Tímea Kiss
Biographic Data
| ID | 7509752 |
|---|---|
| NAME | Tímea Kiss |
| GIVEN NAMES | Tímea |
| FAMILY NAME | Kiss |
| SIGNATURE | KISS T |
| AFFILIATIONS | University of Szeged |
| ORCID | 0000-0002-2597-5176 |
| VERIFIED | Yes |
| TOTAL WORKS | 8 |
| TOTAL CITATIONS | 0 |
| AUTHOR COUNT | 8 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2007 |
| LATEST PUBLICATION YEAR | 2023 |
| H-INDEX | 0 |
The Role of Past Climatic Variability in Fluvial Terrace Formation, a Case Study from River Mureş (Maros), Romania
Fluvial terrace formation is a complex process governed by the interplay of climatic and tectonic forcings. From a climatic perspective, an incision is usually related to climatic transitions, while valley aggradation is attributed to glacial periods. We have reconstructed the formation of Late Pleistocene fluvial terraces along the middle, mountainous section of a temperate zone river (Mureş/Maros) in order to identify the roles of different cli…
Late Pleistocene and Holocene aeolian activity in the Deliblato Sands, Serbia
The Deliblato Sands is among the largest uniform dune fields of Europe, with a very pronounced topography reflecting extensive past aeolian events. Although lacking numerical age data, previous researchers have hypothesized various periods of dune formation. Our research goals were to map the main morphological units of the Deliblato Sands, and to provide the first optically stimulated luminescence (OSL) ages for the major dune types. Mapping was…
Floodplain forms along the lowland Maros River, Hungary
The floodplain forms of lowland rivers act as fluvial archives, as their morphology, material and spatial characteristics refer to the hydromorphological changes of the river and (dis)connectivity of the alluvial system. The aims of the research are (1) to identify natural levees, crevasses, and point-bars on the Hungarian floodplain section of the Maros River, (2) to measure their morphometric parameters, and (3) to analyse their spatial and tem…
Additional figures in Ady Endre’s poem: A magyar Ugaron and in its English translations: The magyar fallow by Nyerges Anton and On the Hungarian fallow by Bernard Adams
My paper examines the figures of speech in English translations of Ady’s poem. The main organizers in Ady’s texts are repetition, parallelism, antithesis and other figures. The connection between these figures is an important component of his style. I examine whe-ther the translations are showing these figures, and if so, what their function is. The paper mostly concentrates on repetition in the translations. An analysis of one poem by Ady is pre…
Climatic fluctuations reflected in the evolution of fluvial systems of Central-Eastern Europe (60–8 ka cal BP)
The evolution of the Great Hungarian Plain fluvial system – Fluvial processes in a subsiding area from the beginning of the Weichselian
Holocene aeolian sand mobilization, vegetation history and human impact on the stabilized sand dune area of the southern Nyírség, Hungary
Almost 20% of the territory of Hungary is covered by stabilized dunes formed during the Pleistocene. With the climate amelioration during the early Holocene the aeolian activity ceased. However, various environmental and anthropogenic factors could have reactivated the aeolian processes. Today, there is an increasing climatic stress on the dune fields of the Carpathian Basin, which is coupled with inadequate land use. It is therefore necessary to…
Investigation of Holocene blown-sand movement based on archaeological findings and OSL dating, Danube-Tisza Interfluve, Hungary
Please click here to download the map associated with this article. The largest blown-sand area of Hungary is located on the Danube-Tisza Interfluve. Here the most significant aeolian activity took place in the Pleistocene, however the aeolian rework of the forms occurred also in the Holocene and even during historical times. The aims of the research were: (1) to map the geomorphology of the study area at the eastern border of the interfluve (2) …
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Investigation of Holocene blown-sand movement based on archaeological findings and OSL dating, Danube-Tisza Interfluve, Hungary
Please click here to download the map associated with this article. The largest blown-sand area of Hungary is located on the Danube-Tisza Interfluve. Here the most significant aeolian activity took place in the Pleistocene, however the aeolian rework of the forms occurred also in the Holocene and even during historical times. The aims of the research were: (1) to map the geomorphology of the study area at the eastern border of the interfluve (2) …
Holocene aeolian sand mobilization, vegetation history and human impact on the stabilized sand dune area of the southern Nyírség, Hungary
Almost 20% of the territory of Hungary is covered by stabilized dunes formed during the Pleistocene. With the climate amelioration during the early Holocene the aeolian activity ceased. However, various environmental and anthropogenic factors could have reactivated the aeolian processes. Today, there is an increasing climatic stress on the dune fields of the Carpathian Basin, which is coupled with inadequate land use. It is therefore necessary to…
Climatic fluctuations reflected in the evolution of fluvial systems of Central-Eastern Europe (60–8 ka cal BP)
The evolution of the Great Hungarian Plain fluvial system – Fluvial processes in a subsiding area from the beginning of the Weichselian
Floodplain forms along the lowland Maros River, Hungary
The floodplain forms of lowland rivers act as fluvial archives, as their morphology, material and spatial characteristics refer to the hydromorphological changes of the river and (dis)connectivity of the alluvial system. The aims of the research are (1) to identify natural levees, crevasses, and point-bars on the Hungarian floodplain section of the Maros River, (2) to measure their morphometric parameters, and (3) to analyse their spatial and tem…
Additional figures in Ady Endre’s poem: A magyar Ugaron and in its English translations: The magyar fallow by Nyerges Anton and On the Hungarian fallow by Bernard Adams
My paper examines the figures of speech in English translations of Ady’s poem. The main organizers in Ady’s texts are repetition, parallelism, antithesis and other figures. The connection between these figures is an important component of his style. I examine whe-ther the translations are showing these figures, and if so, what their function is. The paper mostly concentrates on repetition in the translations. An analysis of one poem by Ady is pre…
Late Pleistocene and Holocene aeolian activity in the Deliblato Sands, Serbia
The Deliblato Sands is among the largest uniform dune fields of Europe, with a very pronounced topography reflecting extensive past aeolian events. Although lacking numerical age data, previous researchers have hypothesized various periods of dune formation. Our research goals were to map the main morphological units of the Deliblato Sands, and to provide the first optically stimulated luminescence (OSL) ages for the major dune types. Mapping was…
The Role of Past Climatic Variability in Fluvial Terrace Formation, a Case Study from River Mureş (Maros), Romania
Fluvial terrace formation is a complex process governed by the interplay of climatic and tectonic forcings. From a climatic perspective, an incision is usually related to climatic transitions, while valley aggradation is attributed to glacial periods. We have reconstructed the formation of Late Pleistocene fluvial terraces along the middle, mountainous section of a temperate zone river (Mureş/Maros) in order to identify the roles of different cli…
Geography (7 works) · Geomorphology (7 works) · Physical geography (7 works) · Geology and Paleoclimatology Research (6 works) · Geology (5 works) · Marine and environmental studies (5 works) · Pleistocene (5 works) · Aeolian processes and effects (4 works) · Archaeology (4 works) · Fluvial (4 works)