HIGHLIGHTS of SLOVENIA Walking from Two Centres in the Julian Alps
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Slovenian Alps
SLOVENIAN ALPS Mangart, Photo by Bor Rojnik Slovenian Alps are truly remarkable, easily discovered by road as well as by trails suitable for hikers and cyclists. Marvellous panoramas, blooming meadows, alpine pastures and forests are surely never to be forgotten and are one of the most fascinating tourist spots in Slovenia. The high summits of the Julian Alps, the Karavanken chain and the Kamnik-Savinja Alps, open up amazing panoramas of the surrounding territory. It is hardly to find such a blooming meadows, alpine pastures and forests, elsewhere in the world within easy reach. The Julian Alps are a mountain range of the great Alps that stretches from northeastern Italy to Slovenia. They cover an estimated 4400 km², of which 1542 km² lies in Slovenia, and rise to 2,864 m at Mount Triglav, the highest peak in Slovenia. The entire mountain range constitutes about 150 mountains and is divided into two sections - the Western Julian Alps and the Eastern Julian Alps. 1 The Triglav National Park, boasting a number of peculiarities, is the largest and the earliest protected natural heritage site in the country. It is located in the north-west of Slovenia, more precisely in the Julian Alps. The park was named after the highest mountain of Slovenia, the Triglav, which is located nearly at the center of the park. It is the only National Park in Slovenia and among the earliest European parks. Pokljuka, is the southernmost highland marsh in Europe and a natural habitat of sphagnum moss. Near Kranjska Gora you can find nature reserve, the Zelenci, whom lakes provide Sava Dolinka with its source. -
Reka SAVA DOLINKA in BELCA ČN Tabre in MČN Belca (Stalni Letni Monitoring Od Leta 2001)
LABORATORY OF PLANT CYTOGENETICS Use of Allium M test for purpose of establishing quality of waters; since 1998 LABORATORIJ ZA RASTLINSKO APLIKATIVNO CITOGENETIKO Testna rastlina: navadna čebula (Allium cepa L.) Splošna strupenost (dolžina korenin) in genotoksičnost (indukcija kromosomskih poškodb) Reka SAVA DOLINKA in BELCA ČN Tabre in MČN Belca (stalni letni monitoring od leta 2001) Naročnik: Občina Kranjska Gora Kolodvorska 1b, SI – 4280 Kranjska Gora April 2015 Testno poročilo z rezultati raziskav obsega 9 strani, 2 preglednici in 4 fotografije 1 LABORATORY OF PLANT CYTOGENETICS Use of Allium M test for purpose of establishing quality of waters; since 1998 PROTOKOL METODE ALLIUM METAFAZNI GENOTOKSIČNI TEST ZA TESTIRANJE OKOLJSKIH VZORCEV, KEMIKALIJ IN PITNE VODE Peter Firbas, univ. dipl. biol., Zasebni raziskovalec, Laboratorij za rastlinsko citogenetiko E-pošta: [email protected] 1. Uvod ALLIUM metafazni test je test za ugotavljanje splošne celične strupenosti (citotoksičnosti) in ravni genotoksičnosti v vodnih, kopenskih in zračnih ekosistemih, kjer dokazujemo potencialne genotoksične snovi. Test je kratkotrajen in pokaže usklajen in celokupen učinek onesnaževanja in medsebojno delovanje med testno rastlino (Allium cepa L.) in potencialnimi genotoksiki, nato se še rezultati statistično ovrednotijo. Rezultate raziskav s statistično kalkulacijo prikazuje Fisher’s Exact Test. V 2x2 frekvenčnih tabelah dvosmerna p-vrednost determinira statistično značilnost ali neznačilnost dveh kategoričnih vzorcev. Biološki test ALLIUM ali čebulni test razkriva celosten vpliv na rast in razvoj živih celic ali organizmov ter zaznava prisotnost škodljivih snovi v koncentracijah, ki so bistveno nižje od 1 ppb (part per billion – en del snovi na eno milijardo raztopine ali 1 µg na liter ali kilogram). Od približno 700 prepoznavnih snovi, ki se lahko znajdejo na primer v pitni vodi, jih z običajnimi fizikalno-kemijskimi analizami nadzorujemo le okrog 10 odstotkov (Vir: EU Chemical Bureau, Natural Resources Defence Council: Think before you drink). -
