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Artykuły w czasopismach na temat "B.C"

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Rue, David, David Webster i Alfred Traverse. "LATE HOLOCENE FIRE AND AGRICULTURE IN THE COPAN VALLEY, HONDURAS". Ancient Mesoamerica 13, nr 2 (lipiec 2002): 267–72. http://dx.doi.org/10.1017/s095653610213210x.

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Pollen and charcoal analysis of a 5.3-m sediment core from Aguada Petapilla, a peat bog, provides evidence of late Holocene vegetation and fire history in the Copan Valley, Honduras. Low concentration and preservation problems characterized the pollen flora, but there are taxa present indicative of major agricultural trends, including Zea mays. Microscopic charcoal fragments are well represented and record continued burning in the region since the lowest level of the core (5700 B.P. [3750 B.C.]). Presence of Zea indicates that maize farming was initiated by as early as 2300 B.C. Three peaks in charcoal-fragment frequencies occur in periods centered approximately at 900 B.C., 400 B.C., and A.D. 600. Fires in this relatively dry region of the southern Maya Lowlands (whose mean annual rainfall is about 1,400 mm) could have resulted from natural forest fires or human agricultural clearing at any time in the Holocene. This contrasts with wetter areas of tropical Central and South America (mean annual rainfall of about 2,500–4,000 mm) where significant climatic drying is required to ignite primary tropical forest.
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Wilbur, Terence H. "Northwest hispania ca. 1200 b.c. to 19 b.c." Mankind Quarterly 26, nr 3 (1986): 195–205. http://dx.doi.org/10.46469/mq.1986.26.3.1.

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Herbert-Brown, Geraldine. "Jerome's dates for Gaius Lucilius,satyrarum scriptor". Classical Quarterly 49, nr 2 (grudzień 1999): 535–43. http://dx.doi.org/10.1093/cq/49.2.535.

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TheChronicleof Jerome states that Gaius Lucilius was born in 148 B.C. and died in 103 B.C. in his forty-sixth year. TheOxford Classical Dictionary(1996) says that Gaius Lucilius was probably born in 180 B.C. and died in 102/1 B.C.
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Street-Perrott, F. A., R. A. Perrott i D. D. Harkness. "Anthropogenic Soil Erosion around Lake Patzcuaro, Michoacan, Mexico, during the Preclassic and Late Postclassic-Hispanic Periods". American Antiquity 54, nr 4 (październik 1989): 759–65. http://dx.doi.org/10.2307/280680.

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Lake Pátzcuaro (2,035 m asl), situated in the temperate highland-forest region of central Mexico, was the focus of Postclassic Tarascan civilization. Today, the lake is bordered by wide, swampy flats, which can be interpreted as low-angle fans of colluvial material derived from the deeply eroded, lower-valley side slopes. A gully near the northwest shore exposed two colluvial units: The lower one was dated at 2,300 years B.P. (350 B.C.) at the base of the exposure, while the upper one yielded three 14C ages ranging from 270 years B.P. (A.D. 1680) to "modern." Both units contained abundant charcoal. Pollen studies by Watts and Bradbury (1982) suggest that the first phase was initiated by the widespread introduction of maize cultivation around 1550 B.C. The second, more intense, phase of forest clearance, although it may have begun during the Late Postclassic period, probably culminated during the great expansion of colonial plough agriculture and livestock rearing in the late sixteenth and seventeenth centuries.
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Magny, Michel. "Successive Oceanic and Solar Forcing Indicated by Younger Dryas and Early Holocene Climatic Oscillations in the Jura". Quaternary Research 43, nr 3 (maj 1995): 279–85. http://dx.doi.org/10.1006/qres.1995.1034.

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AbstractThe recent extension of (1) the residual Δ14C curve back to 11,400 cal yr B.P. and (2) the lake-level reconstruction in the Jura back to ca. 13,500 cal yr B.P. offers the opportunity of testing by proxy data the relationships between climate, atmospheric 14C, the sun, and the ocean recently suggested from the atmospheric 14C record. The climatic significance of the Jura record is supported by correlations with climatic oscillations reconstructed in the Alps from glaciers and timberline movements. Correspondence between the 14C and paleoclimatic record from the Jura suggests a working hypothesis: two intervals within the Holocene can be distinguished in the middle latitudes of western and central Europe. An early Holocene period shows abrupt climatic oscillations linked to ocean forcing. Major colder climate phases developed between ca. 9000 and 8800, and between ca. 8000 and 7000 cal yr B.C. that coincide with higher Δ14C values. After 6000 cal yr B.C., a second period is characterized by smoother multicentury climatic oscillations linked to solar forcing.
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Fugami, Tracey. "B.C. and A.D." Afterimage 33, nr 4 (styczeń 2006): 43–44. http://dx.doi.org/10.1525/aft.2006.33.4.43.

