{"id":1936,"date":"2022-01-10T12:52:57","date_gmt":"2022-01-10T11:52:57","guid":{"rendered":"https:\/\/wgsr.uw.edu.pl\/pisg\/?p=1936"},"modified":"2022-01-10T12:52:57","modified_gmt":"2022-01-10T11:52:57","slug":"t-66-3-s-89-103","status":"publish","type":"post","link":"https:\/\/pisg.wgsr.uw.edu.pl\/?p=1936","title":{"rendered":"T. 66.3, s. 89-103"},"content":{"rendered":"\n<h1 class=\"has-text-align-center wp-block-heading\"><strong>Przekszta\u0142cenie obszaru wysoczyzny lessowej pod wp\u0142ywem gospodarczej dzia\u0142alno\u015bci cz\u0142owieka w neoholocenie (na wybranych przyk\u0142adach z okolic Mozgawy, Ponidzie Pi\u0144czowskie)<\/strong><\/h1>\n\n\n\n<h2 class=\"has-text-align-center wp-block-heading\">Transformation of the loessic plateau due to the human economic activity in the Neoholocene (a case study of Mozgawa area, SE part of Nida River basin)<\/h2>\n\n\n\n<h5 class=\"has-text-align-center wp-block-heading\"><strong>Piotr SZWARCZEWSKI<\/strong><\/h5>\n\n\n\n<h5 class=\"has-text-align-center wp-block-heading\">Uniwersytet Warszawski<br \/>Wydzia\u0142 Geografii i Studi\u00f3w Regionalnych<br \/>e-mail: pfszwarc@uw.edu.pl<br \/>ORCID: 0000-0002-6104-1426<\/h5>\n\n\n\n<p><strong>Abstract:<\/strong> The Mozgawa area, located in the Ponidzie Pi\u0144czowskie Region (SE part of the Nida River Basin), is a very good example of response of the natural environment to the progressive human impact. The research conducted there indicates that before the appearance of the first Neolithic farmers, the relief of the area was different to the modern one. Constant and intensive agricultural use of the loess plateau and the adjacent slopes (started in the Neolithic period some 5890\u00b1100 BP) led to the filling of the valley bottoms and local depressions with deluvial deposits, the thickness of which reaches up to 12 m. The deposition of these sediments and elevation of the surface level in the subordinate areas resulted in the creation of the Mozgawka River channel since the begining of the Roman Period. Formerly it was impossible (as it was within the depression) and the runoff was only through the karst system. Since that moment it has also started the accumulation of the alluvial fan, the progradation of which leads to the pushing of the Nida River channel towards the East.<\/p>\n\n\n\n<p><strong>Key words:<\/strong> land use changes, the Neolith period, radiocarbon dating, deluvial deposits, Ponidzie<\/p>\n\n\n\n<p><strong>Zalecany spos\u00f3b cytowania \/ Cite as:<\/strong> Szwarczewski P., 2021, Przekszta\u0142cenie obszaru wysoczyzny lessowej pod wp\u0142ywem gospodarczej dzia\u0142alno\u015bci cz\u0142owieka w neoholocenie (na wybranych przyk\u0142adach z okolic Mozgawy, Ponidzie Pi\u0144czowskie), Prace i Studia Geograficzne, 66.3, Wydzia\u0142 Geografii i Studi\u00f3w Regionalnych Uniwersytetu Warszawskiego, Warszawa, 89\u2013103, DOI: 10.48128\/pisg\/2021-66.3-07.<\/p>\n\n\n\n<p>Wp\u0142yn\u0119\u0142o: 17.11.2021<br \/>Zaakceptowano: 29.12.2021<\/p>\n\n\n\n<p><a href=\"https:\/\/pisg.wgsr.uw.edu.pl\/wp-content\/uploads\/2022\/01\/PiSG_66_3_s89-103.pdf\">Pobierz ca\u0142y tekst w pdf \/ Get full text (pdf format)<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Przekszta\u0142cenie obszaru wysoczyzny lessowej pod wp\u0142ywem gospodarczej dzia\u0142alno\u015bci cz\u0142owieka w neoholocenie (na wybranych przyk\u0142adach z okolic Mozgawy, Ponidzie Pi\u0144czowskie) Transformation of the loessic plateau due to the human economic activity in the Neoholocene (a case study of Mozgawa area, SE part of Nida River basin) Piotr SZWARCZEWSKI Uniwersytet WarszawskiWydzia\u0142 Geografii i Studi\u00f3w Regionalnyche-mail: pfszwarc@uw.edu.plORCID: 0000-0002-6104-1426 [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_monsterinsights_skip_tracking":false,"_monsterinsights_sitenote_active":false,"_monsterinsights_sitenote_note":"","_monsterinsights_sitenote_category":0,"footnotes":""},"categories":[317,365],"tags":[831,841,843,1475,1799,2027,2159,2605,2961],"class_list":["post-1936","post","type-post","status-publish","format-standard","hentry","category-szwarczewski-piotr","category-t-66-z-3","tag-datowania-radioweglowe","tag-deluvial-deposits","tag-deluwia","tag-land-use-changes","tag-neolit","tag-ponidzie","tag-radiocarbon-dating","tag-the-neolith-period","tag-zmiany-uzytkowania-ziemi"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.5 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>T. 66.3, s. 89-103<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, 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