake in dunes with little vegetation, allowing the lens to develop. Conversely, in the low-lying and densely vegetated sectors, where water uptake exceeds recharge, the lens cannot develop and seawater intrusion occurs. This combined modeling method constitutes an original approach to evaluate effective groundwater recharge in such environments.
[Comte, J.-C., O. Banton, J.-L. Join, and G. Cabioch (2010), Evaluation of effective groundwater recharge of freshwater lens in small islands by the combined modeling of geoelectrical data and water heads, Water Resour. Res., 46, W06601, doi:10.1029/2009WR008058.]

Assessing spatio-temporal patterns of groundwater salinity in small coral islands in the Western Indian Ocean

We investigated groundwater salinity as a key element in both the short and long-term evolution of the island of Grande Glorieuse. Firstly, we demonstrated that its evolution involved the integration of the whole range of variables forcing climate change. Piezometric surveys designed to sample the salinity of the subsoil waters of Grande Glorieuse could therefore provide an objective indicator of the environment’s evolution. Then, based on information from geoelectrical investigations, we proved that the spatial distribution of salinity is strongly dependent on the geological structure of the island. Structural heterogeneities can influence vulnerability of the island environment to salinization of the freshwater lens. Thus, characterization and monitoring of the freshwater lens will provide a reliable means of observing and managing anticipated climate changes on small islands. [Join J.-L., Banton O., Comte J.-C., Leze J., Massin F., Nicolini E. (2011), Assessing spatio-temporal patterns of groundwater salinity in small coral islands in the Western Indian Ocean, Western Indian Ocean Journal of Marine Science, 10(1), 1-12]