SNAPSEE-Fild-Trip-Guide.Pdf2.83 MB
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
By Bus Around the Julian Alps
2019 BY BUS AROUND THE JULIAN ALPS BLED BOHINJ BRDA THE SOČA VALLEY GORJE KRANJSKA GORA JESENICE rAdovljicA žirovnicA 1 2 INTRO 7 BLED, RADOVLJICA, ŽIROVNICA 8 1 CHARMING VILLAGE CENTRES 10 2 BEES, HONEY AND BEEKEEPERS 14 3 COUNTRYSIDE STORIES 18 4 PANORAMIC ROAD TO TRŽIČ 20 BLED 22 5 BLED SHUTTLE BUS – BLUE LINE 24 6 BLED SHUTTLE BUS – GREEN LINE 26 BOHINJ 28 7 FROM THE VALLEY TO THE MOUNTAINS 30 8 CAR-FREE BOHINJ LAKE 32 9 FOR BOHINJ IN BLOOM 34 10 PARK AND RIDE 36 11 GOING TO SORIŠKA PLANINA TO ENJOY THE VIEW 38 12 HOP-ON HOP-OFF POKLJUKA 40 13 THE SAVICA WATERFALL 42 BRDA 44 14 BRDA 46 THE SOČA VALLEY 48 15 HOP-ON HOP-OFF KOBARID – RED LINE 50 16 HOP-ON HOP-OFF KOBARID – ORANGE LINE 52 17 HOP-ON HOP-OFF KOBARID – GREEN LINE 54 18 HOP-ON HOP-OFF KOBARID – PURPLE LINE 56 19 HOP-ON HOP-OFF KOBARID – BLUE LINE 58 20 THE TOLMINKA RIVER GORGE 62 21 JAVORCA, MEMORIAL CHURCH IN THE TOLMINKA RIVER VALLEY 64 22 OVER PREDEL 66 23 OVER VRŠIČ 68 KRANJSKA GORA 72 24 KRANJSKA GORA 74 Period during which transport is provided Price of tickets Bicycle transportation Guided tours 3 I 4 ALPS A JULIAN Julian Alps Triglav National Park 5 6 SLOVEniA The Julian Alps and the Triglav National Park are protected by the UNESCO Man and the Biosphere Programme because the Julian Alps are a treasury of natural and cultural richness. The Julian Alps community is now more interconnected than ever before and we are creating a new sustainable future of green tourism as the opportunity for preserving cultural and natural assets of this fragile environment, where the balance between biodiversity and lifestyle has been preserved by our ancestors for centuries. -
Projekt Frisco1
PROJEKT FRISCO1 PREKOGRANIČNO USKLAĐENO SLOVENSKO-HRVATSKO SMANJENJE RIZIKA OD POPLAVA – NEGRAĐEVINSKE MJERE ČEZMEJNO USKLAJENO SLOVENSKO-HRVAŠKO ZMANJŠEVANJE POPLAVNE OGROŽENOSTI – NEGRADBENI UKREPI MURA DRAVA SOTLA/SUTLA KOLPA/KUPA BREGANA DRAGONJA 4 O projektu (ENG, HR, SI) 9 Rezultati projekta Unaprijeđene baze podataka za upravljanje rizicima od poplava 10 Izboljšane baze podatkov za obvladovanje poplavne ogroženosti Zajedničke prekogranične studije integriranog upravljanja rizicima od poplava 12 Skupne čezmejno usklajene študije celovitega obvladovanja poplavne ogroženosti Unaprijeđeni hidraulički modeli 14 Izboljšani hidravlični modeli Unaprijeđeni modeli za prognoziranje poplava 16 Izboljšani modeli za napovedovanje poplav Unaprijeđene i prekogranično usklađene karte opasnosti od poplava i 18 karte rizika od poplava Izboljšane in čezmejno usklajene karte poplavne nevarnost in poplavne ogroženosti Zajednički projekti provedbe građevinskih mjera (Priprema projektne i druge tehničke dokumentacije) 20 Skupni projekti za izvedbo gradbenih ukrepov (priprava projektne in ostale tehnične dokumentacije) Sustavi ranog upozoravanja 22 Sistemi zgodnjega opozarjanja Podizanje svijesti javnosti o rizicima od poplava 24 Ozaveščanje o poplavni ogroženosti in krepitev zmogljivosti 26 Opis porečij in prikaz možnih gradbenih ukrepov 28 Sliv Kupe / Porečje Kolpe 34 Sliv Sutle / Porečje Sotle 40 Sliv Mure / Porečje Mure 46 Sliv Drave / Porečje Drave 51 Sliv Dragonje / Porečje Dragonje 56 Sliv Bregane / Porečje Bregane Kazalo About the project ENG In -
JULIANA TRAIL: Stage 1 Kranjska Gora - Mojstrana