JULIAN ALPS TRIGLAV NATIONAL PARK 2The Julian Alps
1 JULIAN ALPS TRIGLAV NATIONAL PARK www.slovenia.info 2The Julian Alps The Julian Alps are the southeast- ernmost part of the Alpine arc and at the same time the mountain range that marks the border between Slo- venia and Italy. They are usually divided into the East- ern and Western Julian Alps. The East- ern Julian Alps, which make up approx- imately three-quarters of the range and cover an area of 1,542 km2, lie entirely on the Slovenian side of the border and are the largest and highest Alpine range in Slovenia. The highest peak is Triglav (2,864 metres), but there are more than 150 other peaks over 2,000 metres high. The emerald river Soča rises on one side of the Julian Alps, in the Primorska re- gion; the two headwaters of the river Sava – the Sava Dolinka and the Sava Bohinjka – rise on the other side, in the Gorenjska region. The Julian Alps – the kingdom of Zlatorog According to an ancient legend a white chamois with golden horns lived in the mountains. The people of the area named him Zlatorog, or “Goldhorn”. He guarded the treasures of nature. One day a greedy hunter set off into the mountains and, ignoring the warnings, tracked down Zlatorog and shot him. Blood ran from his wounds Chamois The Triglav rose and fell to the ground. Where it landed, a miraculous plant, the Triglav rose, sprang up. Zlatorog ate the flowers of this plant and its magical healing powers made him invulnerable. At the same time, however, he was saddened by the greed of human beings. -
TRIGLAV NATIONAL PARK (Slovenia)
Strasbourg, 6 January 2003 PE-S-DE (2002) 22 [diplome/docs/2003/de06e_03] English only Committee for the activities of the Council of Europe in the field of biological and landscape diversity (CO-DBP) Group of specialists – European Diploma of Protected Areas 20-21 January 2003 Room 2, Palais de l'Europe, Strasbourg TRIGLAV NATIONAL PARK (Slovenia) APPLICATION for the European Diploma of Protected Areas Document established by the Directorate of Culture and Cultural and Natural Heritage This document will not be distributed at the meeting. Please bring this copy. Ce document ne sera plus distribué en réunion. Prière de vous munir de cet exemplaire. PE-S-DE (2003) 22 - 2 - INFORMATION FORM FOR NEW APPLICATION FOR THE EUROPEAN DIPLOMA OF PROTECTED AREAS Council of Europe European Diploma Information form for Candidate Sites This form is also available on diskette Site code (to be given by the Council of Europe) 1. SITE IDENTIFICATION 1.1. SITE NAME Triglavski narodni park 1.2. COUNTRY Slovenija 1.3. DATE CANDIDATURE 1.4. SITE INFORMATION COMPILATION DATE Y Y Y Y M M D D - 3 - PE-S-DE (2003) 22 1.5. ADDRESSES: administrative authorities National authority Regional authority Local authority Name: Name: Name: Javni zavod Triglavski Address: Address: narodni park Address: Triglavski narodni park, Kidričeva 2, 4260 Bled, Slovenija Tel. +386 4 5780 200 ............. Tel.......................................... Tel. ......................................... Fax.+ 386 4 5780 201............. Fax. ........................................ Fax......................................... -
Naslednja Stran
LAND DEGRADATION IN A COMPLEX ENVIRONMENT: CHALLENGES OF LAND MANAGEMENT AT THE CONTACT OF FOUR MAJOR EUROPEAN GEOGRAPHICAL UNITS BOOK OF ABSTRACTS AND FIELD GUIDE Commission on Land Degradation and Desertification (COMLAND) of the International Geographical Union (IGU) Meeting and Field Trip in Slovenia June 23rd–June 27th, 2016 LJUBLJANA 2016 LAND DEGRADATION IN A COMPLEX ENVIRONMENT: CHALLENGES OF LAND MANAGEMENT AT THE CONTACT OF FOUR MAJOR EUROPEAN GEOGRAPHICAL UNITS BOOK OF ABSTRACTS AND FIELD GUIDE Commission on Land Degradation and Desertification (COMLAND) of the International Geographical Union (IGU) Meeting and Field Trip in Slovenia June 23rd–June 27th, 2016 Edited by: MATIJA ZORN MATEJA FERK JURE TIČAR PRIMOŽ GAŠPERIČ LJUBLJANA 2016 LAND DEGRADATION IN A COMPLEX ENVIRONMENT: CHALLENGES OF LAND MANAGEMENT AT THE CONTACT OF FOUR MAJOR EUROPEAN GEOGRAPHICAL UNITS: BOOK OF ABSTRACTS AND FIELD GUIDE © 2016, Geografski inštitut Antona Melika ZRC SAZU Edited by: Matija Zorn, Mateja Ferk, Jure Tičar, Primož Gašperič Issued by: Geografski inštitut Antona Melika ZRC SAZU Published by: Založba ZRC Represented by: Drago Perko, Oto Luthar DTP: Matija Zorn Printed by: Megacop First edition, print run: 40 issues Ljubljana, 2016 Front cover photography: Land degradation in the Julian Alps is either human induced, e.g. as a result of mining activity (on the left), or induced by natural processes, e.g. landslide (on the right) (photograph: Matija Zorn). CIP - Kataložni zapis o publikaciji Narodna in univerzitetna knjižnica, Ljubljana 911.2:631.459(082) -
Planica, Pot Po Dolini
preoblikovanje reshaping asinger sirarna okrog leta 1920, fotografija last Olge R Pot se konča na skupnem pašnikom rateških kmetov, imenovanim Zelje. Gore in doline se v geološkem procesu nenehno preoblikujejo in Konec 19. stoletja je bila tam ovčja sirarna z leseno ogrado. Takim spreminjajo. Spreminjanje in preoblikovanje je vidno zlasti v številnih ogradam so rekli tamar. meliščihpodstenami. The trail ends on a communal pasture named Zelje. Farmers from Rateče built Mountains and valleys constantly change during the geologic process. The here a sheep cheese dairy at the end of the 19th century, that was fenced by changes and transformations are best seen on the numerous scree slopes a wooden pen. Such enclosures were called "tamar". under the mountain clifs. Zelje Zelje Preoblikovanje doline Preoblikovanje valley of the Reshaping transport balvanov boulder transport ugo svetovno vojno pridobivanje krede pred dr v Radovni (fototeka Gorenjskega muzeja) v Radovni Ko so se ledeniki umikali, so na dno dolin odlagali drobnozrnat material, ki Skalni bloki na dnu alpskih dolin, ki jih je pred 14.000 leti na današnje mu pravimo jezerska kreda. Ljudje so jo izkoriščali v razne industrijske mesto odložil ledenik, so balvani. Tja jih je lahko prinesel le premikajoči namene. led. As the glaciers retreated they left a sediment of fine-grain marlstone. This lake Large rock stones that were left on the valley floor by the glacier 14.000 years sediment was mined for various industrial purposes. It has similar ago are called "boulders". Such large rocks could only be transported by the characteristics to clay. moving ice. Jezerska kreda sediment Lake Balvani rocks Boulder izvir, slap izvir, spring, Zelenci waterfall foto Andrej Mežik potek toka Nadiže the Nadiža stream Letalo Consolidated B-24 Liberator je 22.11.1944 strmoglavilo na Na pobočju Zadnje Ponce se začne skrivnostni tok reke Nadiže, ki teče čez območju Kotovega sedla. -
HIKING in SLOVENIA Green
HIKING IN SLOVENIA Green. Active. Healthy. www.slovenia.info #ifeelsLOVEnia www.hiking-biking-slovenia.com |1 THE LOVE OF WALKING AT YOUR FINGERTIPS The green heart of Europe is home to active peop- le. Slovenia is a story of love, a love of being active in nature, which is almost second nature to Slovenians. In every large town or village, you can enjoy a view of green hills or Alpine peaks, and almost every Slove- nian loves to put on their hiking boots and yell out a hurrah in the embrace of the mountains. Thenew guidebook will show you the most beauti- ful hiking trails around Slovenia and tips on how to prepare for hiking, what to experience and taste, where to spend the night, and how to treat yourself after a long day of hiking. Save the dates of the biggest hiking celebrations in Slovenia – the Slovenia Hiking Festivals. Indeed, Slovenians walk always and everywhere. We are proud to celebrate 120 years of the Alpine Associati- on of Slovenia, the biggest volunteer organisation in Slovenia, responsible for maintaining mountain trails. Themountaineering culture and excitement about the beauty of Slovenia’s nature connects all generations, all Slovenian tourist farms and wine cellars. Experience this joy and connection between people in motion. This is the beginning of themighty Alpine mountain chain, where the mysterious Dinaric Alps reach their heights, and where karst caves dominate the subterranean world. There arerolling, wine-pro- ducing hills wherever you look, the Pannonian Plain spreads out like a carpet, and one can always sense the aroma of the salty Adriatic Sea. -
