Rozwój doliny dolnej Łupawy w późnym plejstocenie
| dc.contributor.author | Czerniawska, Jolanta | |
| dc.date.accessioned | 2017-01-10T11:23:18Z | |
| dc.date.available | 2017-01-10T11:23:18Z | |
| dc.date.issued | 2007 | |
| dc.description.abstract | The lower £upawa valley is situated in the Gardno Phase marginal zone. The Gardno Phase represents a short ice readvance on the North Polish Plain. According to ROTNICKI (2001) Gardno Phase should be situated between 14 700 and 14 500 years B.P. The fossil ice-dammed lake has been discovered in the lower £upawa valley. Based on the analysis of the materials the extent of ice-dammed lake has been determined. Its dimensions are: width – 1,2 km, length – 5 km. During the first ice recession phase the ice-dammed lake disappeared. The first ice recession phase is situated between 14 300 and 14 000 years B.P. (ROTNICKI 2001). After that the aggradation of the alluvial fan of the £upawa began. Fossil channels of braided £upawa can be found in its top part. The oldest organogenic infillings of these channels started to accumulate 13 800± 270 years B.P. (ROTNICKI & BORÓWKA 1995). According to ROTNICKI & BORÓWKA (1995) one of the youngest organogenic infillings of these channels started to accumulate 6 700±70 years B.P. | pl_PL |
| dc.identifier.citation | Badania Fizjograficzne, Seria A, Tom 58, 2007, s. 21-30 | pl_PL |
| dc.identifier.isbn | 978-83-7063-538-1 | |
| dc.identifier.issn | 0067-2807 | |
| dc.identifier.uri | http://hdl.handle.net/10593/17332 | |
| dc.language.iso | pol | pl_PL |
| dc.publisher | Wydawnictwo Poznańskiego Towarzystwa Przyjaciół Nauk | pl_PL |
| dc.relation.ispartofseries | Seria A - Geografia Fizyczna TOM 58; | |
| dc.rights | info:eu-repo/semantics/openAccess | pl_PL |
| dc.title | Rozwój doliny dolnej Łupawy w późnym plejstocenie | pl_PL |
| dc.type | Artykuł | pl_PL |