Relevant bibliographies by topics / Bunger Hills

Academic literature on the topic 'Bunger Hills'

Author: Grafiati
Published: 10 December 2022
Last updated: 28 January 2023

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Journal articles on the topic "Bunger Hills"

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Tucker, Naomi M., Martin Hand, and Chris Clark. "The Bunger Hills: 60 years of geological and geophysical research." Antarctic Science 32, no. 2 (February 27, 2020): 85–106. http://dx.doi.org/10.1017/s0954102019000403.

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AbstractCorrelation of Rodinian and Gondwanan crustal domains relies on a thorough knowledge of those vestiges preserved today. The Bunger Hills hold a critical place in East Antarctica, recording the Mesoproterozoic assembly of Australo-Antarctica in Rodinia and the Neoproterozoic–Cambrian amalgamation of Indo- and Australo-Antarctica in Gondwana. It is situated in a region of disputed overlap between the different components of Rodinia and Gondwana, where there is little consensus on the location of sutures in this region and thus often speculative geological interpretations. The Bunger Hills therefore provide an opportunity to better understand the tectonic setting and palaeogeography during the assembly of these supercontinents. Recent work has confirmed that the Bunger Hills are one of few rare outcrops in Wilkes Land, East Antarctica that can be directly correlated with the broader Musgrave–Albany–Fraser–Wilkes Orogen (MAFWO). Whilst other constituent terranes of the MAFWO have been intensely studied, our geological knowledge of the Bunger Hills was comparatively limited until recently. In light of recent geological and geophysical developments, this contribution serves as an updated and concise standalone reference for the present state of knowledge of the Neoarchean–Cambrian evolution of the Bunger Hills region.
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Gore, Damian B., and Michelle R. Leishman. "Salt, sediments and weathering environments in Bunger Hills." Antarctic Science 32, no. 2 (February 27, 2020): 138–52. http://dx.doi.org/10.1017/s0954102020000073.

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AbstractTerrestrial environments at Bunger Hills, East Antarctica, vary from vegetation-rich, little-weathered rock surfaces retaining glacial polish and striations near the glacier and ice-sheet margins to salty, vegetation-poor, extensively weathered regions near to and downwind of marine bays and inlets. Weathering forms include tafoni and orientated pits, which record former wind directions. Although salts are found all over Bunger Hills, the strongly weathered area is coincident with the distribution of halite (NaCl) and thenardite (Na2SO4), both of which are derived from seawater and marine salt spray. Salts elsewhere in Bunger Hills are either subglacial calcium carbonates or rock weathering products including gypsum (CaSO4⋅2H2O) and a range of rarer minerals. These other salt minerals do not weather rocks and sediment. The distribution of halite and thenardite acts as a major control on the geomorphology, sediment geochemistry and biogeography of Bunger Hills.
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Leishman, Michelle R., John A. E. Gibson, and Damian B. Gore. "Spatial distribution of birds and terrestrial plants in Bunger Hills." Antarctic Science 32, no. 2 (February 27, 2020): 153–66. http://dx.doi.org/10.1017/s0954102020000012.

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AbstractIn this paper, we synthesize recorded observations of moss, lichen and bird species in Bunger Hills, East Antarctica, and assess the role of environmental controls, including sediment, salinity, moisture and geology, on species' distributions. The distribution of snow petrels (Pagodroma nivea) appears to be associated with geology; they nest by preference in crevices in bedrock outcrops around the margins of the hills or wherever jointed cliffs are found. South polar skuas (Catharacta maccormicki) are seen throughout Bunger Hills, where they nest and prey on snow petrels. Mosses and lichens were most abundant around the ice margins where fresh snow and ice meltwater are abundant. In the central area of Bunger Hills, where the highest salt concentration in sediments is found and exposure to abrasion by wind-driven mineral sand grains and ice particles is greatest, mosses and lichens are reduced in abundance and diversity. Exposure of parts of Bunger Hills from the ice sheet throughout the Last Glacial Maximum, c. 20 ka bp, means that some land and lakes could have acted as regional refugia and as a locus of recolonization of other ice-free areas.
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Gore, Damian B., and Sonja Berg. "Bunger Hills: the hidden Antarctic oasis." Antarctic Science 32, no. 2 (February 27, 2020): 71. http://dx.doi.org/10.1017/s0954102020000115.

