Josef Hromada
Biographic Data
| ID | 6527186 |
|---|---|
| NAME | Josef Hromada |
| GIVEN NAMES | Josef |
| FAMILY NAME | Hromada |
| SIGNATURE | HROMADA J |
| AFFILIATIONS | Institute of Archaeology of the Slovak Academy of Sciences |
| VERIFIED | No |
| TOTAL WORKS | 2 |
| TOTAL CITATIONS | 3 |
| WORKS AS AUTHOR | 2 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 1995 |
| LATEST PUBLICATION YEAR | 1998 |
| H-INDEX | 1 |
Correlation between Loess profiles on the basis of mineralogical, malacological, and anthropogenic indicators
Moravany-Lopata, located in the complex of sites in the middle Vah basin, dates to the period immediately preceding the LGM. The authors use this site to demonstrate the usefulness of mineralogical, sedimentological, palaeomalacological, and anthropogenic criteria for the correlation of loess profiles. This analysis is especially concerned with sites in loess territories where the loess layers covering archaeological levels are not thick. Such si…
Site formation processes in loess areas
The site of Moravany‐Žakovska in western Slovakia is situated in a loessic terrain and is dated to the end of the Late Glacial Maximum. This article shows the importance of analyzing the 0.01‐0.1 mm fraction to interpret the sedimentological environment and a number of measured anthropogenic indices, such as burnt quartz grains, charcoal, radiolarite chips, microflakes, and microfragments of bone. Analysis of the profile of the site through time …
Site formation processes in loess areas
The site of Moravany‐Žakovska in western Slovakia is situated in a loessic terrain and is dated to the end of the Late Glacial Maximum. This article shows the importance of analyzing the 0.01‐0.1 mm fraction to interpret the sedimentological environment and a number of measured anthropogenic indices, such as burnt quartz grains, charcoal, radiolarite chips, microflakes, and microfragments of bone. Analysis of the profile of the site through time …
Site formation processes in loess areas
The site of Moravany‐Žakovska in western Slovakia is situated in a loessic terrain and is dated to the end of the Late Glacial Maximum. This article shows the importance of analyzing the 0.01‐0.1 mm fraction to interpret the sedimentological environment and a number of measured anthropogenic indices, such as burnt quartz grains, charcoal, radiolarite chips, microflakes, and microfragments of bone. Analysis of the profile of the site through time …
Correlation between Loess profiles on the basis of mineralogical, malacological, and anthropogenic indicators
Moravany-Lopata, located in the complex of sites in the middle Vah basin, dates to the period immediately preceding the LGM. The authors use this site to demonstrate the usefulness of mineralogical, sedimentological, palaeomalacological, and anthropogenic criteria for the correlation of loess profiles. This analysis is especially concerned with sites in loess territories where the loess layers covering archaeological levels are not thick. Such si…
Ancient and Medieval Archaeology Studies (2 works) · Archaeology (2 works) · Geography (2 works) · Geology (2 works) · Geomorphology (2 works) · Image Processing and 3D Reconstruction (2 works) · Loess (2 works) · Physical geography (2 works) · Aeolian processes (1 work) · Hearth (1 work)