Journal articles: 'Jutland'

1

Lyle, Colin. "A Nelsonian Jutland?" RUSI Journal 140, no. 1 (February 1995): 56–60. http://dx.doi.org/10.1080/03071849508445892.

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2

Bucholz, Arden, and Keith Yates. "Flawed Victory: Jutland 1916." German Studies Review 24, no. 2 (May 2001): 405. http://dx.doi.org/10.2307/1433503.

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3

Black, Jeremy. "Jutland. The Unfinished Battle." European Review of History: Revue européenne d'histoire 27, no. 4 (February 4, 2020): 563–78. http://dx.doi.org/10.1080/13507486.2020.1715035.

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4

Laurberg, Peter, Klaus M. Pedersen, Astradur Hreidarsson, Nikulas Sigfusson, Eigil Iversen, and Preben R. Knudsen. "Iodine Intake and the Pattern of Thyroid Disorders: A Comparative Epidemiological Study of Thyroid Abnormalities in the Elderly in Iceland and in Jutland, Denmark." Journal of Clinical Endocrinology & Metabolism 83, no. 3 (March 1, 1998): 765–69. http://dx.doi.org/10.1210/jcem.83.3.4624.

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Thyroid abnormalities are common in all populations, but it is difficult to compare results of epidemiological studies, because different methods have been used for evaluation. We studied the importance of the population iodine intake level for the prevalence rate of various thyroid abnormalities in elderly subjects. Random samples of elderly subjects (68 yr) were selected from the central person registers in Jutland, Denmark, with low (n = 423) and, in Iceland, with longstanding relatively high (n = 100) iodine intake. Females from Jutland had a high prevalence of goiter or previous goiter surgery (12.2%), compared with males from Jutland (3.2%) and females (1.9%) and males (2.2%) from Iceland. Abnormal thyroid function was very common in both areas, with serum TSH outside the reference range in 13.5% of subjects from Jutland and 19% of those from Iceland. In Jutland, it was mainly thyroid hyperfunction (9.7% had low, 3.8% had high serum TSH), whereas in Iceland, it was impaired thyroid function (1% had low, 18% had high serum TSH). All subjects with serum TSH more than 10 mU/L had autoantibodies in serum, but antibodies were, in general, more common in Jutland than in Iceland. Thus, thyroid abnormalities in populations with low iodine intake and those with high iodine intake develop in opposite directions: goiter and thyroid hyperfunction when iodine intake is relatively low, and impaired thyroid function when iodine intake is relatively high. Probably, mild iodine deficiency partly protects against autoimmune thyroid disease. Thyroid autoantibodies may be markers of an autoimmune process in the thyroid or secondary to the development of goiter.

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5

Overgaard, Søren, Harald M. Knudsen, Lise N. Hansen, and Niels Mossing. "Hip arthroplasty in Jutland, Denmark." Acta Orthopaedica Scandinavica 63, no. 5 (January 1992): 536–38. http://dx.doi.org/10.3109/17453679209154731.

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6

Boe, Andreas M. B., Thomas J. Simonsen, Camilla T. Colding-Jørgensen, Philip H. Folman, Thomas T. Jensen, Kian J. Spencer, Philip F. Thomsen, and David R. Nash. "Spatial and Temporal Patterns of Genetic Diversity and Structure in Danish Populations of the Alcon Blue Butterfly Phengaris alcon (Denis & Schiffermüller)." Diversity 14, no. 12 (December 11, 2022): 1098. http://dx.doi.org/10.3390/d14121098.

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Phengaris alcon is an endangered, ant-associated butterfly found, amongst other places, in Denmark, where it has undergone a severe decline during the last century. However, the population genetic consequences of this decline remain unknown. To explore past and current patterns in population structure in relation to the decline, we analyzed DNA microsatellite data from 184 recent and 272 historical P. alcon specimens from 44 spatiotemporal locations in Denmark. We thus generated the most temporally and spatially comprehensive population genetic dataset for P. alcon in Denmark so far. Our results for the Bayesian population assignment of recent samples revealed three major current genetic clusters: western Jutland, northern Jutland, and the island of Læsø. Estimates of genetic diversity showed signs of inbreeding in several extant populations. When including data from museum specimens, only a single locatSion showed a decline in heterozygosity between 1967 and 2021. We suggest that the two distinct clusters in western and northern Jutland indicate two temporally separated Holocene colonizations of Denmark, the latter of which may have been aided by changes in agricultural practice in the late Neolithic period. The unique genetic signature of the Læsø populations may be a result of the admixture of northern Jutland and western Swedish populations.

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7

Jakobsen, Flemming. "The Wind Influence on the Jutland Coastal Current Interpreted on the Basis of som Observations." Hydrology Research 31, no. 2 (April 1, 2000): 127–48. http://dx.doi.org/10.2166/nh.2000.0009.

