Autor: Mazurek, M. M. - Katalog OPAC zbiorów

Skocz do pozycji: 1.

Tytuł:: The 9th International Conference on Geomorphology in New Delhi, 2017 : report
Autorzy:: Mazurek, M.
Powiązania:: https://bibliotekanauki.pl/articles/294380.pdf
Data publikacji:: 2017
Wydawca:: Stowarzyszenie Geomorfologów Polskich
Tematy:: geomorphology
IAG/AIG
IGI
New Delhi
India
geomorfologia
IAG / AIG
Nowe Delhi
Indie
Opis:: This report contains short information about the 9th International Conference on Geomorphology in New Delhi in 2017 organised by the International Association of Geomorphologists and the Indian Geomorphology Institute.
Źródło:: Landform Analysis; 2017, 35; 3-7
1429-799X
Pojawia się w:: Landform Analysis
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 2.

Tytuł:: Obszary źródliskowe ogniwem łączącym system stokowy z systemem korytowym, dorzecze Parsęty
Autorzy:: Mazurek, M.
Powiązania:: https://bibliotekanauki.pl/articles/294563.pdf
Data publikacji:: 2008
Wydawca:: Stowarzyszenie Geomorfologów Polskich
Tematy:: obszar źródliskowy
system stokowy
system korytowy
dorzecze Parsęty
Źródło:: Landform Analysis; 2008, 9; 63-67
1429-799X
Pojawia się w:: Landform Analysis
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 3.

Tytuł:: Formation and development of a 1st-order valley network in postglacial areas (the Dębnica catchment)
Autorzy:: Mazurek, M.
Paluszkiewicz, R.
Powiązania:: https://bibliotekanauki.pl/articles/294444.pdf
Data publikacji:: 2013
Wydawca:: Stowarzyszenie Geomorfologów Polskich
Tematy:: valley network
erosional-denudational valleys
unchanneled colluvial valley
headwater alcoves
Dębnica catchment
Opis:: This article describes the formation and development of the 1st-order valley network in the postglacial catchment of the Dębnica River (NW Poland). Its valley network is an example of a system of polygenetic depressions, and its 1st-order sections are comprised of denudational hollows and valleys, dissections, and erosional-denudational valleys. In the article, both landforms with no permanent flow and those nourished by groundwater and included in the river runoff network are characterised. In the course of their development, dry valleys have continued to grow in width and length, while the gradient of their bottom has decreased due to slope wash processes. In groundwater outflow zones, in turn, the modelling of their slopes indicate retreat as a result of seepage erosion and mass movements, which has led to the preservation of their convex parts and the development of a concave section at the foot, passing into the flat bottom of an alcove. In headwater alcoves, which mark the start of a valley or are inserted into older valley landforms, morphological contrasts are enhanced because of an increase in their width and depth, as well as changes in their cross-profile.
Źródło:: Landform Analysis; 2013, 22; 75-87
1429-799X
Pojawia się w:: Landform Analysis
Dostawca treści:: Biblioteka Nauki