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Literatura académica sobre el tema "Faroe Islands"

Autor: Grafiati

Publicado: 4 de junio de 2021

Última modificación: 26 de enero de 2023

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Artículos de revistas sobre el tema "Faroe Islands"

Adler-Nissen, Rebecca. "The Faroe Islands". Cooperation and Conflict 49, n.º 1 (10 de enero de 2014): 55–79. http://dx.doi.org/10.1177/0010836713514150.

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Joensen, Poul. "The Faroe Islands". Practical Neurology 15, n.º 4 (3 de febrero de 2015): 323–26. http://dx.doi.org/10.1136/practneurol-2015-001085.

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HANSEN, LEIVUR JANUS y GÍSLI MÁR GÍSLASON. "Trichoptera in the Faroe Islands". Zoosymposia 18, n.º 1 (12 de junio de 2020): 127–34. http://dx.doi.org/10.11646/zoosymposia.18.1.16.

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In this paper the literature on Trichoptera in the Faroe Islands is reviewed and occurrence of species in recent research on freshwater insects is added. The first record of Trichoptera dates from 1782, without any recognisable species. Today, 20 species are known from the islands, but their frequency of occurrence differs between the Northern Islands and the other islands. A difference in topography of the island groups has previously been hypothesized as an explanation, and data presented in this paper support this hypothesis.

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Weihe, P. y P. Grandjean. "FAROE ISLANDS PROSPECTIVE COHORTS". Epidemiology 16, n.º 5 (septiembre de 2005): S139. http://dx.doi.org/10.1097/00001648-200509000-00352.

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Gaini, Firouz. "Altered Islands: Young Faroe Islanders’ Future Landscapes". Suomen Antropologi: Journal of the Finnish Anthropological Society 43, n.º 4 (21 de julio de 2019): 3–18. http://dx.doi.org/10.30676/jfas.v43i4.73270.

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This paper explores scenarios created by young Faroe Islanders reflecting on the future of their local community and islands. The main objective is to outline and analyse the dynamic relationship between young people’s future images and present-day realities. Based on data from an ethnographic study from 2014, the paper discusses young people’s future-oriented essays in relation to their islands’ history, culture, and values. The essays, as methodological schemes, encourage the youth to draw a ‘future landscape’ without necessarily linking it directly to their personal (intimate) perspectives. They offer an opportunity to discuss the relation between micro- and macro-level events and between material and cultural shifts. In these narratives, we notice a strong commitment to connect the future to the past in a collective Faroese project. The future is often drawn as altered islands—a mesmerizing breakaway from present-day realities. The opportunity to dream and to imagine tomorrow is an important part of young people’s everyday life practices and identities.

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Ackrén, Maria. "The Faroe Islands: Options for Independence". Island Studies Journal 1, n.º 2 (2006): 223–38. http://dx.doi.org/10.24043/isj.195.

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The Faroe Islands are currently at a crossroads in their constitutional status. Discussions concerning changes in the current constitutional status are ongoing and several analyses about possible trajectories of future development are being proposed. Argued in a context of Faroese nationalism, this article tries to assess these trajectories in the future jurisdictional and political development of the Faroe Islands in terms of three possible scenarios: independence or full sovereignty (as is Iceland); a freely associated statehood (as are Niue and the Cook Islands in relation to New Zealand); or a confederation, probably involving changes at both the central level of the Danish state and the European Union level. This article argues that the most likely future development is that of a state in free association with Denmark. Meanwhile, island politics can change very quickly and the traditional cleavages in Faroese politics are liable to changing degrees of public support.

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Mikkelsen, Bjarni. "A note on the harbour seal (Phoca vitulina) in the Faroe Islands". NAMMCO Scientific Publications 8 (1 de septiembre de 2010): 143. http://dx.doi.org/10.7557/3.2681.