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The Jutland Coastal Current (JCC) is a freshwater-influenced coastal current localised in the south-eastern part of the North Sea. Its main sources are the Elbe, the Weser, and the Ems, which run into the German Bight, as well as smaller rivers along the Danish west coast. Tides, buoyancy and wind mainly determine the flow field in the Jutland Coastal Current. The Ekman transport in the North Sea far away from land feeds the coastal current along the Jutland coastline within approximately one Rossby radius of the coastline. In this study the influence of the wind on the Jutland Coastal Current (JCC) is investigated on the basis of measurements of wind, salinity, nitrate and current. The wind determines the spatial extent of the current and only during south-southwesterly winds does the JCC flow into the Skagerrak. The major river discharge into the German Bight in 1995 was followed by a decrease in the salinity outside Hirtshals after only 21-45 days in connection with changing southerly and westerly winds. On the 50-hour time-scale the wind determines the gross and residual transport in the JCC as expected from the Ekman transport, together with minor contributions from the buoyancy and tide. The spatial nitrate distributions clearly indicate an inter-annual variation in the nitrate concentrations and thus influence the transport of nitrate.

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8

Muir, Malcolm, and John Campbell. "Jutland: An Analysis of the Fighting." Military Affairs 51, no. 3 (July 1987): 160. http://dx.doi.org/10.2307/1987527.

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9

Durflinger, Serge. "Book Review: Flawed Victory: Jutland, 1916." International Journal of Maritime History 13, no. 1 (June 2001): 367–69. http://dx.doi.org/10.1177/0843871401013001103.

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10

Smith, Simon. "Voices from Jutland: A centenary commemoration." Mariner's Mirror 102, no. 4 (October 2016): 489–90. http://dx.doi.org/10.1080/00253359.2016.1241011.

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11

Grove, Eric. "The Jutland Paradox: A keynote address." Mariner's Mirror 103, no. 2 (April 3, 2017): 168–74. http://dx.doi.org/10.1080/00253359.2017.1304698.

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12

Hamilton, C. I. "Book Review: Flawed Victory: Jutland 1916." War in History 11, no. 3 (July 2004): 371–72. http://dx.doi.org/10.1177/096834450401100311.

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13

Osborne, Eric W. "Nicholas Jellicoe, Jutland: The Unfinished Battle." European History Quarterly 50, no. 1 (January 2020): 163–65. http://dx.doi.org/10.1177/0265691419897533m.

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14

Siemen, Palle. "House‐type chronology in SW Jutland." Norwegian Archaeological Review 23, no. 1-2 (January 1990): 161–71. http://dx.doi.org/10.1080/00293652.1990.9965522.

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15

Hansen, J., and T. Hansen. "Stratigraphy and sea-level fluctuations in the Upper Miocene Gram Formation, south-western Denmark." Bulletin of the Geological Society of Denmark 50 (December 15, 2003): 157–69. http://dx.doi.org/10.37570/bgsd-2003-50-13.

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Correlation between four published and one unpublished lithological logs from the Gram clay pit permits a comparison between previous studies of this critical exposure. The boundary between the Gram Clay and the Gram Silt in the Gram clay pit is redefined. A sea-level curve, based mainly on foraminiferal data from the Sæd, Gram and Lille Tønde borings in southern Jutland, is constructed and compared with a published sea-level curve from the North Sea. It appears that sea level recorded from southern Jutland was controlled mainly by eustacy.

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16

Nielsen, S. A. "Présentation de Culicoides (Culicoides) boyi sp.n. découvert au Jutland du Nord, Danemark." Revue d’élevage et de médecine vétérinaire des pays tropicaux 62, no. 2-4 (February 1, 2009): 170. http://dx.doi.org/10.19182/remvt.10074.

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During 2008 and 2009 intensive sampling of Culicoides was carried out near cowsheds all over Denmark. All species of the subgenus Culicoides so far recorded from Denmark were represented at the sites. However, at two sites in Northern Jutland a small number of individuals having a strong resemblance to Culicoides pulicaris, C. punctatus and C. halophilus were found. A careful morphological analysis revealed conclusive morphological differences between the specimens from Northern Jutland and other species of the subgenus Culicoides known from Northern Europe. The aberrant specimens are described as Culicoides (Culicoides) boyi sp. n.

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17

DOD, BARBARA, CATHY LITEL, PATRICK MAKOUNDOU, ANNIE ORTH, and PIERRE BOURSOT. "Identification and characterization of t haplotypes in wild mice populations using molecular markers." Genetical Research 81, no. 2 (April 2003): 103–14. http://dx.doi.org/10.1017/s0016672303006116.

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As part of a population genetics survey of the hybrid zone between mouse subspecies Mus musculus domesticus and M. m. musculus, we identified and characterized the t haplotypes in 1068 mice from 186 different populations in a 2500 km2 area in central Jutland. On the basis of two t-specific PCR markers, 130 mice possessed this haplotype. The allele frequencies at six microsatellites on the third and fourth chromosomal inversions of the t region were sufficiently different between t-bearing and non-t-bearing mice, and linkage disequilibria sufficiently marked on the t haplotype, to be able to reconstitute the genotype of most t haplotypes. A total of three frequent and 15 rarer haplotypes were identified. These haplotypes resemble each other more than they resemble a panel of known haplotypes from a wide range of geographical regions, except for tw73, which was also extracted from Jutland. The patterns of variation at the microsatellite loci suggest that the Jutland haplotypes were derived from a small number of haplotypes, followed by recombination between complementing haplotypes. Further evidence of recombination came from complementation tests that we performed, showing the lack of concordance between the degrees of complementation and of molecular resemblance between haplotypes. This study shows that it is possible to characterize the presence and variation of t haplotypes by a population genetics approach using simple molecular markers. However recombination between t haplotypes has occurred frequently enough to obscure the links between this variation and the biological properties of distortion and lethality of the haplotypes that originally colonized Jutland.

