Verbi a supporto nel latino tardo: il caso di facio

2020 ◽  
Vol 59 (1-4) ◽  
pp. 145-160
Author(s):  
Giovanbattista Galdi
Keyword(s):  
Direct Object ◽  
Late Period ◽  
Present Contribution ◽  
Verbal Noun ◽  
Verb Constructions ◽  
History Of ◽  
Semantic Evolution

SummarySupport verb constructions are documented throughout the history of Latin. These syntagms are characterized by the presence of a support verb with a more or less reduced semantic force, and a predicative (abstract or verbal) noun that often constitutes its direct object. The present contribution deals, specifically, with the use of facio as a support verb (as in bellum facere, iter facere, insidias facere etc.), focussing on the post-classical and late period. Two main questions shall be discussed: (a) whether, and if so, how facio becomes more productive in later centuries in both non-Christian and Christian sources; (b) what type of semantic evolution the verb undergoes in later Latin and whether, in this respect, continuity or rupture should be assumed with regard to the earlier period. This last point will enable us to suggest a more convincing explanation of an often-quoted passage of Cicero (Phil. 3. 22), in which the expression contumeliam facere is found.

On the use of facio as support verb in late and Merovingian Latin

2018 ◽  
Vol 17 (2) ◽  
pp. 231-257 ◽  
Author(s):  
Giovanbattista Galdi
Keyword(s):  
Direct Object ◽  
Late Period ◽  
Present Contribution ◽  
Verbal Noun ◽  
Verb Constructions ◽  
History Of ◽  
Semantic Evolution

Abstract Support verb constructions are documented throughout the history of Latin as well as other (typologically also irrelated) languages. As shown in several studies, such constructions are characterized by the presence of a support verb exhibiting a more or less reduced semantic force, and a predicative (abstract or verbal) noun that often constitutes its direct object. The present contribution deals, specifically, with the use of facio as support verb (as in bellum facere, iter facere, insidias facere, etc.), focussing on the post-classical and late period. In particular, three questions shall be investigated: (i) whether, and if yes, how facio increases its popularity in later centuries both in non-Christian and Christian sources; (ii) how is the spread of use of facio-support verb constructions in the Mulomedicina Chironis and in the Itinerarium Egeriae to be accounted for; (iii) what type of semantic evolution does the verb undergo in later Latin and whether, in this respect, continuity or rupture should be assumed with regard to the archaic and classical periods. This last point will enable us to suggest a more convincing explanation for an often-quoted passage of Cicero (Phil. 3,22), in which the construction contumeliam facere occurs.

Metasedimentary rocks, intrusions and deformation history in the south-east part of the c. 1800 Ma Ketilidian orogen, South Greenland: Project SUPRASYD 1996

1997 ◽  
pp. 60-65
Author(s):  
Adam A. Garde ◽  
Brian Chadwick ◽  
John Grocott ◽  
Cees Swager
Keyword(s):  
Field Work ◽  
Deformation History ◽  
The South ◽  
Present Contribution ◽  
East Part ◽  
Metasedimentary Rocks ◽  
Deformational History ◽  
Base Camp ◽  
History Of ◽  
Geological Map