Hiking trail JULIANA TRAIL: stage 1 Kranjska Gora - Mojstrana 18.5km 6:06h 270m 441m Difficulty moderate km 0 0.7 1.4 2.8 4.2 Base Map: outdooractive Cartography; ©OpenStreetMap (www.openstreetmap.org) 1 / 5 Hiking trail JULIANA TRAIL: stage 1 Kranjska Gora - Mojstrana 18.5km 6:06h 270m 441m Difficulty moderate km 0 0.8 1.6 3.2 4.8 Base Map: outdooractive Cartography; ©OpenStreetMap (www.openstreetmap.org) 2 / 5 Hiking trail JULIANA TRAIL: stage 1 Kranjska Gora - Mojstrana Road surface Elevation profile Length 18.5km m 1200 1000 800 600 km 2 4 6 8 10 12 14 16 18 Tour data Best time of year Ratings Hiking Trail Difficulty moderate Authors JAN FEB MAR Distance 18.5 km Stamina Experience APR MAY JUN Duration 6:06 h Technique JUL AUG SEP Landscape Ascent 270 m Altitude OCT NOV DEC 971 m Descent 441 m 650 m More tour data Source Julische Alpen Properties Bled, Ljubljanska c. 27 Public transport friendly Multi-stage tour 4260 Bled Scenic Geological highlights Phone +386(0)4 / 578 02 00 Faunistic highlights Healthy climate Fax In and out Cultural/historical value [email protected] Botanical highlights The stage leads you along the Sava Dolinka Valley and Awards partially on the edges of the Karavanke mountain range, and connects the winter and summer tourist With refreshment stops centre of Kranjska Gora with Mojstrana, which is located at the entry to the valley of Vrata. Family friendly The trail leads us from the centre of Kranjska Gora, a Marko Lenarcic winter and summer tourist centre, known for alpine world cup competitions and to nearby Planica, one of Updated: February 14, 2020 the world’s major ski jumping and ski flying centres. -
TO SLOVENIA First Time Cultivating Wine in Protestant Literature
Compiled by FACTS Neža Lukančič & VINARIUM TOWER Benjamin Wolf The Pannonian Eiffel Tower is the SLOVENIA highest observation tower in Slovenia POPULATION: and allows a view in four countries: 2,067,000 Slovenia, Croatia, Hungary and Austria. CAPITAL CITY: LJUBLJANA (288,250) ŽIČE CHARTERHOUSE The ruins of this 12th century GDP: €43 BILLION monastery complex, overgrown with GDP PER CAPITA: ivy and moss, are a magical place. €21,000 MEŽICA MINE CROATIA ZAGREB POPULATION: The underground of Slovenia also offers hidden treasures. Sit in a small train and descend to a mine The history of Croatia’s capital dates back 4,167,000 universe that has been active for over 350 years. to the Romans. Today, the area houses a CAPITAL CITY: quarter of the country's population. ZAGREB (806,920) Zagreb’s old town boasts buildings from the 13th to the 19th century. GDP: €49 BILLION GDP PER CAPITA: OTOČEC €11,700 PREDJAMA CASTLE The only water castle in Slovenia was build on a small Source: Eurostat (2017). This Renaissance castle is built within a cave, island on Krka River. It is a favorite wedding venue, pressed next to a cliff under the original while the nearby leisure park offers fun times. Medieval fortification. METAL DAYS (SOČA) LJUBLJANA Every July, the peaceful Soča River is Slovenia’s capital stands at the middle the setting for one of the biggest heavy of a trade route between the northern metal music festivals in Europe with Adriatic Sea and the Danube region. the fitting motto: “Hell over Paradise.” Among the sights of this green city are Tivoli Park and Ljubljana Castle. -
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). -
Case Study of Kupa River Watershed in Croatia
J. Hydrol. Hydromech., 67, 2019, 4, 305–313 DOI: 10.2478/johh-2019-0019 Long term variations of river temperature and the influence of air temperature and river discharge: case study of Kupa River watershed in Croatia Senlin Zhu1, Ognjen Bonacci2, Dijana Oskoruš3, Marijana Hadzima-Nyarko4*, Shiqiang Wu1 1 State Key Laboratory of Hydrology-Water resources and Hydraulic Engineering, Nanjing Hydraulic Research Institute, Nanjing 210029, China. 2 Faculty of Civil Engineering and Architecture, University of Split, Matice hrvatske 15, 21000 Split, Croatia. 3 Meteorological and Hydrological Service, Gric 3, 10000 Zagreb, Croatia. 