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ПРИЧИНЫ ДЕПРЕССИВНОГО СОСТОЯНИЯ СТАДА АТЛАНТИЧЕСКОГО ЛОСОСЯ РЕКИ ВАРЗУГА (КОЛЬСКИЙ ПОЛУОСТРОВ)

ПРИЧИНЫ ДЕПРЕССИВНОГО СОСТОЯНИЯ СТАДА АТЛАНТИЧЕСКОГО ЛОСОСЯ РЕКИ ВАРЗУГА (КОЛЬСКИЙ ПОЛУОСТРОВ)

Author(s): Maksim Yu. Alekseev,Aleksandar V. Zubchenko / Language(s): Russian Issue: 2 (163)/2017

The problem of negative trends in numerical strength dynamics in the species of Atlantic salmon inhabiting the Varzuga River (the White Sea basin) is studied in the article. A retrospective review of the fisheries in focus and their regulations are described. Dynamics of the spawning stock’s numerical strength are considered; the impact of different volumes of the fish yield is estimated. Based on the results of the long-term ongoing research describing the density of juveniles’ distribution on the nursery grounds, research data on the significant decrease in the parrs’ numerical strength (up to a complete absence in some parts of the river) were obtained. This fact coupled together with plummeting numbers of spawning migrants speaks of the unsatisfying state of salmon stock reproduction. This effect was conditioned by the unsustainable exploitation of the stock by massive illegal and unreported fishing. The method of mathematical simulation has defined a contemporary level of commercial exploitation of the Varzuga River’s salmon stock. It was concluded that a contemporary harvest of local producers, obtained by all types of fisheries, composes no less than 85 %. The implementation of the advised fish protection activities can assist in Atlantic salmon population recovery during 6–12 years.

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ОСОБЕННОСТИ ПИТАНИЯ РЫБ ЛИТОРАЛЬНОЙ ЗОНЫ ОНЕЖСКОГО ОЗЕРА

ОСОБЕННОСТИ ПИТАНИЯ РЫБ ЛИТОРАЛЬНОЙ ЗОНЫ ОНЕЖСКОГО ОЗЕРА

Author(s): Aleksandra S. Lobanova,Yuri A. Shustov / Language(s): Russian Issue: 2 (163)/2017

Characteristic nutrition features of massive fish species found in the littoral zone of the lake Onega are considered in the article. The intensive distribution of such invasive species as Baikal amphipods Gmelinoides fasciatus in the lake Onega has led to its significant numerical strength and growth in biomass. Our research showed that Baikal amphipod became an important ingredient (up to 50 % of the food bolus) in the diet of perch fish – perch and ruff in the northern, western and eastern coasts. This new object of zoobenthos is not included into the diet of local roach – a rather mass species of carp fish. The Baikal crustacean was found in the diet of some types but not all types of fish inhabiting investigated in our research areas of Onega Lake. An assumption can be made that the aboriginal fish will start consuming amphipod once it spreads in multiple shallow areas.

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ОЦЕНКА ЭКОЛОГИЧЕСКОГО СОСТОЯНИЯ СНЕЖНОГО ПОКРОВА ТЕРРИТОРИИ, ПРИЛЕГАЮЩЕЙ К САКМАРСКОЙ ТЭЦ Г. ОРЕНБУРГА

ОЦЕНКА ЭКОЛОГИЧЕСКОГО СОСТОЯНИЯ СНЕЖНОГО ПОКРОВА ТЕРРИТОРИИ, ПРИЛЕГАЮЩЕЙ К САКМАРСКОЙ ТЭЦ Г. ОРЕНБУРГА

Author(s): Anastasia A. Shaykhutdinova,Olga V. Chekmareva,Olga S. Markova / Language(s): Russian Issue: 2 (163)/2017

An integrated assessment of the degree of the snow cover pollution, as an indicator of the state of the atmospheric air, and a subsequent ranking of the areas adjacent to Sakmarskaya CHP plant (Orenburg) are presented. Priority pollutant masses and their toxicity are analyzed. A degree of the enterprise’s danger level is calculated. Selected samples of the snow cover were investigated for the content of harmful substances using titrimetric, photocolorimetric, and gravimetric methods. The ecological quality of the areas adjacent to stationary sources of pollution was evaluated. The assessment was calculated by the ratio of pollutant concentration, by the level of chemical pollution in precipitations, by the environmental load of contaminants, and by the total load of all impurities released by the sediment detachment into the atmospheric air in focus. According to these indicators, the ranking of studied territories in the zones of ecological challenge was conducted based on the existing evaluation criteria. In the course of our research it was established that all investigated pollutants were dispersed over considerable distances from Sakmarskaya CHP plant and crossed the sanitary-protective zone of the enterprise. Therefore, the health of the people residing in the western direction from the plant’s location could be seriously affected. The area of contamination covers the territory of 1200 m from the source of emission.