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EAST, HARRY, i AMBER ADAMS. "B.C. VICKERY: BIBLIOGRAPHY". Journal of Documentation 44, nr 3 (marzec 1988): 205–15. http://dx.doi.org/10.1108/eb026825.

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Nagle, D. Brendan, i Keith R. Bradley. "Slavery and Rebellion in the Roman World, 140 B.C.-70 B.C." American Historical Review 96, nr 5 (grudzień 1991): 1516. http://dx.doi.org/10.2307/2165310.

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Bates, Richard L., i Keith R. Bradley. "Slavery and Rebellion in the Roman World, 140 B.C.-70 B.C." Classical World 84, nr 4 (1991): 333. http://dx.doi.org/10.2307/4350847.

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Harrington, J. Drew, i Michael C. Alexander. "Trials in the Late Roman Republic 149 B.C. to 50 B.C." Classical World 85, nr 6 (1992): 732. http://dx.doi.org/10.2307/4351164.

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Rozprawy doktorskie na temat "B.C"

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Wong, Wai-yi Winnie, i 黃慧怡. "A study of Empress Lu (241 B.C.-180 B.C.)". Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 1999. http://hub.hku.hk/bib/B31952471.

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Loube, Heather. "The "Metz Epitome": Alexander (July, 330 B.C.-July, 325 B.C.). A commentary". Thesis, University of Ottawa (Canada), 1995. http://hdl.handle.net/10393/10107.

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This historical commentary on the Metz Epitome, a late fragmentary account of Alexander's exploits, compares the work with the extant early Alexander historians. The sources of the anonymous author have much in common with the Cleitarchan historians, in particular, Diodorus Siculus and Quintus Curtius Rufus. Non-Cleitarchan elements in the text seem to reflect a certain affinity with a Hebraic tradition concerning Alexander. An examination of the author's methodology suggests that "epitome" is not an accurate description of the work in question. The anonymous author has achieved a unique portrait of Alexander and included information not found elsewhere. In view of its late authorship and the few new crumbs of historical fact it offers, the value of the Metz Epitome lies in its interpretation of Alexander's career rather than as a source for it.
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Wong, Wai-yi Winnie. "A study of Empress Lu (241 B.C.-180 B.C.) Lü hou yan jiu /". Click to view the E-thesis via HKUTO, 1999. http://sunzi.lib.hku.hk/hkuto/record/B31952471.

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Savela, Sarunas <1992&gt. "The conceptualisation of music in ancient Greek thought (V century B.C. – II century B.C.)". Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2022. http://amsdottorato.unibo.it/10446/1/The%20Conceptualisation%20of%20Music%20in%20Ancient%20Greek%20Thought.pdf.

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The focus of this dissertation is the analysis of the music-related philosophical passages from the 5th century B.C. to the 2nd century B.C. It aims to provide a multifaceted view towards music as a cultural phenomenon, which is based primarily on the philological and culturological explorations instead of the technical-musicological approach. The texts from our selected period attest that mousikē had an extremely broad conceptualisation which led to the attribution of the different, sometimes completely opposite value: from an insignificant performative practice to an activity which corresponds to the divine laws and directly affects the human soul. The discussed testimonia provide evidence of defining music both as an exclusively acoustic phenomenon and as a philosophically significant concept that oversteps the sonic definition. Our sources clearly demonstrate that mousikē was a polysemous term: it was understood as an interdisciplinary form of art (as the arts of the Muses), though it was also used to indicate the exclusively instrumental music or a philosophical concept, which does not necessarily define sound as its essential quality. The aim of this dissertation is to clarify the arguments behind each of these positions, to analyse whether such different modes of conceptualisation are compatible among themselves, and to see how they fit together into explaining what was understood as music in Antiquity. In this thesis we explore the conceptual framework of mousikē and analyse what enabled the musical thought to be worthy of the attention of the greatest philosophical minds. We will demonstrate that it was not the sound or the artistic practices that were central in the philosophical thought on music, but instead the embedded structural qualities that have correspondence to the universal proportions of the cosmic world and which are perceptible to the listeners through the medium of sound.
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Handley-Schachler, Iain-Morrison. "Achaemenid religion, 521-465 B.C". Thesis, University of Oxford, 1992. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.357523.

