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Articles de revues sur le sujet « Peterhead »

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Auteur : Grafiati
Publié le 27 juillet 2024
Mis à jour le 28 juillet 2024

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1

Bertie, D. M. « A history of museums in Peterhead, Grampian Region, Scotland ». Geological Curator 6, no 4 (septembre 1995) : 149–55. http://dx.doi.org/10.55468/gc503.

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The geological collections of the Arbuthnot Museum, Peterhead, Grampian Region, have their origins in the private museum of Adam Arbuthnot (1775-1850) and the museum of the Peterhead Institute. The former was bequeathed to the town in 1850 and absorbed the latter in 1863. The present museum building was opened in 1893. The Arbuthnot Museum became part of North East of Scotland Museums Service in 1975; rationalisation across the Service saw geology displays concentrated instead at Banff Museum.
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2

Bertie, David M. « The Peterhead Institute, 1857-67 ». Northern Scotland 10 (First Serie, no 1 (mai 1990) : 47–71. http://dx.doi.org/10.3366/nor.1990.0005.

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3

DUNCAN, R. S., S. T. WHARTON et T. J. BOTTERILL. « A Replacement Outfall for Peterhead ». Water and Environment Journal 5, no 3 (juin 1991) : 265–71. http://dx.doi.org/10.1111/j.1747-6593.1991.tb00619.x.

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4

Buchan, Alex R. « SS Windward—whaler and Arctic exploration ship ». Polar Record 24, no 150 (juillet 1988) : 213–22. http://dx.doi.org/10.1017/s0032247400009177.

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AbstractWindward, a three-masted barque, was built in Peterhead in 1860 for the whaling trade, and fitted with steam engines in 1866. Almost every year for 33 years she visited the Arctic in pursuit of whales and seals, latterly belonging to the Grays, an outstanding Peterhead whaling family. Sold in 1894 to Captain Joseph Wiggins, she was bought later in the same year by Alfred Harmsworth for the use of Frederick G. Jackson in his exploration of Zemlya Frantsa-Iosifa (Franz Josef Land). Windward was Jackson's ship for three years, including one winter beset in the ice; journeying from her, Jackson substantially recharted Zemlya Frantsa-Iosifa, and the ship brought home Fridtjof Nansen after his epic drift with the polar ice. In 1897 Harmsworth offered the vessel to Robert Peary, who was planning an assault on the North Pole from the northern tip of Greenland or from Ellesmere Island. After four years with Peary, including two winters trapped in the ice, Windward returned to her roots in whaling from Scotland. She was lost in Davis Strait in 1907.
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Spence, Bill, Denise Horan et Owain Tucker. « The Peterhead-goldeneye Gas Post-combustion CCS Project ». Energy Procedia 63 (2014) : 6258–66. http://dx.doi.org/10.1016/j.egypro.2014.11.657.

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6

BUCHAN, AR, AM ROBERTSON et JM LEONARD. « DISCUSSION. PETERHEAD, SCOTLAND`S 100-YEAR HARBOUR OF REFUGE. » Proceedings of the Institution of Civil Engineers 78, no 5 (octobre 1985) : 1237–39. http://dx.doi.org/10.1680/iicep.1985.926.

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7

Strachan, Richard, Andrew Dunwell, A. Clarke, M. Cressey, C. McGill, R. Pelling et G. Warren. « Excavations of Neolithic and Bronze Age sites near Peterhead, Aberdeenshire, 1998 ». Proceedings of the Society of Antiquaries of Scotland 133 (30 novembre 2004) : 137–71. http://dx.doi.org/10.9750/psas.133.137.171.

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Several archaeological sites were located and excavated by the Centre for Field Archaeology, University of Edinburgh (CFA) during a watching brief associated with the construction of a c 13km gas pipeline from St Fergus to Peterhead, Aberdeenshire, in the summer of 1998. The discoveries comprised two Neolithic artefact scatters, Bronze Age structures and an enclosure, and two features akin to burnt mounds. Penspen Limited commissioned the work on behalf of Scottish Hydro-Electric plc.
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8

Sim, Joe. « Repressing the Living Dead : Penal Policy and the Peterhead Demonstration ». Critical Social Policy 7, no 1 (juin 1987) : 68–72. http://dx.doi.org/10.1177/026101838700700105.

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9

Cotton, Alissa, Lilian Gray et Wilfried Maas. « Learnings from the Shell Peterhead CCS Project Front End Engineering Design ». Energy Procedia 114 (juillet 2017) : 5663–70. http://dx.doi.org/10.1016/j.egypro.2017.03.1705.