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18

Leth, Jørgen O., Birger Larsen, and Dennis Anthony. "Sediment distribution and transport in the shallow coastal waters along the west coast of Denmark." Geological Survey of Denmark and Greenland (GEUS) Bulletin 4 (July 20, 2004): 41–44. http://dx.doi.org/10.34194/geusb.v4.4779.

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Until recently, studies of the regional distribution of seabed sediments off the littoral zone of the Danish North Sea coast had been concentrated on the Jutland Bank area (Fig. 1; Leth 1996, 1998). Knowledge on the sedimentary conditions and processes along the entire west coast of Jutland has, however, significantly increased as a result of 2000 km of newly acquired high-resolution seismic and side-scan sonar data, supplemented by about 100 vibrocores. These data were collected by the Geological Survey of Denmark and Greenland (GEUS) during joint projects with the Danish Coastal Authority between 1998 and 2001 (Leth et al. 1999; Larsen & Leth 2001). The coastal zone off west Jutland displays a highly dynamic environment, where sediment transport is governed by strong tidal and wave-induced currents. The net wavegenerated current is south going, while the coastal current has a net direction towards the north (Knudsen et al. 2002). The direction of the net littoral drift is southward from the outlet of Limfjorden to Blåvands Huk, with net erosion north of Nymindegab and aggregation to the south; the offshore part of this depositional system has recently been studied (Larsen & Leth 2001).

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19

Kiss, László. "Jutland szemtanúi - Az ENGADINE és a WARRIOR." Haditechnika 52, no. 3 (2017): 41–47. http://dx.doi.org/10.23713/ht.51.2.09.

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20

ODGAARD, BENT VAD, and HANS ROSTHOLM. "A Single Grave Barrow at Harreskov, Jutland." Journal of Danish Archaeology 6, no. 1 (January 1987): 87–100. http://dx.doi.org/10.1080/0108464x.1987.10589979.

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21

Kronborg, Christian, Henry Bender, Regnar Bjerre, Rud Friborg, Hans O. Jacobsen, Lars Kristiansen, Poul Rasmussen, Poul R. Sørensen, and Gunnar Larsen. "Glacial stratigraphy of East and Central Jutland." Boreas 19, no. 3 (January 16, 2008): 273–87. http://dx.doi.org/10.1111/j.1502-3885.1990.tb00451.x.

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22

Sumida, Jon Tetsuro. "Jutland: World War I’s greatest naval battle." First World War Studies 8, no. 2-3 (September 2, 2017): 236–37. http://dx.doi.org/10.1080/19475020.2017.1408740.

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23

Orlando., Salvatore. "TECHNICAL RESULTS OF THE BATTLE OF JUTLAND." Journal of the American Society for Naval Engineers 33, no. 3 (March 18, 2009): 606–12. http://dx.doi.org/10.1111/j.1559-3584.1921.tb04925.x.

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24

Nielsen, Simon Kjær. "Site Locations on the Jutland Peninsula across the Late Funnel Beaker – Early Corded Ware Period Transition and Their Implications." Acta Archaeologica 93, no. 2 (February 5, 2024): 403–26. http://dx.doi.org/10.1163/16000390-09401058.

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Abstract The extent of spatial overlap between late Funnel Beaker (TRB) and early Corded Ware or ‘Single Grave’ finds has figured prominently in discussions of how the latter became established on the Jutland Peninsula after 2850 BCE. Working mainly from regional distribution maps and often framing the issue in terms of ‘territories’, decades of debate have focused not least on the question of whether elements of Corded Ware culture primarily arrived in this region with incoming migrants or whether the late TRB groups that already inhabited the region during the early 3rd millennium BCE played a central role in adopting a new tradition. Recently, the results of aDNA research have shifted the relevant questions from whether migration played a role to which role migration played, how it interacted with other factors and how both processes and outcomes varied. The task of answering these questions calls for local-scale analyses and for comparisons across cases and contexts. This article examines site locations and the more detailed location of burials, ritual structures and funerary monuments at specific sites within a 40 × 40 km large area in northern Jutland across the late TRB – early Corded Ware period transition. The results show a high degree of continuity in the location of cemeteries in the landscape, in some cases down to individual burials superposing one another, and this leads to a discussion of different scenarios that may explain the apparent correspondence across the general shift in burial customs. The results obtained in the selected area in northern Jutland are also compared with site locations in another part of the peninsula, i.e. the Horsens Fjord area in eastern-central Jutland, which has also been studied thoroughly recently and where a very different pattern is found (Madsen 2020). The article concludes by discussing the background of these two different patterns and the presumably rather different cultural processes that took place across the late TRB – early Corded Ware transition in these two areas.