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The harbour seal was exterminated as a breeding species in the Faroe Islands in the mid-19th Century. Historical sources document that the harbour seal used to be a common inhabitant of the sheltered fjords where breeding occurred. It was reported to be more common than the grey seal, the other pinniped specie resident around the Faroes. But the number of harbour seals seemingly decreased as human settlements and other anthropogenic activities increased. Seal hunting was apparently already introduced by the Norse that arrived on the islands in the 7th century, a hunt that finally lead to the extermination of the harbour seal. For the last 40 years the harbour seal has only been positively identified twice in the Faroe Islands, in 2001 and 2005.

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Jørgensen, Ole. "The regional distribution of zeolites in the basalts of the Faroe Islands and the significance of zeolites as palaeotemperature indicators". Geological Survey of Denmark and Greenland (GEUS) Bulletin 9 (31 de mayo de 2006): 123–56. http://dx.doi.org/10.34194/geusb.v9.4865.

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The first maps of the regional distribution of zeolites in the Palaeogene basalt plateau of the Faroe Islands are presented. The zeolite zones (thomsonite-chabazite, analcite, mesolite, stilbite-heulandite, laumontite) continue below sea level and reach a depth of 2200 m in the Lopra-1/1A well. Below this level, a high temperature zone occurs characterised by prehnite and pumpellyite. The stilbite-heulandite zone is the dominant mineral zone on the northern island, Vágar, the analcite and mesolite zones are the dominant ones on the southern islands of Sandoy and Suðuroy and the thomsonite-chabazite zone is dominant on the two northeastern islands of Viðoy and Borðoy. It is estimated that zeolitisation of the basalts took place at temperatures between about 40°C and 230°C. Palaeogeothermal gradients are estimated to have been 66 ± 9°C/km in the lower basalt formation of the Lopra area of Suðuroy, the southernmost island, 63 ± 8°C/km in the middle basalt formation on the northernmost island of Vágar and 56 ± 7°C/km in the upper basalt formation on the central island of Sandoy. A linear extrapolation of the gradient from the Lopra area places the palaeosurface of the basalt plateau near to the top of the lower basalt formation. On Vágar, the palaeosurface was somewhere between 1700 m and 2020 m above the lower formation while the palaeosurface on Sandoy was between 1550 m and 1924 m above the base of the upper formation. The overall distribution of zeolites reflects primarily variations in the maximum depth of burial of the basalt rather than differences in heat flow. The inferred thinning of the middle and upper basalt formation from the central to the southern part of the Faroes is in general agreement with a northerly source area for these basalts, centred around the rift between the Faroes and Greenland. The regional zeolite distribution pattern is affected by local perturbations of the mineral zone boundaries that reflect local differences in the temperature, perhaps related to the circulation of water in the underground. The zonal distribution pattern suggests that these temperature anomalies are in part related to NW–SE-trending eruption fissures or zones of weakness separating the present islands and are subparallel to transfer zones in the Faroe–Shetland Basin. Both the regional and the local distribution of zeolite assemblages are probably a reflection of the basic volcanic-tectonic pattern of the Faroe Islands.

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Jemec, Gregor B. E., Michael Heidenheim, Tomas N. Dam y Edith Vang. "Teledermatology on the Faroe Islands". International Journal of Dermatology 47, n.º 9 (septiembre de 2008): 891–93. http://dx.doi.org/10.1111/j.1365-4632.2008.03718.x.

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Jakobsen, Linda P., Kirsten Mølsted y Kaare Christensen. "Occurrence of Cleft Lip and Palate in the Faroe Islands and Greenland from 1950 to 1999". Cleft Palate-Craniofacial Journal 40, n.º 4 (julio de 2003): 426–30. http://dx.doi.org/10.1597/1545-1569_2003_040_0426_ooclap_2.0.co_2.

