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Journal articles on the topic 'West Friesland'

Author: Grafiati

Published: 4 June 2021

Last updated: 16 February 2022

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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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11

Manby, G. M. "The petrology of the Harkerbreen Group, Ny Friesland, Svalbard: protoliths and tectonic significance." Geological Magazine 127, no. 2 (March 1990): 129–46. http://dx.doi.org/10.1017/s0016756800013820.

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AbstractThe late Precambrian–early Palaeozoic rocks of Ny Friesland, which have been subjected to Caledonian deformation and metamorphism, constitute part of the Eastern Province or Terrane of Svalbard. The Harkerbreen group and other divisions of the Stubendorffbreen supergroup form a high-grade and intensely deformed core complex to this terrane which is bounded to the west by the Billefjorden Fault Zone and to the east by a major north–south shear zone. The Stubendorffbreen rocks exhibit two gneissic foliations, one axial planar to a large scale, F1 fold nappe closing to the east and the other axial planar to kilometre-scale upright F2 folds subsidiary to the Atomfjella Arch. Metamorphism in the mid-amphibolite facies range coincided with generation of these folds, and F3.crenulation folding was accompanied by waning P–T conditions. A significant proportion of the gneisses within the Harkerbreen group display silica–major element covariation patterns consistent with their position in the granodiorite field on the AFM plot. Incompatible, immobile element ratios Zr/Ti v. Nb/Y indicate affinities with rhyolites to rhyodacites which is also suggested by their REE profiles. Normalized multi-element plots of the gneisses are similar to those of granites from attenuated within-plate settings such as Mull and Skaergaard. The amphibolites which were intruded in the D1–D2 interval appear to be derivatives of fractionated basalts. They plot across the calk-alkaline tholeiite boundary on the AFM diagram, and the calc-alkaline character of some of the amphibolites is further suggested by their Yb-normalized Ce-Ta abundances. Zr-Ti-Y and REE abundances would support their derivation from a related suite of fractionated basalt liquids. On the Zr/Y v. Zr discrimination diagram the amphibolites appear to have compositions transitional between Mid Ocean Ridge and Within-Plate basalts whilst the Zr-Nb-Ta plot indicates Volcanic Arc Basalt affinities. Th-Hf-Ta and multi-element plots, however, indicate a marginal to back-arc basin setting possibly above a mature subduction zone. The late Caledonian Chydenius granite is an adamellite with mixed within-plate and syn-orogenic characteristics typical of post-collisional granites.

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12

Köbler, Gerhard. "Brom, Christian, Urteilsbegründungen im „Höge Raad van Holland, Zeeland en West-Friesland“ am Beispiel des Kaufrechts im Zeitraum 1704-1787." Zeitschrift der Savigny-Stiftung für Rechtsgeschichte: Germanistische Abteilung 126, no. 1 (August 1, 2009): 639–40. http://dx.doi.org/10.7767/zrgga.2009.126.1.639.

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13

van Mourik, Jan, and Wim Ligtendag. "Relicts of a peat cover in the Westerkoggepolder (West Friesland, North-Holland, The Netherlands): The genesis of an eluvial clay soil." CATENA 132 (September 2015): 105–13. http://dx.doi.org/10.1016/j.catena.2014.12.005.

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14

Bosch, A. G. "M.-Ch. Le Bailly, Recht voor de Raad. Rechtspraak voor het Hof van Holland, Zeeland en West-Friesland in het midden van de vijftiende eeuw." BMGN - Low Countries Historical Review 118, no. 1 (January 1, 2003): 86. http://dx.doi.org/10.18352/bmgn-lchr.5795.

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15

Zavrelova, H., T. Hoekstra, M. Alssema, L. M. C. Welschen, G. Nijpels, A. C. Moll, H. C. W. de Vet, B. C. P. Polak, and J. M. Dekker. "Progression and Regression: Distinct Developmental Patterns of Diabetic Retinopathy in Patients With Type 2 Diabetes Treated in the Diabetes Care System West-Friesland, the Netherlands." Diabetes Care 34, no. 4 (March 29, 2011): 867–72. http://dx.doi.org/10.2337/dc10-1741.