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25

Lylloff, Kirsten. "Kampen om de tyske skoler i Danmark efter 1945." Fund og Forskning i Det Kongelige Biblioteks Samlinger 55 (March 3, 2016): 525. http://dx.doi.org/10.7146/fof.v55i0.118924.

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Kirsten Lylloff: The Struggle on the German schools in Denmark after 1945 In 1945 there were 58 private and 31 public German schools in Southern Jutland [private school and public school are defined following US-standards], all founded after the reunion of the former German region with Denmark in 1920, and one private German school in Copenhagen founded in 1575.Since Hitler’s seizure of power in 1933 a part of the German minority in Southern Jutland openly opposed the Danish hegemony, demanding return of the region to Germany, and part of the Danish majority feared, as a consequence of Germany’s rising power, a German reacquisition of the region, especially after the German occupation of Denmark in 1940. During the occupation 9 new private German schools were build and 10 of the older buildings restored, and the budgets, which always had been partly subsidized from Germany, were raised. Germany’s payment to the schools was drawn on the German-Danish clearing account, which at the end of the war showed a huge deficit for the Danes.With the German surrender 1945 the time was ripe for revenge for the Danish majority, and as a consequence all German schools in Southern Jutland were closed in the summer of 1945.From January 1946 special classes for German-speaking pupils were established in some of the public schools, but it was no success, partly because of local opposition from the Danish majority, and the classes were suspended in the summer of 1946. The private German schools were allowed to reopen from January 1946, but two other post-war laws, which weren’t intended to harm the German schools, in fact closed the schools, as the laws led to the confiscation of the school buildings. The first law resulted in the confiscation of all German property in Denmark. Because mortgages in some of the school buildings were owned by German juridical persons, the Danish custodian for German property seized the mortgages and required them redeemed. The second law intended to force Danish firms, which have had an unreasonable high profit by trading with and servicing the Germans, to repay to the Danish state the excess profit. It meant that the schools were asked to repay all the payments received over the German-Danish clearing account, and as they of course weren’t able to do this, the buildings were confiscated as security. The Danish public school only had the capacity to absorb 1⁄3 of the pupils from the German schools, and for that reason a large part of the children from the German minority couldn’t attend school until after the summer of 1946, where they were allowed entrance to the public school.The German school in Copenhagen, Sankt Petri School, wasn’t exposed to the same national hatred towards all Germans as the schools in Southern Jutland, even though a considerable part of the pupils were German citizens. The reason was probable, that the school was “less visible” in the Copenhagen environment, than the German schools in Southern Jutland. Sankt Petri School had drawn considerable larger amounts from the German-Danish clearing account than all the German schools in Southern Jutland together, most of it used to build a new prestigious school building in Copenhagen, the rest used to salaries to the teachers.Sankt Petri School wasn’t closed, but managed to hold on with a few pupils and by subordinating to the Danish demand, that teaching and examination were done in Danish.At last in 1949 the social democratic government was able to push through, that Sankt Petri School’s debt to the Danish state was eliminated, and from 1959 the school was again allowed to teach and examine in German. In 1949 too, the government allowed that German private schools in Southern Jutland reacquired 13 school buildings. But pupils were not allowed to pass exams, which were meritorious to further education in Denmark, and they were under strict supervision of the local authorities, – the supervision was eventually lifted in 1952.In 1955 the Danish Prime Minister H. C. Hansen and the German Chancellor Konrad Adenauer agreed on the Copenhagen-Bonn Declaration, concerning minority-rights on both sides of the German-Danish border. In this agreement German private schools in Southern Jutland were permitted to pass exams to their pupils, giving them right to further education in Denmark. That was the end of the struggle, equality between German and Danish private schools was a fact. But the struggle had been expensive for the German minority. The number of pupils has never since reached the heights of the period 1920–1945.Especially the social democrats Hartvig Frisch and H. C. Hansen were at the forefront in reestablishing the German schools, the strongest opposition coming from the political parties, Danmarks Kommunistiske Parti and Dansk Samling. Most of the Danish majority in Southern Jutland and a considerable part of the civil servants were against a reopening of the German schools, but the high ranking civil servants in the ministries followed the intentions of the various governments and did what they were told to do by their ministers, whether they were for or against reopening of German schools.

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26

Madirazza, Ivan, Bo Holm Jacobsen, and Niels Abrahamsen. "Late Triassic tectonic evolution in northwest Jutland, Denmark." Bulletin of the Geological Society of Denmark 38 (April 25, 1990): 77–84. http://dx.doi.org/10.37570/bgsd-1990-38-08.

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A model for the Late Triassic tectonic development in northwest Jutland is discussed in light of gravity, aeromagnetic and reflection seismic data. A wrench pull apart concept yields a simple explanation for both the present Zechstein basement configuration and the spatial distribution of salt structures in this part of the Danish basin.