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10

Gaston, Anthony J., Stephen A. Smith, Robert Saunders, G. Ilya Storm et Jane A. Whitney. « Birds and marine mammals in southwestern Foxe Basin, Nunavut, Canada ». Polar Record 43, no 1 (janvier 2007) : 33–47. http://dx.doi.org/10.1017/s0032247406005651.

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The southwestern part of Foxe Basin is a little known region of the Canadian Arctic, being difficult to access during the summer because of heavy and unpredictable ice conditions. Surveys of birds and marine mammals in the area were carried out by lightweight expeditions in the summers of 1994 and 1995, using sea-kayaks, as well as a Peterhead boat from the nearest community, at Repulse Bay. The area supports important populations of narwhal, bowhead whales and walrus, as well as significant concentrations of shorebirds, common eiders, black guillemots, and perhaps one third of the world's Thayer's gulls. New information was obtained on the status and abundance of these species and novel observations were made on the feeding ecology and breeding phenology of the gulls.
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11

Torsvik, T. H. « Paleomagnetic results from the Peterhead granite, Scotland ; implication for regional late Caledonian magnetic overprinting ». Physics of the Earth and Planetary Interiors 39, no 2 (juillet 1985) : 108–17. http://dx.doi.org/10.1016/0031-9201(85)90077-9.

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12

Holligan, Chris. « Life in a Forgotten Scottish Gulag : Punishment and Social Regulation in HM Peterhead Convict Prison ». Journal of Historical Sociology 31, no 2 (18 août 2017) : 165–81. http://dx.doi.org/10.1111/johs.12170.

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13

Grandi, Samantha, Marcella Dean et Owain Tucker. « Efficient Containment Monitoring with Distributed Acoustic Sensing : Feasibility Studies for the Former Peterhead CCS Project ». Energy Procedia 114 (juillet 2017) : 3889–904. http://dx.doi.org/10.1016/j.egypro.2017.03.1521.

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14

Ballin, Torben Bjarke, et Ian Suddaby. « Late Neolithic and Late Bronze Age lithic assemblages associated with a cairn and other prehistoric features at Stoneyhill Farm, Longhaven, Peterhead, Aberdeenshire, 2002–03 ». Scottish Archaeological Internet Reports, no 45 (2010) : 1–52. http://dx.doi.org/10.9750/issn.2056-7421.2011.45.1-52.

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Prehistoric remains were recorded by CFA Archaeology Ltd (CFA) in 2002–03 during a programme of fieldwork at the landfill site within the boundaries of Stoneyhill Farm, which lies 7km to the southwest of Peterhead in Aberdeenshire (NGR: NK 078 409). These included a clearance cairn with a Late Bronze Age lithic assemblage and a burial cairn, with Late Neolithic and Early Bronze Age lithics and Beaker ceramics. Other lithic scatters of similar date had no certain associations, although pits containing near-contemporary Impressed Wares were nearby. Additional lithic assemblages included material dated to the Mesolithic and Early Neolithic. What may be proto-Unstan Wares in an isolated pit were associated with radiocarbon dates (barley) of the first half of the 4th millennium BC. These findings represent a substantial addition to the local area's archaeological record and form an important contribution to the understanding of lithic technology and ceramics in earlier prehistoric Scotland.
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15

Busch, A., S. J. T. Hangx, J. D. Marshall et H. M. Wentinck. « Swelling clay minerals and containment risk assessment for the storage seal of the Peterhead CCS project ». International Journal of Greenhouse Gas Control 94 (mars 2020) : 102924. http://dx.doi.org/10.1016/j.ijggc.2019.102924.

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16

Paul, M. A., et L. M. Jobson. « Geotechnical properties of soft clays from the Witch Ground Basin, central North Sea ». Geological Society, London, Engineering Geology Special Publications 7, no 1 (1991) : 151–56. http://dx.doi.org/10.1144/gsl.eng.1991.007.01.12.

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AbstractThe Witch Ground Basin to the northeast of Peterhead is occupied by Late to Postglacial clays which reach a maximum thickness of over forty metres. High resolution seismic surveys have shown that the Sediments can be divided into two stratigraphic units on the basis of their acoustic signatures: the upper Witch Ground Formation shows in its lower part a finely detailed pattern of laterally continuous multiple reflectors, whereas the lower Swatchway and Coal Pit Formations present a disorganised signature in which few reflectors are continuous.Profiles of bulk density, water content and undrained shear strength have been obtained from two continuously sampled, adjacent boreholes which penetrated the sediments to a depth of forty metres. These show that the deposits of the Witch Ground Basin comprise a single geotechnical unit with the properties expected of a fine grained sediment of glaciomarine origin. The principal geotechnical properties change gradationally as a result of changes in composition and from selfweight compression. The different seismic signatures on which the basin stratigraphy is based are not reflected by major geotechnical changes within the sediment, but may well result from secondary features of the geotechnical profile.
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17

Erskine, Angus B., et Kjell-G. Kjær. « The polar ship Scotia ». Polar Record 41, no 2 (avril 2005) : 131–40. http://dx.doi.org/10.1017/s0032247405004237.

