Academic literature on the topic 'Peary Arctic Expedition'

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Journal articles on the topic "Peary Arctic Expedition"

1

Junker, Clara. "Race to the Pole: Matthew Henson, Arctic Explorer." American Studies in Scandinavia 54, no. 2 (December 12, 2022): 62–87. http://dx.doi.org/10.22439/asca.v54i2.6740.

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In his memoir, A Negro Explorer at the North Pole (1912), Matthew Henson describes the toll of his and Peary’s race to the Pole. This record of the 1908-09 Arctic expedition complicates established understandings of the “Dash to the Pole” and his own role as Peary’s assistant. Donald B. Macmillan declared in How Peary Reached the Pole: The Personal Story of His Assistant (2008) that Peary could not have done it without Henson (275), whose text uncovers an accomplished writer and explorer at work. The complicated character of Robert E. Peary figures prominently in his pages, though in a less independent version than in other accounts. Henson details the highly skilled labor he performs in the Arctic, and his own personality and perceptions. He shares, to a degree, the value systems of his Commander and the white members of the expedition, including the emphasis on heroic masculinity. But he also inscribes his racial heritage into his memoir, and his close, if complex, relation to the Inughuit. The result of intricate balancing acts, Henson’s silences echo in his text, revealing what could not be articulated by an African American member of Peary’s legendary expeditions. Henson’s contemporaries paid little attention to his accomplishments, since white American and European explorers dominated the field of Arctic travel, but his contribution received more attention as the 20th Century progressed. His experience suggests the costs and the crises—personal, national, and international—of a contested icescape increasingly visible and accessible in the 21st Century.
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Wærp, Henning Howlid. "Sverdrup´s Arctic Adventures. Or: What makes an Expedition Report worth reading? – Otto Sverdrup: New Land. Four years in the Arctic Regions (1903)." Nordlit 12, no. 1 (February 1, 2008): 305. http://dx.doi.org/10.7557/13.1347.

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Otto Sverdrup, born 1854, is one of the main polar explorers in Norway. However he is much less known not only than Fridtjof Nansen and Roald Amundsen, but also than Hjalmar Johansen, who was a member of Nansen´s Fram expedition 1893-96, and also lesser known than Eivind Astrup, who took part in two of Robert Peary´s expeditons across northern Greenland in 1891-92 and 1893-94. Hjalmar Johansen and Eivind Astrup published their own accounts from the expeditons: Selv-anden paa 86°14'. Optegnelser fra Den Norske polarfærd 1893-96 (1898) and Blandt Nordpolens naboer (1895). Astrup´s book was reprinted in 1990 and 2004, and Johansen´s book was reprinted in 1942, 1949 and 2003. They are both included in the Polar Library, together with books by Nansen and Amundsen (the Polar Liberary is by Kagge publishing house).Otto Sverdrup´s polar expedition report New Land (Nyt land), a two volume work from 1903, from the second Fram expedition 1898-1902 to north-west Greenland and northern Canada, is in comparison never reprinted. He is not in the Polar library. And his name is among readers of travelogues very much forgotten. Why is this, and what kind of book is New Land?
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Blanchette, Robert A., Benjamin W. Held, Joel Jurgens, Amanda Stear, and Catherine Dupont. "Fungi attacking historic wood of Fort Conger and the Peary Huts in the High Arctic." PLOS ONE 16, no. 1 (January 26, 2021): e0246049. http://dx.doi.org/10.1371/journal.pone.0246049.

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Historic wooden structures in Polar Regions are being adversely affected by decay fungi and a warming climate will likely accelerate degradation. Fort Conger and the Peary Huts at Lady Franklin Bay in northern Ellesmere Island are important international heritage sites associated with early exploration in the High Arctic. Fort Conger, built by Adolphus Greely and expedition members during the First International Polar Year in 1881, was dismantled and used by Robert Peary and his expedition crew in the early 1900’s to build several smaller shelters. These historic structures remain at the site but are deteriorating. This investigation examines the fungi associated with wood decay in the historic woods. Soft rot was observed in all 125 wood samples obtained from the site. The major taxa found associated with the decayed wood were Coniochaeta (18%), Phoma (13%) Cadophora (12%), Graphium (9%), and Penicillium (9%) as well as many other Ascomycota that are known to cause soft rot in wood. Micromorphological observations using scanning electron microscopy of historic wooden timbers that were in ground contact revealed advanced stages of type I soft rot. No wood destroying Basidiomycota were found. Identification of the fungi associated with decay in these historic woods is a first step to better understand the unusual decomposition processes underway in this extreme environment and will aid future research to help control decay and preserve this important cultural heritage.
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Barr, W., and W. Blake. "The site of Fort Magnesia, Payer Harbour, Pirn Island, NWT." Polar Record 26, no. 156 (January 1990): 39–42. http://dx.doi.org/10.1017/s0032247400022750.