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27

Penney, David Norman. "Ostracoda of the Holsteinian Interglacial in Jutland, Denmark." Danmarks Geologiske Undersøgelse Serie B 10 (June 1, 1987): 33–67. http://dx.doi.org/10.34194/serieb.v10.7077.

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Ostracoda are described from several marine Holsteinian deposits in Jutland, Denmark. The faunas are extremely uniform all over Jutland. Very little difference is seen between them and the faunas present in Late Elsterian deposits of the same area. They are largely boreal in aspect but contain a few species from warmer realms. With the exception of Callistocythere sp and Semicytherura sp, all the species are extant, though Carinocythereis whitei and Pterygocythereis coronata do not live in Danish inshore waters today. The environment at all the investigated localities was one of open, shallow waters (10-30 m depth) and normal marine salinities. No shallower water facies have as yet been identified. The Holsteinian ostracod faunas of Denmark are analogous to those recorded in North Germany, and show similarities to those reported from Mid-Pleistocene deposits in Great Britain.

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28

Chapman, Alfred Crawhall. "A Contribution towards the Ornithology of West Jutland." Ibis 36, no. 3 (April 3, 2008): 339–51. http://dx.doi.org/10.1111/j.1474-919x.1894.tb03563.x.

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29

Mowat, Robert J. C. "Jutland 1916: The archaeology of a naval battlefield." Mariner's Mirror 103, no. 2 (April 3, 2017): 246–47. http://dx.doi.org/10.1080/00253359.2017.1312169.

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30

Nudd, Derek. "The Battle of Jutland, Through a Looking-glass." Mariner's Mirror 105, no. 4 (October 2, 2019): 425–41. http://dx.doi.org/10.1080/00253359.2019.1665340.

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31

BOAS, NIELS AXEL. "Rude Mark—A Maglemosian Settlement in East Jutland." Journal of Danish Archaeology 5, no. 1 (January 1986): 14–30. http://dx.doi.org/10.1080/0108464x.1986.10589956.

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32

RICHTER, JANE. "Brown Bear (Ursus arctos) from Kainsbakke, East Jutland." Journal of Danish Archaeology 5, no. 1 (January 1986): 125–34. http://dx.doi.org/10.1080/0108464x.1986.10589962.

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33

ETHELBERG, PER. "Early Bronze Age Houses at Højgård, Southern Jutland." Journal of Danish Archaeology 5, no. 1 (January 1986): 152–67. http://dx.doi.org/10.1080/0108464x.1986.10589964.

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34

BOAS, NIELS AXEL. "Bronze Age Houses at Hemmed Church, East Jutland." Journal of Danish Archaeology 8, no. 1 (January 1989): 88–107. http://dx.doi.org/10.1080/0108464x.1989.10590021.

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35

ANDERSEN, SØREN H., and ERIK JOHANSEN. "An Early Neolithic Grave at Bjørnsholm, North Jutland." Journal of Danish Archaeology 9, no. 1 (January 1990): 38–58. http://dx.doi.org/10.1080/0108464x.1990.10590034.

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36

Lyle, Colin. "JUTLAND, OR A SECOND ‘GLORIOUS FIRST OF JUNE’?" Mariner's Mirror 82, no. 2 (January 1996): 190–99. http://dx.doi.org/10.1080/00253359.1996.10656595.

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37

Kaa, Elisabet, and Markil Gregersen. "Fatal poisonings in Jutland (Denmark) during the 1980s." International Journal of Legal Medicine 105, no. 3 (May 1992): 133–38. http://dx.doi.org/10.1007/bf01625164.

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38

Lindgaard Christensen, Jesper. "Constraints on Innovation Finance in North Jutland, Denmark." European Planning Studies 15, no. 9 (August 29, 2007): 1163–80. http://dx.doi.org/10.1080/09654310701529045.

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39

Knudsen, Lars Loumann, Hans-Henrik Lervang, Søren Lundbye-Christensen, and Anders Gorst-Rasmussen. "The North Jutland County Diabetic Retinopathy Study (NCDRS)." Acta Ophthalmologica 88, no. 4 (August 14, 2009): 443–48. http://dx.doi.org/10.1111/j.1755-3768.2009.01555.x.

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40

Yule, Paul A. "Early Bronze Age Tombs of Jebel Hafit. By Bo Madsen." Journal of the American Oriental Society 141, no. 2 (August 27, 2021): 501. http://dx.doi.org/10.7817/jaos.141.2.2021.brev005.

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The Early Bronze Age Tombs of Jebel Hafit. By Bo Madsen. Aarhus: Jutland Archaeological Society and Moesgaard Museum, 2017. Pp. 245, illus. DKK 350. [Distributed by Aarhus University Press]

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41

Madirazza, Ivan. "The influence of tectonics on the land forms in west Jutland, Denmark." Bulletin of the Geological Society of Denmark 49 (December 31, 2002): 63–72. http://dx.doi.org/10.37570/bgsd-2003-49-07.