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16

Havinga, A. J., R. M. van den Berg, and R. M. van Saparoea. "Pollen and macrofossil analyses of a unique peat remnant of the former extensive peat bogs in West Friesland, The Netherlands: a detailed record of coastal raised bog formation." Vegetation History and Archaeobotany 1, no. 3 (October 1992): 185–88. http://dx.doi.org/10.1007/bf00191558.

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17

Pfeil, Tom. "Albert Scheffers, Om de kwaliteit van het geld. Het toezicht op de muntproductie in de Republiek en de voorziening van kleingeld in Holland en West-Friesland in de achttiende eeuw." BMGN - Low Countries Historical Review 129, no. 3 (June 24, 2014): 43. http://dx.doi.org/10.18352/bmgn-lchr.9555.

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18

Bijl, D., H. W. J. van Marwijk, A. T. F. Beekman, M. de Haan, and W. van Tilburg. "A randomized controlled trial to improve the recognition, diagnosis and treatment of major depression in elderly people in general practice: design, first results and feasibility of the West Friesland Study." Primary Care Psychiatry 8, no. 4 (August 1, 2003): 135–40. http://dx.doi.org/10.1185/135525702125000895.

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19

Nève, Paul. "C. Brom, Urteilsbegründungen im ‘Hoge Raad van Holland, Zeeland en West-Friesland’ am Beispiel des Kaufrechts im Zeitraum 1704–1787. [Rechtshistorische Reihe, 377]. Peter Lang, [Frankfurt am Main 2008]. [IV] + 440 S." Tijdschrift voor Rechtsgeschiedenis / Revue d'Histoire du Droit / The Legal History Review 78, no. 3-4 (2010): 481–83. http://dx.doi.org/10.1163/157181910x527571.

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20

Antoine, Samir. "The chemical analysis of prehistoric bones. A palaeodietary and ecoarchaeological study of Bronze Age West-Friesland. By L. T. Runia. 234 pp., 37 figs, 93 tables. Oxford: British Archaeological Reports, International Series 363, 1987. £13.00." Proceedings of the Prehistoric Society 54 (1988): 335–36. http://dx.doi.org/10.1017/s0079497x00005922.

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21

Hofmeister, Adolf E. "Bremen, Harderwijk und die Zuiderzee." Hansische Geschichtsblätter 134 (April 18, 2020): 1–18. http://dx.doi.org/10.21248/hgbll.2016.40.

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Bremen, Harderwijk and the ZuiderzeeThe Harderwijk peace treaty of 8 May 1446, negotiated by envoys of the duchy of Burgundy and the Hanse town Bremen and ratified by duke Philip the Good of Burgundy on 8 July 1446, brought to an end a war which had lasted for four years, during which Bremen had waged war on the Burgundian territories of Holland, Zealand, Flanders and Brabant in order to gain compensation for ships and goods which had been captured (mainly by privateers) in the conflict between Holland and the Wendish towns (1438– 41). During the latter conflict, neutral ships were been seized if they were suspected to be carrying Dutch or Flemish goods – a practice which also affected skippers and merchants from Kampen, Harderwijk and Deventer. Therefore Kampen repeatedly took the initiative to midwife an agreement between Bremen and Holland. At first, this failed to produce an acceptable result because Flanders could not be included. In the end, however, the negotiations in Harderwijk in April and May 1446 succeeded in bringing the war to an end. Bremen and Stade obtained financial compensation, to be funded by the towns of Holland and Zealand. Evidence of direct connections between Bremen and the Zuiderzee towns begins in the 14th century and concerns quarrels with citizens of Kampen and Deventer or the naturalization of immigrants from the Zuiderzee towns in Bremen. Beginning in the 12th and 13th centuries, vessels from Holland, Utrecht and Flanders on the one hand and from Bremen and Stade on the other used the shipping route via Vecht, Almere (later Zuiderzee) and Vlie for traffic and trade. From the 13th century, merchants from Bremen and from the Zuiderzee are found side by side in Norway and Scania trading in fish. In the 15th century, merchants of Kampen bought grain in Bremen, whereas merchants of Bremen purchased cloth in Deventer. Furthermore, Kampen, Deventer and Zwolle mediated in Bremen’s quarrels with merchants from Osnabrück and Cologne, with the town of Groningen and especially with Antwerpen. In the 16th century, the political and economic situation of the Zuiderzee towns changed radically, as they were first incorporated into the state of emperor Charles V, and then joined the Republic of the United Netherlands. At the same time, Bremen’s trade shifted to West Friesland and Amsterdam. Thus the intermediary position of the Zuiderzee Hanse towns – poised between Bremen and Holland – came to an end.