4 Josip Juraj Strossmayer University of Osijek, Faculty of Civil Engineering and Architecture Osijek, Vladimira Preloga 3, 31000 Osijek, Croatia. * Corresponding author. E-mail: [email protected] Abstract: The bio-chemical and physical characteristics of a river are directly affected by water temperature, which therefore affects the overall health of aquatic ecosystems. In this study, long term variations of river water temperatures (RWT) in Kupa River watershed, Croatia were investigated. It is shown that the RWT in the studied river stations in- creased about 0.0232–0.0796ºC per year, which are comparable with long term observations reported for rivers in other regions, indicating an apparent warming trend. RWT rises during the past 20 years have not been constant for different periods of the year, and the contrasts between stations regarding RWT increases vary seasonally. Additionally, multi- layer perceptron neural network models (MLPNN) and adaptive neuro-fuzzy inference systems (ANFIS) models were implemented to simulate daily RWT, using air temperature (Ta), flow discharge (Q) and the day of year (DOY) as predic- tors. -
Neolithisation of Sava-Drava-Danube Interfluve at the End of the 6600–6000 BC Period of Rapid Climate Change> a New Solutio
Documenta Praehistorica XLIII (2016) Neolithisation of Sava-Drava-Danube interfluve at the end of the 6600–6000 BC period of Rapid Climate Change> a new solution to an old problem Katarina Botic´ Institute of Archaeology, Zagreb, CR [email protected] ABSTRACT – The idea of the Neolithisation of the Sava-Drava-Danube interfluve has undergone very little change since S. Dimitrijevi≤'s time. Despite their many shortcomings, new archaeological exca- vations and radiocarbon dates of Early Neolithic sites have provided us with new insight into the process of Neolihisation of this region. Using the recently published work by B. Weninger and L. Clare (Clare, Weninger 2010; Weninger et al. 2009; Weninger et al. 2014) as a starting point, the available radiocarbon and archaeological data are used to build up a time frame comparable to the wider region of Southeast Europe and climate conditions for specific period. The results fit the model of Neolithisation well (Weninger et al. 2014.9, Fig. 4), filling in the geographical gaps. IZVLE∞EK – Premise o neolitizaciji v medre≠ju Save, Drave in Donave se od ≠asa S. Dimitrijevi≤a niso veliko spremenile. Nova arheolo∏ka izkopavanja in radiokarbonski datumi zgodnjega neolitika so, kljub mnogim pomanjkljivostim, prinesli nove vpoglede v proces neolitizacije na tem obmo≠ju. Za os- novo pri interpretaciji smo uporabili nedavno objavljena dela B. Weningerja in L. Clarea (Clare, We- ninger 2010; Weninger et al. 2009; Weninger et al. 2014), dosegljive radiokarbonske datume in arheo- lo∏ke podatke pa smo uporabili za izdelavo ≠asovnega okvirja, ki je primerljiv s ∏ir∏im obmo≠jem ju- govzhodne Evrope in s klimatskimi pogoji za posamezna obdobja. -
PRILOGA 1 Seznam Vodnih Teles, Imena in Šifre, Opis Glede Na Uporabljena Merila Za Njihovo Določitev in Razvrstitev Naravnih Vodnih Teles V Tip
Stran 4162 / Št. 32 / 29. 4. 2011 Uradni list Republike Slovenije P R A V I L N I K o spremembah in dopolnitvah Pravilnika o določitvi in razvrstitvi vodnih teles površinskih voda 1. člen V Pravilniku o določitvi in razvrstitvi vodnih teles površin- skih voda (Uradni list RS, št. 63/05 in 26/06) se v 1. členu druga alinea spremeni tako, da se glasi: »– umetna vodna telesa, močno preoblikovana vodna telesa in kandidati za močno preoblikovana vodna telesa ter«. 2. člen V tretjem odstavku 6. člena se v drugi alinei za besedo »vplive« doda beseda »na«. 3. člen Priloga 1 se nadomesti z novo prilogo 1, ki je kot priloga 1 sestavni del tega pravilnika. Priloga 4 se nadomesti z novo prilogo 4, ki je kot priloga 2 sestavni del tega pravilnika. 4. člen Ta pravilnik začne veljati petnajsti dan po objavi v Ura- dnem listu Republike Slovenije. Št. 0071-316/2010 Ljubljana, dne 22. aprila 2011 EVA 2010-2511-0142 dr. Roko Žarnić l.r. Minister za okolje in prostor PRILOGA 1 »PRILOGA 1 Seznam vodnih teles, imena in šifre, opis glede na uporabljena merila za njihovo določitev in razvrstitev naravnih vodnih teles v tip Merila, uporabljena za določitev vodnega telesa Ime Zap. Povodje Površinska Razvrstitev Tip Pomembna Presihanje Pomembna Pomembno Šifra vodnega Vrsta št. ali porečje voda v tip hidro- antropogena različno telesa morfološka fizična stanje sprememba sprememba 1 SI1118VT Sava Radovna VT Radovna V 4SA x x x VT Sava Sava 2 SI111VT5 Sava izvir – V 4SA x x x Dolinka Hrušica MPVT Sava 3 SI111VT7 Sava zadrževalnik MPVT x Dolinka HE Moste Blejsko VTJ Blejsko 4 SI1128VT Sava J A2 x jezero jezero VTJ Bohinjsko 5 SI112VT3 Sava Bohinjsko J A1 x jezero jezero VT Sava Sava 6 SI11 2VT7 Sava Sveti Janez V 4SA x x Bohinjka – Jezernica VT Sava Jezernica Sava 7 SI1 1 2VT9 Sava – sotočje V 4SA x x Bohinjka s Savo Dolinko Uradni list Republike Slovenije Št. -
