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Relevant bibliographies by topics / West Friesland

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Academic literature on the topic 'West Friesland'

Author: Grafiati

Published: 4 June 2021

Last updated: 16 February 2022

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Journal articles on the topic "West Friesland"

1

van Bezooijen, Renée, and Johannes Ytsma. "Accents of Dutch." Variation in (Sub)standard language 13 (December 31, 1999): 105–29. http://dx.doi.org/10.1075/bjl.13.07bez.

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Abstract. This experimental study deals with the perception of regionally colored accents of Standard Dutch (from Groningen, Friesland, Limburg, Zuid-Holland, and West-Flanders) as compared to 'pure' Standard Dutch. Three different aspects were investigated: speech-based personality impression, perceived linguistic divergence, and geographic identifiability. Listeners originated from different parts of the Netherlands. As for personality impression, speakers of 'pure' Standard Dutch were perceived to be significantly more dominant (arrogant, self-assured, and active) than accented speakers from Groningen, Friesland, Limburg, and West-Flanders, and they received significantly higher ratings on the integrity dimension (reliable, fair, and education) than accented speakers from Limburg. No other significant differences (e.g. related to social attractiveness) were found. With respect to linguistic divergence, the speakers from the south (Limburg and West-Flanders) were perceived to have significantly stronger and more homogeneous accents than the speakers from the north (Groningen and Friesland) and the west (Zuid-Holland). Finally, the geographic origin of the speakers from Limburg appeared to be the easiest to identify and that of the speakers from West-Flanders and Groningen the most difficult.

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2

Borger, G. J. "M. Hameleers, West-Friesland in oude kaarten." BMGN - Low Countries Historical Review 105, no. 1 (January 1, 1990): 87. http://dx.doi.org/10.18352/bmgn-lchr.3182.

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3

Mensink, Gerda. "Huisartsen en huisartsenpost in West-Friesland testen WDH en EMD." SynthesHis 11, no. 4 (December 2012): 28–29. http://dx.doi.org/10.1007/s12494-012-0070-4.

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4

Harland, W. Brian. "Chapter 7 Northeastern Spitsbergen." Geological Society, London, Memoirs 17, no. 1 (1997): 110–31. http://dx.doi.org/10.1144/gsl.mem.1997.017.01.07.

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The land (area) considered here is bounded on the west by Wijdefjorden and on the east by Hinlopenstretet and Storfjorden. The southern boundary is somewhat indefinite. For descriptive convenience Carboniferous through Triassic stratigraphy is treated in Chapters 4 and 5 and Devonian strata to the northwest in Chapter 8. It makes geological sense for these chapter areas to overlap where they meet.Ny Friesland was the name for most of the area under consideration. However, after the accession of the Norwegian King Olav V in 1957 his name was given to what had previously been a somewhat indefinite territory, mostly ice covered (the Terre Glacee Russe of some older maps) to the south east of Ny Friesland. Olav V Land was defined to take in some of what had been referred to as Ny Friesland and early accounts should be read with this in mind (Miloslavskiy et al. 1993, map D8G). This chapter thus concerns Ny Friesland and north western Olav V Land and for descriptive economy Ny Friesland will be used for the area where most of the older rocks crop out.Much of the interior is covered by highland ice rather than an ice cap, meaning that the ice is not thick enough for the surface to be independent of the underlying relief. Indeed the ice cover is broken here and there by rocky cliffs of submerged valley glaciers. The three largest areas of continuous ice are Lomonosovfonna, Asgardfonna and Valhallfonna. The inland ice flows out along valley

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5

Harland, W. B., R. A. Scott, K. A. Auckland, and I. Snape. "The Ny Friesland Orogen, Spitsbergen." Geological Magazine 129, no. 6 (November 1992): 679–707. http://dx.doi.org/10.1017/s0016756800008438.

