Stanisław Kędzia
Biographic Data
| ID | 8816904 |
|---|---|
| NAME | Stanisław Kędzia |
| GIVEN NAMES | Stanisław |
| FAMILY NAME | Kędzia |
| SIGNATURE | KĘDZIA S |
| AFFILIATIONS | Institute of Geography and Spatial Organization, Polish Academy of Sciences |
| ORCID | 0000-0002-5864-1463 |
| VERIFIED | Yes |
| TOTAL WORKS | 3 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 3 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2017 |
| LATEST PUBLICATION YEAR | 2023 |
| H-INDEX | 0 |
Debris flow activity in the Slovak part of the High Tatras in the light of lichenometric dating
Rock walls and talus slopes, which are the most common features of high-mountain relief, have been researched for many years. Geomorphologists have taken particular interest in debris flows, which play a major role in the development of talus slopes. This paper presents the results of the first lichenometric dating of debris flows on the southern slopes of the Tatra Mountains. The greatest debris flow activity took place in the Little Ice Age and…
Lichenometric curve for the southern slope of the Tatra Mountains (Slovak Tatras)
This paper presents the first lichenometric curve of Rhizocarpon geographicum for the southern slope of the Tatra Mts (Slovak Tatras). The curve was developed based on measurements carried out in the years 2018-2019. The curve was constructed using measurement results from 9 objects of known time of origin, situated in the Tatra Mts. at an altitude of 1,250-1,900 m a.s.l. On each of them, the diameter of the 5 largest thalli was measured. Their a…
The Little Ice Age in the Tatra Mountains
The Little Ice Age (LIA) in the Tatras was characterized by both long and short rainy periods (mostly long cold rainy summers) alternated with warm periods that sometimes were very dry. Definite, precise identification of the onset and ending of the LIA in the Tatras is not possible. Depending on the criteria adopted, the limits of the actual onset and ending vary slightly. During the LIA in the Tatras, there were no fully developed glaciers, and…
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The Little Ice Age in the Tatra Mountains
The Little Ice Age (LIA) in the Tatras was characterized by both long and short rainy periods (mostly long cold rainy summers) alternated with warm periods that sometimes were very dry. Definite, precise identification of the onset and ending of the LIA in the Tatras is not possible. Depending on the criteria adopted, the limits of the actual onset and ending vary slightly. During the LIA in the Tatras, there were no fully developed glaciers, and…
Lichenometric curve for the southern slope of the Tatra Mountains (Slovak Tatras)
This paper presents the first lichenometric curve of Rhizocarpon geographicum for the southern slope of the Tatra Mts (Slovak Tatras). The curve was developed based on measurements carried out in the years 2018-2019. The curve was constructed using measurement results from 9 objects of known time of origin, situated in the Tatra Mts. at an altitude of 1,250-1,900 m a.s.l. On each of them, the diameter of the 5 largest thalli was measured. Their a…
Debris flow activity in the Slovak part of the High Tatras in the light of lichenometric dating
Rock walls and talus slopes, which are the most common features of high-mountain relief, have been researched for many years. Geomorphologists have taken particular interest in debris flows, which play a major role in the development of talus slopes. This paper presents the results of the first lichenometric dating of debris flows on the southern slopes of the Tatra Mountains. The greatest debris flow activity took place in the Little Ice Age and…
Geography (3 works) · Geology (3 works) · Physical geography (3 works) · Geology (2 works) · Geology and Paleoclimatology Research (2 works) · Geomorphology (2 works) · Glacier (2 works) · Oceanography (2 works) · Aeolian processes and effects (1 work) · Altitude (triangle) (1 work)