NOTE: This article was published in a former series of GEUS Bulletin. Please use the original series name when citing this article, for example: Garde, A. A., Chadwick, B., Grocott, J., & Swager, C. (1997). Metasedimentary rocks, intrusions and deformation history in the south-east part of the c. 1800 Ma Ketilidian orogen, South Greenland: Project SUPRASYD 1996. Geology of Greenland Survey Bulletin, 176, 60-65. https://doi.org/10.34194/ggub.v176.5063 _______________ The south-east part of the c. 1800 Ma Ketilidian orogen in South Greenland (Allaart, 1976) is dominated by strongly deformed and variably migmatised metasedimentary rocks known as the ‘Psammite and Pelite Zones’ (Chadwick & Garde, 1996); the sediments were mainly derived from the evolving Julianehåb batholith which dominates the central part of the orogen. The main purpose of the present contribution is to outline the deformational history of the Psammite Zone in the region between Lindenow Fjord and Kangerluluk (Fig. 2), investigated in 1994 and 1996 as part of the SUPRASYD project (Garde & Schønwandt, 1995 and references therein; Chadwick et al., in press). The Lindenow Fjord region has high alpine relief and extensive ice and glacier cover, and the fjords are regularly blocked by sea ice. Early studies of this part of the orogen were by boat reconnaissance (Andrews et al., 1971, 1973); extensive helicopter support in the summers of 1992 and 1994 made access to the inner fjord regions and nunataks possible for the first time.A preliminary geological map covering part of the area between Lindenow Fjord and Kangerluluk was published by Swager et al. (1995). Hamilton et al. (1996) have addressed the timing of sedimentation and deformation in the Psammite Zone by means of precise zircon U-Pb geochronology. However, major problems regarding the correlation of individual deformational events and their relationship with the evolution of the Julianehåb batholith were not resolved until the field work in 1996. The SUPRASYD field party in 1996 (Fig. 1) was based at the telestation of Prins Christian Sund some 50 km south of the working area (Fig. 2). In addition to base camp personnel, helicopter crew and the four authors, the party consisted of five geologists and M.Sc. students studying mafic igneous rocks and their mineralisation in selected areas (Stendal et al., 1997), and a geologist investigating rust zones and areas with known gold anomalies.

History of Recording Demotic Epigraphy

2020 ◽  
pp. 491-507
Author(s):  
Jan Moje
Keyword(s):  
Nineteenth Century ◽  
Seventh Century ◽  
First Century ◽  
Third Century ◽  
Late Period ◽  
Greco Roman ◽  
Rosetta Stone ◽  
Roman Egypt ◽  
History Of ◽  
Twenty First Century

This chapter gives an overview of the history of recording and publishing epigraphic sources in Demotic language and script from the Late Period to Greco-Roman Egypt (seventh century bce to third century ce), for example, on stelae, offering tables, coffins, or votive gifts. The history of editing such texts and objects spans over two hundred years. Here, the important steps and pioneering publications on Demotic epigraphy are examined. They start from the beginning of the nineteenth century, when Napoleon’s expedition to Egypt found the Rosetta stone, until the twenty-first century.

scholarly journals Interrogating the Egypto-Sudanic Arabic Connection

Languages ◽  
2021 ◽  
Vol 6 (3) ◽  
pp. 123
Author(s):  
Thomas A. Leddy-Cecere
Keyword(s):  
The Novel ◽  
Present Contribution ◽  
Phonological Processes ◽  
Verbal Inflection ◽  
Segmental Phonology ◽  
Language Data ◽  
History Of ◽  
Novel Method ◽  
Dialect Classification ◽  
Arabic Speaking

The Arabic dialectology literature repeatedly asserts the existence of a macro-level classificatory relationship binding the Arabic speech varieties of the combined Egypto-Sudanic area. This proposal, though oft-encountered, has not previously been formulated in reference to extensive linguistic criteria, but is instead framed primarily on the nonlinguistic premise of historical demographic and genealogical relationships joining the Arabic-speaking communities of the region. The present contribution provides a linguistically based evaluation of this proposed dialectal grouping, to assess whether the postulated dialectal unity is meaningfully borne out by available language data. Isoglosses from the domains of segmental phonology, phonological processes, pronominal morphology, verbal inflection, and syntax are analyzed across six dialects representing Arabic speech in the region. These are shown to offer minimal support for a unified Egypto-Sudanic dialect classification, but instead to indicate a significant north–south differentiation within the sample—a finding further qualified via application of the novel method of Historical Glottometry developed by François and Kalyan. The investigation concludes with reflection on the implications of these results on the understandings of the correspondence between linguistic and human genealogical relationships in the history of Arabic and in dialectological practice more broadly.

scholarly journals Different Tectonic Evolution of Fast Cooling Ophiolite Mantles Recorded by Olivine-Spinel Geothermometry: Case Studies from Iballe (Albania) and Nea Roda (Greece)

Minerals ◽  
2022 ◽  
Vol 12 (1) ◽  
pp. 64
Author(s):  
Micol Bussolesi ◽  
Giovanni Grieco ◽  
Alessandro Cavallo ◽  
Federica Zaccarini
Keyword(s):  
Tectonic Evolution ◽  
Early Stage ◽  
Mineral Chemistry ◽  
Northern Greece ◽  
Present Contribution ◽  
Cooling Rates ◽  
History Of ◽  
Ferrian Chromite ◽  
Fast Cooling ◽  
Subduction Setting