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The structural development and its influence on the present land forms is discussed on the basis of the reflection seismic and gravity data. The study area covers the western part of Jutland which was not glaciated during the Weichselian and is delimited by two Weichsel main stationary lines: the line extending from west to east and the line extending from north to south (these two lines join at Dollerup). The southern border of the study area corresponds approximately to the northern limit of the buried Ringkøbing-Fyn High. In this part of west Jutland the base Zechstein faults can be traced to the surface where they control the drainage system. The faults are mainly NW-SE trending strike slip faults which are active also at the present time. Zechstein evaporates are present in the entire area discussed here.

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42

Rasmussen, E. S. "Sequence stratigraphie subdivision of the Oligocène and Miocene succession in South Jutland." Bulletin of the Geological Society of Denmark 43 (December 1996): 143–55. http://dx.doi.org/10.37570/bgsd-1996-43-14.

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The present study is based on seismic data and log interpretation from six wells located in the southern part of Jutland (Denmark). The Oligocène and Miocene succession has been subdivided into six depositional sequences. Most of the sequences are of Type 1. The development of the Oligocène and Miocene sequences suggests a strong relationship with glacio-eustatic sea-level variations. Each sequence consists of a lowstand systems tract, which either corresponds to detached prograding intervals or coarse-grained deposits, a transgressive systems tract, and a highstand systems tract. Changes in the overall pattern of the Oligocène and Miocene succession, however, suggest variation in elevation of the hinterland due to different uplift of Fenno-Scandia and Baltic Shields. The depositional environment was characterized by shelf and nearshore sediments in a rapidly changing environment where the shoreline migrated/retreated across South Jutland several times.

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Grabowski, Radoslaw. "Identification and delineation of settlement space functions in the south Scandinavian Iron Age: theoretical perspectives and practical approaches." Journal of Archaeology and Ancient History, no. 12 (February 13, 2023): 1–57. http://dx.doi.org/10.33063/jaah.vi12.136.

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This article presents an overview of methods used in south Scandinavian archaeology for identification and delineation of settlement space functions. The overview includes commonly utilised archaeological approaches, such as artefact distribution studies and inferences based on assessment of house and settlement morphologies, as well as archaeobotanical, geochemical and geophysical approaches to functional analysis. The theoretical potential and limitations of each presented functional parameter are outlined and thereafter applied and compared using material from five case study sites in east-central Jutland, Halland and Bohuslän. The presentation of the site of Gedved Vest in east-central Jutland also incorporates a comparison of two common approaches to geochemical sampling: 1) sampling and analysis of soil retrieved from feature fills, and 2) horizontal sampling of soil from the interface between the topsoil (A/ Ap) and the subsoil (C) - horizons along a pre-determined grid.

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Rahmani, Zakia, Aneta Kochanek, Jesper Johnsen Astrup, Jeppe Nørgaard Poulsen, and Parisa Gazerani. "Helmet-induced headache among Danish military personnel." Scandinavian Journal of Public Health 45, no. 8 (September 15, 2017): 818–23. http://dx.doi.org/10.1177/1403494817731417.

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Aims: External compression headache is defined as a headache caused by an external physical compression applied on the head. It affects about 4% of the general population; however, certain populations (e.g. construction workers and military personnel) with particular needs of headwear or helmet are at higher risk of developing this type of headache. External compression headache is poorly studied in relation to specific populations. This study aimed to investigate the prevalence and pattern of helmet-induced external compression headache among Danish military personnel of the Northern Jutland region in Denmark. Methods: Data acquisition was based on a custom-made questionnaire delivered to volunteers who used helmets in the Danish military service and who agreed to participate in this study. The military of the Northern Jutland region of Denmark facilitated recruitment of the participants. The questionnaires were delivered on paper and the collected (anonymous) answers (total 279) were used for further analysis. Results: About 30% of the study participants reported headache in relation to wearing a military helmet. Headache was defined as a pressing pain predominantly in the front of the head with an average intensity of 4 on a visual analogue scale of 0 (no pain) to 10 (worst pain imaginable). It was also found that helmets with different designs influenced both the occurrence of headache and its characteristics. Conclusions: This study is the first to demonstrate the prevalence and pattern of compression headache among military personnel in North Jutland, Denmark. The findings of this study call for further attention to helmet-induced external compression headache and strategies to minimize the burden.

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Rasmussen, Erik S., Karen Dybkjær, and Stefan Piasecki. "The Billund delta: a possible new giant aquifer in central and western Jutland." Geological Survey of Denmark and Greenland (GEUS) Bulletin 4 (July 20, 2004): 21–24. http://dx.doi.org/10.34194/geusb.v4.4773.

