1. General Restrictions 9N Sundays, Public Holidays and Non-Working
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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. -
Presoja Poplavne Varnosti in Analiza Vzrokov Poplav V Pesniški Dolini Avgusta 2009
S. BUKOVNIK - 22 - STANJE, VZDRŽEVANJE IN B. IVANUŠA OBRATOVANJE GRAJENIH HIDROSISTEMOV Stanislav BUKOVNIK* Blaž IVANUŠA ** PRESOJA POPLAVNE VARNOSTI IN ANALIZA VZROKOV POPLAV V PESNIŠKI DOLINI AVGUSTA 2009 1. SPLOŠNO Urejanje voda in dolinskih povodij manjših hidrosistemov, kot so v Severovzhodnem delu Slovenije, reke Pesnica, Dravinja, Polskava, Sejanca, Savinja, Ledava, Ščavnica, Kobiljski potok….., se je intenzivneje pričelo v šestdesetih letih prejšnjega stoletja. Osnovni cilj urejanja celotnih hidrosistemov, je bila zaščita premoženja prebivalcev in države ter izboljšati pogoje kmetovanja in kmetijske proizvodnje na ravninskih območjih ob vodotokih. Celotni sistemi so se zgradili v okviru Zelenega plana RS. Izgrajene sisteme – osnovno odvodnjo, je prevzelo v upravljanje in vzdrževanje pristojno Ministrstvo za okolje in prostor, hidromelioracijske sisteme pa Ministrstvo za kmetijstvo, gozdarstvo in prehrano. Kot dober gospodar so lastniki posameznih delov sistema, vse do nedavnega, sisteme tudi vzdrževali in upravljali. Približno po letu 1990 so se pričele razmere na terenu slabšati. V zadnjem obdobju prihaja do vse pogostejših in intenzivnejših poplav ter posledično vedno večjih škod na premoženju, infrastrukturi in intenziviranih kmetijskih površinah oziroma kmetijski proizvodnji. Pogostost in povečevanje trajanja poplav, kaže na to, da se poplavna varnosti iz leta v leto slabša. Vzroki za tak trend so v sumiranju vseh dejavnikov, ki vplivajo na odvodni režim primarne in sekundarne odvodne mreže. Ti dejavniki so: 1. Posegi v prostor, ki vplivajo na vodni režim 2. Krčenje retenzijskih površin 3. Vzdrževanje sistema osnovne in sekundarne odvodnje 4. Obratovanje grajenih zadrževalnikov 5. Klimatske spremembe V nadaljevanju podajamo poplavno varnost in Analizo vzrokov zmanjševanja poplavne varnosti v Pesniški dolini oz. hidrosistema reke Pesnice na območju občin Maribor, Pesnica, Lenart in Sveta Trojica. -
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. -
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. -
95/2006, Uredbeni
PRILOGA Priloga: deli vodnih teles površinskih voda, na katerih se pravica do uporabe hidroelektrarne na podlagi pravnomočnega uporabnega dovoljenja spreminja v koncesijo za proizvodnjo električne energije v hidroelektrarnah do 10 MW Površinska voda Potencialna (Ime vodotoka, na Kota zgornje Kota spodnje energija Pretok faktor katerem je del vodnega Občina vode vodnega vode vodnega vodnega Št. Q pretočnosti telesa, ki se rabi za (Ime) telesa telesa telesa (m3/s) Fp** proizvodnjo električne Hzg (m.n.m.) Hsp (m.n.m.) Wp* energije) (MWh/leto) 1 Temnak Tolmin 455,00 400,00 0,140 0,263 174 2 Batava Tolmin 591,00 507,00 0,032 0,119 27 3 Medvedji potok Tolmin 480,00 419,00 0,030 0,233 37 4 Poreznica Tolmin 840,00 740,00 0,060 0,426 219 5 Manjški potok Idrija 635,00 591,00 0,030 0,201 23 6 Čerinščica Cerkno 473,00 454,00 0,080 0,840 110 7 Cerknica Cerkno 518,00 480,00 0,110 0,171 61 8 Zapoška Cerkno 668,00 592,00 0,070 0,320 146 9 Črna Cerkno 521,12 470,00 0,155 0,242 165 10 Črna Cerkno 591,00 552,66 0,155 0,143 73 11 Oresovka Cerkno 425,00 383,00 0,145 0,131 69 12 Zapoška Cerkno 331,00 325,00 0,150 0,201 16 13 Črna Cerkno 635,00 600,00 0,120 0,030 11 14 izvir Tresilo Kobarid 607,00 547,00 0,015 0,201 