Journal articles: 'Financial and geomorphological systems'

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STEPHENSON, P. "Modelling geomorphological systems." Earth-Science Reviews 27, no. 4 (June 1990): 374–77. http://dx.doi.org/10.1016/0012-8252(90)90062-z.

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Goldsmith, Victor. "Coastal sand dunes as geomorphological systems." Proceedings of the Royal Society of Edinburgh. Section B. Biological Sciences 96 (1989): 3–15. http://dx.doi.org/10.1017/s0269727000010824.

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SynopsisThe importance of aeolian deposition is clearly shown by the size and bulk of coastal dunes. Sand dunes occur where there is a large supply of sand, a wind to move it, and a place in which it can accumulate. A dune classification is presented which takes into account the origin, internal geometry and surface geomorphology of coastal dunes. Since the main element that distinguishes coastal dunes from desert dunes is vegetation, the relative amount of vegetation may be used as a typology. Four dune types are distinguished: vegetated dunes, parabolic dunes, medanos (i.e. large sand hills devoid of vegetation), and artificially-inseminated dunes. Vegetated and medano dunes are the end members, with parabolic dunes in between. Parabolic dunes are “anchored” by vegetation, but the centre of the dunes has migrated in the down-wind direction. The artificially-inseminated dunes are formed by vegetation plantings, fencing, or other artificial means, but with natural sand accumulation around these obstacles. These now account for a very substantial portion of the world's coastal dunes.The role of wind and its relation to the internal geometry (i.e. cross-bed dip and direction) are discussed in some detail, with examples from Brazil, U.S. east and south coasts, Israel and China. Differences in these characteristics are detailed, and related to the different modes of formation of the four dune types.The role of the wind in transporting and depositing sand in coastal areas is being quantified through both wind tunnel and field transport measurements. An example from a field study along the coast of Israel illustrates the differences between desert and coastal dune transport, where the role of vegetation and beach topography must be taken into account. From the Israeli study, and others, it appears that transport in coastal dunes is reduced by one-third to one-half of that in deserts, due to these factors.Coastal dunes provide a useful, and often necessary, buffer against storm waves and the presently rising sea level. They form primarily through vertical sand accretion trapped by the sensitive dune vegetation. Provided that sufficient space exists between the high tide line and developed areas, planned dunes can be easily formed with the aid of plantings and fencing.

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Zielhofer, Christoph, Hans von Suchodoletz, Tobias Lauer, and Jürgen Heinrich. "Climatic signals in geomorphological systems: Approaches from aeolian, fluvial, colluvial, periglacial, coastal, and man-made geomorphological systems." Zeitschrift für Geomorphologie, Supplementary Issues 58, no. 1 (February 1, 2014): 1–3. http://dx.doi.org/10.1127/0372-8854/2014/s-00167.

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Payo, Andres, Jim W. Hall, Jon French, James Sutherland, Barend van Maanen, Robert J. Nicholls, and Dominic E. Reeve. "Causal Loop Analysis of coastal geomorphological systems." Geomorphology 256 (March 2016): 36–48. http://dx.doi.org/10.1016/j.geomorph.2015.07.048.

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Carrivick, Jonathan L., and Tobias Heckmann. "Short-term geomorphological evolution of proglacial systems." Geomorphology 287 (June 2017): 3–28. http://dx.doi.org/10.1016/j.geomorph.2017.01.037.

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Rulev, Aleksandr, and Valeriy Yuferev. "Theory of geoinformatic mapping of erosion geomorphological systems." Vestnik Volgogradskogo Gosudarstvennogo Universiteta. Serija 11. Estestvennye nauki, no. 4 (December 2015): 62–67. http://dx.doi.org/10.15688/jvolsu11.2015.4.7.

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Humlum, Ole, and Ketil Isaksen. "Permafrost geomorphological systems in a changing global climate." Norsk Geografisk Tidsskrift - Norwegian Journal of Geography 59, no. 2 (June 2005): 75–77. http://dx.doi.org/10.1080/00291950510038403.

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Borodavko, Pavel S., Elena S. Volkova, Mariya A. Mel`nik, Alexey S. Litvinov, and Otgonbayar Demberel. "Climate change impact on high-altitude geomorphological systems." IOP Conference Series: Earth and Environmental Science 211 (December 17, 2018): 012004. http://dx.doi.org/10.1088/1755-1315/211/1/012004.