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The ship that the oceanographer Dr William Speirs Bruce used on the Scottish National Antarctic Expedition, 1902–04, was originally a sealer named Hekla, built in Norway in 1872. In 1889 the Norwegian skipper Ragnvald Knudsen explored the northeast coast of Greenland between latitudes 74° and 75°, and in 1891–92 the ship was used by the Danish naval officer, Lieutenant C. Ryder, to explore the inner recesses of Scoresby Sund, finally visiting Angmagssalik. In 1902, re-named Scotia and captained by Tam Robertson from Peterhead, she sailed to the Weddell Sea under the leadership of Bruce. The southern winter of 1903 was spent at Laurie Island in the South Orkney Islands, and in March–April 1904 the party discovered 150 miles of previously unknown coastline of the Antarctic continent, reaching a farthest south of 74°01′S, 22°00′W. An extensive programme of marine survey and biological research was carried out. Back in the UK, Bruce sold the ship, and she returned to sealing, based in Dundee until appointed to be the first international North Atlantic Ice Patrol ship after the tragedy of Titanic. The Great War caused her to become a freighter in the English Channel area until she caught fire and was burnt out on a sandbank in the Bristol Channel on 18 January 1916.
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18

Dean, Marcella, et Owain Tucker. « A risk-based framework for Measurement, Monitoring and Verification (MMV) of the Goldeneye storage complex for the Peterhead CCS project, UK ». International Journal of Greenhouse Gas Control 61 (juin 2017) : 1–15. http://dx.doi.org/10.1016/j.ijggc.2017.03.014.

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19

Capelotti, P. J. « Benjamin Leigh Smith's third Arctic expedition : Svalbard, 1873 ». Polar Record 46, no 4 (18 mars 2010) : 359–71. http://dx.doi.org/10.1017/s003224740999057x.

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ABSTRACTIn 1873, the British explorer Benjamin Leigh Smith concluded the private oceanographic and geographical explorations in the seas around Svalbard that he had begun in 1871 and continued in 1872. The logistics of the 1873 expedition, however, were far more complicated than those of the first two voyages. Rather than using a single ship as he had done with the sailing vessel Samson the previous summers, Leigh Smith chartered James Lamont's Arctic steamer Diana and employed Samson as a reserve supply tender. With the added supplies Samson afforded, Leigh Smith planned to round the northeast limit of Svalbard, which he had discovered in 1871, and survey Kong Karls Land. Among those invited to join to expedition was a twenty-three-year-old member of the Royal Engineers, Lieutenant Herbert C. Chermside, who would visit the Arctic for the first and last time in a long life of military service. It was to Chermside that Leigh Smith entrusted the keeping of the expedition's logbooks. These three unpublished journals, along with a log kept by Samson's captain, William Walker, provide details of an expedition that, while it failed in its primary objective to round Nordaustlandet, did succeed in relieving Adolf Erik Nordenskiöld's Swedish polar expedition beset near Mosselbukta. It also maintained an array of contacts with whalers and sealers, for example the Peterhead whaler David Gray and the Norwegian skipper Frederick Christian Mack, regarding local conditions around Svalbard. At Augustabukta, Chermside's observations of uplifted skeletons of remotely harvested whales give estimated death ranges of between 1569–1691 and 1764–1807. The expedition would end with a major island in Svalbard being named for Chermside.
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20

Moore, Kathryn L. « The Northeast of Scotland's Coastal Trading Links Towards the End of the Nineteenth Century Evidence from the daybook of three ports : Aberdeen, Peterhead and Gardenstown ». Journal of Scottish Historical Studies 21, no 2 (1 novembre 2001) : 95–120. http://dx.doi.org/10.3366/jshs.2001.21.2.95.

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Kjaer, Kjell-G., et Hilary Foxworthy. « The Arctic ship Danmark ». Polar Record 40, no 1 (janvier 2004) : 31–38. http://dx.doi.org/10.1017/s0032247403003231.