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Gaskell, Edmund James. "Peloponnesian politics : 371-361 B.C". Thesis, University of Liverpool, 2002. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.250555.

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Anderson, Wendy R. M. "The significance of Middle Nubian C-group mortuary variability, ca. 2200 B.C. to ca. 1500 B.C". Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1997. http://www.collectionscanada.ca/obj/s4/f2/dsk3/ftp04/nq29875.pdf.

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Anderson, Wendy R. M. "The significance of Middle Nubian C-Group mortuary variability, ca. 2200 B.C. to ca. 1500 B.C. /". Thesis, McGill University, 1996. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=41966.

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Several twentieth century archaeological expeditions to Lower Nubia recovered the skeletal and cultural remains of C-Group populations mainly from cemetery sites between Shellal and the Second Cataract. Along with the remains of the more or less contemporary Pangrave and Kerma peoples, the C-Group archaeological sequence was assigned to the Middle Nubian Period which lasted from the Sixth to the Eighteenth Egyptian Dynasties and is dated from ca. 2200 B.C. to ca. 1500 B.C. Conflicting interpretations of C-Group socioeconomic conditions are inevitable since no systematic analysis of the data resulting from the excavations of Middle Nubian cemeteries has ever been undertaken. In an attempt to assess the extent of C-Group economic contact with the Egyptians and to resolve the issue of possible growing social differentiation within the C-Group community, a quantitative analysis of the mortuary remains from fifteen C-Group cemeteries was undertaken. The results indicate that the flow of a small number of Egyptian artefacts into Lower Nubia was relatively constant and that contact between Lower Nubians and Egyptians was probably quite limited. Egyptian portrayals of constant fluctuation in Egyptian-Nubian political relations do not correspond with the evidence from the Nubian archaeological record. The analysis also indicated that economic inequality amongst the Middle Nubian population was present in each date category and tended to increase over time. Socioeconomic differences were greatest during the middle of the Second Intermediate Period. These findings indicate that the Middle Nubian socioeconomic system tolerated increasingly conspicuous differences amongst its members. They are not consistent with the hypothesis that no increase in differential access to burial resources occurred between ca. 2100 and ca. 1550 B.C. and that C-Group social and economic conditions remained virtually unchanged throughout their 800-year history.
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Anderson, Wendy Rose Marie. "The significance of Middle Nubian C-group mortuary variability ca. 2200 B.C. to ca. 1500 B.C. /". Ottawa : National Library of Canada, 1999. http://tinyurl.com/24snk.

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Leung, Ming-fong Selina. "A study of Li Guang (?-119 B.C.)". Click to view the E-thesis via HKUTO, 1995. http://sunzi.lib.hku.hk/hkuto/record/B31950899.

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Książki na temat "B.C"

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Craddock, Erik. B.C. mambo. New York: Random House Children's Books, 2009.

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Sanitan, B. C. B.C. Sanitan. Reading: B.C. Sanitan, 1986.

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M, Thom Ian, i Weder Adele 1961-, red. B.C. Binning. Vancouver: Douglas & McIntyre, 2006.

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British Columbia. Ministry of Environment and Parks., red. Maps-B.C.: Catalogue. [Victoria, B.C.]: BC Ministry of Environment and Parks, 1987.

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British Columbia. Ministry of Labour and Consumer Services. B.C. consumer educator. British Columbia: Queen's Printer for British Columbia, 1987.

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Thornicroft, Cassius. B.C. 2000 millennium. [Lusaka]: C. Thornicroft, 2000.

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McConnell, R. G. Texada Island, B.C. Ottawa: Govt. Print. Bureau, 1997.

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(Firm), MapArt. B.C. interior cities. Wyd. 2. [Whitby, Ont.]: Peter Heiler Ltd., 2000.

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Hydro, B. C. Public attitudes toward B.C. Hydro research report for B.C. Hydro. [Victoria: B.C. Hydro], 1988.

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Harlan, Michael. Roman Republican moneyers and their coins, 63 B.C.-49 B.C. London: Seaby, 1995.

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Części książek na temat "B.C"

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"Genesis: 4,000 B.C. OR 1,000,000 B.C.?" W Origin of the Human Species, 121–28. BRILL, 2001. http://dx.doi.org/10.1163/9789004493971_017.