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Bazhenova, O. I., E. M. Tyumenseva, and S. A. Tukhta. "Assessment of the geomorphological safety of the Daurian region for the purpose of effective nature management." IOP Conference Series: Earth and Environmental Science 885, no. 1 (October 1, 2021): 012038. http://dx.doi.org/10.1088/1755-1315/885/1/012038.

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Abstract The risk assessment of the dangerous geomorphological processes development in the Dauria steppes in conditions of pronounced cyclical fluctuations in climate and high dynamism of geomorphological systems is carried out on a five-point scale. The analysis of the spatial and temporal structure of fluvial and aeolian processes for the purposes of nature management is fulfilled. The role of extreme geomorphological events is shown, which are a serious limiting factor of conflict-free nature management in the Daurian region. The revealed catastrophic manifestations of fluvial and aeolian processes require careful planning of economic activities and serious environmental protection measures. The result of the assessment is the zoning of the Dauria territory according to the degree of geomorphological risk. The types of economic activities that do not violate the stability of the regime of geomorphological systems, and, on the other hand, are undesirable, increasing the risk of critical natural situations, are indicated.

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Veselova, L., and I. Shmarova. "Geomorphological systems of the state national natural park «Sharyn»." Journal of Geography and Environmental Management 42, no. 1 (2016): 16–22. http://dx.doi.org/10.26577/jgem.2016.1.277.

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Koshim, A., R. Bekseitova, and A. Shergeeva. "Recreational potential of the geomorphological systems of Mangystau territory." Journal of Geography and Environmental Management 47, no. 4 (2017): 53–61. http://dx.doi.org/10.26577/jgem.2018.2.436.

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Peña-Alonso, Carolina, Juan B. Gallego-Fernández, Luis Hernández-Calvento, Antonio I. Hernández-Cordero, and Eduard Ariza. "Assessing the geomorphological vulnerability of arid beach-dune systems." Science of The Total Environment 635 (September 2018): 512–25. http://dx.doi.org/10.1016/j.scitotenv.2018.04.095.

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Knight, Jasper, and Stephan Harrison. "Evaluating the Impacts of Global Warming on Geomorphological Systems." AMBIO 41, no. 2 (August 10, 2011): 206–10. http://dx.doi.org/10.1007/s13280-011-0178-9.

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Reynard, E., C. Lambiel, and S. N. Lane. "Climate change and integrated analysis of mountain geomorphological systems." Geographica Helvetica 67, no. 1/2 (November 22, 2012): 5–14. http://dx.doi.org/10.5194/gh-67-5-2012.

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Kupach, T., and T. Mykhailenko. "Analysis of the recreational resources of Kaniv in the context of the programme of development of Ukrainian small-cities." Journal of Geology, Geography and Geoecology 28, no. 3 (October 5, 2019): 457–74. http://dx.doi.org/10.15421/111942.

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The purpose of the article is to highlight the problem of using the potential of local territory in the processes of promoting local uniqueness as a consumer product. This study aimed at analysis and appraisal of the recreational resources of Kaniv for the organization of recreational activities in the planning strategies of the city as a recreational and tourist center. The study of the entire set of recreational resources of the city resulted in a constructive analysis and evaluation of the recreational benefits of the city’s resources. In the course of the survey, the directions of recreational environmental management in the city were determined in accordance with the programme of development of small Ukrainian cities. The analysis and assessment of the territory’s resources was conducted using integrated methodologies of studying recreational assets that take into account the evaluation methods of medical geography, recreology etc. Our study found that geomorphological, climatic, water, biotic, and landscape recreational natural resources are significant for the organization of recreational activity in the city and which, according to the estimation of recreational favourability, are highly conducive and convenient for both winter and summer recreation. A number of indicators of natural resources are of high value for the treatment and prevention of a wide range of diseases, including problems with respiratory, cardiovascular, nervous systems. The development of recreation and tourism in the city is also influenced by the existing historical and cultural resources, which include a whole set of archaeological, architectural and historical monuments, ethnographic features and crafts, museums and exhibitions, places and areas of significant events, places of life and creativity for prominent personalities, heroes and figures, etc. The socioeconomic resources and infrastructure of the city have a significant impact on the functioning of the recreational affairs, such as the state of the existing and prospective territorial organization, transport accessibility and level of its development, the public service and its condition (food establishments, residence, etc.). Nowadays, Kaniv is characterized by partly lower indicators of socio-economic development, business activity and, at the same time, enjoys a powerful natural, recreational and tourist, historical and cultural potential. Development of recreational and tourist activity in the city should be considered as a tool for increasing economic indicators (employment, business activity and growth of its financial indicators) and improvement of demographic indicators (reduction of labour migration, etc.), etc. The natural and cultural heritage of Kaniv is a source of socio-economic and human development through the integration of cultural monuments into the national tourist network. This can be achieved through the creation of new museum programmes, the development of a network of establishments based on authentic cuisine, traditional interiors, etc. It can further be promoted through creation of a network of ecological trails and routes which give access to the area’s unique natural ecosystems. Recreation and tourist activity can also be encouraged through popularization of environmental affairs, creation of programmes for development of the resort business, programmes of family recreation, development of different types of water, hiking, educational (culture, events, research, etc.) and eco-tourism, and the development of programmes and events in the field of sport fishing and hunting.