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1859 YILINDAKİ ŞAMAHI VE ERZURUM DEPREMLERİ HAKKINDA RUSYA BİLİMLER AKADEMİSİ ÜYESİ HERMANN VON ABICH’İN RAPORU 1859 YILINDAKİ ŞAMAHI VE ERZURUM DEPREMLERİ HAKKINDA RUSYA BİLİMLER AKADEMİSİ ÜYESİ HERMANN VON ABICH’İN RAPORU

1859 YILINDAKİ ŞAMAHI VE ERZURUM DEPREMLERİ HAKKINDA RUSYA BİLİMLER AKADEMİSİ ÜYESİ HERMANN VON ABICH’İN RAPORU 1859 YILINDAKİ ŞAMAHI VE ERZURUM DEPREMLERİ HAKKINDA RUSYA BİLİMLER AKADEMİSİ ÜYESİ HERMANN VON ABICH’İN RAPORU

Author(s): M. Yasin Taşkesenlioğlu,Muhammed Taşkesenligil / Language(s): Turkish Issue: 20/2020

The Caucasus, where the mountains extending from the Black Sea to the Caspian Sea, is almost divided into two parts, has been one of the expansion areas of Russia since the 18th century. Russia, which managed to dominate the entire Caucasus, including the South Caucasus region, which was called ZaCaucasia in the following century, not only politically and militarily, but also through scientific studies with the studies it has established within the Academy of Sciences, it has managed to create an inventory that concerns many disciplines, especially history, geography and sociology. Moreover, these scientific studies were carried out in the territory of other states, such as the Ottoman State. In 1859, upon the simultaneous earthquakes in Shamakhy and Ottoman-dominated Erzurum, the Academy of Sciences commissioned the German geologist Abich, who has been conducting research in the Caucasus, to conduct seismic surveys in these regions. This report, which was published in Russian shortly after presenting her field research to the academy in French, constitutes the most important part of our study. In the introduction part of the report before the conclusion of the field researches on the related earthquakes, Abich, who made evaluations about geology, emphasized the importance of the Caucasus region for this branch of science. Abich, who carried out his investigations on the Shamakhy and Erzurum earthquakes with the help of barometers and technical devices, also gave important information about the topography of the cities and the destruction they suffered. In the sections of this study other than the translation of the report, there is also an evaluation by us in the light of first hand sources regarding both earthquakes and the destruction caused by it.

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Stari natpisi u nekim hrvatskim špiljama

Stari natpisi u nekim hrvatskim špiljama

Author(s): Vlado Božić / Language(s): Croatian Issue: 1/2006

One proof of ancient visitors to and research of caves, especially those which are easy to approach and therefore very often visited, are the inscriptions left there. Those new inscriptions, it is believed, ruin the caves, while those ancient, especially if the years are inscribed, today represent an important document and speleologists record them and try to protect them. The oldest such inscriptions were found in the area of Senj, in Vlaška Peć cave, written in Bosančica (a type of cyrillic alphabet), originally from 1600 and 1650. After this, there is an inscription in Druška Peć cave on Mount Učka from 1637 written in Glagolitic; more inscriptions in Latin alphabet from the Kraljičina Špilja (the Queen’s Cave) on the island of Vis written in 1643, 1641, 1665 and later in 1815 and later; from Gospodska Špilja (the Lord’s Cave) on the source of the Cetina from 1775 and 1776 and many others from the 19th and 20th centuries. The inscriptions from the 19th centuries are numerous and the most important are: from the cave Samograd near Perušić from 1835 and 1888, from the Rače cave on the island of Lastovo from 1848, from Donja Baraćeva cave near Rakovica written in 1892 and more inscriptions from the end of the 19th century near the cave Biserujka on the island of Krk. Amongst the inscriptions from the 20th century, other valuable inscriptions are those in Špiljareva or Dezerterska cave on Crnopuc from 1915, the inscription from 1917 from the Metešićeva cave near Slunj and inscription from 1934 from the cave Veternica near Zagreb.