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Objective To describe the occurrence of cleft lip with or without cleft palate (CL/P) and isolated cleft palate (CP) in the Faroe Islands and Greenland over a 50-year time period that has included substantial changes in lifestyle. Design A prevalence study based on patient records obtained from the Institute of Speech and Hearing Disorders in Copenhagen, Denmark, at which the treatment of patients with CP and CL/P from Greenland, the Faroe Islands, and Denmark is coordinated. Participants All live-born children in the Faroe Islands, Greenland, and Denmark with CL/P or CP born in the period 1950 to 1999 (Faroe Islands and Greenland) and 1950 to 1987 (Denmark). Results and Conclusion The mean prevalence of CL/P in the Faroe Islands and Greenland during the period 1950 to 1999 was 1.0 and 0.6 per 1000 live births, respectively. This is significantly lower than the mean prevalence of 1.4 (p < .05 and p < .001) per 1000 live births found in Denmark. The mean prevalence of CP in the Faroe Islands and Greenland was 1.5 and 1.1 per 1000 live births, respectively, which is significantly higher than the Danish prevalence of 0.5 per 1000 live births (p < .001 in both tests). There was no clear time trend in the prevalence, indicating that genetic factors or timetable environmental factors play a dominating role in the etiology of CL/P and CP in the Faroe Islands and Greenland.

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Tesis sobre el tema "Faroe Islands"

Richardson, Kristina Ruth. "Crustal structure around the Faroe Islands". Thesis, University of Cambridge, 1998. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.624800.

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Schuler, Juerg. "Seismic wave propagation through flood basalts and stratigraphic correlation on the Faroes shelf". Thesis, University of Cambridge, 2013. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.648372.

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Fängström, Britta. "Human exposure to organohalogen compounds in the Faroe Islands". Doctoral thesis, Stockholm University, Department of Environmental Chemistry, 2005. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-428.

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The Faroe Islands in the North Atlantic are part of the sub-Arctic region, a remote region far from industrial activity. In spite of this remoteness, the Islands are not a sanctuary: exposures and effects of environmental pollutants mar its natural beauty and wildlife. In the Arctic regions, fish, sea mammals and seabirds have shown to contain elevated levels of the classical persistent organic pollutants (POPs) such as polychlorinated biphenyls (PCBs), as well as more recent POPs such as the polybrominated diphenyl ethers (PBDEs). Human populations living in the Arctic regions are usually highly dependent on seafood and seabirds as food sources, and diet becomes their major source of exposures to POPs. As reported in the 1980’s, residents of the Faroe Islands were shown to have high concentrations of organohalogen substances (OHS) in their breast milk. Long-finned pilot whales (Globicephala melas) blubber and meat have been shown to be a major source of OHS exposure for some of the Faroe Islanders.

The main objective of this thesis is to investigate the sources and concentrations of some POPs and their metabolites for the Faroese population. First, human milk and serum from pregnant women (mothers) and children were analyzed for PBDEs, PCBs, and polychlorinated biphenylols (OH-PCB), the major PCB metabolites. Second, POPs were measured in seabirds, i.e. PCBs in fulmars (Fulmarus glacialis) and guillemots (Uria algae), and PBDEs in fulmars to search for other potential sources of POPs exposure.

The results reinforce previous findings that part of the Faroe Island population is highly exposed to OHS. Median concentrations (430 ng/g lipid weight (l.w.) of CB-153) in maternal serum (1994-95) are among the highest in the world. Serum concentrations of CB-153 in children (age 7, samples collected in the early 2000’s) were approximately 90% of those in the mothers, sampled 1994-95. Similarly high CB-153 concentrations (380 ng/g l.w.) were measured in samples of mother’s milk, collected in 1999. The OH-PCB concentrations were also high in segments of the population, with 2.9 ng/g fresh weight as the sum of five OH-PCBs. Except for 4-OH-CB107, concentrations of OH-PCBs were generally lower in children than in mothers.

The ΣPBDE median concentrations in maternal serum and human milk (1999) are at the higher end of those reported in Europe, with levels of 9.5 and 8.2 ng/g l.w. respectively. ΣPBDE levels increase in human milk samples collected at three different time points (1987-1999), mainly due to increasing BDE-153 concentrations. The range of serum ΣPBDE concentrations in mothers and children are similar, although the congener patterns show differences. BDE-47 is the dominant congener in maternal serum, while BDE-153 is the major congener in children. The differences seen in PBDE congener patterns may arise differences in dates of sampling (7 years) for the two populations, maternal serum sampled in 1994-95 and children serum sampled in 2000-01, rather than from differences in uptake/metabolism or in contemporary exposures.

