scholarly journals On variation in Faroese verb placement

Nordlyd ◽  
2010 ◽  
Vol 36 (2) ◽  
pp. pp ◽  
Author(s):  
Kristine Bentzen ◽  
Piotr Garbacz ◽  
Caroline Heycock ◽  
Gunnar Hrafn Hrafnbjargarson

<p class="NL-Abstract" style="margin: 0cm 14.2pt 12pt;"><span style="font-size: small;"><span style="font-family: Times;"><span style="mso-ansi-language: EN-GB;" lang="EN-GB">In this paper, we present and discuss results from an investigation of verb placement in modern Faroese in which we collected data from speakers from a number of different dialect areas in the Faroe Islands. Altogether we interviewed 54 informants, aged 15&ndash;67, 29 women and 25 men. Therefore, our study not only investigates the geographical variation claimed to be present in Faroese with respect to verb placement, but also gender and age variation. O</span><span lang="EN-US">ur results indicate that verb movement in non-V2 contexts is no longer commonly available to the speakers of Faroese. However, our results also suggest that verb movement across adverbs like <em style="mso-bidi-font-style: normal;">often</em> and <em style="mso-bidi-font-style: normal;">already</em> tends to be more acceptable than movement across negation and other adverbs like <em style="mso-bidi-font-style: normal;">never </em>and<em style="mso-bidi-font-style: normal;"> undoubtedly</em>. Furthermore, movement of finite auxiliaries generally receives a slightly higher score than movement of finite main verbs. Our results do not show any differences in the judgements of speakers below and above the age of 25. Contrary to Jonas (1996), we find that speakers in the North are, if anything, more likely to accept verb movement than speakers in the South.</span></span></span></p>

Nordlyd ◽  
2009 ◽  
Vol 36 (2) ◽  
pp. pp ◽  
Author(s):  
Øystein Alexander Vangsnes

<p class="MsoNormal" style="margin: 0cm 0cm 0pt;"><span lang="EN-US"><span style="font-family: Cambria; font-size: small;">This paper presents a survey of Faroese <em style="mso-bidi-font-style: normal;">wh</em>-nominals, in particular (i) the <em style="mso-bidi-font-style: normal;">hv&oslash;r N</em> construction, (ii) the <em style="mso-bidi-font-style: normal;">hvat fyri (ein) N</em> construction, and (iii) the <em style="mso-bidi-font-style: normal;">hvat slag av N.<span style="font-variant: small-caps;">dat</span> </em>construction. The first construction involves a <em style="mso-bidi-font-style: normal;">wh</em>-item which is used both pronominally, corresponding to English <em style="mso-bidi-font-style: normal;">who </em>and <em style="mso-bidi-font-style: normal;">what</em>, and adnominally, corresponding to English <em style="mso-bidi-font-style: normal;">which, what (N)</em>, and <em style="mso-bidi-font-style: normal;">what kind of</em>. The second construction is the Faroese version of the <em style="mso-bidi-font-style: normal;">was f&uuml;r/what for</em> construction, including versions with and without an indefinite article and with and without both the preposition (<em style="mso-bidi-font-style: normal;">fyri</em>) and the indefinite article (i.e. a &ldquo;bare <em style="mso-bidi-font-style: normal;">what</em>&rdquo; construction). The last construction involves an overt <span style="font-variant: small-caps;">kind </span>noun which must be followed by the preposition <em style="mso-bidi-font-style: normal;">av </em>&lsquo;of&rsquo; which in turn assigns dative case to the main/head noun. The survey is based on data collected during the NORMS fieldwork in the Faroe Islands in August 2008, focusing on a number of morphosyntactic issues as well as the semantic distinction between <span style="font-variant: small-caps;">kind </span>and <span style="font-variant: small-caps;">token </span>interpretation. The various findings on Faroese are compared to data on other varieties of Germanic, in particular the North Germanic ones.</span></span></p>