Contaminated Sites and Health
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Impact of the Mean Daily Air Temperature Calculation on the Rainfall-Runoff Modelling
water Article Impact of the Mean Daily Air Temperature Calculation on the Rainfall-Runoff Modelling Nejc Bezak * , Lazar Cerovi´cand Mojca Šraj Faculty of Civil and Geodetic Engineering, University of Ljubljana, 1000 Ljubljana, Slovenia; [email protected] (L.C.); [email protected] (M.Š.) * Correspondence: [email protected]; Tel.: +386-1-4254-052 Received: 12 October 2020; Accepted: 12 November 2020; Published: 13 November 2020 Abstract: Conceptual rainfall-runoff models besides precipitation and discharge data generally require estimates of the mean daily air temperature as input data. For the estimation of the mean daily air temperature, there are different methods available. The paper presents an evaluation of the impact of the mean daily air temperature calculation on the rainfall-runoff modelling results. Additionally, other measured variables and rating curve uncertainty were assessed. Differences in the mean daily air temperature values were evaluated for the 33 meteorological stations in Slovenia and additional investigations were conducted for four selected meso-scale catchments located in different climates. The results of the application of four equations for the mean air temperature calculation yielded the mean absolute error values between 0.56–0.80 ◦C. However, the results of rainfall-runoff modelling showed that these differences had an almost negligible impact on the model results. Differences in the mean simulated discharge values were no larger than 1%, while differences in the maximum discharge values were a bit larger, but did not exceed 5%. A somewhat larger impact on the model results was observed when precipitation and water level measurements’ uncertainty was included. -
Povratne Dobe Velikih in Malih Pretokov Za Merilna Mesta Državnega Hidrološkega Monitoringa Površinskih Voda
POVRATNE DOBE VELIKIH IN MALIH PRETOKOV ZA MERILNA MESTA DRŽAVNEGA HIDROLOŠKEGA MONITORINGA POVRŠINSKIH VODA Sektor za analize in prognoze površinskih voda Urad za hidrologijo in stanje okolje November 2013 Agencija Republike Slovenije za okolje POVRATNE DOBE VELIKIH IN MALIH PRETOKOV Ve čina hidroloških procesov v naravi se zgodi naklju čno, zato je uporaba verjetnostne teorije in matemati čne statistike v hidrologiji neizogibna za reševanje hidroloških problemov in za boljši opis hidroloških procesov. Verjetnost nastopa dolo čenega pojava predstavlja eno izmed najpomembnejših analiz hidroloških podatkov, kjer na podlagi predhodnih dogajanj napovedujemo dogodke v prihodnosti. Vsak napovedan dogodek (pretok) pa ima dolo čeno verjetnost nastopa. Zaradi enostavnosti in lažjega razumevanja v praksi verjetnost nastopa prikazujemo z njeno recipro čno vrednostjo, to je povratno dobo dogodka. Povratna doba je ocena časovnega intervala med dogodki. Pretok s povratno dobo 10 let je koli činska ocena pretoka, ki se v povpre čju pojavi enkrat na 10 let. Pomembno je poudariti, da je pojav dogodka slu čajen, saj se v kronološkem smislu dogodki ne pojavljajo vsakih 10 let, ampak pri čakujemo, da se bo dogodek pojavil 10- krat v 100 letih, ali v povpre čju vsakih 10 let. Povratne dobe smo izra čunali za najve čje letne pretoke (letne visokovodne konice – Qvk) in najmanjše male letne srednje dnevne pretoke (Qnp). Izra čun je narejen za lokacije merilnih mest državnega hidrološkega monitoringa površinskih voda z nizom podatkov vsaj 10 let (slika 1, preglednica 1). V izra čunih so upoštevana razpoložljiva obdobja podatkov do vklju čno leta 2010. Za ra čunanje povratnih dob smo uporabili Pearson III in Log Pearson III porazdelitveni funkciji, ki sta v hidrološki praksi najpogosteje uporabljeni metodi. -