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AbstractThe Caledonides of Ny Friesland comprise the type Hecla Hoek sequence of Svalbard, a succession of late Proterozoic to Ordovician strata greater than 18 km thick. Three supergroups constitute the sequence: the Stubendorffbreen Supergroup (Riphean), the Lomfjorden Supergroup (late Riphean-Sturtian) and the Hinlopenstretet Supergroup (Varanger-mid-Ordovician). Basement elements have recently been identified within the Stubendorffbreen Supergroup, but their extent and significance is yet to be established. The Stubendorffbreen Supergroup records the deposition of sediments and volcanics (both acid and basic) in an unstable marine environment. In contrast, the Lomfjorden and Hinlopenstretet supergroups record sedimentation in a shallow-marine, periodically emergent, stable environment without volcanism. The Ny Friesland Orogen is divided into two subterranes by the Veteranen Line, a zone of attenuation along which sinistral strike-slip displacement has occurred. This line separates the strongly deformed Stubendorffbreen Supergroup rocks in the west from the less-intensely deformed Lomfjorden and Hinlopenstretet supergroup rocks in the east. Despite these contrasts and the obvious displacement, there is no evidence that a significant stratigraphie break occurs across it.All the supergroups were deformed and metamorphosed during the late Ordovician-Silurian Ny Friesland Orogeny. Early compressional deformation produced isoclinal folding and nappes in the Stubendorffbreen Supergroup rocks, accompanied by amphibolite faciès metamorphism; deformation in the Lomfjorden and Hinlopenstretet supergroups was less intense with open, upright folds and greenschist or subgreenschist facies metamorphism. Early compression was followed by a Silurian transpressive deformation that generated a pervasive lineation in the Stubendorffbreen Supergroup rocks. Transpressive deformation and the associated sinistral strike-slip was focused where strata were in a near-vertical attitude conducive to displacement. At a late stage in the orogeny, and probably still under a strike-slip regime, batholiths were emplaced into rocks east of the Veteranen Line.As a result of continued sinistral displacement (transpression, transcurrence and transtension) along the Billefjorden Fault Zone, Ny Friesland (part of the Eastern Province of Svalbard) finally docked against the Central Province during the late Devonian Svalbardian movements. At the same time, the Central Province docked against the Western Province. In total, hundreds of kilometres of Caledonian displacement along the Billefjorden Fault Zone brought the Eastern and Central provinces into their present positions. Pre-Carboniferous Svalbard is thus a composite terrane of at least three provinces, each comprising more than one minor terrane.

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6

Sirks, A. J. B. "Zeeland en West-Friesland, De hoofdlijnen van het procederen in civiele zaken voor het Hof van Holland, Zeeland en West-Friesland zowel in eerste instantie als in hoger beroep." Tijdschrift voor Rechtsgeschiedenis / Revue d'Histoire du Droit / The Legal History Review 77, no. 1-2 (2009): 270–72. http://dx.doi.org/10.1163/004075809x403523.

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7

Bazarnik, Jakub, Abigail Barker, Jarosław Majka, Karolina Kośmińska, Synnønve Elvevold, and Mirosława Bazarnik. "Wstępna charakterystyka geochemiczna amfibolitów i skał ultramaficznych terranu West Ny-Friesland, północny Spitsbergen." Przegląd Geologiczny 69, no. 7 (August 10, 2021): 406–10. http://dx.doi.org/10.7306/2021.24.

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8

Koopmans, J. W. "C.M.O. Verhas, De beginjaren van de Hoge Raad van Holland, Zeeland en West-Friesland." BMGN - Low Countries Historical Review 114, no. 3 (January 1, 1999): 402. http://dx.doi.org/10.18352/bmgn-lchr.5024.

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9

Poelgeest, L. van. "De raadsheren van de Hoge Raad van Holland, Zeeland en West-Friesland in de achttiende eeuw." BMGN - Low Countries Historical Review 103, no. 1 (January 1, 1988): 20. http://dx.doi.org/10.18352/bmgn-lchr.2895.

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10

de Jong, Hylkje. "‘Het quaestieuse verdronkene goud’." Pro Memorie 23, no. 1 (January 1, 2021): 6–31. http://dx.doi.org/10.5117/pm2021.1.002.jong.

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Abstract Zacharias Huber (1669-1732) evaluated in the revised Heedensdaegse Rechtsgeleertheyt arguments, hitherto unknown, which were brought forward in a case, pursued before the Court of Friesland and decided on December 14th 1718. The case dealt with the ownership of a box with gold, found on the beach of Schiermonnikoog in 1710 and which came from the ship De Witte Haas, shipwrecked off the coast in 1674. Newly found civil records show that Maria Wilree (1667-1729) from Amsterdam started the procedure to recover the box with gold, because it purportedly belonged to her father Dirck Wilree (1636-1674), director-general for the West India Company in Guinea and who died in the shipwrecking. She took legal action against Henrica Helmhout, regent of Schiermonnikoog and receiver of wrecks, and Gillis Vermeersch, representative of the West India Company. Only Vermeersch was successful in his argument, which he based on the instructions of the Company: it was forbidden to transport unregistered private goods. Such goods forfeited immediately to the Company. Consequently, Wilree claimed for the Company ownership and possession of the box with gold. Helmhout claimed to be the owner by prescription. Their arguments appear not to have been convincing.

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Dissertations / Theses on the topic "West Friesland"

1

Buurman, Janneke. "The Eastern part of West-Friesland in later Prehistory : agricultural and environmental aspects /." [Leiden] : J. Buurman, 1996. http://catalogue.bnf.fr/ark:/12148/cb361941474.