Nordlyd ◽  
2009 ◽  
Vol 36 (2) ◽  
pp. pp
Author(s):  
Saija Tamminen-Parre

<p class="NL-Abstract" style="margin: 0cm 14.2pt 12pt;"><span lang="EN-US"><span style="font-family: Times; font-size: small;">The study presents the results of a preliminary investigation of the use of a number of pragmatic particles in Faroese: <em style="mso-bidi-font-style: normal;">s&aelig;rt t&uacute;</em> &lsquo;you see&rsquo;, <em style="mso-bidi-font-style: normal;">hoyr(ir) t&uacute;</em> &lsquo;listen&rsquo;, <em style="mso-bidi-font-style: normal;">skilir t&uacute;</em> &lsquo;you understand&rsquo;, and <em style="mso-bidi-font-style: normal;">veitst t&uacute;</em> &lsquo;y&rsquo;know&rsquo;. The data were collected through questionnaires and interviews and analyzed in relation to the social variable settlement. Data were collected from the five settlements of T&oacute;rshavn, Sandur, Tv&oslash;royri, Klaksv&iacute;k, and Fuglafj&oslash;r&eth;ur. The study found geographical variation in the use of the pragmatic particles and discusses the attitudes people in the Faroe Islands have towards the use of pragmatic particles.</span></span></p>


2000 ◽  
Vol 179 ◽  
pp. 201-204
Author(s):  
Vojtech Rušin ◽  
Milan Minarovjech ◽  
Milan Rybanský

AbstractLong-term cyclic variations in the distribution of prominences and intensities of green (530.3 nm) and red (637.4 nm) coronal emission lines over solar cycles 18–23 are presented. Polar prominence branches will reach the poles at different epochs in cycle 23: the north branch at the beginning in 2002 and the south branch a year later (2003), respectively. The local maxima of intensities in the green line show both poleward- and equatorward-migrating branches. The poleward branches will reach the poles around cycle maxima like prominences, while the equatorward branches show a duration of 18 years and will end in cycle minima (2007). The red corona shows mostly equatorward branches. The possibility that these branches begin to develop at high latitudes in the preceding cycles cannot be excluded.


2019 ◽  
Vol 19 (1) ◽  
pp. 121-124
Author(s):  
Sandy Henderson ◽  
Ulrike Beland ◽  
Dimitrios Vonofakos

On or around 9 January 2019, twenty-two Listening Posts were conducted in nineteen countries: Canada, Chile, Denmark, Faroe Islands, Finland, Germany (Frankfurt and Berlin), Hungary, India, Ireland, Israel, Italy (two in Milan and one in the South), Peru, Serbia, South Africa, Spain, Sweden, Taiwan, Turkey, and the UK. This report synthesises the reports of those Listening Posts and organises the data yielded by them into common themes and patterns.


Author(s):  
Esraa Aladdin Noori ◽  
Nasser Zain AlAbidine Ahmed

The Russian-American relations have undergone many stages of conflict and competition over cooperation that have left their mark on the international balance of power in the Middle East. The Iraqi and Syrian crises are a detailed development in the Middle East region. The Middle East region has allowed some regional and international conflicts to intensify, with the expansion of the geopolitical circle, which, if applied strategically to the Middle East region, covers the area between Afghanistan and East Asia, From the north to the Maghreb to the west and to the Sudan and the Greater Sahara to the south, its strategic importance will seem clear. It is the main lifeline of the Western world.


Author(s):  
A., C. Prasetyo

Overpressure existence represents a geological hazard; therefore, an accurate pore pressure prediction is critical for well planning and drilling procedures, etc. Overpressure is a geological phenomenon usually generated by two mechanisms, loading (disequilibrium compaction) and unloading mechanisms (diagenesis and hydrocarbon generation) and they are all geological processes. This research was conducted based on analytical and descriptive methods integrated with well data including wireline log, laboratory test and well test data. This research was conducted based on quantitative estimate of pore pressures using the Eaton Method. The stages are determining shale intervals with GR logs, calculating vertical stress/overburden stress values, determining normal compaction trends, making cross plots of sonic logs against density logs, calculating geothermal gradients, analyzing hydrocarbon maturity, and calculating sedimentation rates with burial history. The research conducted an analysis method on the distribution of clay mineral composition to determine depositional environment and its relationship to overpressure. The wells include GAP-01, GAP-02, GAP-03, and GAP-04 which has an overpressure zone range at depth 8501-10988 ft. The pressure value within the 4 wells has a range between 4358-7451 Psi. Overpressure mechanism in the GAP field is caused by non-loading mechanism (clay mineral diagenesis and hydrocarbon maturation). Overpressure distribution is controlled by its stratigraphy. Therefore, it is possible overpressure is spread quite broadly, especially in the low morphology of the “GAP” Field. This relates to the delta depositional environment with thick shale. Based on clay minerals distribution, the northern part (GAP 02 & 03) has more clay mineral content compared to the south and this can be interpreted increasingly towards sea (low energy regime) and facies turned into pro-delta. Overpressure might be found shallower in the north than the south due to higher clay mineral content present to the north.