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The search for new, deep-seated drinking water resources in Denmark has increased significantly during the past five years as a result of the discovery of excessive amounts of nitrate, pesticides and other pollutants in shallow groundwater boreholes (e.g. Nygaard et al. 2004, this volume). To find and map these aquifers, a multidisciplinary sequence stratigraphic approach has successfully been applied to the Miocene deposits of southern Jutland, where especially the Odderup and Ribe Formations are known as a main aquifer for drinking water from several test wells (Rasmussen et al. 2002). Recently, a more systematic study of the Miocene succession in central and western Jutland has been initiated by the Geological Survey of Denmark and Greenland (GEUS) under contract with local authorities. It includes detailed sedimentological descriptions of outcrops, sedimentological andlog-interpretations of new stratigraphic boreholes and interpretation of new high-resolution seismic data (Fig. 1). A number of outcrops and wells have been studied palynologically, resulting in a detailed dinoflagellate cyst stratigraphy and in palynofacies interpretations. The results of these studies have been integrated in the regional geological and stratigraphic model (Fig. 2). Two new aquifers have been discovered: the Bastrup sand and the Billund sand. The Bastrup sand has already been exploited as a main aquifer in central and southern Jutland, and has been referred to either the Ribe or Odderup Formations. However, new stratigraphic results reveal that the Bastrup sand is a separate unit in the Miocene succession. The Billund sand is a deep-seated aquifer located more than 100 m and often more than 150 m deep, and is therefore not penetrated by standard water supply wells which rarely reach c. 100 m. The Billund sand was first revealed by multichannel seismic data deriving from former oil-exploration carried out in the Billund area (Fig. 3A). The resolution of these seismic data is very poor, but one interpretation of the dipping reflectors (clinoforms) seen in Fig. 3A was of a delta complex. This agrees with outcrop studies along the fjords of eastern Jutland which suggest that a spit complex was deposited in this area during the Early Miocene. The Billund sand was tested by the Vandel Mark well in 2001, which penetrated c. 40 m of sand at a depth of 200 m. The presence of a regional major sand body was later confirmed by new high-resolution seismic data and by the Billund and Løvlund wells in 2002. The Billund well penetrated 50 m of medium- to coarse-grained sand, and chemical tests of the water quality were good. However, a water supply well at Fjand in western Jutland has had problems with so-called ‘brown water’ – water enriched in organic matter (humus). Saline water may also be expected close to older deep-seated faults. This paper summarises the results of a mapping programme of the Billund sand initiated in the summer of 2003.

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Björnberg, Alf, and Ola Stockfelt. "Kristen Klatvask fra Vejle: Danish pub music, mythscapes and ‘local camp’." Popular Music 15, no. 2 (May 1996): 131–47. http://dx.doi.org/10.1017/s0261143000008084.

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The town of Skagen is situated on the northernmost tip of Jutland (i.e., mainland Denmark). This is a remote and crisis-stricken area by Danish standards: the capital, Copenhagen, is eight hours away by train, the County of Northern Jutland has the highest unemployment rates in Denmark, and in recent years the region has been the target of several development projects financed by European Union funds. However, geographically, Skagen's position is quite central in Scandinavia. Ferry routes connect the nearby port of Frederikshavn (40 kilometres/25 miles away) with such relatively large Scandinavian cities as Oslo (9 hours away by ferry) and Gothenburg (3½ hours away). The town can also be reached from the south of Norway via the ferry route between Kristiansand and Hirtshals (also 40 kilometres/25 miles from Skagen). By these and other routes, tourists from Norway and Sweden, as well as from other parts of Denmark, regularly invade the town, in the summer season roughly doubling its 15,000 population.

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Petersen, Jan Heegård. "Phonological Individuation in a Former Danish Settlement in South Dakota, USA." Journal of Germanic Linguistics 30, no. 2 (April 18, 2018): 97–133. http://dx.doi.org/10.1017/s1470542717000071.

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The article describes the manifestation and distribution of 15 phonological variables in a rural heritage language community in South Dakota, USA. I discuss to what extent dialect convergence has occurred in this former Danish settlement. The data sample encompasses speakers born in Northwest Jutland in Denmark, as well as speakers born in South Dakota to parents who emigrated from Northwest Jutland. The analysis shows that dialectal convergence has not occurred to any significant degree, in spite of what may be expected; speakers born in South Dakota have significantly more dialectal features in their speech than the speakers born in Denmark. The analysis also reveals a sizeable degree of inter-speaker variation within both groups, as well as a considerable variation between the variables with respect to how likely they are to be realized dialectally versus nondialectally. The results are discussed in relation to theories of shared linguistic repertoire and individuation in small speech communities.*

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Andersen, Liselotte Wesley, Magnus Jacobsen, Christina Vedel-Smith, and Thomas Secher Jensen. "Mice as stowaways? Colonization history of Danish striped field mice." Biology Letters 13, no. 7 (July 2017): 20170064. http://dx.doi.org/10.1098/rsbl.2017.0064.

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Species from the steppe region of Eastern Europe likely colonized northwestern Europe in connection with agriculture after 6500 BP. The striped field mouse ( Apodemus agrarius Pallas, 1783), is a steppe-derived species often found in human crops. It is common on the southern Danish islands of Lolland and Falster, which have been isolated from mainland Europe since approximately 10 300–8000 BP. Thus, this species could have been brought in with humans in connection with agriculture, or it could be an earlier natural invader. We sequenced 86 full mitochondrial genomes from the northwestern range of the striped field mouse, analysed phylogenetic relationships and estimated divergence time. The results supported human-induced colonization of Denmark in the Subatlantic or Subboreal period. A newly discovered population from Central Jutland in Denmark diverged from Falster approximately 100–670 years ago, again favouring human introduction. One individual from Sweden turned out to be a recent introduction from Central Jutland.