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Špilja Pijavica nekad i danas

Špilja Pijavica nekad i danas

Author(s): Vlado Božić / Language(s): Croatian Issue: 1/2005

About 2 kilometres from Senj, along the seaside, is a little cave named Pijavica. It can be seen that the cave has significantly changed its size, form and function. Stjepan Vuksan was the first who described the cave in 1907 as a gorge. There seawater mixes with freshwater of the cave and the water comes out as two undersea sources. He noticed that the cave has an undersea and underground entrance to the hall the size of 18m x 15m. Josip Poljak confirmed the source of the freshwater in 1914. He measured the size of the cave hall as 26m x 15m and the depth of the brackish water as 3.4m. He found a strong source of freshwater in the cave but he did not find where the sea disappeared underground the cave. Vlado Božić entered into the cave for the first time in 1985 through the cave entrance, using a rope and he found the cave hall, which was already filled with some material from the surface and it had the size 20m x 10m. An undersea entrance was visible in the hall with a specific blue effect during afternoon as the undersea entrance is facing southwest towards sized 30m x 3m. The potholer Branko Jalžić organised a few diving actions. The divers entered from the seaside through a channel into the cave hall from the seaside. Anđelko Novosel, a member of the team, noticed in 1993 that someone was throwing building material through the ground entrance of the cave, which could cause the backfilling of the cave. He organised an action to protect the cave but without any success. At the beginning of April 1994 someone threw a large quantity of building waste, which completely closed the ground entrance of the cave. The undersea entrance to the cave was also closed. This destroyed a cave with a specific blue effect like the Blue Cave on the island of Biševo.

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Episode with strong downslope wind in the Southern and Curvature Carpathians in the period 5-6 february 2020

Episode with strong downslope wind in the Southern and Curvature Carpathians in the period 5-6 february 2020

Author(s): M.H. HUȘTIU,Adrian Boariu / Language(s): English Issue: 1/2021

The phenomenon that occurred during the blizzard from February 5-6 in the mountains and especially on the southern slopes of the Southern Carpathians, is known in the literature as "strong downslope winds". This phenomenon occurred in a typical blizzard configuration, in which the differentiated advection of temperature led to the formation of a very stable air layer, with thermal inversion approximately between the levels of 850 and 700 hPa; and it also contributed in this layer to the change of wind direction to vertical. Thus, the existence in the same air layer of two factors favorable to the formation of a critical level, created the ideal conditions for generating strong downslope winds.

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The ‘Hess-Brezowsky’ concept applied in the northern part of Moldova between 2000 to 2018

The ‘Hess-Brezowsky’ concept applied in the northern part of Moldova between 2000 to 2018

Author(s): Ilie N. / Language(s): English Issue: 1/2021

This paper presents the general aspects linked with the atmospheric circulation and how to determine the air-circulation types based upon the ‘Hess-Brezowsky’ concept over the northern part of Moldova to get in an easily way the pluvial risks. Once the classification is done, there were shown the evolution of atmospheric circulation from the annual to seasonal level by weights. In the wake of study into the studied area, the most representative types were Through over Central Europe; followed by those from North-Westerly Cyclonic; Westerly Cyclonic; and SouthWesterly Cyclonic. Also, during the cold half-yearly, by importance was NorthEasterly into Anti-Cyclonic type.

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Characteristics of the floods in Pechea village, Galați county

Characteristics of the floods in Pechea village, Galați county

Author(s): Emilia Avram / Language(s): English Issue: 1/2021

This study aims to develop risk analysis methodologies on floods, analyze floods produced on the Suhu River in Pechea village (Galați county), and factors that favor flooding. Flood analysis represents one of the main concerns of researchers in hydrology in the context of climate change. It is increasingly leaving its mark on the frequency of precipitation and, implicitly, on the production of floods. We presented the definitions of floods, and we presented the study area in the first part of the article. The monthly and seasonal frequency of floods were analyzed, and there were calculated specific parameters of a flood produced in the study area. Then, the factors that favor the occurrence of floods were analyzed. The results obtained will contribute to the complete information on floods in small basins in the plain area on the Romanian territory.