PCB concentrations in fulmars and pilot whales show similar ranges. In contrast, PBDE concentrations are 100 times higher in pilot whales than in fulmars. Consequently, Faroese may be especially exposed to PCBs via consumption of fulmars and fulmar eggs, while the exposure to PBDEs is less pronounced.

Results from this thesis highlight the pronounced exposures to PCBs, OH-PCBs, and PBDEs among residents of the Faroe Islands, a remote region in the Northern Atlantic far away from industrial and urban sources of pollution.

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Fängström, Britta. "Human exposure to organohalogen compounds in the Faroe Islands /". Stockholm : Department of environmental chemistry, Stockholm university, 2005. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-428.

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Mitchinson, J. "Danish in the Faroe Islands : a post-colonial perspective". Thesis, University College London (University of London), 2012. http://discovery.ucl.ac.uk/1348494/.

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This thesis examines from a post-colonial perspective the position of the Danish language in Faroese society. It aims to demonstrate that post-colonial theory, which originally emerged as a methodology for literary analysis in the 1970s, offers a framework by which very different post-colonial linguistic scenarios, such as those in the Faroes and Greenland, can be analysed, compared and contrasted. In addition to established ideas within post-colonialism, from scholars such as Althusser and Spivak, three new concepts – saming, language othering and linguistic autonomy – are developed and used in the analysis of linguistic developments that have taken place on the islands since Danish was introduced. It is argued that the colonial history of the Faroes provides the most rewarding perspective for such an examination. Recurrent themes in language research on the islands, both historical and contemporary, such as Gøtudanskt, are contextualised within the post-colonial framework. Similarly, topics which have received little academic attention, such as the role of the heavily Danish-influenced Suðuroy dialect, are also analysed from this perspective. A considerable part of the investigation stems from field research (predominantly questionnaires). The thesis suggests that the Faroes constitute an atypical case within post-colonial studies due to the common cultural/linguistic heritage of the coloniser and the colonised. However, the non-standard characteristics of post-colonial Faroese society can only be fully appreciated in comparison with a ‘typical’ post-colonial society, and Greenland is proposed as this standard example. The final chapter therefore provides a comparative study between the language situations in the two societies. In addition to the introductory and concluding sections, the thesis contains five chapters, which deal with the following: theory and methodology; colonisation and the cementing of Danish into Faroese society; the field research; decolonisation and the reassessment of the position of Danish in Faroese society; and the afore-mentioned comparative study.

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Walker, Richard James. "The structural evolution of the Faroe Islands, NE Atlantic Margin". Thesis, Durham University, 2010. http://etheses.dur.ac.uk/134/.