Mg-Fe2+ diffusion patterns in olivine and chromite are useful tools for the study of the thermal history of ultramafic massifs. In the present contribution, we applied the exponential modeling of diffusion patterns to geothermometry and geospeedometry of chromitite ores from two different ophiolite contexts. The Iballe ophiolite (Northern Albania) hosts several chromitite pods within dunites. Primary and re-equilibrated Mg#, estimated by using an exponential function, provided re-equilibration and primary temperatures ranging between 677 and 996 °C for chromitites and between 527 and 806 °C for dunites. Cooling rates for chromitites are higher than for dunites, suggesting a different genesis for the two lithologies, confirmed also by spinel mineral chemistry. Chromitites with MORB affinity formed in a SSZ setting at a proto-forearc early stage, explaining the higher cooling rates, while dunites, with boninitic affinity, were formed deeper in the mantle in a more mature subduction setting. At the Nea Roda ophiolite (Northern Greece) olivine in chromitites do not show Mg-Fe variations, and transformation into ferrian chromite produced “fake” diffusion patterns within chromite. The absence of diffusion patterns and the low estimated temperatures (550–656 °C) suggest that Nea Roda chromitites were completely re-equilibrated during an amphibolite-facies metamorphic event that obliterated all primary features.

scholarly journals A new catalogue of earthquakes in the historical Armenian area from antiquity to the 12th century

1995 ◽  
Vol 38 (1) ◽  
Author(s):  
E. Guidoboni ◽  
G. Traina
Keyword(s):  
Historical Earthquakes ◽  
Historical Seismicity ◽  
Seismic Events ◽  
Specific Nature ◽  
Present Contribution ◽  
12Th Century ◽  
Literary Sources ◽  
New Localities ◽  
History Of ◽  
Catalogue Of Earthquakes

The present contribution describes the method of work, the types of source materia] used, and the historio- graphical and historico-eismic tradition of Armenia. The catalogue' s territorial frame of reference is that of socalled historical Armenia (which included part of present Eastern Turkey, and part of present Azerbaijan). The sources belong to different languages and cultures: Armenian, Syriac, Greek, Arab, Persian and Georgian. A comparison of the local sources with those belonging to other cultures enab]es the historical and seismological I"adition of the Mediterl'anean to be "linked" with that of the Iranian p]ateau, traditionally considered as two separate areas. We analyzed historical events listed in the most recent catalogues of earthquakes in the Armenian area compiled by Kondorskaya and Shebalin (1982) and Karapetian (1991). Important and valuable though these catalogues are, they are in need of revision. We found evidence for six hitherto unrecorded seismic events. Numerous errors of dating and location have been corrected, and several new localities and seismic effects have been evidenced. Each modification of the previous catalogues has been documented on the hasis of the historiographical and literary sources and the data from the written sources have been linked with those concerning the history of Armenian cities and architecture (monasteries, churches, episcopal complexes). On the whole. the revised earthquakes seem underestimated in the previous catalogues. The aim of this catalogue is to make a contribution to the knowledge of historical seismicity in Armenia, and at the same time to underline the specific nature of the Armenian case, thus avoiding a procedure which has generally tended to place this area in a marginal position, within the wider field of other research on historical earthquakes.

Expelling demons at Nineveh: The visibility of benevolent demons in the palaces of Nineveh

Iraq ◽  
2004 ◽  
Vol 66 ◽  
pp. 83-92
Author(s):  
Tallay Ornan
Keyword(s):  
Ninth Century ◽  
Present Contribution ◽  
North West ◽  
The North ◽  
Recent Scholarship ◽  
History Of Art ◽  
Religious Subject ◽  
History Of ◽  
Historical Themes ◽  
First Time

