Wyniki wyszukiwania - Biblioteka Nauki

1

Rola plytkich ruchow osuwiskowych w ksztaltowaniu stokow fiszowych [na przykladzie Beskidu Wyspowego i Bieszczadow]

100%

Gorczyca E.

|

2008

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tom 80

|

nr 1

105-126

2

Slope relaxation following landslides in the Łososina River Basin, Beskid Wyspowy Mts., Poland

100%

Gorczyca E.

Landform Analysis

|

2010

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tom Vol. 14

3-11

EN

The paper presents results from a study of the functioning of slopes in conditions where the dynamic equilibrium has been upset and sliding has been followed by slope relaxation. The research was an attempt to analyze large-scale changes in slope morphology in the Łososina River basin in the Beskid Wyspowy mountain range caused by an extreme rainfall event in 1997. The enormous scale of the sliding process that occurred on the slopes of the Łososina basin provided an opportunity to study the role of mass movements in landform development in mountains of medium height. The paper attempts to summarize the rate and course of slope relaxation processes using geomorphological mapping done from 1997 to 2000. The study tested the hypothesis that following the occurrence of an extreme event, slope relaxation processes will slow down mass movement processes to the point where they stop acting on the slope, and ultimately a new set of slope development processes will emerge.

3

Przysmaki znad Wisloka

100%

Gorczyca E.

|

tom 51A

|

nr 08

19-21

4

The geomorphological effectiveness of extreme meteorological phenomena on flysch slopes

100%

Gorczyca E.

|

2008

|

tom Vol. 6

15--27

EN

Extreme events tend to cause large-scale slope system changes. During the last ten years, a series of extreme meteorological events caused considerable transformation of the slopes and valleys in various parts of the Carpathian Mountains. This paper presents the geomorphological effects of extreme rainfall and thaw events on the slopes of two catchments: the lososina catchment (Beskid Wyspowy) and the Hoczewka catchment with an area around the Solinskie Lake (Bieszczady Niskie). The bulk of the discussion concerns a study carried out in the Lososina catchment after three separate extreme events that were followed by a considerable transformation of the slopes due to landsliding. The studies carried out in the Biesr.cr.ady Range, where a single extreme event produced only spatially limited effects, were mainly used for comparison. '[he disparity between the responses of the two slope systems was a result of differences between the systems themselves, including their geology, geomorphology and landslide record, and of the difference in the scale of the extreme events.

5

Rola dróg i ścieżek turystycznych w modelowaniu rzeźby gór strefy umiarkowanej

63%

Gorczyca E. , Krzemien K.

Roczniki Bieszczadzkie

|

2010

|

tom 18

6

Rola antropopresji w przekształcaniu obszarów wysokogórskich na przykładzie Tatr i Monts Dore

63%

Gorczyca E. , Krzemien K.

Prace i Studia Geograficzne

|

2009

|

tom 41

EN

Under an extensive tourist penetration, mountain areas have been experiencing a high degree of anthropogenic degradation. Tourist traffic leads to the destruction of vegetation along roads and paths and nearby facilities, largely as a result of a considerable acceleration of geomorphologic processes. The paper presents certain environmental considerations, including relief, geology and climate, as well as micro-relief within tourist paths and morphogenetic processes influencing slope transformation within tourist areas in selected mountain areas. The general issue of the tourist-influenced degradation was discussed using two high mountain areas: the Tatras and Monts Dore mountains (Massif Central, France). In all of those areas, the anthropogenic geomorphologic features are highly diversified and well visible in the overall land relief. Tourist paths, roads and ski pistes constitute areas of overlapping natural and anthropogenic degradation. Wherever the natural vegetation, and especially the turf cover has been destroyed a state of permanent imbalance can be observed, as well as the development of crionival, aeolian and pluvial relief. The natural and anthropogenic processes influencing the morphodynamics of the roads and paths greatly vary in rate depending on the ground resistance, slope inclination and exposure, morphodynamical tier, type of surface, vegetation cover, season of the year and the intensity of the tourist traffic. Human activity in the mountains accelerates the circulation of energy and matter within individual slopes but sometimes also within entire massifs. The Monts Dore massif revealed the greatest degradation of its paths and tourist roads, followed by the Tatras.