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ABSTRACTThe site of Fort Magnesia, the base hut of a three-man expedition to Payer Harbour, Pirn Island, in the Canadian Arctic, has recently been rediscovered by a party from the Geological Survey of Canada. Erected by Robert Stein's party in summer 1899, and used by them for two years, the hut was almost certainly moved to another site by Robert E. Peary for his over-wintering in 1901–02. Only fragments of the hut now remain. Five graves, probably of Peary's Eskimo helpers, are located nearby.
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Wamsley, Douglas W. "Albert L. Operti: chronicler of Arctic exploration." Polar Record 52, no. 3 (December 16, 2015): 276–93. http://dx.doi.org/10.1017/s0032247415000753.

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ABSTRACTThe great wave of immigrants to the United States during the late 1800s brought many talented individuals who enriched American culture and society. Notable among them stands the Italian-born artist, Albert L. Operti (1852–1927), a versatile painter, illustrator and sculptor. For much of his professional career, Operti served as a scenic artist for the Metropolitan Opera House and later as an exhibit artist for the American Museum of Natural History. However, he maintained an avid personal interest in polar explorers and the history of polar exploration, ultimately turning his artistic skills to the subject. Operti served as official artist for Robert E. Peary during his Arctic expeditions of 1896 and 1897, producing paintings, drawings and even plaster casts of the Inuit from the expedition. Over the course of his lifetime he painted a number of ‘great’ pictures depicting, in a factually accurate manner, important incidents in Arctic history along with numerous smaller paintings, sketches, illustrations and studies. The quality of his work never rivaled his more talented contemporaries in the field of ‘great’ paintings, such as the prominent artists William Bradford and Frederic Church. Nonetheless, Operti achieved some recognition in his time as a painter of historical Arctic scenes, but the full extent of his contributions are little known and have been largely unexamined. Unlike the explorers themselves whose legacy rests upon geographic or scientific accomplishments and written narratives, Operti's legacy stands upon the body of distinctive artwork that served to convey, in realistic and graphic terms, the hardships and accomplishments of those explorers. This article recounts the life of Operti and his role as an historian in disseminating knowledge of the polar regions and its explorers to the public.
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6

Van der Stijl, Frank W., and Greg Z. Mosher. "The Citronen Fjord massive sulphide deposit, Peary Land, North Greenland: discovery, stratigraphy, mineralization and structural setting." Geology of Greenland Survey Bulletin 179 (July 29, 1998): 1–44. http://dx.doi.org/10.34194/ggu-bulletin.v179.6270.