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Laursen, Jesper. "Jysk Arkæologisk Selskab i mere end 50 år." Kuml 50, no. 50 (August 1, 2001): 33–36. http://dx.doi.org/10.7146/kuml.v50i50.103099.

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The Jutland Archaeological SocietyFor more than fifty yearsThe Jutland Archaeological Society was founded in 1951 (figs. 1-2). According to the objects clause, it is the purpose of the society to ”support archaeological research through the largest possible participation of all interested. It should make archaeology accessible to the public by – among other things – publishing an annual and a number of scientific publications, by having yearly meetings, excursions to larger excavations and in any other way, which the governing body sees fit.”The Jutland Archaeological Society was therefore not meant to deal just with matters concerning Jutland, and if one looks at the activities of the society during the first ten years the object was obviously more extensive. Whereas more than half of the articles in the annual Kuml dealt with the Prehistory and Middle Ages in Denmark, the second half included the related disciplines of ethnology, ethnography, philology and science, and also classical archaeology and the archaeology of the Near East – the latter because of the Danish expeditions to the countries along the Arabian Gulf.One initiative, which helped in making the society known, was the institution of the J.J.A.Worsaae Medal in 1956 as a celebration of the fifth anniversary of the society. This is a gold medal and a sum of money, which is given for special merits within Nordic archaeology. One may have a critical approach to the fact that a narrow circle of colleagues are handing nice medals to each other. However, the institution of the Worsaae Medal with its stress on ”Nordic archaeology” has increased the public understanding of the Jutland Archaeological Society as the representative of a judicious mixture of local, national, Nordic and international interests (fig. 3).Another cunning move was made in connection with the fifth anniversary, when twenty-eight leading archaeologists from seventeen European countries and the Soviet Union, the United States, and Mexico were appointed corresponding members. At the tenth anniversary this list was supplemented by another eleven highly respected foreign scholars. The reason for appointing a person as a corresponding member was ”credits within archaeological research”, and by this move the society and its activities no doubt became known in the right places.From the start, summaries in the most common foreign languages in Kuml and in the monographs (which were later to an increasing extent published in a principal language) made the publications internationally accessible. Through the ordinary members abroad, the corresponding members and – not the least – the many exchange connections to archaeological institutions abroad, this was fully accomplished.Finally, another remarkable initiative should be mentioned, which only a few would connect with the Jutland Archaeological Society. This is the archaeological newsletter, which was started by the then museum keeper Harald Andersen. The name of this periodical is ”Skalk” (old Germanic for ”servant” or ”marshal”, later terming a prankster). This periodical set a fashion for a long row of popular magazines not only in Denmark, but also in our neighbouring countries (fig. 4). After just a few years, Skalk had more than 10.000 members. The number later rose to 60.000, and in 1963, Skalk was separated from the society and became an independent enterprise under Harald Andersen’s leadership.When drawing up the balance sheet for the first ten years of the Jutland Archaeological Society, one realises that not only did the society justify its existence, it also made itself known as a shining example, not just to the members, but to the archaeological environment as such. Starting from the provincial level, within a few years it had gained national, Nordic and international status. Setting off from a concept embracing the diversity of human life, the society settled on a wide history-of-culture approach to its activities and encouraged a fruitful, mutual inspiration rather than sterile and pent-up specialist delimitation.In time Kuml developed a specialist character with many, thoroughly prepared and well-documented find presentations (fig. 5). Not only did Kuml develop into one of our best-edited archaeological journals; it also differed in design from other publications. From 1958 it had a hard cover, and since 1970 the cover has been decorated with remarkable graphic variations on a theme presented in the volume concerned.Since 1951, various scholarly volumes have been published, four in the 1950s, four in the 1960s and seven in the 1970s. However, since then the number of publications has risen dramatically, with fifteen volumes in the 1980s and twenty-five from 1990 to 2000 (see the list of Jutland Archaeological Society publications in the back of this book). The explanation to this explosive development is partly the fact that a number of large excavation projects have begun to bear fruit – as for instance the investigations in the Arabian Gulf countries, in the valley of Illerup, and in Sarup – partly the increased excavation activity of archaeological institutions and the excavation boom experienced since the 1970s.What may then be expected from the Jutland Archaeological Society in the future? Apart from offering good lectures and exciting travels to near and remote places, the society must of course live up to the decisions of its objects clause, i.e. to support archaeological research and make archaeology accessible for the public by publishing an annual and larger scholarly publications.It is a sign of the times that the books in the scholarly publication series will play a large part in the society’s future activities. The publication demand is enormous, as the museum s have been excavating more than ever over the past twenty years and there are no signs of this developm entchanging.Jesper LaursenMoesgård MuseumTranslated by Annette Lerche Trolle

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Midwinter, M. J. "Commentary on “Surgical Experiences in the Battle of Jutland”." Journal of The Royal Naval Medical Service 100, no. 2 (June 2014): 144–47. http://dx.doi.org/10.1136/jrnms-100-144.

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Journal articles on the topic 'Jutland'

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