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Aspects regarding the trend of the average annual, seasonal and monthly drainage of river water from the Căliman Mountains in the period 1950-2010

Aspects regarding the trend of the average annual, seasonal and monthly drainage of river water from the Căliman Mountains in the period 1950-2010

Author(s): Hirlav Costin / Language(s): English Issue: 1/2021

The Căliman Mountains are the highest volcanic mountains in Romania, being positioned on the western side of the Eastern Carpathians, between their central strip (north and east), south – the Harghita Mountains, and west – the Transylvanian Depression. This positioning gives special features of the water drainage, with both spatial and temporal differentiations. This paper analyzed the trend of average drainage from rivers in the studied group for the period 1950-2010, both multi-annually and seasonally and in the extreme months; the months taken into account being those with the lowest flows (January), respectively the largest (May). To evaluate the mentioned parameters, we used the help of Excel MAKESENS (Mann-Kendall test for trend and Sen’s slope estimates), which identified the type of drainage trend (positive or negative), and using the Sen nonparametric method to estimate the slope of the trend. Based on the type of trend obtained, 9 trend classes were obtained, and with the help of the slope, the net change rate was obtained.

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The springs from the ”Făget” area of Cluj.

The springs from the ”Făget” area of Cluj.

Author(s): Vigh Melinda,Szilárd Poszet,Wanek Ferenc / Language(s): English Issue: 1/2021

To the south of the city of Cluj, in the perimeter called “Făget”, there are numerous springs often frequented by locals. From a geological point of view, there is a great variety of rocks of different ages and characteristics. The waters cantoned in these geological structures appear on the surface along the valleys, on the slopes or even in the unevenness of the interfluves. Their existence was facilitated by vertical erosion processes and mass movements of the material. Through the inventory of the area, 28 sources were identified and located. They can be divided into several categories: with drain, wells, inactive, dried, captured. Spatial coordinates were determined for each source. Where possible, the flow rate, temperature and concentration of dissolved in water substances were measured. There is a large gap in flow variation, relatively constant temperatures and wide limits of TDS values. The expansion of the urban area involves potential risks of a quantitative and qualitative nature.

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GEBCO and ETOPO1 gridded datasets for GMT based cartographic Mapping of Hikurangi, Puysegur and Hjort Trenches, New Zealand

GEBCO and ETOPO1 gridded datasets for GMT based cartographic Mapping of Hikurangi, Puysegur and Hjort Trenches, New Zealand

Author(s): Polina Lemenkova / Language(s): English Issue: 19/2020

The study focused on the comparative analysis of the submarine geomorphology of three oceanic trenches: Hikurangi Trench (HkT), Puysegur Trench (PT) and Hjort Trench (HjT), New Zealand region, Pacific Ocean. HjT is characterized by an oblique subduction zone. Unique regional tectonic setting consist in two subduction zones: northern (Hikurangi margin) and southern (Puysegur margin), connected by oblique continental collision along the Alpine Fault, South Island. This cause variations in the geomorphic structure of the trenches. PT/HjT subduction is highly oblique (dextral) and directed southwards. Hikurangi subduction is directed northwestwards. South Island is caught in between by the “subduction scissor”. Methodology is based on GMT (The Generic Mapping Tools) for mapping, plotting and modelling. Mapping includes visualized geophysical, tectonic and geological settings of the trenches, based on sequential use of GMT modules. Data include GEBCO, ETOPO1, EGM96. Comparative histogram equalization of topographic grids (equalized, normalized, quadratic) was done by module ’grdhisteq’, automated cross-sectioning – by ’grdtrack’. Results shown that HjT has a symmetric shape form with comparative gradients on both western and eastern slopes. HkT has a trough-like flat wide bottom, steeper gradient slope on the North Island flank. PT has an asymmetric V-form with steep gradient on the eastern slopes and gentler western slope corresponding to the relatively gentle slope of a subducting plate and steeper slope of an upper one. HkT has shallower depths  6,000 m for HjT. The surrounding relief of the HjT presents the most uneven terrain with gentle slope oceanward, and a steep slope on the eastern flank for PT, surrounded by complex submarine relief along the Macquarie Arc. Data distribution for the HkT demonstrates almost equal pattern for the depths from ₋600 m to ₋2,600 m. PT has a bimodal data distribution with 2 peaks: 1) ₋4,250 to ₋4,500 m (18%); 2) ₋2,250 to ₋3,000 m, < 7,5%. The second peak corresponds to the Macquarie Arc. Data distribution for HjT is classic bell-shaped with a clear peak at ₋3,250 to ₋3,500 m. The asymmetry of the trenches resulted in geomorphic shape of HkT, PT and HjT affected by geologic processes.