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Augustinus, Paul C., Damian B. Gore, Michelle R. Leishman, Dan Zwartz, and Eric A. Colhoun. "Reconstruction of ice flow across the Bunger Hills, East Antarctica." Antarctic Science 9, no. 3 (September 1997): 347–54. http://dx.doi.org/10.1017/s0954102097000424.

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In the Bunger Hills, mapping of glacial drift sheets and examination of striae patterns and other palaeo-ice flow direction indicators show that the largely ice-free region records the imprint of ice sheet expansion(s) during the late Cenozoic. In particular, ice moulded features and striae in southern Bunger Hills suggest formation during at least two episodes of ice sheet expansion, although whether they were formed during separate events or merely different phases of the same expansion of the ice sheet is not able to be discerned at present. The older event relates to thin ice with flow constrained by the topography, whilst the younger event relates to regional expansion of thick ice across the area. Discrimination of the order of emplacement of the cross-cutting striae patterns is possible at a number of sites. Palaeo-ice flow indicators confirm that ice sheet expansion over southern Bunger Hills was purely from the southern and eastern margins, although minor advances of the north-east flowing Edisto Glacier onto coastal areas occurred following retreat of the last extensive ice sheet phase.
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Colhoun, Eric A., and Donald A. Adamson. "Former glacial lakes of the Bunger Hills, Antarctica." Australian Geographer 20, no. 2 (November 1989): 125–35. http://dx.doi.org/10.1080/00049188908702984.

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Verkulich, Sergey R., and Achim Hiller. "Holocene deglaciation of the Bunger Hills revealed by 14C measurements on stomach oil deposits in snow petrel colonies." Antarctic Science 6, no. 3 (September 1994): 395–99. http://dx.doi.org/10.1017/s0954102094000593.

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Solidified stomach oil deposits in snow petrel colonies in the Antarctic proved to be suitable for 14C dating and provide important palaeobiogeographical and palaeoenvironmental information. Following earlier studies in the Untersee oasis (Central Dronning Maud Land) we present here 14C measurements on comparable deposits from the Bunger Hills (66°10′S, 101°E). The conventional 14C age of the basal layer reflects the occupation age of any particular nesting site and therefore a minimum age for the time when this area became ice-free. According to the 14C results the occupation of the southern part of the Bunger Hills by petrels started about 10000yr ago. The breeding colonies expanded continuously following local ice retreat. The most intensive phases of colonization seem to have been from 8–6 kyr BP and during the past 2 kyr.
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Gibson, John A. E., Damian B. Gore, and Enn Kaup. "Algae River: an extensive drainage system in the Bunger Hills, East Antarctica." Polar Record 38, no. 205 (April 2002): 141–52. http://dx.doi.org/10.1017/s0032247400017526.

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AbstractAn extensive terrestrial drainage system, centred on Algae Lake in southern Bunger Hills, is described. The 25-km-long Algae River is the third longest known in Antarctica after Onyx River (Wright Valley, Victoria Land) and Druzhby River (Vestfold Hills, Queen Elizabeth Land). Algae River receives meltwater from the Antarctic ice sheet, Apfel Glacier, and ephemeral and permanent snow banks in the ice-free area of the Bunger Hills. Water flows through a series of epiglacial lakes before reaching the extensive Algae Lake, which in turn has an outlet to Transkriptsii Gulf, a largely fresh-water, tidal epishelf lake connected to the ocean under the Edisto Ice Tongue and Shackleton Ice Shelf. Total flow from Algae Lake was estimated to be greater than 1 x 107 m3 a-1 from data collected in the 1986/87 summer. Some portions of the drainage system that were flowing during the 1946/47,1985/86, 1986/87, 1994/95, 1995/96, and 1998/99 summers were not flowing during the 1999/2000 summer, indicating the variable nature of discharge in the river and emphasising that parts of the drainage network may become disconnected readily.
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Gore, Damian B., John A. E. Gibson, and Michelle R. Leishman. "Human occupation, impacts and environmental management of Bunger Hills." Antarctic Science 32, no. 2 (February 27, 2020): 72–84. http://dx.doi.org/10.1017/s0954102019000348.