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"1. B.C." W Terminated for Reasons of Taste, 5–70. Duke University Press, 2020. http://dx.doi.org/10.1515/9780822373896-003.

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Littauer, M. A., J. H. Crouwel i J. Morel. "Earlier Second Millennium B.C. (ca 2000-1600 B.C.)". W Wheeled Vehicles and Ridden Animals in the Ancient Near East, 48–72. BRILL, 1987. http://dx.doi.org/10.1163/9789004495593_010.

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Littauer, M. A., J. H. Crouwel i J. Morel. "Later First Millennium B.C. (ca 612-330 B.C.)". W Wheeled Vehicles and Ridden Animals in the Ancient Near East, 144–60. BRILL, 1987. http://dx.doi.org/10.1163/9789004495593_013.

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Littauer, M. A., J. H. Crouwel i J. Morel. "Later Second Millennium B.C. (ca 1600-1000 B.C.)". W Wheeled Vehicles and Ridden Animals in the Ancient Near East, 73–98. BRILL, 1987. http://dx.doi.org/10.1163/9789004495593_011.

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Littauer, M. A., J. H. Crouwel i J. Morel. "Later Third Millennium B.C. (ca 2375-2000 B.C.)". W Wheeled Vehicles and Ridden Animals in the Ancient Near East, 37–47. BRILL, 1987. http://dx.doi.org/10.1163/9789004495593_009.

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Littauer, M. A., J. H. Crouwel i J. Morel. "Earlier First Millennium B.C. (ca 1000-600 B.C.)". W Wheeled Vehicles and Ridden Animals in the Ancient Near East, 99–143. BRILL, 1987. http://dx.doi.org/10.1163/9789004495593_012.

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Melville, Herman. "Timoleon: (394 B.C.)". W The Writings of Herman Melville: The Northwestern-Newberry Edition, Vol. 11: Published Poems: Battle-Pieces; John Marr; Timoleon, redaktorzy Robert C. Ryan, Harrison Hayford, Alma A. MacDougall i G. Thomas Tanselle, 253–756. Northwestern University Press, 2009. http://dx.doi.org/10.1093/oseo/instance.00214333.

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Arnold, Kenneth R., Michael R. Rose i John C. Avise. "384–322 B.C". W Conceptual Breakthroughs in The Evolutionary Biology of Aging, 7–9. Elsevier, 2023. http://dx.doi.org/10.1016/b978-0-12-821545-6.00010-8.

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Davis, Paul K. "Zama 202 B.C." W 100 Decisive Battles, 47–50. Oxford University PressNew York, NY, 2001. http://dx.doi.org/10.1093/oso/9780195143669.003.0012.

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Abstract In 218 B.C., the Second Punic War had just gotten under way. Hannibal Barca, Carthaginian commander in Spain, had challenged Roman power in 219 B.C. by laying siege to the city of Saguntum. According to the treaty concluded at the end of the First Punic War, the city lay within a region recognized as under Carthage’s suzerainty, but the fact that Saguntum had a pro-Roman government brought a Roman declaration of war. Hannibal responded by capturing the city and then staging a brilliant forced march through the Pyrenees, southern Gaul (France), and through the Alps into northern Italy.
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Streszczenia konferencji na temat "B.C"

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Quane, Steve, Geoff Mullins i Tenea Dillman. "BATHYMETRY AND DYNAMICS OF GARIBALDI LAKE, B.C". W GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-284415.

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Papadopoulou, Konstantina. "3-dimensional bearing capacity envelopes of bridge shallow foundations on cohesionless soils and scour effects". W 7th International Conference on Road and Rail Infrastructure. University of Zagreb Faculty of Civil Engineering, 2022. http://dx.doi.org/10.5592/co/cetra.2022.1407.

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The effects of the combined loading on the bearing capacity (B.C.) shallow bridge foundations on cohesionless soil are investigated by 2D and 3D finite element analyses (F.E.A.), in conjunction with the main parameters involved, as the embedment depth. For the better visual understanding how the various loading or inherent parameters affect the ultimate B.C. the results of F.E.A. are presented as interaction diagrams of the normalized vertical load, moment and horizontal load. The scour effects on the B.C. of shallow foundation are investigated, through the normalized scour depth.
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Meyr, Katherine Irma. "EVALUATION OF WATER QUALITY IN THE TAKU WATERSHED, B.C". W 72nd Annual GSA Rocky Mountain Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020rm-346781.