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The Citronen Fjord massive sulphide deposit in the Lower Palaeozoic of North Greenland is the world's most northerly base metal mineralization. Since discovery in 1993, it has been intensively investigated by geological and geophysical surveys, and by drilling. The deposit is generally flat lying with a thickness up to 50 m; it extends from outcrop level to depths of 300 m. Three main stratiform sulphide sheets occur within a 200 m thick stratigraphic sequence; these are composed of massive and bedded pyrite with variable amounts of sphalerite and minor galena. The proven mineralization is continuous over a strike length of at least 3 km with a maximum width of 500 m; an additional 5 km of mineralization along the same trend is suggested by geological mapping and gravity surveys. The total tonnage of sulphides is estimated to exceed 350 million tons. The overall base metal resource is estimated at 20 million tons of 7 per cent zinc, with a higher grade core of 7 million tons containing 9 per cent zinc and 1 per cent lead. The Citronen Fjord deposit is located at the eastern end of the Palaeozoic Franklinian Basin that extends through the Arctic Islands of Canada and across northern Greenland. Its discovery is an example of a successful exploration strategy based on regional evaluation, sparse but telltale surface mineralization observations and low-cost logistics: a skidoo-sledge expedition. The stratiform mineralization is hosted in the dark argillaceous rocks of the Amundsen Land Group of latest Ordovician to Early Silurian age that comprises a starved basin sequence of cherts and shales with siltstones and mudstones, punctuated by carbonate debris flow conglomerates derived from the nearby southern carbonate shelf. The Lower Palaeozoic strata at Citronen Fjord are part of the southern margin of the North Greenland Fold Belt characterized by southerly-facing folds and thrust faults. A new geological map of the Citronen Fjord area is presented featuring Cambrian, Ordovician and Silurian strata, with two north-south cross-sections illustrating the main structure. Twelve informally-named lithostratigraphic units are recognized and comments given on correlation to the regional stratigraphy. Tectonic contacts separate Lower Cambrian strata from the Ordovician-Silurian part of the succession. It is concluded that the Citronen Fjord stratigraphy could be of local development in a sub-basin controlled by syn-genetic faults. The lead-zinc deposit is interpreted to be of sedimentary-exhalative origin formed by the precipitation of sulphides from metal-bearing fluids introduced onto the sea-floor through underlying fractures. The significant components of this deposition model include the existence of a tensional tectonic regime, deep-seated fractures and a restricted sub-basin morphology. Massive to dendritic-textured pyrite is interpreted to represent vent-facies deposition while the bedded sulphides are taken to be the corresponding distal facies. The precise tectonic control of the fractures is debatable, as is the role of the so-called Navarana Fjord Escarpment - a palaeo-topographic feature marking the junction between shelf and trough that is assumed to lie immediately to the south of the Citronen Fjord.
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Van der Stijl, Frank W., and Greg Z. Mosher. "The Citronen Fjord massive sulphide deposit, Peary Land, North Greenland: discovery, stratigraphy, mineralization and structural setting." Geology of Greenland Survey Bulletin 179 (July 29, 1998): 1–44. http://dx.doi.org/10.34194/ggub.v179.6270.

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The Citronen Fjord massive sulphide deposit in the Lower Palaeozoic of North Greenland is the world's most northerly base metal mineralization. Since discovery in 1993, it has been intensively investigated by geological and geophysical surveys, and by drilling. The deposit is generally flat lying with a thickness up to 50 m; it extends from outcrop level to depths of 300 m. Three main stratiform sulphide sheets occur within a 200 m thick stratigraphic sequence; these are composed of massive and bedded pyrite with variable amounts of sphalerite and minor galena. The proven mineralization is continuous over a strike length of at least 3 km with a maximum width of 500 m; an additional 5 km of mineralization along the same trend is suggested by geological mapping and gravity surveys. The total tonnage of sulphides is estimated to exceed 350 million tons. The overall base metal resource is estimated at 20 million tons of 7 per cent zinc, with a higher grade core of 7 million tons containing 9 per cent zinc and 1 per cent lead. The Citronen Fjord deposit is located at the eastern end of the Palaeozoic Franklinian Basin that extends through the Arctic Islands of Canada and across northern Greenland. Its discovery is an example of a successful exploration strategy based on regional evaluation, sparse but telltale surface mineralization observations and low-cost logistics: a skidoo-sledge expedition. The stratiform mineralization is hosted in the dark argillaceous rocks of the Amundsen Land Group of latest Ordovician to Early Silurian age that comprises a starved basin sequence of cherts and shales with siltstones and mudstones, punctuated by carbonate debris flow conglomerates derived from the nearby southern carbonate shelf. The Lower Palaeozoic strata at Citronen Fjord are part of the southern margin of the North Greenland Fold Belt characterized by southerly-facing folds and thrust faults. A new geological map of the Citronen Fjord area is presented featuring Cambrian, Ordovician and Silurian strata, with two north-south cross-sections illustrating the main structure. Twelve informally-named lithostratigraphic units are recognized and comments given on correlation to the regional stratigraphy. Tectonic contacts separate Lower Cambrian strata from the Ordovician-Silurian part of the succession. It is concluded that the Citronen Fjord stratigraphy could be of local development in a sub-basin controlled by syn-genetic faults. The lead-zinc deposit is interpreted to be of sedimentary-exhalative origin formed by the precipitation of sulphides from metal-bearing fluids introduced onto the sea-floor through underlying fractures. The significant components of this deposition model include the existence of a tensional tectonic regime, deep-seated fractures and a restricted sub-basin morphology. Massive to dendritic-textured pyrite is interpreted to represent vent-facies deposition while the bedded sulphides are taken to be the corresponding distal facies. The precise tectonic control of the fractures is debatable, as is the role of the so-called Navarana Fjord Escarpment - a palaeo-topographic feature marking the junction between shelf and trough that is assumed to lie immediately to the south of the Citronen Fjord.
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8

Zonn, I. S. "Geographical space and cinema images of the white Arctic on a white screen (Part II)." Post-Soviet Issues 10, no. 1 (July 6, 2023): 80–102. http://dx.doi.org/10.24975/2313-8920-2023-10-1-80-102.