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Zmiany morfologiczne koryta Pilicy między Domaniewicami a Nowym Miastem nad Pilicą na podstawie analizy kartograficznej

Zmiany morfologiczne koryta Pilicy między Domaniewicami a Nowym Miastem nad Pilicą na podstawie analizy kartograficznej

Author(s): Kinga Jędrzejczyk / Language(s): Polish Issue: 19/2020

The article presents the morphological changes of the former, post-glacial riverbeds of the Pilica River between Domaniewice and Nowe Miasto nad Pilicą on the basis of cartographic materials from 1802–2017. The aim of the article was also to assign the Pilica to a specific type of bed based on its characteristic morphological features. It has been shown that the nature of the river valley bottom, as well as the Pilica bed itself, was largely influenced by the construction of the Sulejowski Reservoir.

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Przyczyny pożarów i skuteczność systemu ochrony przeciwpożarowej Lasów Państwowych w latach 2010–2019 na przykładzie Nadleśnictwa Kielce

Przyczyny pożarów i skuteczność systemu ochrony przeciwpożarowej Lasów Państwowych w latach 2010–2019 na przykładzie Nadleśnictwa Kielce

Author(s): Tomasz Kalicki,Paweł Przepióra,Grzegorz Żarnowiecki,Grzegorz Król,Marcin Frączek / Language(s): Polish Issue: 19/2020

The aim of the study is to determine the causes of the forest fires and the effectiveness of the State Forests fire protection system in Kielce Forest District. A comparative analysis of the course of selected meteorological data favoring the occurrence of fires and forest fires data (databases TETRAX electronic, SILP, Llas.2) in 2010–2019, with particular emphasis on fires with unknown causes was obtained and analyzed. This allowed to establish the dominance of anthropogenic over natural factors in forest fires ignition. The high effectiveness of the fire protection system was confirmed, which is related to i.e. with a dense network of roads and the lack of large, compact forest complexes.

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Zmiany klimatu jako zagrożenie dla bezpieczeństwa narodowego w świetle dokumentów administracji amerykańskiej XXI wieku

Zmiany klimatu jako zagrożenie dla bezpieczeństwa narodowego w świetle dokumentów administracji amerykańskiej XXI wieku

Author(s): Maciej Hacaga / Language(s): Polish Issue: 60/2019

The issue of climate change has started to be implemented in official strategic documents of the United States (US) in the first decade of the 21st century. This paper describes briefly the hierarchy of the US national security documents and climate change-related definitions. In the main part it makes an analysis of how climate change-related issues were introduced into the US national security strategic documents by the three 21st century American presidents. The paper comes to a conclusion, that climate change is treated as a national security threat and therefore reflected in a number of the US strategic documents.

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PO VELEBITU OD SVETOG BRDA DO PODPRAGA ILI OD SPOMENA BOŽJIH ZAPOVIJEDI DO SPOMINJANJA HRVATSKIH BRANITELJA

PO VELEBITU OD SVETOG BRDA DO PODPRAGA ILI OD SPOMENA BOŽJIH ZAPOVIJEDI DO SPOMINJANJA HRVATSKIH BRANITELJA

Author(s): Tomislav Baričević / Language(s): Croatian Issue: 1/2002

Velebna gora Velebit pruža se u smjeru sjeverozapada do jugoistoka Hrvatske. Dobro je ograđena počevši sa zapada prijevojem Vratnik do kanjona Zrmanje na istoku, te Velebitskim kanalom Jadranskoga mora s juga, a sa sjevera Gackim i Ličkim poljem te poljem Velike i Male Popine. Od zapada prema istoku dug je oko 145 km, a od juga prema sjeveru od 10 km (Starigrad -Paklenica, Bojin kuk i Počitelj) do 30 km (Jablanac, Zavižan, Markovica Rudina)."

