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  • Articles  (141)
  • AERODYNAMICS
  • Geology
Collection
  • 1
    Publication Date: 2017-04-04
    Description: Geoethics is born with the intent to highlight the social role of Geosciences, to encourage a critical analysis on the use of natural resources, to promote the enhancement and protection of the Geosphere, the correct information on risks, hoping the involvement of the scientific community in the idea of a common and shared “geological” heritage. But what is the deep meaning of the word “geoethics”, its origins, its use? The word derives from the combination of “geology” and “ethics”. “Geology” is simply “the study of Earth”. The etymological analysis of the word “ethics” is more complicated: it seems that at its origin there is a root of dual meaning: on the one hand it contains the sense of belonging to a community, it defines the relationship between men; on the other hand it expresses the individual, the ego in relationship to itself. It follows that ethics concerns what is common, but also what is personal, what distinguishes the individual. Ethics is both “being part” and “belonging to oneself”. In addition, a Semitic base assigns to this word the original meaning of “experience”. Thus, ethics is defined as the research of criteria that enable the individual to properly manage their freedom with respect for others, in the attempt to find the meaning of human life, understood as individual life and in relation with the Planet Earth. It is subjective when it deals with the subject acting, objective, when the action is related to common values and institutions. Consequently, we can define geoethics on the one hand as the investigation and reflection on the behaviour of men towards the Geosphere, on the other hand as the analysis of the relationship between the geologist who acts and his own action, with clear implications of responsibility both in scientific research and in professional practice. Starting from the etymology of some words related to the world of Geosciences, it will be tried to grasp the meaning of the geologist’s activity.
    Description: Published
    Description: Rimini
    Description: 5.9. Formazione e informazione
    Description: open
    Keywords: Geoethics ; Geology ; 05. General::05.03. Educational, History of Science, Public Issues::05.03.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Abstract
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  • 2
    Publication Date: 2017-04-04
    Description: This research is deemed of importance in the solution of one of the main complex problems in geological map production, the transfer from the 1:25.000 geologic data base, that has a resolution corresponding to that at which data are gathered in the field, to the printing of 1:50.000 geological maps. The problems relate mainly to the greater detail of information contained in the database and the smaller printing scale. They can be classified into the design of a geological database scheme that allows the generalization process based on the rules relating the geological objects to one another, symbol overcrowding, and symbol overlapping. The challenge is to specify and implement a digital version of the decision rules used by geologists and cartographers to generate the final map. Often in practice these rules tend to be highly ambiguous, subjective, and inadequate in view of the modern need of automated generalization of geological information for land-use planning. The proposed system is based on the application of conventional and artificial intelligence computer techniques to the production of digital geological cartography, from the gathering of geologic data in the field to some printed product of wide usability. The objectives can be summarised as follows: 1A support system for the iterative identification and characterization of geological objects based on an ad hoc geological and stratigraphic dictionary; 2The identification and implementation of a hierarchical geological database schema for the automated reclassification or generalization of a geological database; 3A hierarchical expert system for the automated revision and multiple representation of a geological database in view of new interpretation criteria of the geological information or for the production of maps on demand; 4A system for avoiding symbol overcrowding or overlapping during the production of a geological map, which identifies the geological rules interacting between the geological objects represented in a map.
    Description: The Open University Milton Keynes, UK
    Description: Published
    Description: 5.4. TTC - Sistema Informativo Territoriale
    Description: open
    Keywords: Geology ; Mapping ; Cartography ; Symbology ; Expert system ; Database ; GIS ; 04. Solid Earth::04.04. Geology::04.04.11. Instruments and techniques
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: thesis
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  • 3
    Publication Date: 2012-02-03
    Description: Monte Corchia is one of the most typical geological structure of the Alpi Apuane but this is not the only peculiar aspect of this territory. Within a very small area it is possible to combine structural geology, marble exploitation, geomorphology and ore deposits. The last point is of worth of interest because the area has been the subject of ore exploitation until the recent past. Within the marble succession of the Corchia synclinal core develops the longest Italian cave with 52 km of passages and galleries. Ongoing researches are exploring the huge paleoclimatic archives preserved within the carbonate concretion of the cave and are reconstructing, with extreme detail the climatic and environmental evolution of this sector of the Mediterranean basin.