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SASATANI, Yasuyuki, and Yoshio NAKAMURA. "A Study on Geomorphological Cognition of River through Vocabulary Systems." ENVIRONMENTAL SYSTEMS RESEARCH 18 (1990): 7–12. http://dx.doi.org/10.2208/proer1988.18.7.

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Lovell, Harold, Douglas I. Benn, Sven Lukas, Matteo Spagnolo, Simon J. Cook, Darrel A. Swift, Chris D. Clark, Jacob C. Yde, and Tom Watts. "Geomorphological investigation of multiphase glacitectonic composite ridge systems in Svalbard." Geomorphology 300 (January 2018): 176–88. http://dx.doi.org/10.1016/j.geomorph.2017.10.024.

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18

ANDERSON, R. "Eolian ripples as examples of self-organization in geomorphological systems." Earth-Science Reviews 29, no. 1-4 (October 1990): 77–96. http://dx.doi.org/10.1016/0012-8252(0)90029-u.

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Anderson, R. "Eolian ripples as examples of self-organization in geomorphological systems." Earth-Science Reviews 29, no. 1-4 (October 1990): 77–96. http://dx.doi.org/10.1016/0012-8252(90)90029-u.

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Viles, H. A., L. A. Naylor, N. E. A. Carter, and D. Chaput. "Biogeomorphological disturbance regimes: progress in linking ecological and geomorphological systems." Earth Surface Processes and Landforms 33, no. 9 (August 2008): 1419–35. http://dx.doi.org/10.1002/esp.1717.

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21

Zawadowski, Adam. "Entangled Financial Systems." Review of Financial Studies 26, no. 5 (March 6, 2013): 1291–323. http://dx.doi.org/10.1093/rfs/hht008.

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22

Dvořák, Lubomír. "Application of the ARC/INFO GIS for Geomorphological Research with Special Attention to Morphostructural Analysis." Geografie 100, no. 1 (1995): 3–9. http://dx.doi.org/10.37040/geografie1995100010003.

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Many different Geographical Information Systems (GIS) exist nowadays; geographers, however, have sometimes problems with GIS applications in their respective field. The use of GIS in geomorphological research is presented. Special attention is given to the connection between the ARC/INFO GIS and morphostructural analysis which belongs among modern methods of geomorphological research. The study area is located in the northern part of Zábřežská Highland, Bohemian Highlands, Czech Republic.

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Kharchenko, S. V. "Automatic recognition of the landforms origin in the Kola Peninsula based on morphometric variables." Geodesy and Cartography 980, no. 2 (March 20, 2022): 12–25. http://dx.doi.org/10.22389/0016-7126-2022-980-2-12-25.

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The automatic geomorphological mapping based on the Earth’s surface remote sensing data has been developed in recent years. The aim of the research is an attempt of automatic creation of the Kola Peninsula geomorphological map at the morphogenetic legend’s principle. It was gained based on the random forest classification technique. As input data a several geomorphometric variables were used only (the basic ones – elevation, slope angle, curvatures etc., and many those of surface texture). Developing such algorithms for different territories and hierarchical levels of landforms analysis contributes to propagate the techniques of the fast geomorphological mapping. On the training data covering only 1,3 % of the study area with known labels for one of thirteen probable landform types, the reconstruction of geomorphological boundaries and the automatic creation of the geomorphological map were carried out. The accuracy of the resulting map was 81 %. Elevation has the greatest discrimination power according to Kola Peninsula landform types. In addition, some area-based local geomorphometric variables characterizing terrain pattern has big discrimination power. The lowest power relates with the “classical” local-based geomorphometric variables. The results of the work can be used in the development of automated landforms mapping systems at the level of morphogenetic types.