2019 ◽  
Author(s):  
Hamed D. Ibrahim

North and South Atlantic lateral volume exchange is a key component of the Atlantic Meridional Overturning Circulation (AMOC) embedded in Earth’s climate. Northward AMOC heat transport within this exchange mitigates the large heat loss to the atmosphere in the northern North Atlantic. Because of inadequate climate data, observational basin-scale studies of net interbasin exchange between the North and South Atlantic have been limited. Here ten independent climate datasets, five satellite-derived and five analyses, are synthesized to show that North and South Atlantic climatological net lateral volume exchange is partitioned into two seasonal regimes. From late-May to late-November, net lateral volume flux is from the North to the South Atlantic; whereas from late-November to late-May, net lateral volume flux is from the South to the North Atlantic. This climatological characterization offers a framework for assessing seasonal variations in these basins and provides a constraint for climate models that simulate AMOC dynamics.


Author(s):  
Andrei Sokolov ◽  
Andrei Sokolov ◽  
Boris Chubarenko ◽  
Boris Chubarenko

Three dumping sites located at the south-eastern part of the Baltic Sea (Kaliningrad Oblast) at shallow depths are considered. The first one is located to the south of the Vistula Lagoon inlet in front of a permanently eroded open marine shore segment. The second one is located to the north of the Vistula Lagoon inlet, and is used now for disposing of dredged material extracted from the Kaliningrad Seaway Canal. The third dumping site is located near the northern shore of the Sambian Peninsula to the east of the Cape Gvardeijski and assigned for disposing the dredged material extracted from the fairway to the Pionerskij Port located nearby. The last site is planned to be used for disposing of dredged material from the future port that should be constructed there before the beginning of the FIFA World Cup 2018. All three dumping sites are located not far from the eroded segments of the shore. The question behind the study is: would it possible that disposed material will naturally transported from the damping site to the shore and accumulate there to protect it from erosion? A numerical hydrodynamic-transport 3D model (MIKE) was used to model sediment transport under different wind actions. The winds with the speed stronger than 15 m/s complete wash out disposed material from the dumping site and spreading it over the wide area with a negligible layer thickness. Winds of about 7-10 m/s transport material along the shore at a distance of few kilometers that may be useful for shore protection. The first location of the dumping site (to the south of the Vistula Lagoon inlet) looks very ineffective for potential protection the shore nearby. At the other hand, the second and especially the third locations are favorable for transport of disposed material to the shore, the most favorable conditions are at onshore or alongshore currents.


2000 ◽  
Vol 151 (12) ◽  
pp. 502-507
Author(s):  
Christian Küchli

Are there any common patterns in the transition processes from traditional and more or less sustainable forest management to exploitative use, which can regularly be observed both in central Europe and in the countries of the South (e.g. India or Indonesia)? Attempts were made with a time-space-model to typify those force fields, in which traditional sustainable forest management is undermined and is then transformed into a modern type of sustainable forest management. Although it is unlikely that the history of the North will become the future of the South, the glimpse into the northern past offers a useful starting point for the understanding of the current situation in the South, which in turn could stimulate the debate on development. For instance, the patterns which stand behind the conflicts on forest use in the Himalayas are very similar to the conflicts in the Alps. In the same way, the impact of socio-economic changes on the environment – key word ‹globalisation› – is often much the same. To recognize comparable patterns can be very valuable because it can act as a stimulant for the search of political, legal and technical solutions adapted to a specific situation. For the global community the realization of the way political-economic alliances work at the head of the ‹globalisationwave›can only signify to carry on trying to find a common language and understanding at the negotiation tables. On the lee side of the destructive breaker it is necessary to conserve and care for what survived. As it was the case in Switzerland these forest islands could once become the germination points for the genesis of a cultural landscape, where close-to-nature managed forests will constitute an essential element.


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