Wyniki wyszukiwania - Biblioteka Nauki

1

Records of the Late Glacial-Holocene palaeoenvironmental changes in landslide forms and deposits of the Beskid Makowski and Beskid Wyspowy Mts. area (Polish Outer Carpathians)

100%

Margielewski W.

|

2006

|

tom nr 76

149-149

EN

In the Beskid Makowski and Beskid Wyspowy Mts., Polish Outer Carpathians, 23 peat-bogs of different ages, situated in landslide depressions (fen mountainous peat-bogs) were studied and dated. Mineral horizons, illuvial horizons and mineral covers were invesligated in the sediments of these peat-bogs. Deposition of mineral sediments was connected with the humid climatic phases in the Late Glacial and Holocene, during which delivery of allochthonous material to peat-bog basins took place. Climate changes are recorded in differing ways within the sediments, which were conditioned by the specificity of the depositional environment of particular peat-bog basins, which react differently to climatic changes and human impact. Detailed and complex investigations of peat-bog profiles were conducted including lithological descriptions (loss on ignition, grain size and peat analyses) and numerous radiocarbon datings, using samples mainly from the horizons of the lithological changes (as diagnostic). Complete palynological profiles were made for eight sections. These investigations have documented that the deliveries of mineral material to the peat-bog basins took place mainly during the humid climate phases in the Bolling and Allerod Interstadials, at the beginning of the Holocene (YD/PB) and the boundary of the PB/BO, at the boundary of the BO/AT phases and the beginning of the Atlantic Phase, at the end of the Atlantic Phase and at the beginning of the Subboreal Phase (ca 5.5-4.8 and ca 4.5-4.1 ka BP), in the Subboreal Phase ca 3.5-3.0 ka BP, at the beginning of the Subatlantic Phase (ca 2.4 -1.8 ka BP), in the 5-7th centuries, in the 10-11th centuries, and during the Little Ice Age. The recorded humid phases are correlated with phases of fluvial activity of the Upper Vistula River as well as with phases of climate moistening observed in various sediments' facies of Europe. The use of probability density function for statistical analysis of distribution of the radiocarbon dates of the landslides in the Carpathians (66 dates) and mineral horizons in the studied peat-bogs (93 selected, representative datings) makes possible the determination (in the BC/AD age) of the phases of intensification of slope processes, which took place: 14,600-14,400 BC; 11,500-11,100 BC; 10,100-9,700 BC; 9,200-8,600 BC; 7,700-7,200 BC; 6,400-5,600 BC; 5,000-4,400 BC; 3,900-3,400 BC; 2,800-2,600 BC; 2,200-2,000 BC; 1,700-1,300 BC; 800 BC-AD 0; AD 600-1,000; AD 1,200-1,400; and AD 1,600-1,800.

2

Zasiedlanie przez plazy nowopowstalych zbiornikow wodnych

83%

Basta G. , Guzik M. , Zamachowski W.

Przegląd Przyrodniczy

|

2002

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tom 13

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nr 3

121-128

3

Sklad pokarmu puszczyka zwyczajnego Strix aluco L. z Beskidu Wyspowego [Dobra k.Limanowej]

83%

Ruprecht A. L.

Przegląd Przyrodniczy

|

2002

|

tom 13

|

nr 1-2

191-197

4

Awifauna srodkowej czesci Beskidu Wyspowego - propozycje ochrony

83%

Kajtoch L. , Piestrzynska-Kajtoch A.

|

tom 62

|

nr 3

33-46

5

Okazaly owocnik grzyba podziemnego Choiromyces meandriformis Vitt. z Beskidu Wyspowego

71%

Guminska B. , Turnau K.

Chrońmy Przyrodę Ojczystą

|

1997

|

tom 53

|

nr 2

90-93

6

Tourist products buyers in the Luboń Wielki area

71%

Warcholik W.

Annales Universitatis Paedagogicae Cracoviensis Studia Geographica

|

2015

|

tom 9

194-205

EN

The article presents segmentation of tourist products buyers in the Luboń Wielki area. The results are shown in the context of attempts to create market for tourist services in Beskid Wyspowy. Tourist profile was created based on the monitoring of tourism traffic and surveys, including the perception of the image of this part of the mountains. Elements registered as essential in the planning and development of tourist services are: the existence of two peaks in the daily presence of tourists, predominance of individual hikers, specialisation for cycling routs and the close relationship between the intensity of tourist traffic and meteorological conditions. There are significant differences in terms of planned and actual traffic on tourist routs, without relation to the location near the potential tourist attractions. Tourists more often consider as such PTTK shelters and approach of the Rabka spa, than for example, the values of Inanimate Nature Reserve of Luboń Wielki.

7

Structure of land utilisation in the Western Carpathian Mountains as exemplified by the Beskid Wyspowy and Zywiecki

71%

Kopec S.

|

1999

|

tom 87 supl.

169-176

8

Czarne chmury nad Mogielnica

71%

Kajtach L.

|

2006

|

nr 04

29

9

Tourist products buyers in the Luboń Wielki area

71%

Warcholik W.

Annales Universitatis Paedagogicae Cracoviensis Studia Geographica

|

2015

|

tom 9

194-205

EN

The article presents segmentation of tourist products buyers in the Luboń Wielki area. The results are shown in the context of attempts to create market for tourist services in Beskid Wyspowy. Tourist profile was created based on the monitoring of tourism traffic and surveys, including the perception of the image of this part of the mountains. Elements registered as essential in the planning and development of tourist services are: the existence of two peaks in the daily presence of tourists, predominance of individual hikers, specialisation for cycling routs and the close relationship between the intensity of tourist traffic and meteorological conditions. There are significant differences in terms of planned and actual traffic on tourist routs, without relation to the location near the potential tourist attractions. Tourists more often consider as such PTTK shelters and approach of the Rabka spa, than for example, the values of Inanimate Nature Reserve of Luboń Wielki.

10

Wystepowanie siwerniaka Anthus spinoletta w Beskidzie Wyspowym

71%

Kajtoch L. , Piestrzynska-Kajtoch A.

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tom 46

|

nr 3

187-189

11

Interesujace stanowisko kreczynki jesiennej Spiranthes spiralis w Pasmie Jaworzna [Beskid Wyspowy]

59%

Szewczyk M.

Chrońmy Przyrodę Ojczystą

|

2003

|

tom 59

|

nr 3

80-82

12

Ochrona elementow rzezby osuwiskowej Mogielicy [Beskid Wyspowy]

59%

Margielewski W.

Chrońmy Przyrodę Ojczystą

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1997

|

tom 53

|

nr 4

85-97

13

Ryjkowce [Coleoptera, Curculionidae] Beskidu Wyspowego

59%

Petryszak B.

Studia Ośrodka Dokumentacji Fizjograficznej

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1993

|

tom 21

281-303

14

Porosty Beskidow Wyspowego i Zywieckiego, Pasma Jalowca i Masywu Babiej Gory

59%

Nowak J.

Monographiae Botanicae

|

1998

|

tom 83

361

15

Sowy Strigiformes Pogorza Wielicko-Wisnickiego i Beskidu Wyspowego

48%

Kajtoch L.

Notatki Ornitologiczne

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2006

|

tom 47

|

nr 4

252-259

16

Flora i zbiorowiska chwastow zboz w Beskidzie Wyspowym w zaleznosci od usytuowania siedlisk w rzezbie terenu

42%

Hochol T.

Fragmenta Agronomica

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2001

|

tom 18

|

nr 3

7-122

17

Refleksje popowodziowe

36%

Klimek M.

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1998

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nr 08

19-20