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Суриков, И. Е. "Who was buried in the Melek-Chesmenski Tumulus?" W Древности Боспора. Crossref, 2023. http://dx.doi.org/10.25681/iaras.2020.978-5-94375-339-8.372-380.

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The tumulus in question belongs to the group of Bosporan royal tombs. The author suggests that, first, one of Paerisades I’s sons, who was named Gorgippus and died in 330es B.C. as a child, was buried in this tumulus; and, second, in 300es B.C. another Paerisades’ son, Satyrus II, who became the king after his father’s death but soon perished in a civil war, was also buried there.
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"About the institution [Dr. B.C. Roy Engineering College, Durgapur (BCREC)]". W 2012 National Conference on Computing and Communication Systems (NCCCS). IEEE, 2012. http://dx.doi.org/10.1109/ncccs.2012.6412969.

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Mulas, Marco, i Marcello Manna. "Exact outlet b.c. for steady supersonic flows - Application to cascades". W 12th Applied Aerodynamics Conference. Reston, Virigina: American Institute of Aeronautics and Astronautics, 1994. http://dx.doi.org/10.2514/6.1994-1835.

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Park, Choon B., Richard D. Miller, Jianghai Xia, Julian Ivanov, James A. Hunter, R. L. Good i R. A. Burns. "Multichannel analysis of underwater surface waves near Vancouver, B.C., Canada". W SEG Technical Program Expanded Abstracts 2000. Society of Exploration Geophysicists, 2000. http://dx.doi.org/10.1190/1.1815635.

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Zhang, Weibin, i Kimberly L. Turner. "Thermoelastic Damping in the Longitudinal Vibration: Analysis and Simulation". W ASME 2004 International Mechanical Engineering Congress and Exposition. ASMEDC, 2004. http://dx.doi.org/10.1115/imece2004-59898.

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The thermoelastic damping (TED), one of the main energy lost sources in MEMS and NMEMS, is analyzed for the longitudinal vibration mode. Two approximations based on the insulated thermal boundary condition (B.C.) and the modified fixed temperature B.C. are developed and compared. Until now, the highest reported experimental Q factors for the longitudinal vibrating MEMS device are still more than one order less than the predicted TED Q factors. Therefore, a numerical simulation approach is proposed and used for validation. The aim of this paper is to provide a prediction of TED for the fast developing bulk mode micro and sub-micro oscillators operating in a longitudinal vibrating mode.
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Sirles, Phil. "Seepage Investigation Using Geophysical Techniques at Coursier Lake Dam, B.C., Canada". W Symposium on the Application of Geophysics to Engineering and Environmental Problems 1997. Environment and Engineering Geophysical Society, 1997. http://dx.doi.org/10.4133/1.2922404.

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Chavez, Rene E. "Inversion of gravity data from the Laguna Salada Basin, B.C., Mexico". W SEG Technical Program Expanded Abstracts 1986. Society of Exploration Geophysicists, 1986. http://dx.doi.org/10.1190/1.1893152.

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Raporty organizacyjne na temat "B.C"

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Tod, J., i M. Pilkington. Regional Aeromagnetic Surveys in B.c. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/131235.

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McMechan, M. E., i R. A. Price. The B.C. Rockies: an overview. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2008. http://dx.doi.org/10.4095/225112.

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Shives, R. B. K., P. B. Holman i L. Rebolledo. Airborne geophysical survey, Fish Lake, B.C., 1995. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1995. http://dx.doi.org/10.4095/205345.

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Seemann, D. A., D. W. Halliday i J. F. Sweeney. Regional Gravity Survey, Williston Lake area, B.c. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/131228.

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Miles, F. W. Gravity-Bouguer anomalies, northern B.C., Yukon and N.W.T. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1994. http://dx.doi.org/10.4095/194286.

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Shives, R. B. K., P. B. Holman, L. Rebolledo i R. J. Hetu. Airborne geophysical survey, Mount Polley area, B.C., 1995. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1995. http://dx.doi.org/10.4095/205346.

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Harris, D. C. Mineralogy of the Sulphurets - Brucejack Lake area, B.c. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/131204.

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Ricketts, B. D. Sedimentology of the Lower Bowser Lake Group, B.c. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/131225.

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Rea, J., R. Knight i B. D. Ricketts. Ground penetrating radar, Brookswood aquifer, Lower Fraser Valley, B.C. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1994. http://dx.doi.org/10.4095/193981.

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Dunn, C. E. Trees and Seaweeds: Use As Metal Indicators, southern B.c. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/131197.

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