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AbstractThe types and distributions of anthropogenic rubbish have been documented at Bunger Hills, East Antarctica. The area has been the site of scientific research stations from 1958 to the present. Rubbish types include deliberately or negligently discarded items (gas cylinders, broken glass), abandoned unserviceable equipment (boats, vehicles, scientific equipment), spills (chemicals, fuel, oil) and the slow collapse of old buildings. Some rubbish remained where it was left, while other material was redistributed by strong winds. Modern expeditioner training should limit the production of new rubbish, while inadvertent wind dispersal of rubbish from old station buildings could be minimized by better management of these structures and their surrounds. Buildings and other constructed items need ongoing maintenance if they are not to break down and be distributed by wind, or they should be removed within a reasonable period.
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Augustinus, Paul C. "Weathering Characteristics of the Glacial Drifts, Bunger Hills, East Antarctica." Arctic, Antarctic, and Alpine Research 34, no. 1 (February 2002): 65. http://dx.doi.org/10.2307/1552510.

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Dissertations / Theses on the topic "Bunger Hills"

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Abelin, Bruna Arozi. "A SIMPLICIDADE MORDENTE DE UM PROTAGONISTA-ESCRITOR OUTSIDER: ESTUDO DE ASK THE DUST E DREAMS FROM BUNKER HILL DE JOHN FANTE." Universidade Federal de Santa Maria, 2015. http://repositorio.ufsm.br/handle/1/9934.

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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior
In Ask the Dust (1939) and Dreams from Bunker Hill (1983), John Fante (1909-1983) represents the obliterated side of American life during the Great Depression by making use of an apparently simple narrative style. Besides focusing on the importance of the marginal side of the United States in the 1930s, Fante presents young Arturo Bandini as the protagonist who survives in Los Angeles during the economic crisis and aims at becoming a great writer that contends for space in the cultural market of the metropolis of entertainment. Through obscene vocabulary and scenes, Fante represents the most negative aspects experienced by those who live in a metropolis, such as isolation, solitude, vice, and madness. Therefore, Fante s fiction has thematic and formal aspects that allow us to establish relations with the New Realism, a movement of the Arts in the first half of the twentieth century, which also crudely explored the negative aspects of life in the United States. Thus, this study discusses the potential meaningfulness of thematic and aesthetic aspects of Ask the Dust and Dreams from Bunker Hill, two novels that present the relation established by the writer, who is an outsider, with the city, the people, and the craft of writing in modern times.
Em Ask the Dust (1939) e Dreams from Bunker Hill (1983), John Fante (1909-1983) representa o lado esquecido da vida estadunidense durante o período da Grande Depressão por meio de uma estética aparentemente simples. Além de dar enfoque e devida importância ao lado marginal dos Estados Unidos da década de 1930, Fante apresenta como protagonista o jovem Arturo Bandini que, durante a crise econômica, sobrevive em Los Angeles com a ambição de ser um grande escritor que disputa espaço em meio ao mercado cultural da metrópole do entretenimento. Por meio de vocabulário e cenas marcadas por obscenidade, Fante cria representações dos aspectos mais negativos que a vida na metrópole pode proporcionar aos sujeitos, tais como isolamento, solidão, vícios e loucura. Assim, sua obra apresenta aspectos temáticos e formais que permitem aproximá-la do Novo Realismo, movimento das artes plásticas da primeira metade do século XX que também explorou de forma crua os aspectos negativos da vida nos Estados Unidos. Desse modo, discutem-se neste estudo significados potenciais dos aspectos temático-estéticos de Ask the Dust e Dreams from Bunker Hill, romances que abordam a relação do escritor outsider com a cidade, as pessoas e o ofício da escrita nos tempos modernos.
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Scott, John. "The structural setting of proterozoic gold mineralisation at the Bunkers Hill open cut mine, the Granites, Northern Territory /." Title page, abstract and contents only, 1993. http://web4.library.adelaide.edu.au/theses/09SB/09sbs427.pdf.