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2

Brom, Christian. "Urteilsbegründungen im "Hoge Raad van Holland, Zeeland en West-Friesland" am Beispiel des Kaufrechts im Zeitraum 1704 - 1787." Frankfurt, M. Berlin Bern Bruxelles New York, NY Oxford Wien Lang, 2007. http://d-nb.info/989940888/04.

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3

Le, Bailly Marie Charlotte. "Recht voor de Raad : rechtspraak voor het Hof van Holland, Zeeland en West-Friesland in het midden van de vijftiende eeuw /." [S.l. : s.n], 2001. http://catalogue.bnf.fr/ark:/12148/cb40195442r.

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Deelstra, Oetze Theodoor. "Stora författare från periferin : En jämförande studie mellan minoritetslitteratur från Friesland och Svenskfinland, med romanerna de fûke (1966) och Där vi en gång gått (2006) som utgångspunkt." Thesis, Uppsala universitet, Litteraturvetenskapliga institutionen, 2016. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-296226.

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This master’s thesis considers the differences between the minority literature from Friesland, a province in the northwest of the Netherlands, and that of the Swedish-speaking part of Finland. The author of this paper tries to draw attention to the literatures of those minorities, which often are not well-known outside their own regions. The main issue discussed in this paper is: How is minority culture problematized in the novels de fûke (1966) by the Frisian author Rink van der Velde and Där vi en gång gått (2006) by the Finland-Swedish author Kjell Westö? The Frisian population in the Netherlands is considered by many as a very old people, because famous writers of the Roman Empire, such as Pliny the Elder, wrote specifically about their region and its people. Despite this, the Frisian language has been in a peripheral situation for many centuries. The Swedish minority in Finland, on the contrary, is much younger. Finland gained autonomy in 1809 and before that time the region currently known as Finland, was the eastern part of the Kingdom of Sweden. This meant that Swedish was the predominant language until that year. Later on Finnish became the main language in Finland. However, both the Frisian and the Finland-Swedish literature were not established before the nineteenth century. This changed partially as a result of ideas of the Romanticism, but also because of historical reasons. By analyzing the previously mentioned novels, Oetze Deelstra shows how the minorities in both countries fare in opposite situations. The Swedish-speaking population has often been, and continues to be, examined as upper-class. On the other hand, in Frisia should a very old countryside culture has been preserved. Those ideas have been important in forming the images of both minorities. A noticeable distinction is that the Frisian literature is defined by language, while the Finland-Swedish literature is characterized by political and ideological arguments.
Dizze masterskripsje rjochtet him op de ferskillen tusken de literatuer fan Fryslân en dy fan de Sweedsktalige minderheid yn Finlân. De skriuwer fan dit wurk besiket op dy wize mear omtinken te freegjen foar de literatuer fan dizze minderheden, dy’t faak net sa bekend is bûten de eigen regio. De fraach dy’t sintraal stiet is: Op hokker wize wurdt stal jûn oan minderhedeproblematyk yn de romans de fûke (1966) fan de Fryske skriuwer Rink van der Velde en Där vi en gång gått (2006) fan de Finlânsweedske skriuwer Kjell Westö? Faak wurde de Friezen beskôge as in âld folk. Mooglik komt dat trochdat se al neamd wurde soene troch ferneamde skriuwers fan it Romeinske Ryk, lyk as Plinius de Aldere. Dochs hat it Frysk iuwenlang in net al te wichtige rol spile yn Fryslân en dêrbûten. De Sweedske minderheid yn Finlân is lykwols folle jonger. Finlân is pas sûnt 1809 autonoom en foar dy tiid wie dat wat wy hjoed-de-dei Finlân neame, it eastlike diel fan it Sweedske Ryk. Dat betsjut ek dat it Sweedsk oant doe ta de oerhearskjende taal wie. Letter waard it Finsk de wichtichste taal yn Finlân. Sawol de Fryske as de Finlânsweedske literatuer wiene lykwols net fêstige foar de njoggentjinde iuw. Dat feroaret pas yn de Romantyk, foar in diel fanwege de idealen út dy tiid, mar ek om politike redenen. Troch de earderneamde romans te analysearjen, lit Oetze Deelstra sjen hoe’t de minderheden fan beide lannen eins yn tsjinstelde situaasjes operearje. De Sweedsktalige befolking fan Finlân is faak, en wurdt no noch hieltyd, besjoen as de boppeklasse. Yn Fryslân soe oan ’e oare kant in iuwenâlde lanboutradysje bewarre bleaun wêze. Dizze opfettings hawwe wichtich west foar de byldfoarming fan beide minderheden. In opfallend ferskil is dat de Fryske literatuer fan de eigen taal út definiearre wurdt, wylst de Finlânsweedske literatuer karakterisearre wurdt troch politike en ideologyske útgongspunten.