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The second part of the article is devoted to the consideration of two genres of Arctic fi lms — animal (faunal) and adventure. The basis for their implementation on the screen was Russian America, Alaska — the cinematic state of Hollywood, Chukotka and the Far North of Russia. The Arctic with its boundless snow-ice expanses and mythological obscurity forced its conquerors to seek and rely on a faithful friend — a dog — Siberian husky, husky, Alaskan malamute. As the polar explorer Robert Peary wrote, «life here is dog’s, but the work is worthy of a real person». Almost all the scripts of animal science fi lms are, borrowed from the literary works of the classics of the North — Jack London and James Curwood. Dogs and animals of the North have become full-fl edged actors of these fi lms. One of the pillars of the Arctic fi lms is adventures, including man’s struggle with the harsh nature of the Arctic, the formation of a new life for the indigenous peoples of the North, the search for missing expeditions and individuals — hunters, pilots, extreme athletes.
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Rapp, Hans Tore. "A monograph of the calcareous sponges (Porifera, Calcarea) of Greenland." Journal of the Marine Biological Association of the United Kingdom 95, no. 7 (November 15, 2013): 1395–459. http://dx.doi.org/10.1017/s0025315413001070.

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Greenland has more than 200 years of history of studies of the sponge fauna and is the type locality for a number of species. Many of these have not been encountered since, and as the type material has been hard to find or even lost, their taxonomic status has remained uncertain. In this study all species of calcareous sponges previously reported from Greenland are reviewed. The revision is based predominantly on new or unidentified material collected during various expeditions, but also on material used by previous authors. This includes samples from all coasts of Greenland, from the southernmost Kap Farvel area to Peary Land on the northern coast, some of the northernmost records of calcareous sponges ever. Greenland is a transition zone between the western and eastern Atlantic boreal calcareous sponge faunas, being home to species from both sides of the North Atlantic combined with some true Arctic species. There is also a strong link between the Canadian and Greenlandic sponge faunas. Twenty-eight species have been identified, from which six are new to Greenland and one is new to science. New records for Greenland are: Clathrina arnesenae (Rapp, 2006); Clathrina camura (Rapp, 2006); Clathrina pellucida (Rapp, 2006); Sycon abyssale Borojevic & Graat-Kleeton, 1965; Leucandra valida Lambe, 1900; and Sycettusa thompsoni (Lambe, 1900). Clathrina tendali sp. nov. has been described from western Greenland and Leucosolenia corallorrhiza (Haeckel, 1872) and Leucandra penicillata (Schmidt, 1869) have been resurrected. Keys for identification of higher taxa and the different species of Greenlandic Calcarea are provided.
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Nagy, Murielle. "Sex, lies and northern explorations: Recent books on Peary, MacMillan, Stefansson, Wilkins and Flaherty. CHRISTOPHER, Robert J., 2005 Robert and Frances Flaherty: A documentary life, 1883-1922, Montreal and Kingston, McGill-Queen’s University Press, 453 pages. JENNESS, Stuart E., 2004 The making of an explorer. George Hubert Wilkins and the Canadian Arctic Expedition 1913-1916, Montreal and Kingston, McGill-Queen’s University Press, 417 pages. MacMILLAN, Donald B., 2008 How Peary reached the Pole. The personal story of his assistant, introduction by Genevieve M. LeMoine, Susan A. Kaplan, and Anne Witty, Montreal and Kingston, McGill-Queen’s University Press, 307 pages. PÁLSSON, Gísli, 2005 Travelling passions. The hidden life of Vilhjalmur Stefansson, translated from the Icelandic by Keneva Kunz, Winnipeg, University of Manitoba Press, 374 pages." Études/Inuit/Studies 32, no. 2 (2008): 169. http://dx.doi.org/10.7202/038221ar.

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Dissertations / Theses on the topic "Peary Arctic Expedition"

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Phillips, Caroline J. "Eastern Canadian High Arctic exploration as an example of frontier change, with particular emphasis on the Robert Peary North Pole expeditions." 1988. http://hdl.handle.net/1993/16747.