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The NE Atlantic margin plays host to numerous basins, developed in phases from the Devono-Carboniferous through to the Cenozoic, which record the build up to plate separation and formation of the North Atlantic Ocean. Existing models for this invoke broadly NW-SE extension within the basins, which are segmented by regional-scale NW-SE trending strike-slip lineaments, which are commonly termed ‘transfer zones’. However, there is a general paucity of information concerning the true kinematics of the so-called transfer zones. In this study, the Palaeogene and later structural evolution of the NE Atlantic margin is investigated using abundant field data collected on the Faroe Islands, and systematic observations that characterise the related deformation structures developed in the Faroe Islands Basalt Group (FIBG). Structures in the Faroe Islands provide evidence for a 6-stage tectonic evolution, here split into 3 broad phases: (1a) E-W to NE-SW extension, accommodated by dip-slip N-S and NW-SE trending faults. Continued NE-SW extension (1b) was then accommodated by the emplacement of a regionally significant NW-SE- and NNE-SSW-oriented dyke swarm. Event 1 affects the majority of the FIBG stratigraphy, resulting in thickness variations, most notably across the Judd, Brynhild and Westray (‘transfer’) fault-zones. Continued magmatism and anticlockwise rotation of the extension vector led to (2a) the emplacement of ENE-WSW and ESE-WNW conjugate dykes, followed by intrusion of the large, saucer-shaped sills on the islands. Their intrusion heralded the onset of N-S crustal extension and was followed by (2b) crustal extrusion involving both E-W shortening and further N-S extension facilitated primarily by slip on ENE-WSW (dextral) and ESE-WNW (sinistral) conjugate strike-slip faults, interlinked with minor NE and SW dipping thrust faults. During the final stages of this event (2c), the regional extension vector rotated into a NW-SE orientation that was accommodated predominantly by slip along NE-SW oriented dextral-oblique-slip faults. Event 2 began towards the end of magmatism associated with the FIBG, and most likely continued through to the onset of oceanic-spreading on the Aegir ridge (ca. 55 Ma). Finally, (3) Event 1 and 2 structures were reactivated as extension and extensional-hybrid features, characterised best by the entrainment of clastic material along fault planes. Relative timings of Event 3 structures suggest they formed during a period of compression and uplift following the formation of a through-going mid-ocean ridge system (i.e. on the Reykjanes, Kolbeinsey and Mohns ridges). The progressive anticlockwise rotation of the extension vector identified here is broadly consistent with the most recent NE Atlantic continental break-up reconstructions. Importantly, this model does not require basin-scale transfer zones during the Palaeogene, suggesting instead that these NW-SE faults formed as normal faults during a pre-cursor margin-parallel extension episode (Event 1) prior to the onset of oceanic spreading in the Faroe-Iceland sector. This study emphasises the importance of carrying out detailed field studies in addition to the more usual regional-scale modelling studies, in order to validate and add further detail to basin kinematic histories. Mineralised syn- to post-magmatic fault sets display a recurring zeolite-calcite-zeolite trend in mineralisation products, which precipitate during successive phases of fault development during each individual event. Fault style and damage zone width appear to be related to the stage of fault development, with early fault/vein meshes linking to form through-going structures with associated damage zones. Dykes and sills are found to form their own fractures, rather than exploiting pre-existing sets. Dyke propagation appears to be buoyancy-driven, with magmatic pressure overcoming the minimum compressive stress. Sills, however, most likely seeded at an interface in the stratigraphy between a weak, more ductile material (i.e. a sedimentary horizon), and a rigid material (i.e. basalt lavas) above. Following this initial development, sill growth and propagation would likely be controlled by viscous dissipation, leading to the complex ramp and flat architecture, with rapid intrusion resulting in upward ramping of the sill. The alternation from fault events, to dyke events and back again corresponds to a switch from faulting with mineralisation along extensional hybrid veins, to magmatic intrusions into extension fractures followed by extensional hybrids (conjugates), and back to extensional and shear hybrid faults (again as conjugates). This alternation reflects variations in the differential regional stress, as well as the magmatic evolution of the margin, and most likely relates to the migration of lithospheric thinning northwestwards across the area, towards the eventual axis of break-up. We find that, in particular, faults in basalts are in many ways comparable to faults formed at shallow crustal depths in carbonate rocks and crystalline basement, most likely reflecting the similarities in their mechanical properties under near-surface pressures and temperatures. The nature and style of the post-magmatic fault infills provides compelling evidence to suggest that subterranean cavities associated with faults were persistent open features within the FIBG. Structures equivalent to these late, clastic-filled faults of the Faroes may occur in other parts of the NE Atlantic margin, particularly along the axes of gentle regional-scale folds that are widely developed in the region. The late fault displacements observed are all well below seismic resolution, and such structures may be more widespread across the region than previously anticipated. Importantly, the probable unsealed nature of the clastic infills makes them potential fluid-migration pathways, both up- and across-faults within the Cenozoic volcanic sequences of the NE Atlantic region.

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Fischer, Frances J. "A comparison of ballads in Scotland and the Faroe Islands". Thesis, University of Edinburgh, 2000. http://hdl.handle.net/1842/22215.