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The steam barque Danmark, used on Ludvig Mylius-Erichsen's expedition to northeast Greenland (1906–08), was originally a Scottish whaler named Sir Colin Campbell, built in 1855 in Sunderland. After nine years of whaling out of Peterhead, in 1865 Sir Colin Campbell started the transportation of cryolite from the mines of Ivigtut in southwest Greenland to the United States and several European ports. This trade lasted for 103 years, until 1968. In the early 1870s, the ship was sold to Norwegian owners, renamed Magdalena, fitted with a steam-engine, and used as part of the Tønsberg sealing fleet. In 1894 she was the ship in which Roald Amundsen made his first voyage to the Arctic. In 1905 Magdalena was chartered by the estate of William Ziegler for a relief expedition to Bass Rock, northeast Greenland, to search for members of the Fiala-Ziegler expedition. The next year she was sold to the Danmark-Expedition and renamed Danmark. The main task for the expedition was to survey the coast from 77°N to Independence Bay, an area that was completely unknown. In addition to geographical exploration, much ethnographical, ornithological, zoological, hydrographical, meteorological, and botanical work was carried out on the expedition. In 1909, Danmark was sold to the mining company Grønlandske Minedrifts Aktieselskab of Copenhagen. She made voyages every year to Greenland, returning with copper and graphite. In 1916 she was chartered by the American Museum of Natural History to bring home the members of the Crocker Land Expedition. When in December 1917 she returned to Denmark, her captain did not know that, in their two years' absence, the coastal signals had been changed due to conditions in World War I. Danmark grounded off Høganes, Sweden; condemned, she was sold to a breaker's yard, and her masts, sails, engine, and other fittings were sold at auction the following year.
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Karlsson, Rikard, Malin Tivefälth, Iris Duranović, Svante Martinsson, Ane Kjølhamar et Kari Mette Murvoll. « Artificial hard-substrate colonisation in the offshore Hywind Scotland Pilot Park ». Wind Energy Science 7, no 2 (4 avril 2022) : 801–14. http://dx.doi.org/10.5194/wes-7-801-2022.

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Abstract. Artificial substrates associated with renewable offshore energy infrastructure, such as floating offshore wind farms, enable the establishment of benthic communities with a taxonomic composition similar to that of naturally occurring rocky intertidal habitats. The size of the biodiversity impact and the structural changes in benthic habitats will depend on the selected locations. The aim of the study is to assess colonisation and zonation, quantify diversity and abundance, and identify any non-indigenous species present within the wind farm area, as well as to describe changes in the epifouling growth between 2018 and 2020, with regards to coverage and thickness. This article is based on work undertaken within the offshore floating Hywind Scotland Pilot Park, the first floating offshore wind park established in the world, located approximately 25 km east of Peterhead, Scotland. The floating pilot park is situated in water depths of approximately 120 m, with a seabed characterised predominantly by sand and gravel substrates with occasional patches of mixed sediments. The study utilised a work class remotely operated vehicle with a mounted high-definition video camera, deployed from the survey vessel M/V Stril Explorer. A total of 41 structures, as well as their associated sub-components, including turbines substructures, mooring lines, suction anchors and infield cables, were analysed with regards to diversity, abundance, colonisation, coverage and zonation. This approach provides comprehensive coverage of whole structures in a safe and time-saving manner. A total of 11 phyla with 121 different taxa were observed, with macrofauna as well as macroalgae and filamentous algae being identified on the different structures. The submerged turbines measured approximately 80 m in height and exhibited distinct patterns of zonation. Plumose anemones (Metridium senile) and tube-building fan worms (Spirobranchus sp.) dominated the bottom and mid-sections (80–20 m) of the turbines, while kelp and other Phaeophyceae with blue mussels (Mytilus spp.) dominated top sections of the turbines (20–0 m). A general increase in the coverage of the epifouling growth between 2018 and 2020 was observed, whereas the change in thickness between years was more variable.
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23

Stewart, D. Bruce, Jeff W. Higdon, Randall R. Reeves et Robert EA Stewart. « A catch history for Atlantic walruses (Odobenus rosmarus rosmarus) in the eastern Canadian Arctic ». NAMMCO Scientific Publications 9 (15 décembre 2014) : 219. http://dx.doi.org/10.7557/3.3065.