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GEOMORFOLOŠKE KARAKTERISTIKE I GEOLOŠKI ZNAČAJ PODRUČJA BAŠKIH OŠTARIJA NA VELEBITU

GEOMORFOLOŠKE KARAKTERISTIKE I GEOLOŠKI ZNAČAJ PODRUČJA BAŠKIH OŠTARIJA NA VELEBITU

Author(s): Srećko Božičević / Language(s): Croatian Issue: 1/2002

Moramo priznati kao dobri poznavatelji planine Velebit da je na njemu malo područja gdje se nalazi jedna tako zanimljiva zaravan na visini nešto iznad 900 m n.m., koja na toj svojoj stepenici vrvi mnogim površinskim raznolikostima. Na dužini od oko 4000 m te širini od 700 do 1700 metara nalazimo sve morfološke karakteristike naslaga mezozojske starosti s izgledom krške bezvodne goleti, te s vlažnim - povremeno plavljenim - dijelom u sredini prostora, ovisno o meteorološkim uvjetima, te s dijelom terena u kojemu dominiraju nepropusne paleozojske naslage s izvorima i vodenim tokom na njegovoj površini.

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LEDENA JAMA U LOMSKOJ DULIBI

LEDENA JAMA U LOMSKOJ DULIBI

Author(s): Igor Jelinić,Nada Horvatinčić,Vlado Božić / Language(s): Croatian Issue: 1/2001

Lomska duliba is a glacier valley with WNW-ESE strike and is located between Veliki Rajinac to the north and Hajdučki kukovi to the south of Mt. Velebit. The entrance to Ledena jama Ice Pit) is situated on the most eastern part of this one kilometre long valley at the level of 1235 above the sea. Ledena jama, just as most pits located on the northern part of Velebit, has a rather simple morphology. Nevertheless, its simplicity is in inverse proportion with the speed and simplicity of exploration, which makes it very different in comparison with other deep pits in this part of Velebit. consider today, it takes three hours for a coordinated team of three speleologists to reach the bottom, the complexity and duration of its investigation in the past is surprising. The complexity the performed investigation makes the story of Ledena jama in Lomska duliba much more interesting. The initial investigations were performed by the members of the Croatian speleological society in 1962. Further investigations were continued in 1977, when a team of speleologists from Željezničar" mapped the pit to the depth of-50 m. The floor of the pit was covered by a thick Since the Croatian speleologists considered they had definitely reached pit's bottom, no further investigations were performed. During the summer of 1992, a team of Slovakian speleogists visited the pit, found a hole in ice and descended through it to the depth of-90 m. Since the pit extended further, the following the investigations continued with the participation of both Slovak and Croatian speleologists. During 1993 and 1994 investigations were performed in combination with the investigators of Lukina jama (-1392 m). In the period between 1995 and 1997 further investigations were undertaken the pit by widening the passage at 473 m and by reaching the bottom of the pit at the depth of-536 m. On the 29th June 1997 during a sport tour of the pit occurred one of the most serious accidents in the Craotian speleology. At the depth of 160 m a landslide of rock and ice caused severe injuries (multiple fracture of various limbs and bones and also muscle ruptures) to B. Bukovčak, who was hanging on the rope. The rescue of the injured speleologists was performed by members of his team and by the Mountain Rescue Service from Karlovac. After a long-lasting recovery, B. Bukovčak is an active speleologist again. In the summer of 1993 it was determined that there was a passage between the ice and the north wall of the pit wide enough for a person to pass. This led to a discovery of an ice plug twenty meters in diameter, well bedded and 40 m thick. Several branches were found to be peeking out of the ice. There was a possibility that the ice originated from the Ice Age, since the Lomska duliba was formed by a glacier. So, speleologists in agreement with the scientists from the Institute Ruder Bošković in Zagreb collected some samples of ice, branches and speleothems for dating. The results of analysis were surpassing. Dating with radioactive isotopes tritium (3H), carbon (14C) and thorium and uranium (230Th/234U) gave an approximate age of ice of 500 years. Said age indicated that the samplings of ice were badly performed (contaminated by more recent waters) or that larger temperature variations existed on Velebit, which should be confirmed by other methods. The branches were younger, which means that they fell into the crack and froze. The most surprising was the age of the speleothem from the depth of 60 m, which was estimated at 300.000 years. This is the oldest registered age of Speleothems measured in Croatia so far although by method not used before on speleothems from other caves and pits. In order to determine the age of this largest piece of old ice in Croatia and speleothems from this pit and other caves and pits, further investigations with modern methods would be required in the future.