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Kolesik, P. "U–Pb geochronology of volcano–sedimentary moraine sediments of the Bunger Hills: implications for Mesoproterozoic evolution of East Antarctica." Thesis, 2016. http://hdl.handle.net/2440/120941.

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The Bunger Hills and adjacent areas of Wilkes Land and Queen Mary Land occupy the very western periphery of the Musgrave–Albany–Fraser Orogen, and represent one of the few exposures within east Antarctica with direct correlations to Australian constituent terrains of this continental-scale system. U–Pb analyses of detrital zircons from volcano–sedimentary moraine sediments of the Bunger Hills yield concordant 206Pb/238U ages ranging from ca. 1364 Ma to ca. 1040 Ma (n = 842), with a main late Mesoproterozoic magmatic zircon population clustered at ca. 1179–1161 Ma. Strong parallels with the time profile of in-situ rocks from the Stage 2 Albany–Fraser Orogen (AFO), the Bunger Hills and Windmill Islands, suggest these were the likely provenances for the associated moraine detritus. The Bunger Hills lie downstream from outcrops of the geographically inaccessible Sandow Group, which comprises clastic and mafic volcanoclastic rocks. It is interpreted that the sedimentary moraine materials of the Bunger Hills were derived from the glacial erosion of the Sandow Group supracrustal successions. The lithological character, sedimentary fill pattern and advanced diagenesis suggest that the Sandow Group formed within an active intra-continental rift-basin and represents the upper-crustal expression of extensional tectonism. Reconnaissance U–Pb geochronology of authigenic titanite suggests basin development occurred close to or within the time frame of the high-grade metamorphism recorded in the Bunger Hills. Therefore basin development was probably directly associated with the second major thermo–tectonic phase of the AFO (Stage 2; ca. 1215–1140 Ma). Due to the essentially non-metamorphosed volcano–sedimentary nature of the detritus in the sedimentary rocks, it seems likely that the evolving Mesoproterozoic orogenic system was not deeply exhumed during basin development.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2016
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Henry, Chuck, Sally Brown, Rufus Chaney, and Harry Compton. "Bunker Hill, ID : ecological restoration." 1998. http://hdl.handle.net/2429/10385.

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The Bunker Hill Superfund site in Idaho is the second largest in the nation. From smelting operations, soils on the mountainsides became severely acidic and contaminated with high concentrations of metals. Erosion from these hillsides, as well as an estimated 70 million tonnes of mine tailings were purposely dumped into the river; potentially depositing up to 700 million tonnes of contaminated sediment to the river. USDA, U of Washington, U of Idaho, and the Northwest Biosolids Management Association members installed Phases I and II of this demonstration in spring and fall 1997, consisting of surface application of "supermulch" to tailings and steep, eroded hillsides. Biosolids from King County, Everett, Tacoma and Cowlitz County, WA, and Post Falls, Hayden, and Coeur d'Alêne, ID were mixed with wood ash from Washington Water Power, Louisiana Pacific or Kimberly- Clark. Plant establishment has been dramatic, as well as there being reestablishment of soil microbial communities and evidence of wildlife usage, suggesting that these treatments are highly successful in revegetation and erosion control.
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Weiler, Emily A. "50 years after independence : preservation of places, spaces and memory." 2012. http://liblink.bsu.edu/uhtbin/catkey/1671231.