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That Scandinavian ballads are somewhat similar to Scottish ballads is one of the standard beliefs of ballad study. Yet another is that ballads diffuse across geographic and linguistic frontiers. This thesis seeks to examine these tenets in terms of examples from the Faroe Islands and from Scotland. The Faroe Islands are chosen for geographic and linguistic reasons. Although they are a dependency of Denmark, they lie geographically much closer to Scotland. Since they shared a West Scandinavian language with the Scottish islands of Shetland and Orkney for almost a thousand years these islands are considered as a possible cultural bridge between the Scottish and Faroese ballad communities. The organisation of material is in terms of the history of a shared culture and language with examples of surviving Norn ballad texts from the Shetland Islands and possible parallels in Scotland and Scandinavia; a brief overview of continued contact after the political separation of 1468-69; a comparative history of ballad collection; a summary of ballads deemed to be parallel and a deeper examination of selected ballad pairs. Since the extensive Faroese ballad corpus is little known in Scotland, considerable attention is also given to the different types of Faroese ballads and their function in tradition.

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Lunnon, Zoë Clare. "Seismic survey of the continental margin northeast of the Faroe Islands". Thesis, University of Cambridge, 2005. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.615253.

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Lewis, Olivia Jane. "Investigations of crustal structure at the Faroes continental margin using multi-channel seismic and ocean bottom seismometer data". Thesis, University of Cambridge, 2013. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.607912.

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Lind, Ewa. "Towards an Early Holocene Tephrochronology for the Faroe Islands: Methodology and first results". Licentiate thesis, Stockholms universitet, Institutionen för naturgeografi och kvartärgeologi (INK), 2011. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-62890.

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The uncertainties regarding future climate change have put considerable notice to the climate variability following the Late Glacial-Holocene transition (ca. 13-9 ka BP) in the North Atlantic region as well as the forcing mechanisms behind climate changes. Much attention has focused on short climate events in order to understand the mechanisms that drove these changes but also to identify the leads and lags in the climate system. Chronological uncertainties for these events remain but an accurate chronological framework for the North Atlantic region would enhance possibilities to solve some of the chronological questions. Tephrochronology uses volcanic ash from a volcanic eruption which creates a marker horizon in marine and lake sediments, peat bogs and glacier ice as the ash is spread over large areas. These time-parallel markers allow precise correlations between archives. The purpose of this thesis is to improve and refine the Early Holocene tephrochronological framework with focus on dating and identification of new and previously known tephra horizons on the Faroe Islands, especially around the climatic events of the Preboreal Oscillation (11,300-11,100 cal. yr BP), the Erdalen events (10,100-10,050 and 10,000-9800 cal. yr BP) and the 9.3 ka BP event. A second goal is to develop the methodology of tephrochronology for finding cryptotephra (not visible by the eye) horizons in lacustrine sediments. The findings of eight tephra horizons spanning ca. 11,350 to 9700 cal yr BP where three are known from other locations in Europe show the potential of tephrochronology for linking records across the North Atlantic region. Refined ages for the Askja-S and Hässeldalen tephra were obtained from an age model built on eight AMS radiocarbon ages with the Saksunarvatn ash as a constrained age. The results from using XRF ITRAX core scanner to locate tephra in lacustrine sediments illustrate that high concentrations of basaltic tephra could be captured but not lower concentrations of rhyolitic shards.

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Libros sobre el tema "Faroe Islands"

Gunnie, Moberg y Patursson Tróndur 1944-, eds. The Faroe Islands. Edinburgh: Birlinn, 2002.

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Hróarsson, Björn y Henrik Solberg. Faroe Islands today. Kópavogur, Iceland: Printskill, 2008.

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The Faroe Islands: Interpretations of history. Lexington, Ky: University Press of Kentucky, 1987.

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Helmsdal, Mikkjal. Landsverkfrøðingsstovnurin 50 ár. Tórshavn: Landsverkfrøðingurin, 1998.

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International, KPMG. Investment in the Faroe Islands. Tórshavn, Faroe Islands]: KPMG, 1999.

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Brot úr Føroya søgu. Tórshavn: Fróðskapur, 2010.

