Academic literature on the topic '(1800-ca. 1840)'

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Journal articles on the topic "(1800-ca. 1840)"

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Gomes, F. "Africans and Petit Marronage in Rio de Janeiro, ca. 1800-1840." Luso-Brazilian Review 47, no. 2 (December 1, 2010): 74–99. http://dx.doi.org/10.1353/lbr.2010.0020.

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Zehnle, Stephanie. "“Where is My Region?” Geographical Representation and Textuality in Sokoto." Islamic Africa 9, no. 1 (May 7, 2018): 10–33. http://dx.doi.org/10.1163/21540993-00901002.

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This paper is devoted to geographical knowledge of the world and the definition of homeland and outland among the elite of the early Sokoto Caliphate (ca. 1800–1840). It argues that with the creation of a territorial jihadist state, geography became an important tool within religious and political discourses because in Sokoto warfare was predicated upon a precise mapping of the “Land of Islam” and the “Land of Unbelief”. The circulation of contradictory accounts about landscapes and rivers in the Sahel via medieval Arabic books, traders, pilgrims and soldiers, will receive special attention. The key argument is that written geographical accounts and cartography from Sokoto were not only restricted by the information available for this task, but also by the characteristics of the genres: texts can express uncertainties about concepts of space, in contrast, cartography requires geographical definition and spatial exactitude. This article is thus dedicated to the analysis of content and form of geographical discourses in the early Sokoto State by the comparison of texts and a map.
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Musser, Jordan. "Carl Czerny's Mechanical Reproductions." Journal of the American Musicological Society 72, no. 2 (2019): 363–429. http://dx.doi.org/10.1525/jams.2019.72.2.363.

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This article reassesses the “mechanical” style of playing featured in Carl Czerny's pedagogical works and keyboard arrangements—specifically, the Complete Theoretical and Practical Piano Forte School, op. 500 (1839), its supplementary text Letters to a Young Lady (ca. 1840), and the four-hand transcription of Beethoven's Symphony no. 9 in D Minor, op. 125 (the “Choral”). The first part of the article situates opus 500 within the larger pedagogical milieu of Biedermeier music culture and Johann Heinrich Pestalozzi's progressivist educational reforms, exploring the way it tasked predominantly women amateurs with assembling basic finger sensations in an exercise-by-exercise—“progressive”—fashion. I propose that this cumulative logic reflects an early-century epistemic norm—what Friedrich Kittler dubs a “mechanical program” of assembly and augmentation. The second part considers Czerny's transcription of the finale of Beethoven's Ninth from the perspective of ludo-musicology and cultural techniques media analysis, outlining the reductive and replicative—“reproductive”—techniques by which Czerny accommodated his former teacher's work to the hands he shaped in the private sphere. I argue that his pedagogies and transcriptions were recursively interrelated. Czerny was simultaneously a mechanic of the hand pedagogically and a mechanical reproducer of symphonies transcriptively, creating a multivalent corpus that forces us to rethink the media-theoretical concept of “mechanical reproduction” vis-à-vis “Discourse Network 1800.”
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Rhodes, R. H., N. A. N. Bertler, J. A. Baker, H. C. Steen-Larsen, S. B. Sneed, U. Morgenstern, and S. J. Johnsen. "Little Ice Age climate and oceanic conditions of the Ross Sea, Antarctica from a coastal ice core record." Climate of the Past 8, no. 4 (July 30, 2012): 1223–38. http://dx.doi.org/10.5194/cp-8-1223-2012.