    Description: Published
    Description: 1-55
    Description: 3.7. Dinamica del clima e dell'oceano
    Description: N/A or not JCR
    Description: open
    Keywords: Geology ; Mineralogy ; Paleoclimate ; Apuan Alps ; 03. Hydrosphere::03.01. General::03.01.06. Paleoceanography and paleoclimatology ; 04. Solid Earth::04.04. Geology::04.04.03. Geomorphology ; 04. Solid Earth::04.04. Geology::04.04.05. Mineralogy and petrology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 4
    Publication Date: 2017-04-04
    Description: The Holocene is the most recent geological epoch spanning from about 11700 years ago to the present day. The most important human civilizations appeared during the Holocene. From the Holocene onwards, environmental changes, and the hazards associated with them, became extremely important for their impact on historical events, in some cases blending with humanity’s vicissitudes and influencing the rise and decline of civilizations. This paper summarises the geological and climatic conditions of Northern Europe during the Holocene and tries to determine whether or not they support the hypothesis formulated by Felice Vinci (Vinci, 2003) about the migration of Baltic populations towards the Mediterranean in the Bronze Age at the end of the “climatic optimum” (Houghton et al., 1990; Rohling & De Rijk, 1999). This study presents data on glacio-eustatic changes and on isostatic uplift together with information on probable tsunamis that occurred in the North Atlantic, North Sea, Scandinavia and the Baltic Sea. Moreover, some data on catastrophic events that affected the Mediterranean region are reported, because these catastrophes could have favoured the settlement of “people coming from the sea” that took advantage of the demographic and socio-economic weakening of indigenous populations (Driessen, 2002). The paper aims to provide geological and palaeogeographic constraints to the hypotheses formulated by Felice Vinci on the migration of Scandinavians towards the Mediterranean. The data analysed have been collected from the available scientific literature (see references). The amount of information available for each geological phenomenon is vast and sometimes theories developed from the same data are in conflict. The comparison between the Mediterranean and the Baltic areas (one of which could have been the theatre of the Homeric events) will be useful to find evidence of geological phenomena within the Homeric texts, giving useful indications to better understand where the poems are set or at least to provide interesting discussion points related to Felice Vinci’s hypothesis (Vinci 2003).
    Description: Published
    Description: 179-197
    Description: 3.10. Storia ed archeologia applicate alle Scienze della Terra
    Description: open
    Keywords: Geology ; Holocene ; Northern Europe ; Mediterranean ; Earthquakes ; Volcanoes ; Ice age ; Tides ; Tsunami ; Glacio-eustatism ; Seismicity ; Uplift ; Submarine landslides ; 04. Solid Earth::04.04. Geology::04.04.99. General or miscellaneous ; 04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous ; 04. Solid Earth::04.06. Seismology::04.06.05. Historical seismology ; 04. Solid Earth::04.08. Volcanology::04.08.99. General or miscellaneous ; 05. General::05.02. Data dissemination::05.02.99. General or miscellaneous ; 05. General::05.02. Data dissemination::05.02.02. Seismological data ; 05. General::05.02. Data dissemination::05.02.03. Volcanic eruptions ; 05. General::05.08. Risk::05.08.99. General or miscellaneous ; 05. General::05.09. Miscellaneous::05.09.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: book chapter
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  • 5
    Publication Date: 2017-04-04
    Description: A comprehensive study of the Late Neogene tectonostratigraphic development of the Crotone Basin is presented. The basin is situated on the accretionary wedge along the external side of the Calabrian Arc (Central Mediterranean). The results of our analysis provide detailed insight into the relative role of local tectonic activity of the thrust wedge and regional relative sea level fluctuations in the creation of unconformity bound depositional sequences. The tectonostratigraphic significances of the sequence boundaries of the Early-Late Miocene and Late Pliocene-middle Pleistocene sequences are remarkably similar. They reflect a “composite tectonic event” comprising an uplift/regression pulse, followed by a rapid subsidence/onlap. Each composite tectonic event, in turn, represents one pulse in the progressive evolution of the accretionary wedge system. We regard the middle Messinian-Early Pliocene phases of basin fill and tectonic inversion, and the Late Pleistocene-Recent uplift phase as reflections of the increase of regional stress in the Central Mediterranean.
    Description: Published
    Description: 259-285
    Description: 3.5. Geologia e storia dei vulcani ed evoluzione dei magmi
    Description: N/A or not JCR
    Description: open
    Keywords: Calabria ; Geodynamics ; Basin ; Geology ; 04. Solid Earth::04.04. Geology::04.04.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 6
    Publication Date: 2021-05-19
    Description: Le littoral étudié est situé sur la frange méridionale de la côte ouest-africaine, localisé dans le golfe du Bénin enire le cap des Trois Pointes et la façade ouest du delta du Niger. 11 s'étend sur 500 km de long et mesure 1 à 25 km de largeur. L!étude porte sur la géomorphologie, l'évolution et la morphodynamiqiue actuelle de deux ensembles distincts: un littoral formé de delta lagunaire, peu complexe avec un front deltaïque caractérisé par une série de flèches sableuses accolées; de cordons associés a un système lagunaire et un littoral ocheux marqué par des falaises taillées dans les roches cristallines et sédimentaires et entrecoupé par des estuaires à lagunes, des baies abritées où se développe une végétation de palétuviers. Le relief est raccordé à un plateàu continental étroit, profond où les conditions hydrodynamiques sont de régime d'énergie modérée à élevée.
    Keywords: Geology ; Geomorphology ; Geomorphology ; Geology
    Repository Name: AquaDocs
    Type: Theses and Dissertations
    Format: 453
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  • 7
    Publication Date: 2021-05-19
    Description: This study investigates the potential of Bojnord and Jarjam cities (Northern Khorasan province) for developments of Aquaculture. First of all, the current condition of Aquacture and fish farms were montiroed and recorde. Then, the information on geology, weather and climate as well as water resources data were gathered and evaluated. Climatology, geology and distribution of water reseources (i.e. reviers, springs, wells, and aqueducts) were prepared using GIS software. Evaluation of selected water resources in study area revealed suitability for culture of cold water fishes. Potentialities of the water resources for aquacture production were determined according to the latest guidline of Shilat organization. The maps of production potentialities were prepared for each water resources.