As has been shown and extensively dealt with in early and more recent scholarship, Neo-Assyrian palatial wall reliefs went through many thematic changes throughout their two hundred and fifty years of existence. One of their conspicuous traits was a gradual abandoning of magical-religious subject matters, represented by protective supernatural beings, in favour of larger and more detailed historical compositions — mostly of a belligerent nature — revealing, for the first time in antiquity, a truer sense of narrative display. As the narrative-historical themes were rightly considered to be an innovative and prominent contribution of Assyrian imagery to the history of art, extensive efforts have been devoted to the study of these compositions within the context of Assyrian palaces.In the present contribution I intend, however, to concentrate on the “losing” side of Assyrian palatial decoration, namely to focus on the visibility of apotropaic fantastic creatures rendered on wall reliefs and to offer some explanation for their gradual expulsion from the pictorial display of the Assyrian palace. Following Porada, in this essay these hybrids are called demons, in accordance with the Greek term daimon. Benevolent demons appear already in early ninth-century Neo-Assyrian wall reliefs, both in temples, as shown by a small number of slabs from the Ninurta Temple at Nimrud, and much more commonly in palaces, in particular within the North-West Palace.

scholarly journals XII.—Ice-Erosion in the Cuillin Hills, Skye

1905 ◽  
Vol 40 (2) ◽  
pp. 221-252 ◽  
Author(s):  
Alfred Harker
Keyword(s):  
Geological Survey ◽  
Dominant Factor ◽  
Glacial History ◽  
Present Communication ◽  
Glacial Erosion ◽  
Present Contribution ◽  
History Of

Since the publication in 1840 of a brief but valuable memoir by J. D. Forbes, in which that author drew attention to “the traces of ancient glaciers” in the Cuillin Hills, that district has remained almost unnoticed by glacial geologists for half a century. This neglect is doubtless attributable chiefly to the difficulty of access to the mountains, a consequence of their peculiar configuration, which in turn is closely bound up with the glacial history of the district. The present contribution is the outcome of observations made during the years 1895–1900 in mapping the central part of Skye for the Geological Survey of Scotland. In traversing the mountains day after day throughout several successive seasons, the writer has been struck especially by the impressive evidence which they present of glacial erosion as the dominant factor in their sculpture, and to enforce this is the chief object of the present communication.

scholarly journals Foreign language attrition

2012 ◽  
Vol 1 (1) ◽  
pp. 102-124 ◽  
Author(s):  
Monika S. Schmid ◽  
Teodora Mehotcheva
Keyword(s):  
Foreign Language ◽  
Theoretical Models ◽  
Foreign Languages ◽  
Language Attrition ◽  
Present Contribution ◽  
Future Directions ◽  
Second Languages ◽  
History Of Research ◽  
Recent Developments ◽  
History Of

The present contribution discusses recent developments and future directions in the attrition of instructed foreign languages, arguing for a distinction between this type of attrition and attrition involving second languages acquired implicitly in an immersion setting. An overview of the history of research in the field and the most prominent findings is provided, followed by a discussion of theoretical models and methodologically problematic issues. We conclude by outlining some future directions for the field.

scholarly journals POLISH-LITHUANIAN HERITAGE IN TVER DIALECTS: STAGES OF SEMANTIC EVOLUTION

2021 ◽  
pp. 104-109
Author(s):  
Ирина Михайловна Ганжина
Keyword(s):  
New Words ◽  
Single Root ◽  
European Languages ◽  
History Of ◽  
Tver Region ◽  
Semantic Evolution

Статья посвящена исследованию этимологической истории некоторых лексических диалектизмов с затемненной внутренней формой в говорах Тверской области. Сделана попытка выявить мотивационные характеристики слов, связанных с польско-литовским влиянием, путем проникновения во внутреннюю форму слов, проследить их семантические связи с однокоренными лексемами в других славянских и индоевропейских языках. Анализируются историко-семантические преобразования, которые имели место при возникновении производных значений, в результате которых возникли новые слова, конкретизирующие в диалектах признаки, явления, действия и предметы. The article deals with the etymological history of some lexical dialecticisms with an implicit inner form in the dialects of the Tver region. An attempt is made to identify the motivational characteristics of the words, related to the Polish-Lithuanian influence, by penetrating into their inner forms, to trace their semantic connections with the single-root lexemes in other Slavic and Indo-European languages. The author analyzes the historical and semantic transformations that took place in the process of emergence of derived meanings, which resulted in the appearance of new words that concretize different features, phenomena, actions and objects in dialects.

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