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Abstract. Increasing paleoclimatic evidence suggests that the Little Ice Age (LIA) was a global climate change event. Understanding the forcings and associated climate system feedbacks of the LIA is made difficult by the scarcity of Southern Hemisphere paleoclimate records. We use a new glaciochemical record of a coastal ice core from Mt. Erebus Saddle, Antarctica, to reconstruct atmospheric and oceanic conditions in the Ross Sea sector of Antarctica over the past five centuries. The LIA is identified in stable isotope (δD) and lithophile element records, which respectively demonstrate that the region experienced 1.6 ± 1.4 °C cooler average temperatures prior to 1850 AD than during the last 150 yr and strong (>57 m s−1) prevailing katabatic winds between 1500 and 1800 AD. Al and Ti concentration increases of an order of magnitude (>120 ppb Al) are linked to enhanced aeolian transport of complex silicate minerals and represent the strongest katabatic wind events of the LIA. These events are associated with three 12–30 yr intervals of cooler temperatures at ca. 1690 AD, 1770 AD and 1840 AD. Furthermore, ice core concentrations of the biogenic sulphur species MS− suggest that biological productivity in the Ross Sea polynya was ~80% higher prior to 1875 AD than at any subsequent time. We propose that cooler Antarctic temperatures promoted stronger katabatic winds across the Ross Ice Shelf, resulting in an enlarged Ross Sea polynya during the LIA.
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Bickford, M. E., T. D. Mock, W. E. Steinhart III, K. D. Collerson, and J. F. Lewry. "Origin of the Archean Sask craton and its extent within the Trans-Hudson orogen: evidence from Pb and Nd isotopic compositions of basement rocks and post-orogenic intrusions." Canadian Journal of Earth Sciences 42, no. 4 (April 1, 2005): 659–84. http://dx.doi.org/10.1139/e04-064.

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U–Pb zircon ages from the exposed Sask craton are 2450–3100 Ma, from the Peter Lake Domain 2575–2640 Ma, and from rocks of the Trans-Hudson orogen 1840–1880 Ma. U–Pb monazite and zircon ages of post-orogenic pegmatites and aplites are 1770–1800 Ma. Common Pb and Sm–Nd isotopic compositions of post-orogenic intrusions, as probes of crust beneath the orogen, were compared to Sask craton rocks and ca. 1850 Ma orogenic rocks to infer the origin and subsurface distribution of the Sask craton within the internides of the Trans-Hudson orogen. Results show that post-orogenic intrusions within most of the Glennie Domain and Hanson Lake block were derived, at least in part, from Archean source materials, demonstrating that the Sask craton lies beneath Paleoproterozoic orogenic rocks present at the surface. In contrast, common Pb and Sm–Nd isotopic compositions from pegmatites and aplites of the La Ronge Domain are essentially identical with those of the Paleoproterozoic orogenic rocks into which they are intruded, indicating derivation by partial melting of similar rocks. Thus, if the Sask craton extended to the west beneath the La Ronge Domain, it was beneath the zone of melting that produced the post-orogenic intrusions, making it unlikely that the Sask craton is a detached part of the Hearne craton. Many samples from the Sask craton have elevated 208Pb/204Pb ratios, unlike Superior craton or Hearne craton rocks, suggesting that the Sask craton was derived from an exotic source, such as the Wyoming craton, which shares similar elevated 208Pb/204Pb ratios.
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LAWERGREN, Bo. "Oxus Trumpets, ca. 2200-1800 BCE." Iranica Antiqua 38 (January 1, 2003): 41–118. http://dx.doi.org/10.2143/ia.38.0.136.

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Fog, Dan. "Dansk musikhistorie og musikformidling ca. 1800-1950." Magasin fra Det Kongelige Bibliotek 10, no. 2 (September 1, 1995): 3–22. http://dx.doi.org/10.7146/mag.v10i2.66397.

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Holm, Daniel, and David Schneider. "40Ar/39Ar evidence for ca. 1800 Ma tectonothermal activity along the Great Falls tectonic zone, central Montana." Canadian Journal of Earth Sciences 39, no. 12 (December 1, 2002): 1719–28. http://dx.doi.org/10.1139/e02-069.