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This thesis will study three specific subjects in order to document changing viewpoints in American culture in relation to nationalism, patriotism, and memories from older generations. It will be studying a space- Bunker Hill, a place- Independence Hall and a person- Marquis Lafayette at approximately fifty years after the signing of the Declaration of Independence. Each subject will explore the ways the memory of the soldiers involved in the American Revolution have been preserved and remembered. It is the intent of this thesis to establish the importance of the passage of time especially when it comes to preserving historic artifacts and buildings and the way the changing associations have on how we preserve these artifacts.
The triumphal tour of Marquis Lafayette -- Independence Hall -- Bunker Hill Monument.
Department of Architecture
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Books on the topic "Bunger Hills"

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Bunker Hill. Naperville, Ill: Sourcebooks Landmark, 2010.

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Dreams from Bunker Hill. London: Panther, 1985.

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1949-, Garnier Philippe, and Matthieussent Brice 1950-, eds. Reves de Bunker Hill. Paris: Christian Bourgois, 1985.

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Tinney, Janet. Bunker Hill: A novel. Nashville: Highland Books, 2000.

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Ingram, Scott. The Battle of Bunker Hill. San Diego, Calif: Blackbirch Press, 2004.

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The Battle of Bunker Hill. New York: Macmillan/McGraw-Hill, 2006.

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The Battle of Bunker Hill. New York: PowerKids Press, 2003.

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The Battle of Bunker Hill. Ann Arbor, Michigan: Cherry Lake Publishing, 2013.

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Stratemeyer, Edward. The minute boys of Bunker Hill. Lake Wales, Fla: Lost Classics Book Co., 1996.

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Figley, Marty Rhodes. John Greenwood's journey to Bunker Hill. Minneapolis: Millbrook Press, 2010.

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Book chapters on the topic "Bunger Hills"

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Mirra, Carl. "From Bunker Hill to Baghdad: We Will Continue the Mission." In Soldiers and Citizens, 67–102. New York: Palgrave Macmillan US, 2008. http://dx.doi.org/10.1057/9780230617223_4.

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Abdrakhmanov, I. A., and Yu L. Gulbin. "Granulite from the Bunger Hills, Eastern Antarctica: Mineral parageneses and terms of metamorphism." In Advances in Raw Material Industries for Sustainable Development Goals, 70–77. CRC Press, 2020. http://dx.doi.org/10.1201/9781003164395-10.

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"Next, Bunker Hill." In The Provisional City. The MIT Press, 2001. http://dx.doi.org/10.7551/mitpress/5659.003.0056.

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"Goodbye, bunker hill." In John Fante's Ask the Dust, 290–95. Fordham University Press, 2020. http://dx.doi.org/10.1515/9780823287888-020.

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Fante, John. "Goodbye, Bunker Hill." In John Fante's Ask the Dust, 290–95. Fordham University Press, 2020. http://dx.doi.org/10.5422/fordham/9780823287864.003.0020.

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Written soon after Ask the Dust appeared in late 1939, this little-known piece of non-fiction by John Fante appeared in the Los Angeles Times. In it, Fante reminisces about his early days in Los Angeles, those days in the early 1930s when he was young and broke and often hungry but filled with dreams of literary greatness. He presents a gallery of character sketches of the people he lived amidst, from the drunk who lived next door in Fante’s beloved Bunker Hill rooming house to the generous Japanese grocer at Grand Central Market. Filled with feeling for a lost time and cherished memories, this piece reveals a side of John Fante that will captivate readers who want to learn more about the author of Ask the Dust.
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"4. Bunker Hill." In Tainted Earth, 73–110. Rutgers University Press, 2019. http://dx.doi.org/10.36019/9780813562803-007.

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Fante, John. "Goodbye, Bunker Hill." In John Fante's Ask the Dust, 290–95. Fordham University Press, 2020. http://dx.doi.org/10.2307/j.ctv102bj6q.22.