7

Stan badań geomorfologicznych w Bieszczadach

51%

Gorczyca E. , Izmailow B. , Krzemien K. , Wronska-Walach D.

|

2011

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tom 19

8

Identyfikacja osuwisk w gminie Łososina Dolna na podstawie danych lotniczego skanowania laserowego

45%

Kroh P. , Strus P. , Gorczyca E. , Wronska-Walach D. , Dlugosz M.

|

2014

|

tom 38

9

Effects of environmental changes and human impact on the functioning of mountain river channels, Carpathians, southern Poland

45%

Krzemien K. , Gorczyca E. , Sobucki M. , Liro M. , Lyp M.

Annals of Warsaw University of Life Sciences - SGGW. Land Reclamation

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2015

|

tom 47

|

nr 3

EN

In the northern slope of the Carpathian Mountains and in their foreland, river and stream channels have been significantly transformed by human impact. These transformations result from changing land use in river basins and direct interference with river channels (alluvia extraction, engineering infrastructure, channel straightening). Anthropogenic impacts cause signifi cant changes in the channel system patterns leading to increased impact of erosion. This mainly leads to the channelling of the fluvial system. This article reviews studies of structure and dynamics of Carpathian river channels conducted based on the methodology of collection of data on channel systems, developed in the Department of Geomorphology of the Institute of Geography and Spatial Management, Jagiellonian University.

PL

W Karpatach i na ich przedpolu ma miejsce współcześnie znaczące przeobrażanie koryt rzek i potoków głównie pod wpływem antropopresji. Przeobrażenia te są uwarunkowane zmianami użytkowania w dorzeczach oraz bezpośrednią ingerencją w korytach (eksploatacja rumowiska, zabudowa hydrotechniczna, prostowanie koryt). W wyniku oddziaływań antropogenicznych następują znaczące zmiany struktury systemów korytowych prowadzące do wzrostu znaczenia erozji. Prowadzi to głównie do skanalizowania systemu fluwialnego. Artykuł jest przeglądem badań nad strukturą i dynamiką koryt rzek karpackich opartych na metodyce zbierania informacji o całych systemach korytowych. Zastosowano raptularz i instrukcję wypracowaną w Zakładzie Geomorfologii Instytutu Geografii i Gospodarki Przestrzennej Uniwersytetu Jagiellońskiego.

10

Polskie badania geomorfologiczne w Karpatach Wschodnich i znaczenie Bieszczadzkiego Parku Narodowego dla ochrony walorów przyrody nieożywionej

45%

Gorczyca E. , Izmailow B. , Klapyta P. , Krzemien K. , Wronska-Walach D.

Roczniki Bieszczadzkie

|

2014

|

tom 22

11

Ochrona przyrody nieożywionej w okresie II Rzeczypospolitej i współcześnie w południowo-wschodniej Polsce i w zachodniej Ukrainie

38%

Krzemien K. , Klapyta P. , Gorczyca E. , Krzemien P. , Nesteruk J. , Troll M.

Roczniki Bieszczadzkie

|

2019

|

tom 27

12

Problemy metodyczne analizy dendrochronologicznej procesów erozyjnych w zlewniach górskich

38%

Wronska-Walach D. , Gorczyca E. , Buchwał A. , Kropak J. , Sobucki M. , Wałdykowski P.

|

nr 1[30]

13

Antropogeniczne przekształcenia rzeźby na obszarze dawnych wsi łemkowskich (na przykładzie Radocyny, Beskid Niski)

26%

Gorczyca E. , Karcz T. , Sobucki M. , Augustyniak A. , Babicka Z. , Bryndza M. , Caputa J. , Jablonski K. , Kapka M. , Lysak S. , Mrosk A. , Szalapata M. , Sliwinska S. , Wieczorek A.

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tom 26