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Late Paleoproterozoic (1900–1600 Ma) tectonothermal activity on all borders of the Archean Wyoming Province has long been established by low-precision K–Ar and Rb–Sr studies. However, recent tectonic models advanced for supercontinent aggregation require improved constraints on the timing of tectonothermal activity along major boundaries. On its northwestern boundary, the Great Falls tectonic zone separates the Archean Wyoming and Hearne provinces. Recently published U/Pb ages and geochemical data reveal the presence of a Paleoproterozoic (ca. 1860 Ma) marginal-arc magmatic complex along a portion of the Great Falls tectonic zone in central Montana. We present nine new 40Ar/39Ar mineral ages (on hornblende and biotite) from these same arc rocks, which indicate ca. 1800 Ma thermal activity (>500°C) and subsequent rapid cooling to below 300°C by 1775 Ma. This new data set constrains the timing of Wyoming–Hearne collision to between 1860 and 1800 Ma and the timing of last significant tectonothermal activity of this portion of the Great Falls tectonic zone (1800–1775 Ma). We note that our data add to a growing geochronologic database indicating ca. 1800 Ma tectonothermal activity (via either initial suturing or continued tectonic activity) associated with Paleoproterozoic docking of the Wyoming Province with Laurentia.
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Sean P. Harvey. "Native Views of Native Languages: Communication and Kinship in Eastern North America, ca. 1800–1830." William and Mary Quarterly 75, no. 4 (2018): 651. http://dx.doi.org/10.5309/willmaryquar.75.4.0651.

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Tveit, Miriam. "Tinget i det nordlige Norge ca. 200-1800." Heimen 52, no. 02 (July 16, 2015): 98–100. http://dx.doi.org/10.18261/issn1894-3195-2015-02-02.

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Dissertations / Theses on the topic "(1800-ca. 1840)"

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Chutko, Per Ivar. "En temmelig vill en : Kontroverser om laks, ca 1800-2009." Thesis, Norges teknisk-naturvitenskapelige universitet, Institutt for tverrfaglige kulturstudier, 2011. http://urn.kb.se/resolve?urn=urn:nbn:no:ntnu:diva-13016.

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Laksen har hatt stor betydning for det norske folk i lang tid. I dag forbindes laksen i stor grad med lakseoppdrett. Lakseoppdrett spiller en viktig økonomisk rolle, både lokalt og nasjonalt. Næringen bidrar vesentlig til sysselsetting og verdiskapning langs kysten, og er samtidig en av landets viktigste eksportnæringer. Forståelsen av hva en laks ”er” og kontroversene om den har utviklet seg over tid. Etter hvert som myndighetene har forsøkt å forvalte og regulere fisket og fisken, i takt med samfunnsutviklingen og nyetablerte praksiser knyttet til fiske og fangst, har nye problem oppstått. Oppdrettsnæringen har vært gjenstand for kritikk i offentligheten. De senere årene har kritikken dreid seg blant annet om rømming av oppdrettslaks og spredning av lakselus. Lakselus har negative konsekvenser både for oppdrettsnæringen og for vill laksefisk. Lakselusproblematikken involverer mange aktører, ofte med motstridende interesser. Jeg viser hvordan laks har vært gjenstand for konflikt i et historisk perspektiv. Oppgaven tar for seg ulike interesser som har vært involvert, og hvordan ulike interesser og forståelser har preget reguleringen og forvaltningen av lakseressursene. Gjennom laksens historie kan man ikke bare følge en næringspolitisk utvikling, men også en miljøpolitisk utvikling.
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Petronis, Vytautas. "Constructing Lithuania : Ethnic Mapping in Tsarist Russia, ca. 1800-1914." Doctoral thesis, Stockholm : Södertörn : Stockholm : Acta Universitatis Stockholmiensis ; Södertörns högskola ; Almqvist & Wiksell [distributör], 2007. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-7163.

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Koudal, Jens Henrik. "For borgere og bønder : stadsmusikantvæsenet i Danmark ca. 1660-1800 /." København : Museum Tusculanums Forlag : Universitet, 2000. http://catalogue.bnf.fr/ark:/12148/cb37106873c.