Evaluation of Wetlands and Floodplain Areas in the Danube River Basin Final Report May 1999
DANUBE POLLUTION REDUCTION PROGRAMME EVALUATION OF WETLANDS AND FLOODPLAIN AREAS IN THE DANUBE RIVER BASIN FINAL REPORT MAY 1999 Programme Coordination Unit UNDP/GEF Assistance prepared by WWF Danube-Carpathian-Programme and WWF-Auen-Institut (Germany) DANUBE POLLUTION REDUCTION PROGRAMME EVALUATION OF WETLANDS AND FLOODPLAIN AREAS IN THE DANUBE RIVER BASIN FINAL REPORT MAY 1999 Programme Coordination Unit UNDP/GEF Assistance prepared by WWF Danube-Carpathian-Programme and WWF-Auen-Institut (Germany) Preface The "Evaluation of Wetlands and Flkoodplain Areas in the Danube River Basin" study was prepared in the frame of the Danube Pollution Reduction Programme (PRP). The Study has been undertaken to define priority wetland and floodplain rehabilitation sites as a component of the Pollution reduction Programme. The present report addresses the identification of former floodplains and wetlands in the Danube River Basin, as well as the description of the current status and evaluation of the ecological importance of the potential for rehabilitation. Based on this evaluation, 17 wetland/floodplain sites have been identified for rehabilitation considering their ecological importance, their nutrient removal capacity and their role in flood protection. Most of the identified wetlands will require transboundary cooperation and represent an important first step in retoring the ecological balance in the Danube River Basin. The results are presented in the form of thematic maps that can be found in Annex I of the study. The study was prepared by the WWF-Danube-Carpathian-Programme and the WWF-Auen-Institut (Institute for Floodplains Ecology, WWF-Germany), under the guidance of the UNDP/GEF team of experts of the Danube Programme Coordination Unit (DPCU) in Vienna, Austria. -
Januar 2017 (Foto: Aleksander Marinšek) Figure 2
VSEBINA METEOROLOGIJA 3 Podnebne razmere v januarju 2017 .........................................................................................................3 Razvoj vremena v januarju 2017 ........................................................................................................... 25 Podnebne razmere v Evropi in svetu v januarju 2017 ........................................................................... 32 Meteorološka postaja Rate če ................................................................................................................ 34 Poro čilo o izdanih opozorilih in obvestilih o vremenskih ujmah v letu 2016 .......................................... 45 Svetovni dan meteorologije – 23. marec 2017 – Razumeti oblake ....................................................... 48 Muzejska razstava: »Kakšno je bilo vreme na Gorenjskem?« .............................................................. 50 AGROMETEOROLOGIJA 55 HIDROLOGIJA 60 Pretoki rek v januarju 2017 .................................................................................................................... 60 Vodnat zahod in jug v letu 2016 ............................................................................................................ 65 Temperature rek in jezer v januarju 2017 .............................................................................................. 74 Dinamika in temperatura morja v januarju 2017.................................................................................... 77 Dinamika in temperatura -
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.