Zobrazeno 1 - 10
of 37
pro vyhledávání: '"Adam Łajczak"'
Publikováno v:
Journal of Maps, Vol 17, Iss 4, Pp 186-193 (2021)
The aim of the paper is to reconstruct differences between the paleotopography and contemporary topography of the historic centre of Krakow city, Poland, during the last millennium. The paleotopography was reconstructed using published contour-line m
Externí odkaz:
https://doaj.org/article/ee68f37972154d2ebe154c3b4d74b999
Publikováno v:
Remote Sensing, Vol 13, Iss 12, p 2286 (2021)
For the area of historic centre of Krakow (area 9.29 km2), southern Poland, base maps were prepared showing hypsometry and distribution of landforms in historical variant (ca. 1000 AD) and current variant, based on published data mainly from archaeol
Externí odkaz:
https://doaj.org/article/e1fcd9c3c6cc4cf99f18feaf760c4d31
Publikováno v:
Land, Vol 10, Iss 2, p 104 (2021)
Geomorphological research in the Fann Mountains of the Pamir-Alay has indicated that subnival processes are occurring. Contemporary subnival sediments indicate that complex relationships occur between the snow patches, subnival waters, and ground. Un
Externí odkaz:
https://doaj.org/article/d4ef06535fbe408d8e1fb0373213b7ac
Autor:
Adam Łajczak, Włodzimierz Margielewski, Tomasz Zielonka, Tomasz Pasierbek, Tomasz Lamorski, Piotr Kozina, Katarzyna Izworska
Publikováno v:
Geographia Polonica. 96:79-101
Cylowa Zerwa landslide – debris flow located on the northern slope of Mt. Babia Góra (1725 m a.s.l.) within the 400 m wide altitude interval (1430-1024 m a.s.l.) is a knowable object which however has not been sufficiently noticed in geomorphologi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a961a60fb642c6b0604f7b56b29de1cd
https://doi.org/10.7163/gpol.0247
https://doi.org/10.7163/gpol.0247
Publikováno v:
Journal of Maps, Vol 17, Iss 4, Pp 186-193 (2021)
The aim of the paper is to reconstruct differences between the paleotopography and contemporary topography of the historic centre of Krakow city, Poland, during the last millennium. The paleotopography was reconstructed using published contour-line m
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6d4df234629307da75f335deebfaac97
https://doi.org/10.1080/17445647.2020.1823253
https://doi.org/10.1080/17445647.2020.1823253
Publikováno v:
Przegląd Geologiczny. 68:102-111
Structural morphology of the area of the Świetokrzyski National Park. A b s t r a c t. The area of the Świetokrzyski National Park is one of the most evident examples of structural morphology in Poland. Its relief is clearly determined by bedrock l
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5ad50060beee56206b9eafcaf93dc147
https://doi.org/10.7306/2020.3
https://doi.org/10.7306/2020.3
Reconstruction of the morphology and hydrography of the centre of Kraków before the mid-13th century
Autor:
Adam Łajczak, Roksana Zarychta
Publikováno v:
Geographia Polonica. 93:25-50
The paper concerns investigations on urban geomorphology. The subject of the paper is the historic centre of Kraków (or Cracow) where the pre-human relief became masked due to the rapid increase in cultural deposits from the mid-13th century onwards
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ea3fcaa3650e5ec7960a12c4a8245c5e
https://doi.org/10.7163/gpol.0161
https://doi.org/10.7163/gpol.0161
Forms related to nival accumulation are recorded worldwide, and the role of nivation in relief formation was studied by many scientists. In classifications used nowadays, adopted in the last two decades, protalus and sub-slope nivation and glacial fo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f976e7bc68857702186317fd5fcaf9ef
https://doi.org/10.5194/egusphere-egu2020-11121
https://doi.org/10.5194/egusphere-egu2020-11121
Autor:
Roksana Zarychta, Adam Łajczak
In the investigations on changes of topography of historical town centres the attention is focused on estimation of the thickness of cultural layers and on determination of changes of land topography in selected small areas or along profiles. Less of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1842be809c54355678415f2471a5f736
https://doi.org/10.5194/egusphere-egu2020-22674
https://doi.org/10.5194/egusphere-egu2020-22674