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Sanders, Rachael Alison. "The social lives of elite Philadelphian women, ca. 1760-1800." Thesis, University of Cambridge, 2009. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.611388.

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Zachariou, Nicholas. "From missionary to merino: Identity, economy and material culture in the Karoo, Northern Cape, South Africa, 1800 - ca. 1870." Doctoral thesis, University of Cape Town, 2017. http://hdl.handle.net/11427/27553.

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This thesis addresses the 19th century sequence of Kerkplaats, a farm in the central Karoo, Northern Cape, South Africa. Over this period different colonialisms of varying power and effect were introduced. The first was to local Khoe, San and Griqua communities in the form of one of the first London Missionary Society stations in the early 19th century. A second phase between 1830 and 1860 was to sheep farmers of German, Dutch and mixed descent, who absorbed and moulded the increasing impacts of British influence and materiality into older worlds of cultural resilience and practice. From 1860, a third phase saw a flood of mass produced British goods enter the region, similar to other colonial contexts around the world. Amount, availability and choice changed significantly and provided the material substrate in which rural stock farmers re-expressed themselves within the growing stature of Empire. It is suggested that for some rural farmers, expressive cultural practice worked to underpin increased affluence brought by merino sheep farming for global markets. Through this sequence different expressions of identity, domesticity, and economic scale are assessed through a close reading of documentary and archaeological evidence. While the material opportunities through the 19th century are the result of global processes, how this material is understood has to consider local context. It is suggested that material expression and identity change is most dramatic from the middle of the 19th century, when patterns of consumption reflect the globalisation of British production.
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Hond, Jan de. "Verlangen naar het Oosten : oriëntalisme in de Nederlandse cultuur, ca. 1800-1920 /." Leiden : Primavera pers, 2008. http://catalogue.bnf.fr/ark:/12148/cb413441602.

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Holecek, Josef. "För musikens skull : studier i interpretativ gitarrspelteknik från tidsperioden ca 1800 - ca 1930, med utgångspunkt från gitarrskolor och etyder /." Göteborg : Göteborg universitet, 1996. http://catalogue.bnf.fr/ark:/12148/cb36963727p.

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Thisner, Fredrik. "Militärstatens arvegods : officerstjänstens socialreproduktiva funktion i Sverige och Danmark, ca 1720-1800 = Das Erbe des Militärstaates : die sozialreproduktive Funktion des Offizerdienstes in Schweden und Dänemark 1720-1800 /." Uppsala : Acta Universitatis Upsaliensis : Uppsala University Library [distributör], 2007. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-7897.

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Villanueva, Zandro Vasquez. "CULTURAL ENCOUNTERS AND TRANSFORMATION OF EARLY HISTORICAL POLITIES ON LUBANG ISLAND, THE PHILIPPINES, CA. A.D. 1200-1800." Diss., The University of Arizona, 2009. http://hdl.handle.net/10150/195058.

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This study explores the nature of culture contact experience of the early historical polities in the Philippines. The historical analysis and the result of the archaeological excavation at Lubang Island allows us to reexamine the entanglements of local populations against the colonial culture and how these entanglements have been perceived, mediated, and even transformed by the actions of native peoples in the past. The present study offers an alternative model for culture contact studies and how to generate questions about human behavior and interaction in the past by using critical analysis of ethnohistorical documents, archaeological data, and anthropological theory.Under the general model of culture contact study and colonialism, the archaeological study focuses on the documentation and analysis of a collection of artifacts and faunal remains excavated from a settlement-fortification site, believed to have been occupied and used from the early A.D. 1200s to the late A.D.1800s.In this dissertation, I use historical data to examine the historical trajectory of local polities on Lubang Island and situate them in a particular context where native people's interactions with other groups define their everyday actions as reflected in the archaeological record. I develop an alternative model using an agency-based approach that focuses on the relationships linking human actors and their behavior in the past. Such a model allows us to rethink the history of Lubang Island and its people according to how they acted and defined themselves. Moreover, the issues of complexity in small-scale polities in the Philipppines need to be teased out in order to elucidate the different levels and scales of complexity in the various historical contexts of early polities in Island Southeast Asia. Only then can we truly understand the variables involved in social reproduction and the ways in which early Filipinos lived and encountered cross-cultural interaction in the past.
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Rijken, Hendrik. "De Leidse lustwarande : de geschiedenis van de tuinkunst op kastelen en buitenplaatsen rond Leiden, ca. 1600-1800 /." Leiden : Primavera pers, 2005. http://catalogue.bnf.fr/ark:/12148/cb399906042.