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SPELEOLOŠKA DJELATNOST IVANA I HELE KRAJAČ

SPELEOLOŠKA DJELATNOST IVANA I HELE KRAJAČ

Author(s): Vlado Božić / Language(s): Croatian Issue: 1/2001

There are numerous articles published about Ivan Krajač (Senj, 1877 - ? 1945) in Croatian mountaineering publications and his important role in the development of mountaineering, while his wife Hela (born Schlacht in Tchehoslovakia in 1899, now living in Austria) is not mentioned so frequently. They were both universal mountaineers as well as speleologists and in 1930 they made noteworthy speleological actions. Ivan Krajač was a lawyer by profession and worked in Jastrebarsko, Belgrade (from 1925 - 1929 as a minister of finance) and Zagreb. He was active in speleology from 1925 to 1933, when he used to make investigations of caves and pits for the most part on Mt Velebit. He hiked together with the forestry engineer Ante Premužić through the regions of northern part of the massive of Velebit, accompanied by his wife Hela. During the summer of 1930 he descended into the pit Vrtlina, on the south part of Velebit, which is a large cave with a pit entrance, to a record depth of - 180 m while his partner reached -195 m, which was the greatest depth achieved by the Croatian speleologists.That same year, in the autumn, he descended with his wife, aided by the alpinist equipment and technique, into the pit Varnjača (ice pit in the region of Rožanski kukovi on the northern part of Velebit), to a depth of 120 m. Hela Krajač was the first woman in Croatia who descended into a pit. Although Ivan Krajač was a great opponent to a record breaking in mountaineering, unintentionally, he and his wife became record breakers in the same year and in different pits. That was the unique example in Croatian that wife and husband, both together broke all the previous speleological recorders.

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TEMELJNA SKICA GEOEKOLOŠKIH OSOBINA VELEBITA

TEMELJNA SKICA GEOEKOLOŠKIH OSOBINA VELEBITA

Author(s): Andrija Bognar / Language(s): English,Croatian Issue: 1/1994

The Mountain Range of Velebit is a part of the mountain zone of the Outer Dinarides, characterized by the prevailing nonkonformed block-folded structure. On the prevailing carbonate basement (limestones, dolomites) linear and bended chains of ridges have been developed in SE, S and central part of the mountain. Norther part of Velebit has mostly character of the mountain massif with the dominant block-folded structure. Velebit is characterized by the steplike transversal profile. Karst is the predominant relief type. Very high relief dissection rate stimulated intensive slope processes and corresponding relief forms (pediments). At the highest sections of the mountain (higher than 1.350 m) there are remnants of glaciation (exaration morphologic forms as well as the corresponding correlative sediments and moraine forms) and periglacial modelling which took place in the Pleistocene. Periglacial processes are active today only above the altitudes of 1.400-1.500 m. The Velebit Mountain represents an important climatic barrier towards the continental part of Croatia. There are climatic differences between the coastal part of the mountain and it's NE slope in Lika. The annual rainfall is around 1.000 mm in the coastal part, while in the higher part of the mountain it exceeds to 3.000 mm. The situation is similar with the temperature contrasts; while on the coast the freezing temperatures are rare, on the higher part of the mountain the winter temperatures sometimes drop below -30°C and -40°C. This results in a number of vegetational peculiarities. It should be noted that vegetation in this region ranges from subtropical laurel forests in the southern part of the coastal zone to spruce forests of the taige type in the higher zone of Velebit. The intensive human influence on the natural vegetation cover of the karst has been present for centuries. It is almost a rule that severe degradation of the vegetation cover is accompanied by degradation and destruction of soil by erosion and deflation. On the limestones and dolomite rocks on the lower hypsometric levels up to approximately 700 m, calcic cambiosol prevails, while on the higher locations orthic rendzina on hard limestone is predominant. On deeper and loose moraine and fluvioglacial materials, orthic rendzina is found.

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