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1
Content available Geomorphological map of the surroundings of Cortina d’Ampezzo (Dolomites, Italy)
100%
Pasuto A. , Soldati M.
Landform Analysis
|
2007
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tom Vol. 5
63--65
2
Content available Knottiness of spruce stems from the Dolomites as the basis for distinguishing quality zones in roundwood
63%
Barszcz A. , Sandak A. , Sandak J.
Folia Forestalia Polonica. Series A . Forestry
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2010
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tom 52
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nr 2
3
Content available Size and localisation of knots in timber from mountain spruce stands in the Dolomites
63%
Barszcz A. , Sandak A. , Sandak J.
Folia Forestalia Polonica. Series A . Forestry
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2010
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tom 52
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nr 1
EN
The aim of the study was evaluation of knots in wood of 150-year-old Norway spruce [Picea abies (L.) Karst.] in stands situated at the altitude of 1450– 1740 m above sea level in the Dolomites in Italian section of the Alps. In selected stands, spruce trees were cut down and their length, stem thickness, height to the crown base and stem diameters at every 1 m along the length of merchantable bole were measured. The diameter of knots was measured and they were classified according to their healthiness and the degree of their tightness with the surrounding wood. The relative knot diameters were calculated and the relative height of their location on stem was determined. In total on sample trees there were analysed 1070 knots, of which sound knots (close to 75%) and tight (more than 60%) prevailed. Sound and tight knots had largest diameters, relative diameters and relative heights of location on merchantable boles. The smallest diameters and relative diameters were indicated by rotten and not tight knots that were located at the lowest merchantable bole parts.
4
Content available Osuwisko Vajont (Włochy) : przykład katastrofy przyrodniczej wywołanej działaniami człowieka
63%
Różycka M. , Duszyński F. , Michniewicz A.
Przegląd Geologiczny
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2017
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tom Vol. 65, nr 9
560--563
EN
Vajont landslide, which affected the northern slope of Monte Toc in the Dolomites (NW Italy), is one of the most famous examples of a natural disaster induced by human activity. A wave, generated by displaced material that filled the Vajont reservoir, overtopped the dam and destroyed a few villages in the nearby Piave valley, resulting in death of approximately 2000people. In this review paper, some facts about the disaster are presented and its triggering factors are discussed. Information related to tourism development in the area is also provided.
5
Content available The uppermost Emsian and lower Eifelian in the Kielce Region of the Holy Cross Mts. Part I: Lithostratigraphy.
63%
Wójcik K.
Acta Geologica Polonica
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2015
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tom Vol. 65, no. 2
141--179
EN
The paper provides a description of primary geological logs, characteristics and formal lithostratigraphy of the uppermost Emsian and lower Eifelian of the Kielce Region of the Holy Cross Mts., central Poland. Nine sections of this interval, representing the whole area of the Kielce Region, and ranging between the Lower Devonian clastics of the Winna Formation and the Middle Devonian carbonates of the Kowala Formation were studied. The succession is divided into the Barania Góra Dolomite and Limestone Formation and the Wojciechowice Dolomite Formation. Six members are distinguished within the former. In the western part of the region these are (in stratigraphical order): Porzecze Claystone Member, Dębska Wola Dolomite Member, Dąbrowa Limestone Member, and Brzeziny Dolomite Member. In the eastern part, the formation is divided into the Janczyce Dolomite Member and the Jurkowice Dolomite Member. Additionally, the Wszachów Dolomite Member and Nowy Staw Dolomite Member are distinguished within the overlying Wojciechowice Formation. The thickness of the uppermost Emsian–Eifelian succession ranges from ca. 200 m in the eastern part to ca. 130 m in the western part of the Kielce Region.
6
Content available remote The ecological significance of solitary coral and bivalve epibionts on Lower Cretaceous (Valangianian-Aptian) ammonoids from the Italian Dolomites
51%
Lukeneder A.
Acta Geologica Polonica
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2008
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tom Vol. 58, no. 4
425-436
EN
Lower Cretaceous deposits of the Puez section in the Dolomites (northern Italy) yielded a rich ammonoid fauna (28 genera, n = 424) showing unique epifaunal encrustations by the ahermatypic solitary scleractinian ?Cycloseris LAMARCK, 1801. The coral encrusted only the outer shell surfaces of the ammonoids; the inner surface remained unaffected. Such a Cretaceous community and the relationship between the two fossil groups are described for the first time. The shells of dead ammonoids sank to the sea bottom and became colonized by the coral larvae, as documented by the location of the epibionts on only one side of the shells. The coral was fixed to the ammonoid shell for its entire life. Only the "sediment free" upper side of the ammonoid shells could be inhabited by epibionts such as corals and serpulids. The encrustation of ammonoid shells by the bivalve Placunopsis represents a different situation in that both sides of the ammonoid shells were affected, pointing to encrustation of floating ammonoids. This long-term infestation in the water column contrasts with coral settlement on the sea-floor. Ammonoid specimens encrusted by Placunopsis never exhibit encrustation by corals. The ammonoid-coral relationship from the Dolomites is documented from the Valanginian to Aptian interval. Examples of coral epibionts on ammonoids and other fossil groups throughout the geological column are briefly reviewed.
7
Content available remote Atrakcje geoturystyczne Europy - zajęcia terenowe studentów Geoturystyki Wydziału Geologii, Geofizyki i Ochrony Środowiska Akademii Górniczo-Hutniczej w Krakowie
38%
Doktor M. , Golonka J.
Geoturystyka
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2006
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tom nr 4
39-62
PL
Artykuł omawia atrakcje geoturystyczne Europy Środkowej objęte w roku 2006 programem zająć terenowych studentów specjalności Geoturystyka na Wydziale Geologii, Geofizyki i Ochrony Środowiska AGH w Krakowie.
EN
The following paper presents selected geotouristic attraction of Central Europe visited in May, 2006 by students of Geotourism from the Faculty of Geology, Geophysics and Environment Protection, AGH-University of Science and Technology in Kraków.
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