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22

Roelofsen, C. G. "R.W.G. Lombarts, P.C.M. Schölvinck, J.Th. de Smidt, H.W. van Soest and M.R. van den Toorn, eds., Memorialen van het Hoffden Raad) van Holland, Zeeland en West-Friesland van den secretaris Jan Rosa (Rechtshistorisch Instituut Leiden, Series I vols. 4, 5 and 6), E.J. Brill/Universitaire Pers, Leyden 1982, 1985, 1988)." Netherlands International Law Review 36, no. 03 (December 1989): 398. http://dx.doi.org/10.1017/s0165070x0000913x.

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23

Haitas, Daniel. "1580 Political Ordinance of the States of Holland and West Friesland." Pro Futuro 10, no. 4 (May 28, 2021). http://dx.doi.org/10.26521/profuturo/2020/4/9459.

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The present study deals with certain influences the 1580 Political Ordinance of the States of Holland and West Friesland had in the English-speaking world, specifically in relation to the Plymouth Colony in the present-day Commonwealth of Massachusetts and South Africa. Regarding the former, there is a survey of the introduction of the institution of civil marriage by the Pilgrims at the Plymouth Colony and the Dutch background to this particular development. In relation to South Africa, there is an analysis of the lack of intestacy inheritance between spouses in that country in the past due to the system of inheritance rooted in the 1580 Political Ordinance, and the changes that took place in connection to this with the passing of time.

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24

"Memorialen van het Hof (den Raad) van Holland, Zeeland en West Friesland, van den secretaris Jan Rosa." Tijdschrift voor Rechtsgeschiedenis / Revue d'Histoire du Droit / The Legal History Review 71, no. 1-2 (2003): 222–25. http://dx.doi.org/10.1163/157181903100362562.

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25

Buurman, Janneke. "Carbonized plant remains from a pre-Roman Iron Age house site at Opperdoes, West Friesland, The Netherlands." Vegetation History and Archaeobotany 2, no. 2 (August 1993). http://dx.doi.org/10.1007/bf00202184.

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26

Van der Waag, Ian. "VERZET IN WEST -FRIESLAND: DE ILLEGALITEIT IN WESTERLIJK WESTFRIESLAND EN IN DE WIERINGERMEER IN DE JAREN 1940-'45." Scientia Militaria - South African Journal of Military Studies 23, no. 3 (February 15, 2012). http://dx.doi.org/10.5787/23-3-304.

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27

"Christel M.O. Verhas, De beginjaren van de Hoge Raad van Holland, Zeeland en West-Friesland, ... tot onderhoudinge van de Politique ordre ende staet der Landen van Hollandt, Zeelandt, Vrieslant ... . [Algemeen Rijksarchief Publikatiereeks, 5]. Algemeen Rijksarchief, Den Haag 1997. 186 + 255 p." Tijdschrift voor Rechtsgeschiedenis / Revue d'Histoire du Droit / The Legal History Review 66, no. 3-4 (1998): 428–31. http://dx.doi.org/10.1163/15718199819683004.

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