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Knowledge of changes in abundance of Atlantic walruses (Odobenus rosmarus rosmarus) in Canada is important for assessing their current population status. This catch history collates available data and assesses their value for modelling historical populations to inform population recovery and management. Pre-historical (archaeological), historical (e.g., Hudson Bay Company journals) and modern catch records are reviewed over time by data source (whaler, land-based commercial, subsistence etc.) and biological population or management stock.Direct counts of walruses landed as well as estimates based on hunt products (e.g., hides, ivory) or descriptors (e.g., Peterhead boatloads) support a minimum landed catch of over 41,300 walruses in the eastern Canadian Arctic between 1820 and 2010. Little is known of Inuit catches prior to 1928, despite the importance of walruses to many Inuit groups for subsistence. Commercial hunting from the late 1500s to late 1700s extirpated the Atlantic walrus from Quebec and the Atlantic Provinces, but there was no commercial hunt for the species in the Canadian Arctic until ca. 1885. As the availability of bowhead whale (Balaena mysticetus) declined, whalers increasingly turned to hunting other species, including walruses. Modest numbers (max. 278/yr) were taken from the High Arctic population in the mid-1880s and large catches (up to 1400/yr) were often taken from the Central Arctic population from 1899 -1911, while the Foxe Basin stock (Central Arctic population) and Low Arctic population were largely ignored by commercial hunters. Land-based traders (ca. 1895-1928) continued the commercial hunt until regulatory changes in 1928 reserved walruses for Inuit use. Since 1950, reported walrus catches have been declining despite a steady increase in the Inuit population. Effort data are needed to assess whether lower catches stem from declining hunter effort or decreased walrus abundance. The recent take of walruses by sport hunting has been small (n=141, 1995-2010), sporadic and local.These landed catch estimates indicate the minimum numbers of walruses removed but do not account for under-reporting or lost animals that were killed but were not secured. Unreported and lost animals may represent a significant fraction of the total removals and must be considered in any modelling exercise. The sources, quality and completeness of the catch data vary widely over time and space and between the different hunt types. This variability confounds interpretation and contributes to the uncertainty that needs to be incorporated into any modelling. The data on Inuit subsistence catches before ca. 1928 are particularly fragmentary and uncertain.
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24

Macdonald, David. « MERRITT, J. W., AUTON, C. A., CONNELL, E. R., HALL, A. M. & ; PEACOCK, J. D. 2003. Cainozoic geology and landscape evolution of north-east Scotland. Memoir for the drift editions of 1:50 000 geological sheets 66E Banchory, 67 Stonehaven, 76E Inverurie, 77 Aberdeen, 86E Turriff, 87W Ellon, 87E Peterhead, 95 Elgin, 96W Portsoy, 96E Banff and 97 Fraserburgh (Scotland). Edinburgh : British Geological Survey. x+178 pp.+CD-ROM. Price £40.00 (paperback). ISBN 0 85 272463 2 ». Geological Magazine 142, no 2 (mars 2005) : 226. http://dx.doi.org/10.1017/s0016756805370786.

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25

« Repressing the living dead : penal policy and the Peterhead demonstration ». Critical Social Policy 7, no 19 (juin 1987) : 68–72. http://dx.doi.org/10.1177/026101838700701905.

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26

Ballin, Torben, Ian Suddaby, M. Cressey, M. Hastie, A. Jackson et M. Johnson. « Late Neolithic and Late Bronze Age lithic assemblages associated with a cairn and other prehistoric features at Stoneyhill Farm, Longhaven, Peterhead, Aberdeenshire, 2002-03 ». Scottish Archaeological Internet Reports 45 (1 janvier 2011). http://dx.doi.org/10.9750/issn.1773.3803.2010.45.

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Prehistoric remains were recorded by CFA Archaeology Ltd (CFA) in 2002-03 during a programme of fieldwork at the landfill site within the boundaries of Stoneyhill Farm, which lies 7km to the southwest of Peterhead in Aberdeenshire. These included a clearance cairn with a Late Bronze Age lithic assemblage and a burial cairn, with Late Neolithic and Early Bronze Age lithics and Beaker ceramics. Other lithic scatters of similar date had no certain associations, although pits containing near-contemporary Impressed Wares were nearby. Additional lithic assemblages included material dated to the Mesolithic and Early Neolithic. What may be proto-Unstan Wares in an isolated pit were associated with radiocarbon dates (barley) of the first half of the fourth millennium bc. These findings represent a substantial addition to the local area's archaeological record and form an important contribution to the understanding of lithic technology and ceramics in earlier prehistoric Scotland.This paper is dedicated to the memory of Ian Shepherd, whose site visits enlightened this and other projects undertaken by one of the authors (IS).
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27

Williams, Gerhild S. « Resisting Pluralization and Globalization in German Culture, 1490–1540 : Visions of a Nation in Decline By PeterHess, Berlin/Boston : DeGruyter, 2020, ix + 389 pp. $115.99 (ebook & ; hardcover), ISBN 978‐3‐11‐067462‐0 ». German Quarterly, 17 mai 2023. http://dx.doi.org/10.1111/gequ.12345.

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