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Books on the topic "Peary Arctic Expedition"

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Fairley, Gillis Kim, and Ayer Silas Hibbard, eds. Boreal ties: Photographs and two diaries of the 1901 Peary Relief Expedition. Albuquerque: University of New Mexico Press, 2002.

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Cook & Peary: The polar controversy, resolved. Mechanicsburg, PA: Stackpole Books, 1997.

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Austin, Horatio T. Sir, 1801-1865., ed. Additional papers relative to the arctic expedition under the orders of Captain Austin and Mr. William Perry. London: G.E. Eyre and W. Spottiswoode, 2001.

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Davis, Gwilym George, and Robert Neff Keely. In Arctic Seas: The Voyage of the Kite with the Peary Expedition. University of Cambridge ESOL Examinations, 2011.

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Heilprin, Angelo. Arctic Problem and Narrative of the Peary Relief Expedition of the Academy of Natural Sciences of Philadelphia. Creative Media Partners, LLC, 2018.

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Heilprin, Angelo 1853-1907. Arctic Problem and Narrative of the Peary Relief Expedition of the Academy of Natural Sciences of Philadelphia. Creative Media Partners, LLC, 2021.

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Davis, Gwilym George, and Robert Neff Keely. In Arctic Seas - The Voyage of the Kite with the Peary Expedition: Together with a Transcript of the Log of the Kite. Cambridge University Press, 2012.

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Keely, Robert N., and G. G. Davis. In Arctic Seas: The Voyage Of The Kite With The Peary Expedition, Together With A Transcript Of The Log Of The Kite. Kessinger Publishing, LLC, 2007.

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Keely, Robert N., and G. G. Davis. In Arctic Seas: The Voyage Of The Kite With The Peary Expedition, Together With A Transcript Of The Log Of The Kite. Kessinger Publishing, LLC, 2007.

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How Peary Reached the Pole: The Personal Story of His Assistant. McGill-Queen's University Press, 2008.

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Book chapters on the topic "Peary Arctic Expedition"

1

Genauer, Rebecca. "Frozen in Motion: Ethnographic Representation in Donald B. MacMillan’s Arctic Films." In Films on Ice. Edinburgh University Press, 2015. http://dx.doi.org/10.3366/edinburgh/9780748694174.003.0023.

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This chapter examines the explorer Donald MacMillan, who accompanied Robert Peary during the 1908-09 Polar expedition, and took tens of thousands of still photographs and exposed nearly 100,000 feet of motion picture footage during his long career as explorer, scientist, lecturer, and ethnographer. Four of MacMillan’s edited single-reel films – Hunting Musk-Ox with the Polar Eskimo (date unknown), Travelling with the Eskimos of the Far North (1930), Eskimo Life in South Greenland (filmed during a 1926 expedition), and Under the Northern Lights (circa 1928) –survive. Genauer’s chapter argues that MacMillan disavowed narrative and generic conventions of ethnographic representation, which allowed his films to break from the supposed verisimilitude characteristic of contemporary explorer films.
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Asma, Stephen T. "Flesh-Eating Beetles and The Secret Art & Taxidermy." In Stuffed Animals & pickled Heads, 3–46. Oxford University PressNew York, NY, 2001. http://dx.doi.org/10.1093/oso/9780195130508.003.0001.

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Abstract Collecting and Displaying natural history specimens is a more complex and dramatic activity than most museum visitors appreciate. The specimens themselves, for example, have intriguing and elaborate histories that largely go untold, because, unlike fine art objects, their individuality must be subjugated to the needs of scientific pedagogy. Generations of visitors at the American Museum of Natural History, for example, examined an Inuit skeleton as part of a general anthropology exhibit, unaware of the skeleton’s own peculiar history. In 1993 the American Museum of Natural History finally returned this particular skeleton, the remains of an Inuit man named Qisuk, to his descendants in western Greenland. Qisuk and other Inuits, including his six-year-old son, Minik, had been “acquired” as living specimens during an Arctic expedition in 1897. After polar explorer Robert Peary convinced the Inuits to return with him, the new emigrants found themselves housed in the basement of the American Museum of Natural History. Shortly after arriving, Qisuk died of tuberculosis, and unbeknownst to Minik, the museum staff removed Qisuk’s flesh, cleaned his bones, and put him on display for New York audiences. Some time later Minik, who originally had been told that his father’s bones had been returned home for proper burial, stumbled across his own father in an exhibit display case.
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