Predmet: Izbirna Geografija
(referat) Predmet: Izbirna geografija 1. KAZALO VSEBINE 1. KAZALO VSEBINE...........................................................................2 2. KAZALO SLIK...................................................................................2 3. REKA SAVA – SPLOŠNO..................................................................4 4. REKA SAVA V SLOVENIJI:...............................................................5 4.1 Rečni režim in pretok..................................................................6 4.2 Ribištvo in turizem......................................................................7 4.3 Električni potencial.....................................................................7 5. REKA SAVA V DRUGIH DRŽAVAH:.................................................8 5.1 Plovnost reke...............................................................................9 6. ONESNAŽENOST REKE..................................................................9 7. VIRI................................................................................................11 2. KAZALO SLIK 1. Izvir reke Save Dolinke__________________________________________ 3 2. Izvir reke Save Bohinjke_________________________________________ 3 3. Reka Sava na Slovenskem in pritoki________________________________4 4. Rečni režim____________________________________________________5 5. trasa v Radečah na reki Savi.______________________________________5 6. Shema hidroelektrarn na Savi_____________________________________6 7. Hidroelektrarna Medvode________________________________________6 -
Crayfish of the Upper Soca and Upper Sava Rivers, Slovenia
Bull. Fr. Pêche Piscic. (1997)347:721-729 — 721 — CRAYFISH OF THE UPPER SOCA AND UPPER SAVA RIVERS, SLOVENIA. Y. MACHINO 13 rue Montorge, 38000 Grenoble, France. Reçu le 04 juillet 1997 Received 04 July, 1997 Accepté le 29 août 1997 Accepted 29 August, 1997 ABSTRACT Crayfish biogeography of northwestern Slovenia was studied in the Upper Soca River (Mediterranean drainage) and the Sava Dolinka River (Danubian drainage). The Mediterranean drainage has white-clawed crayfish (Austropotamobius pallipes) and the Danubian drainage has stone crayfish (A. torrentium). Morphological data of these A. pallipes suggest that the Slovenian white-clawed crayfish belong to the Austropotamobius pallipes italicus complex. The biogeographic and morphological data support the present general knowledge that in Slovenia the white-clawed crayfish belongs to a Po-Adriatic fauna and the stone crayfish to a Danubian fauna. A third species, the noble crayfish (Astacus astacus), was found in Danubian waters, but its biogeographic meaning may not be significant because the species is present in, and has been introduced into, waters of both the Mediterranean and Danubian drainages. The noble crayfish from a Slovenian lake, Blejsko jezero, has certain morphological characteristics that require additional investigations before its taxonomic position can be clarified. The stone crayfish of the Sava Dolinka now survives in only a few sites, relics of a former wider distribution destroyed by human activities. On the other hand, the white-clawed crayfish of the Soca is still distributed widely. But it is timely to consider their protection because the Soca region is now under major tourist development pressure. Key-words : Austropotamobius pallipes, Austropotamobius torrentium, Astacus astacus, biogeography, taxonomy, protection, Slovenia.