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Kregel, Jan. "Financial systems, financial governance and economic development." Brazilian Keynesian Review 3, no. 2 (January 31, 2018): 124. http://dx.doi.org/10.33834/bkr.v3i2.126.

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The idea that seems to be spreading in response to this crisis to promote the substitution of development financing via private sector institutions in place of government development banks means restoring the inequitable sharing of risk of development finance, promoting instability and protecting finance at the expense of labour, and the inevitable worsening of the distribution of income. Private sector financial markets do not have a good record of providing finance to development investments at levels and rates that would ensure expanding employment, and there is no reason to believe that this will change if the role of development banks is minimized. As liquidity preference becomes the dominant decision variable for investment, Brazil will be back to the problems that Keynes originally analysed in the <em>General Theory</em>, with the addition of the prudential requirements that will aggravate the instability of the growth process, even in the presence of a fully developed domestic financial system, and tilt social support in favour of finance at the expense of labour.

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LAFFERTY, KAREN D. "Patient Care Systems vs. Financial Systems." Nursing Management (Springhouse) 18, no. 7 (July 1987): 51???55. http://dx.doi.org/10.1097/00006247-198707000-00014.

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Gorbunova, Yuliya V., Tatyana N. Demyanenko, and Valentina V. Chuprova. "Use of remote Earth sensing for agro-ecological estimation of soil cover structures and optimisation of agriculture in the forest-steppe zone of the Krasnoyarsk territory." E3S Web of Conferences 75 (2019): 02002. http://dx.doi.org/10.1051/e3sconf/20197502002.

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The possibilities of using data of Earth remote sensing for the construction of a geomorphological profile for the purpose of agroecological assessment of soil cover patterns and subsequent land typification as a basis for the design of adaptive landscape agriculture in the Krasnoyarsk Territory are considered. The geomorphological profile illustrates the features of the relief and regularities in the distribution of soil structures with a certain set of agro-ecological conditions and limiting factors that determine the choice of agro-technologies and farming systems.

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PETROVIĆ, Aleksandar S., Jelena ĆALIĆ, and Vojkan GAJOVIĆ. "Paleodrainage network reconstruction on Miroč Mt. (Eastern Serbia)." Revista de Geomorfologie 18, no. 1 (November 14, 2016): 69–76. http://dx.doi.org/10.21094/rg.2016.119.

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The paper represents a geomorphological study related to the transitional forms between fluvial and karstic process. Karst areas of eastern Serbia are distributed in a large number of relatively isolated segments, and therefore abound in contact karst features. In many cases, central parts of karst areas, away from the contacts, host a variety of relict and dry valleys. Morphological analysis of these valleys may reveal the remnants of paleodrainage networks and help to reconstruct the morphological evolution of the area. This is a case study of the karst of Miroč Mt. in north-eastern Serbia, where geomorphological analysis and relief visualization using the Geomorphological Information System enabled the detection of paleodrainage directions and patterns in the vicinity of the Danube Gorge. Three paleo-river systems were detected, the largest of which is that of the Suva Reka (51 km2).

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Antzoulatos, Angelos A., Ekaterini Panopoulou, and Chris Tsoumas. "Do Financial Systems Converge?" Review of International Economics 19, no. 1 (January 18, 2011): 122–36. http://dx.doi.org/10.1111/j.1467-9396.2010.00936.x.

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Roberts, Brian E., and David Streatfield. "Local Financial Management Systems." International Journal of Educational Management 2, no. 2 (February 1988): 20–29. http://dx.doi.org/10.1108/eb023553.

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Mishurinskii, D. V., and A. V. Bredihin. "Comprehensive assessment of the recreational-geomorphological potential of the coasts of the White and Baltic Seas." Geomorphology RAS, no. 1 (April 4, 2019): 38–47. http://dx.doi.org/10.31857/s0435-42812019138-47.

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The approaches to qualitative and quantitative evaluation of recreational-geomorphological potential based on the study of geomorphological safety and attractiveness was applied to the coastal areas of the White and Baltic Seas. The two coasts differ in geomorphological structure, and tourist activities, but they both are attractive for visitors at any time of the year. For more effective conduct of activities in the study areas, it is necessary to take into account the presence of natural monuments, infrastructure development, activity of dangerous processes, historical and cultural characteristics of the area, etc. The best way is to apply different coefficients that give a comprehensive assessment of the territory. The special and integrated indicators obtained in this study can be used for zoning in terms of safety and attractiveness when creating a new tourism product and decision-making related to the foundation and functioning of recreation zones and systems.

