scholarly journals DEM based morphotectonical analysis of the Kisgyőr Basin (Bükk Mts – Hungary)

2021 ◽  
pp. 364-374

The south-eastern part of the Bükk Mountains and the eastern side of its foothill, the Bükkalja are among the less explored regions of Hungary. Based on our examinations on the field, we found that the asymmetrical valley sections, the tipped escarpments and the formation of the Kisgyőr Basin cannot be explained by the differences in the rock quality. The asymmetrical shape of these landforms and the stream captures identified in the research area indicate significant structural geological changes. In our work, we proved the asymmetry in the topography by performing swath profile analysis, and we also examined the elevation data of the areas covered by the welded ignimbrites of the Tar Dacite Tuff Formation. The results confirmed our field observations. We found that, contrary to the results of previous research, the geological structural processes played a fundamental role in the formation of the Kisgyőr Basin and its surroundings.

2021 ◽  
Author(s):  
Gail Higginbottom ◽  
Antonio César González-García ◽  
Miguel Carrero-Pazos ◽  
Benito Vilas-Estévez ◽  
Víctor López-López

This paper investigates the dolmen landscapes of Neolithic communities found within Costa da Morte (Coast of Death), Galicia. Its goal is to uncover whether or not the megalithic monuments of a particular and coherent area of the south-eastern side of the Atlantic Façade are situated in relation to complex locational variables. In particular, in this paper, we explore the entirety of their surrounding topography. For the very first time, we were able to demonstrate that very specific natural landscapes surrounding the dolmens of this region in Iberia were likely selectively drawn upon, expanding our understanding of the Neolithic of this area and the people's relationship with their natural world.


Britannia ◽  
2006 ◽  
Vol 37 ◽  
pp. 53-188 ◽  
Author(s):  
Rosalind Niblett ◽  
William Manning ◽  
Christopher Saunders

ABSTRACTExcavations in Insulae II, III and XIII in the southern half of Verulamium demonstrated the absence of occupation prior to the late first century and the relatively late development of the street grid in this area. This forced a re-evaluation of the date of the 1955 ditch, suggesting it was not dug until the Flavian period. The excavations also demonstrated that Watling Street had never bisected Insula XIII on the south-eastern side of the Forum-Basilica, thus negating a major argument for the presence of a Claudian fort under the centre of the later town. A restricted excavation in the northern corner of Insula XIII revealed evidence for the location of the town’s baths, while excavation in Insula XIII revealed a long sequence of industrial and domestic occupation stretching from the late first to early fifth centuries. Evidence for continued occupation into the fifth century or beyond was recovered from Insula II, and to a lesser extent, in Insula XIII.


Geoadria ◽  
2017 ◽  
Vol 19 (2) ◽  
pp. 205
Author(s):  
Vesna Koščak Miočić-Stošić ◽  
Ana Žmire ◽  
Martina Šekutor ◽  
Ivana Bunjak-Pajdek

Regardless of the fact that the traditional usage of rural landscapes was agricultural, a degradation of landscape values, as well as an onset of natural succession, occur due to contemporary lifestyle. This can lead to negative effects regarding land-use change. This paper focuses on the south-eastern part of Pag island and explores the possibilities for the revitalisation of its neglected areas by envisioning its future development as an olive-growing region. The final goal was to define a planning procedure framework which would enable the creation of a strategic vision to be transformed into a comprehensive spatial development strategy for the research area. This area encompasses the territory between Kaštela in the north-west and the Pag’s bridge in the south-east which administratively belongs to the Zadar County and includes the Town of Pag, and the Kolan and Povljana municipalities. Olive-growing has been recognized as the strategic choice for development because of its tradition in the area and the potential integration with other relatable activities. Based on the SWOT analysis, an appropriate mission, a vision and strategic goals were defined for developing Pag as an olive-growing region. Further landscape planning methods included (1) the Lynch mapping analysis, (2) the Forman and Godron landscape ecology analysis and (3) the landscape pattern analysis. The results were then used together with digital orthophoto imagery to overlay and analyse relevant information. Hand drawings as well as AutoCAD, ArcGIS and image editing computer programmes were used in the process. This analytical phase was then followed by the development of several alternative spatial zonings, diagrams and concepts based on a preferable neighbourhood matrix and the activity sizing table. The planning process resulted in a concept for spatial development of the research area which would enable the implementation of the strategic vision. The main goal of this planning procedure was to preserve and improve the rural landscape of Pag island.


Baltica ◽  
2018 ◽  
Vol 31 (1) ◽  
pp. 73-85 ◽  
Author(s):  
Ewa Bednorz ◽  
Bartosz Czernecki ◽  
Marek Półrolniczak ◽  
Arkadiusz M. Tomczyk

The meteorological forcing on the occurrence of upwelling along the south-eastern Baltic Sea coast (Lithuanian-Latvian sector) is analysed in this study. The sea level pressure patterns and the locations of pressure centres inducing and inhibiting upwelling were identified. The research was performed for the years 1982–2017, for the months of May–September, when the sea waters are thermally stratified and the phenomenon is detectable. The frequency of upwelling is the highest in June (approximately 15%), July and August (11–13%) and the lowest in September (7%). The central and northern part of the Lithuanian–Latvian coast is most favourable for upwelling occurrence (frequency up to 20% in summer months). The main features of the sea level pressure patterns that induce upwelling in the research area are positive pressure anomalies spreading over Northern Europe and the Norwegian Sea, while negative anomalies encompass Southern Europe. Airflow around the anticyclonic centres gives a north-eastern component to the wind direction over the Lithuanian-Latvian shore. Two circulation types were recognized as inducing the occurrence of upwelling along the Lithuanian–Latvian coast. Both of them are characterized by the anticyclonic centres located west or northwest of the study area and intensify the northerly or north-easterly airflow over the research area. Different pressure patterns with the negative anomalies of sea level pressure spreading over the North Sea and the positive anomalies underlying Central Europe inhibit upwelling along the Lithuanian–Latvian coast. Such pressure conditions, bring about the western airflow component. More constant western winds restrain the upwelling process and bring about normal thermal stratification of coastal waters. A detailed analysis allowed the recognition of two circulation types inhibiting coastal upwelling in the study area. They reveal dipole patterns of sea level pressure anomalies, but the two inhibiting patterns differ substantially in the intensities and locations of the pressure centres and in wind conditions.


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