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Waters, Kristin. "“The Great Day Has Arrived” 1." In Maria W. Stewart and the Roots of Black Political Thought, 130–38. University Press of Mississippi, 2021. http://dx.doi.org/10.14325/mississippi/9781496836748.003.0014.

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"The Bunker Hill Young Marines." In African American Men in Crisis, 117–45. Routledge, 2012. http://dx.doi.org/10.4324/9780203054697-8.

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Tate, C. "The Bunker Hill Lead Smelter." In Environmental Ethics For Engineers, 87–90. CRC Press, 2018. http://dx.doi.org/10.1201/9781351071765-8.

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Conference papers on the topic "Bunger Hills"

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Green, Travis, Mark Moore, and W. Robert Hannen. "Stay Cable Vibration Testing at the Leonard P. Zakim Bunker Hill Memorial Bridge." In Structures Congress 2009. Reston, VA: American Society of Civil Engineers, 2009. http://dx.doi.org/10.1061/41031(341)59.

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Martínez-Medina, Andrés, Antoni Banyuls i Pérez, and Andrea Pirinu. "El “Muro Mediterráneo” en el territorio de la Marina Alta: búnkeres y baterías de la Guerra de España (1936-1939)." In FORTMED2020 - Defensive Architecture of the Mediterranean. Valencia: Universitat Politàcnica de València, 2020. http://dx.doi.org/10.4995/fortmed2020.2020.11338.

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The “Mediterranean Wall” in the territory of the Marina Alta: bunkers and batteries of the Spanish War (1936-1939)In 1936-1939 the War of Spain took place, turning its territory into the testing ground of Europe in anticipation of the Second World War; here new weapons were tested: mass media, propaganda and aviation. The national side used Mallorca as “aircraft carrier” from which it launched airstrikes on the Mediterranean coast: a rearguard that required fortification. To defend the cities, the Republican government ordered, in 1937, to build a coastal defensive system (“Mediterranean Wall”). On the Valencian coast there were ten basic enclaves: from the lighthouse of Castellón to the end of Santa Pola. This network of defenses had two built lines. The first was constituted by elements located at zero level, by the sea and on the beaches, which maintained regular distances from each other; these were reinforced concrete bunkers that sought to camouflage themselves. A second was formed by coastal and antiaircraft, concrete and masonry batteries that merged with the land, located in the hills to have a wider horizon and be closer to its objectives. Bunkers and batteries that followed geometric patterns in constant evolution. This communication studies the defensive settlements built by the Republican army in the cities of Xàbia and Dénia (Marina Alta), which had a port, airfield and armament factories, which made them the target of enemy aviation. In these territories many of these architectures have disappeared under real estate pressure, but there are still several bunkers, batteries and ammunition deposits that are intended to be inventoried and documented (especially the 7th of the Montgó and the 8th of the Portixol batteries) to insert into of the tradition of historical military forts (typological genealogies) and their understanding as a networked defensive system that maintains parallels with the system of coastal towers of the system of coastal towers of the Modern Age.
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Reports on the topic "Bunger Hills"

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Neal A. Yancey and Debby F. Bruhn. Bunker Hill Sediment Characterization Study. Office of Scientific and Technical Information (OSTI), December 2009. http://dx.doi.org/10.2172/971372.

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Rademacher, Steven E., and William V. Hoak. Radiological Characterization Survey Report, 1964 B-58 Accident Site, Grissom Air Reserve Base, Bunker Hill, Indiana. Fort Belvoir, VA: Defense Technical Information Center, May 2000. http://dx.doi.org/10.21236/ada379507.

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Rademacher, Steven E., and Brian Renaghan. Remedial Action and Final Radiological Status, 1964 B-58 Accident Site, Grissom Air Reserve Base, Bunker Hill, Indiana. Fort Belvoir, VA: Defense Technical Information Center, December 2000. http://dx.doi.org/10.21236/ada386876.

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Appraisal of ground-water quality in the Bunker Hill Basin of San Bernardino Valley, California. US Geological Survey, 1989. http://dx.doi.org/10.3133/wri884203.

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