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Díaz-Hernández, José Luis, and Ramón Juliá. "Geochronological position of badlands and geomorphological patterns in the Guadix–Baza Basin (SE Spain)." Quaternary Research 65, no. 3 (May 2006): 467–77. http://dx.doi.org/10.1016/j.yqres.2006.01.009.

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AbstractThe Guadix–Baza basin is one of a number of intramontane depressions located within the Betic Cordillera (SE Spain), where the geological and geomorphological evolution is controlled by tectonic activity. The basin ceased to be closed after capture by the Atlantic network, when five main land systems developed. Late Pleistocene geological evolution basically consisted of erosional modelling, when badlands were deeply incised in highly erodible materials (marls and silts). Three travertine platforms and several Palaeolithic sites were used to determine that this main incision period fell within a 115,000–48,000 yr range. There are few signs of geomorphological evolution of this basin in the last 48,000 yr. Based on these geomorphological data and soil development, tectonic uplift of the basin probably played a secondary role in its evolution, and climatic conditions in southern Iberia in the 144,000–48,000 yr period were more humid and variable than later.

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Campos, Néstor, Adolfo Quesada-Román, and Sebastián Granados-Bolaños. "Mapping Mountain Landforms and Its Dynamics: Study Cases in Tropical Environments." Applied Sciences 12, no. 21 (October 26, 2022): 10843. http://dx.doi.org/10.3390/app122110843.

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High mountain areas are critical for water security and natural hazard dynamics, as well as glacier and ecosystem conservation in a warming world. We present a brief account of the methodological steps for geomorphological mapping in mountain areas, including the required scale, the legends, technology, and software. We analyze the best imagery sources and their combination with fieldwork and geographical information systems (GIS), in performing accurate cartography. In addition, we present two case studies in which we apply several methods described previously. Firstly, we carried out a classical and digital geomorphological mapping of Cerro Chirripó (Talamanca Range). Secondly, we studied the Reserva Biológica Alberto Manuel Brenes (Central Volcanic Range), where we used UAVs to map high-resolution fluvial geomorphology. This methodological framework is suitable for future geomorphological surveys in mountain areas worldwide. Moreover, the case studies can give ideas on the application of these approaches to different mountainous environments.

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Zaburaeva, H. Sh, and E. V. Krasnov. "Ecological-and-geomorphological systems of the North-Western Caucasus and its typology." Geomorphology RAS, no. 1 (February 11, 2015): 41. http://dx.doi.org/10.15356/0435-4281-2015-1-41-47.

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Griffiths, J. S., and M. Stokes. "Engineering geomorphological input to ground models: an approach based on Earth systems." Quarterly Journal of Engineering Geology and Hydrogeology 41, no. 1 (February 2008): 73–91. http://dx.doi.org/10.1144/1470-9236/07-010.

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Calista, Monia, Francesco Mascioli, Valeria Menna, Enrico Miccadei, and Tommaso Piacentini. "Recent Geomorphological Evolution and 3D Numerical Modelling of Soft Clastic Rock Cliffs in the Mid-Western Adriatic Sea (Abruzzo, Italy)." Geosciences 9, no. 7 (July 12, 2019): 309. http://dx.doi.org/10.3390/geosciences9070309.