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Fredriksen, Ólavur. 150 impressions of the Faroe Islands. Torshavn: Egid, 2014.

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Nauerby, Tom. No nation is an island: Language, culture and national identity in the Faroe Islands. Arhus, Denmark: SNAI-North Atlantic Publications, 1996.

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Reistrup, Høgni. Valið og valdið: Ein tvørskurður av løgtingsvalinum 2011. Vestmanna, Faroe Islands]: Sprotin, 2011.

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Tíðarkjarr: Hugleiðingar. [Nivå, Denmark]: Mentunargrunnur Studentafelagsins, 1998.

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Capítulos de libros sobre el tema "Faroe Islands"

Sroka, Wendelin. "Faroe Islands". En The Education Systems of Europe, 251–53. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-07473-3_15.

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Pieters, Danny. "Faroe Islands". En Social Security Law in Small Jurisdictions, 95–104. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-78247-4_7.

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Siaroff, Alan. "Faroe Islands". En Comparative European Party Systems, 229–34. Second edition. | New York : Routledge, 2019.: Routledge, 2018. http://dx.doi.org/10.4324/9781315713694-17.

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Ax, P. "Brackish-water Plathelminthes from the Faroe Islands". En Biology of Turbellaria and some Related Flatworms, 45–47. Dordrecht: Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-011-0045-8_8.

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Leivsson, Tróndur G. "Potential Tree Line in the Faroe Islands". En Forest Development in Cold Climates, 463–74. Boston, MA: Springer US, 1993. http://dx.doi.org/10.1007/978-1-4899-1600-6_31.

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Reigner, Nathan, Gestur Hovgaard y Firouz Gaini. "Greenland, the Faroe Islands, and Chinese tourism". En Asian Mobilities Consumption in a Changing Arctic, 56–70. London: Routledge, 2021. http://dx.doi.org/10.4324/9781003039518-7.

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Vijayavarathan-R, Kalpana. "Policy Equity Contexts in Inclusive Education for Immigrant Children in the Faroe Islands". En Springer Polar Sciences, 79–96. Cham: Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-030-97460-2_6.

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AbstractThe aim of this chapter is to examine whether policies on integration and education in The Faroe Islands are fit-for-purpose when viewed from dual lenses: the acknowledgement of the importance of ethnic cultural identity and heritage language (first language/mother tongue) of immigrant children and their inclusion through education towards integration in The Faroe Islands. The focus is on whether existing policies consider the pivotal relationship between language and identity in education for second generation immigrant children and immigrant children in compulsory schools, i.e., grades 1 to 9 to ensure that they have agency in Faroese society.

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Sørensen, Nicolina y Marianne Schwartz. "Incidence of Cystic Fibrosis at the Faroe Islands". En Advances in Experimental Medicine and Biology, 403–4. Boston, MA: Springer US, 1991. http://dx.doi.org/10.1007/978-1-4684-5934-0_50.

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Armstrong, Justin. "On Becoming an Ethnographic Ghost in the Faroe Islands". En Anthropology, Islands, and the Search for Meaning in the Anthropocene, 20–25. London: Routledge, 2022. http://dx.doi.org/10.4324/9781003297581-3.

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Bonté, Rosalind. "Conversion and Coercion: Religious Change in the Faroe Islands". En Medieval Identities: Socio-Cultural Spaces, 93–116. Turnhout: Brepols Publishers, 2014. http://dx.doi.org/10.1484/m.miscs-eb.1.102034.

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Actas de conferencias sobre el tema "Faroe Islands"

Alá’i, Riaz y Eric Verschuur. "Aiming towards imaging beneath basalt : multiple suppression offshore Faroe Islands". En 8th International Congress of the Brazilian Geophysical Society. European Association of Geoscientists & Engineers, 2003. http://dx.doi.org/10.3997/2214-4609-pdb.168.arq_500.

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S. Andersen, M., R. Waagstein, L. Kiørboe y L. O. Boldreel. "Late Cretaceous - Early tertiary tectonics and volcanism around the Faroe Islands". En 58th EAEG Meeting. Netherlands: EAGE Publications BV, 1996. http://dx.doi.org/10.3997/2214-4609.201408985.