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Books on the topic "(1800-ca. 1840)"

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Marco H. D. van Leeuwen. Bijstand in Amsterdam, ca. 1800-1850: Armenzorg als beheersings- en overlevingsstrategie. Zwolle: Waanders, 1992.

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Wettinger, Godfrey. Place-names of the Maltese Islands: Ca. 1300-1800. San Gwann (Malta): PEG, 2000.

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Place-names of the Maltese Islands: Ca. 1300-1800. San Gwann (Malta): PEG, 2000.

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Robert, Dankoff, Kut A. Turgut, and Weitenberg Joseph Johannes Sicco, eds. The versified Armenian-Turkish glossary by Kalayi, ca. 1800. Cleveland, Ohio: Cleveland State University Armenian Publications, 1996.

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Reid, Douglas Adam. Labour, leisure and politics in Birmingham, ca 1800-1875. Birmingham: University of Birmingham, 1985.

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Wettinger, Godfrey. Place-names of the Maltese Islands: Ca. 1300-1800. San Gwann (Malta): PEG, 2000.

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De fynske kornmøller og deres møllere ca. 1660-1800. [Odense]: Landbohistorisk selskab, 1985.

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Brown, A. Peter. The European symphony from ca. 1800 to ca. 1930: Great Britain, Russia, and France. Bloomington: Indiana University Press, 2008.

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Brown, A. Peter. The European symphony from ca. 1800 to ca. 1930: Great Britain, Russia, and France. Bloomington: Indiana University Press, 2008.

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Constructing Lithuania: Ethnic mapping in tsarist Russia, ca. 1800-1914. Stockholm: Stockholm University, 2007.

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Book chapters on the topic "(1800-ca. 1840)"

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Cobb, Cathy, and Harold Goldwhite. "ca. 1800–1848: The Professional Chemist." In Creations of Fire, 185–211. Boston, MA: Springer US, 1995. http://dx.doi.org/10.1007/978-1-4899-2770-5_10.

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Cobb, Cathy, and Harold Goldwhite. "ca. 1800–1848: Après Le Déluge." In Creations of Fire, 171–84. Boston, MA: Springer US, 1995. http://dx.doi.org/10.1007/978-1-4899-2770-5_9.

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Braun, Dietrich. "Vorzeit – bis ca. 1800." In Kleine Geschichte der Kunststoffe, 82–99. München: Carl Hanser Verlag GmbH & Co. KG, 2017. http://dx.doi.org/10.3139/9783446452428.003.

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Braun, Dietrich. "Vorzeit – bis ca. 1800." In Kleine Geschichte der Kunststoffe, 50–67. München: Carl Hanser Verlag GmbH & Co. KG, 2013. http://dx.doi.org/10.3139/9783446436862.003.

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Witter, Hermann. "Perspektiven der Psychiatrie (ca. 1800–1975)." In Unterschiedliche Perspektiven in der allgemeinen und in der forensischen Psychiatrie, 16–30. Berlin, Heidelberg: Springer Berlin Heidelberg, 1990. http://dx.doi.org/10.1007/978-3-642-75162-2_4.

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Batselé, Filip. "England Ca. 1650–1800: Neither Emancipated nor Fully Enslaved." In Liberty, Slavery and the Law in Early Modern Western Europe, 105–37. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-36855-5_4.