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Geomorphological evolution, erosion and retreat processes that affect the rocky coasts of the mid-western Adriatic Sea (Abruzzo, Central Italy) are the subject of this research. This coastal sector, one of the few examples of clastic soft rock coasts in the Mediterranean Sea, is characterized by active, inactive and paleo cliffs, as well as coastal slopes, composed of the clayey-sandy-arenaceous-conglomeratic marine sequence (Early-Middle Pleistocene) covered by continental deposits (Late Pleistocene-Holocene). This study provides geomorphological and 3D modelling stability analyses of the cliffs of Torre Mucchia, Punta Lunga, Punta Ferruccio (Ortona, CH) and Punta Aderci (Vasto, CH), which are popular tourist sites included in natural reserve areas. They are representative of two main types of active cliffs on soft clastic rocks: cliffs on sandstone and cliffs on conglomerate with notches. In order to evaluate the processes and factors that induce cliffs to retreat and their recent evolution, the research was based on a DEM analysis (LIDAR 2 × 2 m data), aerial photos and an orthoimages interpretation, detailed geological–geomorphological surveys, and a structural analysis; field and remote investigations were combined with numerical modelling with a FLAC3D calculation code. Geological and geomorphological field data provided reliable 3D models, and FLAC3D numerical analyses allowed the definition of the most critical and/or failure areas, and the evaluation of the controlling factors, evolution mechanisms of the slopes and the sliding kinematics of gravitational instability phenomena. Different retreat mechanisms have been observed all along the investigated coastal sectors, induced by gravitational processes due to coastal erosion cycles at the foot of the cliffs, and controlled by lithological features and joints systems. The geomorphological analysis combined with the 3D modelling (i) showed that the retreat process of the cliffs is connected to translational slides and rockfalls (cliffs on sandstone), combined rockfalls, and topples (cliffs on conglomerate), largely controlled by main joints; (ii) defined the most critical areas along the cliffs. These results are of great interest in the assessment of hazard connected to potential sliding on the cliffs. Their implementation within Geographical Information Systems provides a valuable contribution to the integrated management of coastal areas, strongly improving the identification and prediction of landscape changes and supporting a new geomorphological hazards assessment, in areas of high tourism, as well as natural and cultural landscape value.

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Detzer, Daniel, Jerome Creel, Fabien Labondance, Sandrine Levasseur, Mimoza Shabani, Jan Toporowski, Judith Tyson, et al. "Financial systems in financial crisis — An analysis of banking systems in the EU." Intereconomics 49, no. 2 (March 2014): 56–87. http://dx.doi.org/10.1007/s10272-014-0489-8.

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Gallik, Jozef, and Lenka Bolešová. "sUAS and their application in observing geomorphological processes." Solid Earth 7, no. 4 (July 14, 2016): 1033–42. http://dx.doi.org/10.5194/se-7-1033-2016.

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Abstract. Methodologies and procedures in processing gained data vary based on possibilities and needs of scientific projects. This paper should help to get a general overview in the choice of small unmanned aircraft systems (sUAS – commonly known as drones) for scientific purposes, namely remote sensing of geomorphologic processes such as soil degradation in high mountainous areas that are hard to access and have unfavourable weather conditions. All high mountain areas in European countries are legislatively protected, and so various permissions and observation of strict procedures are needed in order to not have a negative influence on the environment. Nowadays, several types of UAS exist that could effectively help us in such protection, as well as in full-fledged utilization when answering scientific questions about the alpine lake genesis. We demonstrate it here with selected examples of our photo documentation.

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Benxing, Zheng. "Glacial Geomorphological Map (1:200 000) of Mt. Tomur Region, Tianshan (Abstract)." Annals of Glaciology 8 (1986): 209. http://dx.doi.org/10.3189/s0260305500001610.

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The Glacial Geomorphological Map (1:200 000) of Mt, Tomur Region, Tianshan, covers 78°33′ – 81°10′E and 41° 08′ – 42° 44′N, with high mountains, deep valleys and many snow peaks, the highest being Mt. Tomur (7435.3 a.s.l.). There are many glaciers in this region with a total area of 4553.69 km2. The melt water from glaciers irrigates the large oasis of Aksu, in the piedmont region in southern Xingjiang and waters the valley plain of Teks River in the Yili area. From piedmont plain to highest mountain summit, the vertical zonality of geomorphology is quite clear, rich in various geomorphological types, representing alpine geomorphology of the arid desert in Central Asia.The author joined the glacial/geomorphological expedition to the Mt. Tomur Region in 1963, 1973 and 1974, and, in the process of mapping, cooperated closely with mapping engineers. This involved extensive use of aerial photographs, satellite images, large-scale topographic maps, geological maps, geomorphological maps and other data, and comprehensive analyses, comparisons, and judgements of data.Special emphasis was placed on existing glaciers and the geomorphology of Quaternary glaciers, according to form, composition and relative chronological periods. The geomorphology was divided into five great systems, i.e. glacial, fluvio-glacial, fluvial, arid and artificial. Twenty-four geomorphic types were defined as the basic elements of the geomorphological map and shown in different colours and by various marks, while old and Neozoic faults were shown by black line marks. There are representative heights on all geomorphological zones. Colour brush-shading added much to the stereo effect.Below the main map, the longitudinal and cross sections of Quaternary geology and geomorphology of the Tialan valley, the stratigraphical columnar profile of West Zamtia and the fluvial/lacustrine deposit profile of the Loska basin were attached, showing the stratigraphical relation between the glacial and non-glacial deposit and the basis for the divisions of the glacial and inter-glacial periods.