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Peace, David G., James Schofield, Arnold Orange, Raffaele Servodio, Ron Lansdell y Mark Woodfin. "Marine magneto‐telluric exploration helps unravel secrets of the Faroe Islands". En SEG Technical Program Expanded Abstracts 2002. Society of Exploration Geophysicists, 2002. http://dx.doi.org/10.1190/1.1817322.

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Mushlitz, Emily B., Nicholas L. Balascio, William J. D'Andrea y Raymond S. Bradley. "AN 8000-YEAR RECORD OF CLIMATE AND ENVIRONMENTAL CHANGE FROM LAKE SANDSVATN, FAROE ISLANDS". En 68th Annual GSA Southeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019se-326727.

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Simonsen, Hilmar y Egon Nørmark. "Recognition of intra‐basaltic horizons from challenging marine seismic data in the Faroe Islands". En SEG Technical Program Expanded Abstracts 2009. Society of Exploration Geophysicists, 2009. http://dx.doi.org/10.1190/1.3255471.

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Shaw, F., M. H. Worthington, M. S. Andersen y U. K. Petersen. "A Study of Seismic Attenuation in Basalt Using VSP Data from a Faroe Islands Borehole". En 66th EAGE Conference & Exhibition. European Association of Geoscientists & Engineers, 2004. http://dx.doi.org/10.3997/2214-4609-pdb.3.p015.

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Beyer, Hans-Georg. "Layout of island power supply based on multi-decadal meteorological sets - discussed using the case of the Faroe Islands power system". En EuroSun 2020. Freiburg, Germany: International Solar Energy Society, 2020. http://dx.doi.org/10.18086/eurosun.2020.12.03.

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Varming, T. y F. P. Dalsgarð. "The Use of the CVES Method in a Basaltic Environment - A Case Study from the Faroe Islands". En Near Surface 2006 - 12th EAGE European Meeting of Environmental and Engineering Geophysics. European Association of Geoscientists & Engineers, 2006. http://dx.doi.org/10.3997/2214-4609.201402701.

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Heincke, B., M. Jegen, M. Moorkamp y R. W. Hobbs. "Joint-inversion of magnetotelluric, gravity and seismic data to image sub-basalt sediments offshore the Faroe-Islands". En SEG Technical Program Expanded Abstracts 2014. Society of Exploration Geophysicists, 2014. http://dx.doi.org/10.1190/segam2014-1401.1.

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Eidesgaard, O. "Shallow Geothermal Energy System in Fractured Basalt; A Case Study From Kollafjør∂ur, Faroe Islands, NE-Atlantic Ocean". En EAGE/BVG/FKPE Joint Workshop on Borehole Geophysics and Geothermal Energy. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201903163.

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Informes sobre el tema "Faroe Islands"

Kukushkina, Nataliya. Political administrative map of Faroe Islands. Editado por Nikolay Komedchikov, Alexandr Khropov y Larisa Loginova. Entsiklopediya, noviembre de 2015. http://dx.doi.org/10.15356/dm2016-12-12-3.

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Ormstrup Vestergård, Louise y Lars Johan Rustad. Food self-sufficiency in five Nordic island societies. Nordregio, agosto de 2022. http://dx.doi.org/10.6027/pb2022:4.2001-3876.

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Increasing food self-sufficiency means rethinking global supply chains, (re-)adapting to local contexts, and ensuring optimal conditions for selling and buying locally produced food. Increased self-sufficiency and improved local food systems can have positive environmental, social, and economic consequences. However, whether increased self-sufficiency adds to more sustainable food systems depends on myriad factors, including production methods, the type of food in question, and the availability of local food on the local market. Previous research shows that local food production does not automatically equate to sustainable food production. This project sought to increase knowledge of how greater food self-sufficiency can contribute to increased sustainability and resilience in the food systems of five Nordic island societies: Bornholm, the Faroe Islands, Greenland, Iceland, and Åland.

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