    Description: Iranian Fisheries Science Research Institute
    Description: Published
    Keywords: Geology ; Climatology ; Aquaculture ; Potential ; GIS
    Repository Name: AquaDocs
    Type: Report , Refereed
    Format: 94pp.
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  • 8
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    In:  http://aquaticcommons.org/id/eprint/4643 | 1256 | 2011-09-29 16:08:49 | 4643 | Freshwater Biological Association
    Publication Date: 2021-07-05
    Description: The EC Water Framework Directive (WFD) introduces the concept of the ecological status of surface waters. The WFD requires that water bodies within an ecoregion are divided into waterbody "types" or "ecotypes". The waterbody type is determined by physico-chemical descriptors. A group of representatives from two government environmental agencies (Environment and Heritage Service and the Industrial Research and Technology Unit) and the two universities (Queen's University Belfast and the University of Ulster) in Northern Ireland, has been established to develop methods for measuring the ecological status of lakes, for the purposes of the WFD. The work here is that contributing to the first objective classification into waterbody types.
    Keywords: Management ; Limnology ; Policies ; Alkalinity ; Catchment area ; Classification ; Geology ; Height ; Hydrographic surveys ; Lakes ; Water policy ; Northern Ireland
    Repository Name: AquaDocs
    Type: article , FALSE
    Format: application/pdf
    Format: application/pdf
    Format: 39-64
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  • 9
    Publication Date: 2021-05-19
    Description: During the Quaternary the volume of the world’s oceans fluctuated, with sea level falls as the water has been incorporated into polar and high latitude ice sheets, and sea level rise as these have subsequently melted. Sea-level lowstands were therefore related to the Pleistocene glaciations, while high-stands correlate with interglacials. In general the climate variations in Africa shows a simple relation: Cold or cool climates are associated with dry episodes and warm climates are associated with wet episodes. This applies to the major Milankovich driven glacials and interglacials, as well as to short-lived intervals related to sun spot activities. The reconstruction of palaeoshorelines in the Maputo Bay, and the climate around the Maputo Bay is based on bathymetric maps. At about 18,000 yr BP (-130 meters sea level) the Maputo Bay was located in an inland position. As the sea level rose to about 20 m below present around 9000 - 10000 years BP, a barrier island complex developed in the northern coast, which is well defined by 20 m contour palaeoshoreline. The Maputo Bay is only formed around 8000 – 9000 years BP (when the sea level was 10 to 12 m below the present, and it was a long lasting still stand sea level. A huge island was protecting the bay from the sea. Tidal inlet and its associated ebb delta were separating the island from the peninsula in the south and were connecting the lagoon into the sea. The complete picture of Maputo Bay patterns with its modern sedimentary environments including Inhaca Island may have evolved when the sea level has stood close to its present level around 7000 – 5000 years BP, after which the Maputo Bay became more or less stable. Coral reefs may have also developed during this period. Submarine modifications of the topography during and after the sea-level rise make it difficult to make safe interpretations of the coastal palaeomorphology. However, we believe that many of the present major submarine bottom forms, which are seen on the maps today, are related to coastal processes during the sea-level rise, and were preserved when they were flooded during the Holocene transgression.
    Keywords: Geology
    Repository Name: AquaDocs
    Type: Preprint
    Format: 266193 bytes
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  • 10
    Publication Date: 2021-05-19
    Description: Se realizaron mediciones radiométricas en las formaciones Jordán (Pérmico superior?), Guatapurí (Triásico?), Girón (Triásico-Jurásico), Ranchogrande (problemente Triásico-Jurásico) y Morrocoyal (Jurásico inferior) en el NE de Colombia. Los valores más altos obtenidos (impulsos y por minuto) provienen de las lulitas de la formación Girón. En la región de Bucaramanga (Depto. De Santander), los red beds de las Formaciones Jordán y Girón muestran valores radiométricos bien diferenciados. Se discute la utilidad de las mediciones radiométricas como medio de diferenciación estratigráfica o de facies.
    Description: Background measurements of gamma radiation were made on the Jordán (Upper Permian?) Guatapurí (Triassic?), Giron (Triassic-Jurassic) Ranchogrande (Triassic-Jurassic?) and Morrocoyal (Lower Jurassic). Formations in Northeastern Colombia. The lutites of the Girón Formation produce the highest values (impulses y per minute). In the region of Bucaramanga (Department of Santander), the redbeds of the Jordán and Girón Formations give quite different radiometric values. The usefulness of radiometric measurements as a means of differentiating stratigraphic units and facies changes is discussed.
    Description: Published
    Keywords: Geology ; Geology
    Repository Name: AquaDocs
    Type: Journal Contribution
    Format: pp.93-102
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