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Benxing, Zheng. "Glacial Geomorphological Map (1:200 000) of Mt. Tomur Region, Tianshan (Abstract)." Annals of Glaciology 8 (1986): 209. http://dx.doi.org/10.1017/s0260305500001610.

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The Glacial Geomorphological Map (1:200 000) of Mt, Tomur Region, Tianshan, covers 78°33′ – 81°10′E and 41° 08′ – 42° 44′N, with high mountains, deep valleys and many snow peaks, the highest being Mt. Tomur (7435.3 a.s.l.). There are many glaciers in this region with a total area of 4553.69 km2. The melt water from glaciers irrigates the large oasis of Aksu, in the piedmont region in southern Xingjiang and waters the valley plain of Teks River in the Yili area. From piedmont plain to highest mountain summit, the vertical zonality of geomorphology is quite clear, rich in various geomorphological types, representing alpine geomorphology of the arid desert in Central Asia. The author joined the glacial/geomorphological expedition to the Mt. Tomur Region in 1963, 1973 and 1974, and, in the process of mapping, cooperated closely with mapping engineers. This involved extensive use of aerial photographs, satellite images, large-scale topographic maps, geological maps, geomorphological maps and other data, and comprehensive analyses, comparisons, and judgements of data. Special emphasis was placed on existing glaciers and the geomorphology of Quaternary glaciers, according to form, composition and relative chronological periods. The geomorphology was divided into five great systems, i.e. glacial, fluvio-glacial, fluvial, arid and artificial. Twenty-four geomorphic types were defined as the basic elements of the geomorphological map and shown in different colours and by various marks, while old and Neozoic faults were shown by black line marks. There are representative heights on all geomorphological zones. Colour brush-shading added much to the stereo effect. Below the main map, the longitudinal and cross sections of Quaternary geology and geomorphology of the Tialan valley, the stratigraphical columnar profile of West Zamtia and the fluvial/lacustrine deposit profile of the Loska basin were attached, showing the stratigraphical relation between the glacial and non-glacial deposit and the basis for the divisions of the glacial and inter-glacial periods.

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Gavrilov, A. A. "GEOLOGICAL AND GEOMORPHOLOGICAL RESEARCH METHODOLOGY FOR METALLOGENIC PURPOSES." Bulletin of Kamchatka Regional Association «Educational-Scientific Center». Earth Sciences, no. 3(51) (2021): 84–95. http://dx.doi.org/10.31431/1816-5524-2022-3-51-84-95.

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The basic questions of the methodology of geological and geomorphological study (ore geomorphology, morphostructural analysis, morphotectonics, neotectonics) of ore-bearing territories are considered. The concepts of "geomorphologic systems organization element" as the smallest particle of matter preserving the structure and properties of a mineral, as well as "objectives", "objects" and "subjects" of morphostructural and morphotectonic studies for solving problems of metallogeny have been formulated. In areas with complex geological structure, it is recommended to carry out complex of morphostructural and morphotectonic works with repeated solution of direct and inverse problems: relief and geological environment, geological environment relief. This will make it possible to establish the totality of available deterministic and chronological relations between landforms and structural elements of the lithosphere. Along with the solution of traditional problems of ore geomorphology, it is proposed to use the developed original complex of morphostructural and morphotectonic studies.

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Gavrilov, A. A. "GEOLOGICAL AND GEOMORPHOLOGICAL RESEARCH METHODOLOGY FOR METALLOGENIC PURPOSES." Bulletin of Kamchatka Regional Association «Educational-Scientific Center». Earth Sciences, no. 3(51) (2021): 84–95. http://dx.doi.org/10.31431/1816-5524-2022-3-51-84-95.

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Abstract:

The basic questions of the methodology of geological and geomorphological study (ore geomorphology, morphostructural analysis, morphotectonics, neotectonics) of ore-bearing territories are considered. The concepts of "geomorphologic systems organization element" as the smallest particle of matter preserving the structure and properties of a mineral, as well as "objectives", "objects" and "subjects" of morphostructural and morphotectonic studies for solving problems of metallogeny have been formulated. In areas with complex geological structure, it is recommended to carry out complex of morphostructural and morphotectonic works with repeated solution of direct and inverse problems: relief and geological environment, geological environment relief. This will make it possible to establish the totality of available deterministic and chronological relations between landforms and structural elements of the lithosphere. Along with the solution of traditional problems of ore geomorphology, it is proposed to use the developed original complex of morphostructural and morphotectonic studies.