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Books on the topic "West Friesland"

1

Lambooij, Herman. Een eeuw schipperen: De omstreden kanalisatie van West-Friesland. Schoorl: Pirola, 1991.

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2

Beukers, Eelco, and Fer Beerepoot. Middenstand: Geschiedenis van de detailhandel in West-Friesland (1850-1975). Zwolle: WBOOKS, 2012.

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3

Het vennootschapsrecht van Holland: Het venootschapsrecht van Holland, Zeeland en West-Friesland in de rechtspraak van de Hoge Raad van Holland, Zeeland en West-Friesland. Deventer: Kluwer, 2010.

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4

Hof van Holland, Zeeland en West-Friesland: De hoofdlijnen van het procederen in civiele zaken voor het Hof van Holland, Zeeland en West-Friesland zowel in eerste instantie als in hoger beroep. Hilversum: Verloren, 2008.

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5

Runia, L. T. The chemical analysis of prehistoric bones: A paleodietary and ecoarcheological study of Bronze Age West-Friesland. Oxford, England: B.A.R., 1987.

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6

Brom, Christian. Urteilsbegründungen im "Hoge Raad van Holland, Zeeland en West-Friesland" am Beispiel des Kaufrechts im Zeitraum 1704 - 1787. Frankfurt am Main: P. Lang, 2008.

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7

Urteilsbegründungen im "Hoge Raad van Holland, Zeeland en West-Friesland" am Beispiel des Kaufrechts im Zeitraum 1704 - 1787. Frankfurt am Main: P. Lang, 2008.

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8

Brom, Christian. Urteilsbegründungen im "Hoge Raad van Holland, Zeeland en West-Friesland" am Beispiel des Kaufrechts im Zeitraum 1704 - 1787. Frankfurt am Main: P. Lang, 2008.

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9

Bailly, Maria Charlotte Le. Recht voor de Raad: Rechtspraak voor het Hof van Holland, Zeeland en West-Friesland in het midden van de vijftiende eeuw. Leiden: Universiteit Leiden, 2001.

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10

Verzet in West-Friesland: De illegaliteit in westelijk West-Friesland en in de Wieringermeer in de jaren 1940-'45. Pirola, 1991.

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Book chapters on the topic "West Friesland"

1

"English Translation: a Remonstrantie on the Regulations to Be Instituted in Holland and West Friesland regarding the Jews." In Hugo Grotius’s Remonstrantie of 1615, 199–216. BRILL, 2019. http://dx.doi.org/10.1163/9789004397446_005.

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Emery, K. O., and David Neev. "General Geology." In The Destruction of Sodom, Gomorrah, and Jericho. Oxford University Press, 1995. http://dx.doi.org/10.1093/oso/9780195090949.003.0005.

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The Dead Sea occupies a linear down-dropped region between two roughly parallel faults along the central segment of the major northsouth- trending crustal rift that extends about 1,100 km from the Red Sea through the Gulf of Elath to Turkey. This rift or geosuture separates the Arabian crustal sub-plate on the east from the Sinai one on the west. An origin as early as Precambrian is possible (Bender, 1974; Zilberfarb, 1978). Crystalline crust along the north-south trough of the Sinai sub-plate is about 40 km thick in contrast with a thickness of half as much above ridges along both flanks (Ginsburg and Gvirtzman, 1979). Toward the north the ridges appear to converge (Neev, Greenfield, and Hall, 1985). Since the Miocene period the Arabian plate has moved north about 105 km relative to the Sinai plate. This sort of crustal movement along either side of a rift is termed strike-slip faulting. One result of it was the opening of the Red Sea relative to the Gulf of Suez. The Dead Sea graben, a down-dropped block between two roughly parallel faults, occupies the central segment of the long crustal rift. The boundary between these is rather sharp along the east shore of the sea (Frieslander and Ben-Avraham, 1989). Actual post-Miocene movement was along not just a single major fault but was distributed among numerous sub-parallel faults that form a 100-km-wide belt in which movements were transferred from one fault to another (Eyal et al., 1981; Gilat and Honigstein, 1981). Recent movements have occurred along the south segment of the north-south-trending Arava fault south of the Amazyahu transverse fault (Zak and Freund, 1966). These strike-slip movements probably did not continue after Miocene along the main East fault of the Dead Sea, which is the north extension of the Arava wrench fault. In contrast, recent movements have been present along the north-northeast- trending Jordan or Dead Sea fault (Ben-Menahem et al., 1977, fig. 1). The movements extend south from east of Jericho in the north along the base of the west submarine slope of the sea and the elongate salt diapir of Mount Sedom as far as the Amazyahu fault in the south.

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