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Blakey, Ronald C., and Wayne D. Ranney. "The Cordillera’s Foundations: Paleoproterozoic and Mesoproterozoic Periods: Ca. 1800–1000 Ma." In Ancient Landscapes of Western North America, 55–62. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-59636-5_3.

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Oostindie, Gert. "Intellectual Wastelands? Scholarship in and for the Dutch West Indies up to ca. 1800." In Empire and Science in the Making, 253–80. New York: Palgrave Macmillan US, 2013. http://dx.doi.org/10.1057/9781137334022_11.

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Scheltjens, Werner. "The Dutch Republic as Example of Maritime Transport Services Clusters in Preindustrial Europe (ca. 1650-1800)." In Atti delle «Settimane di Studi» e altri Convegni, 209–27. Florence: Firenze University Press, 2019. http://dx.doi.org/10.36253/978-88-6453-857-0.12.

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By means of a comparative analysis of the ‘Dutch case’ with the Saintonge in South-West France and Bohuslän in South-West Sweden, this paper analyses the rise and decline of maritime services clusters in preindustrial Europe. The leading question for this comparative analysis is: Was the ‘Dutch case’ exceptional or can similar developments be recognised in other parts of Europe as well? A survey of the regional economic origins of communities of maritime transporters is combined with analyses of their operations and institutions. Relying on primary sources, the paper addresses the contribution of a great many ‘anonymous’ people, that literally connected the ‘nodes’ in international maritime trade networks, but whose contribution to the preindustrial European economy has been assumed a priori rather than thoroughly investigated.
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Vernet, Thomas. "East African Travelers and Traders in the Indian Ocean: Swahili Ships, Swahili Mobilities ca. 1500–1800." In Trade, Circulation, and Flow in the Indian Ocean World, 167–202. New York: Palgrave Macmillan US, 2015. http://dx.doi.org/10.1007/978-1-137-56624-9_9.

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Conference papers on the topic "(1800-ca. 1840)"

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Liedtke, Walter. "Optical instruments and realism in European art ca. 1400-1800." In Frontiers in Optics. Washington, D.C.: OSA, 2004. http://dx.doi.org/10.1364/fio.2004.fww2.

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Kim, See Darl, Youngho Jin, Soo Yong Park, and Yong Man Song. "An Evaluation of the Hydrogen Flammability and the Hydrogen Concentration in the Reactor Building for Wolsong 2." In 14th International Conference on Nuclear Engineering. ASMEDC, 2006. http://dx.doi.org/10.1115/icone14-89126.

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Following a core uncovery, the core will heat up and the fuel pin cladding will oxidize in the presence of steam. The reaction follows a parabolic rate law, and a significant cladding oxidation does not occur until the cladding temperature reaches approximately 1800° F. One of the products of the cladding oxidation reaction is hydrogen, which can accumulate in the PHTS if the PHTS is intact or in the reactor building if a pathway exists from the PHTS. If the hydrogen concentration reaches 4 to 6% in the reactor building (which is very possible following a significant core damage), the hydrogen can ignite and cause a spike in the reactor building pressure and temperature. If enough hydrogen is allowed to build up in the reactor building, the ignition of the hydrogen can lead to a pressure spike that exceeds the reactor building ultimate design pressure, thereby jeopardizing the reactor buildings integrity. Even if reactor building integrity is not jeopardized by a global hydrogen burn, the fact that a global hydrogen burn could occur will prevent the TSC from exiting the SAMG. Hydrogen generation and flammability is a concern throughout most of the guidelines in the Wolsong 2 (CANDU 6 type reactor) SAMG. The purpose of this paper is to define whether the hydrogen in the reactor building atmosphere is flammable, and to estimate the hydrogen concentration in the reactor building atmosphere based on an estimated oxidation percentage. For the Wolsong 2 this CA, four sets of hydrogen figures were developed for the case of no venting (no core/concrete interaction), a 15% venting (no core/concrete interaction), a 30% venting (no core/concrete interaction), and no venting (core/concrete interaction for 24 hours resulting in a 114°F superheat and a addition of non-condensable gases).
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