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COLLIER, PAUL, and COLIN MAYER. "THE ASSESSMENT: FINANCIAL LIBERALIZATION, FINANCIAL SYSTEMS, AND ECONOMIC GROWTH." Oxford Review of Economic Policy 5, no. 4 (1989): 1–12. http://dx.doi.org/10.1093/oxrep/5.4.1.

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Diodato, N. "Local models for rainstorm-induced hazard analysis on Mediterranean river-torrential geomorphological systems." Natural Hazards and Earth System Sciences 4, no. 3 (May 28, 2004): 389–97. http://dx.doi.org/10.5194/nhess-4-389-2004.

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Abstract. Damaging hydrogeomorphological events are defined as one or more simultaneous phenomena (e.g. accelerated erosions, landslides, flash floods and river floods), occurring in a spatially and temporal random way and triggered by rainfall with different intensity and extent. The storm rainfall values are highly dependent on weather condition and relief. However, the impact of rainstorms in Mediterranean mountain environments depend mainly on climatic fluctuations in the short and long term, especially in rainfall quantity. An algorithm for the characterisation of this impact, called Rainfall Hazard Index (RHI), is developed with a less expensive methodology. In RHI modelling, we assume that the river-torrential system has adapted to the natural hydrological regime, and a sudden fluctuation in this regime, especially those exceeding thresholds for an acceptable range of flexibility, may have disastrous consequences for the mountain environment. RHI integrate two rainfall variables based upon storm depth current and historical data, both of a fixed duration, and a one-dimensionless parameter representative of the degree ecosystem flexibility. The approach was applied to a test site in the Benevento river-torrential landscape, Campania (Southern Italy). So, a database including data from 27 events which have occurred during an 77-year period (1926-2002) was compared with Benevento-station RHI(24h), for a qualitative validation. Trends in RHIx for annual maximum storms of duration 1, 3 and 24h were also examined. Little change is observed at the 3- and 24-h duration of a storm, but a significant increase results in hazard of a short and intense storm (RHIx(1h)), in agreement with a reduction in return period for extreme rainfall events.

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Harrison, Stephan. "Climate sensitivity: implications for the response of geomorphological systems to future climate change." Geological Society, London, Special Publications 320, no. 1 (2009): 257–65. http://dx.doi.org/10.1144/sp320.16.

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Pledger, Andrew, Matthew Johnson, Philip Brewin, John Phillips, Sarah L. Martin, and Dapeng Yu. "Characterising the geomorphological and physicochemical effects of water injection dredging on estuarine systems." Journal of Environmental Management 261 (May 2020): 110259. http://dx.doi.org/10.1016/j.jenvman.2020.110259.

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Roig‐Munar, Francesc X., Carla Garcia‐Lozano, Josep Pintó, and José A. Martín‐Prieto. "Spatiotemporal evaluation of the geomorphological state of beach‐dune systems using management criteria." Land Degradation & Development 31, no. 18 (July 13, 2020): 2901–13. http://dx.doi.org/10.1002/ldr.3677.

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Cammeraat, L. H. "A review of two strongly contrasting geomorphological systems within the context of scale." Earth Surface Processes and Landforms 27, no. 11 (2002): 1201–22. http://dx.doi.org/10.1002/esp.421.

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Datar, M. K. "Financial Systems and Economic Development." Artha Vijnana: Journal of The Gokhale Institute of Politics and Economics 32, no. 2 (June 1, 1990): 171. http://dx.doi.org/10.21648/arthavij/1990/v32/i2/116124.

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Birts, A., L. McAulay, and M. King. "Financial analysis and expert systems." Journal of Information Technology 8, no. 3 (September 1993): 184–94. http://dx.doi.org/10.1057/jit.1993.25.

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Giesecke, Kay, Gustavo Schwenkler, and Justin A. Sirignano. "Inference for large financial systems." Mathematical Finance 30, no. 1 (July 12, 2019): 3–46. http://dx.doi.org/10.1111/mafi.12222.

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Journal articles on the topic 'Financial and geomorphological systems'

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