16 15 Tbin Tolmin 370,00 170,00 0,100 0,030 51 16 Kamnica Tolmin 230,00 215,00 0,035 0,324 15 17 Volarja Tolmin 192,00 185,00 0,700 0,195 82 18 Volarja Tolmin 198,00 192,00 0,350 0,507 91 19 Hočki potok Hoče- Slivnica 538,00 505,00 0,100 0,161 46 20 Piskrski potok Ruše 688,00 345,00 0,080 0,380 896 21 Oplotnica Sl.Bistrica 600,00 550,00 1,800 0,296 2286 22 Bistrica Ruše 317,20 293,59 0,100 0,068 14 23 Dovžanka Mislinja 595,70 587,30 0,200 0,443 64 24 Velka Podvelka 397,60 394,40 1,200 0,416 137 25 Kamniška Bistrica- Domžale mlinščica 327,11 325,00 1,800 0,370 121 26 Lašek Solčava 820,00 710,00 0,074 0,183 128 27 Zavratnikov potok Luče 780,00 640,00 0,012 0,063 9 28 Stoglejski gr. -
Št. 58 / 20. 8. 1998 / Stran 4429
Uradni list Republike Slovenije Št. 58 / 20. 8. 1998 / Stran 4429 Tabela 1: Obmoèja urejanja v Obèini Kranjska Gora Naziv Planska Oznaka obmoèja Obmoèja urejanja s PIN obmoèja urejanja celota urejanja z navedbo uradne objave veljavnih PIN Rateče–Kamne R H1 UN* Rateèe R SK 1/1 Rateče–vzhod R SK 1/2 Rateče–vzhod 1 R SK 2 ZN* Rateče–vikendi R W1 Planica R R1 UN* Smučišče Planica R R2 Smučišče Lom R R3 Rateèe R E1 Rateče–pokopališče R Z1 Podkoren–hotel KG H1 ZN, UVG 32/97, 34/97, 38/97 (2. 9. 97) Podkoren KG SK1 Podkoren–vzhod KG SK2 Podkoren–vikendi KG W1 Smučišča Podkoren KG R1 Poligon Podkoren KG R2/1 Poligon Podkoren KG R2/2 Korensko sedlo–mejni prehod KG T3 Podkoren–pokopališče KG Z1 Zelenci KG B UN, UVG 32/96 Kranjska Gora–pod Vitrancem KG H2 ZN* Kranjska Gora–Kompas KG H3 Kranjska Gora–Prisank KG H4 Kranjska Gora–Lek KG H5 Kranjska Gora–Casino KG H6 Kranjska Gora KG SK3 Kranjska Gora–Črtenje KG SK4 Kranjska Gora–ob Borovški KG SK5 Kranjska Gora–Log KG SK6/1 Kranjska Gora–Log KG SK6/2 Kranjska Gora–Čičare KG S2 Kranjska Gora–Črtenje KG S3 Kranjska Gora–Log KG S4 ZN, UL RS 30/96 in 50/96 Kranjska Gora–Jasna KG W2 Kranjska Gora–Log KG O1 Kranjska Gora–smučišča KG R3 Kranjska Gora–Porentov dom KG R4 UN* Kranjska Gora–ob Pišnici KG R5 Kranjska Gora–Trebež KG R6 Kranjska Gora–Log KG R7 Kranjska Gora–pokopališče KG Z2 ZN, UVG 26/78 Gozd Martuljek–hotel Špik KG H7 Gozd Martuljek–zahod KG SK7/1 Gozd Martuljek–zahod KG SK7/2 Gozd Martuljek–zahod KG SK7/3 Gozd Martuljek–vzhod KG SK8 Gozd Martuljek–vikendi 1 KG W3 UVG 22/73 Gozd Martuljek–vikendi 2 KG W4 UVG 22/73 Gozd Martuljek–smučišča KG R6 Gozd Martuljek–kamp KG R7 Belca–Podkuže DM SK1 Belca–ob potoku DM SK2 Belca–vzhod DM SK3 Mojstrana–levi breg DM SK4 Mojstrana–desni breg DM SK5 Mojstrana–fabrka DM SK6 UN* Mojstrana–novi del DM S1 Mojstrana–LIP DM P1 Mojstrana–območje KOOP DM P2 Mojstrana–športni center Proda DM R1 Mojstrana–pri Rosu DM R2 UN* Mojstrana–Mlačca DM R3 Mojstrana–smučišča DM R4 Dovje–Vatiš DM SK7/1 Dovje–Vatiš DM SK7/2 Dovje DM SK8 Dovje–vzhod DM S2 Stran 4430 / Št. -
Influence of the Rate of Construction and of Rock
Influence of the rate of construction and of rock mass strength reduction on the stability of deep cuts in marl Influence de taux de construction et de reduction de resistance de roche sur la stabilite des deblais profonds dans la marne K. Štern Geoinženiring d.o.o. - Maribor office, Email: [email protected] ABSTRACT During geotechnical monitoring of anchored retaining structure and marl rock mass in conditions where marl is sensitive to variations in water content, the question appeared if design investigations in such cases generally overestimate strength and stiffness parameters. Another question is concerned with the extent and amount of changes in rock mass properties and with the influence of the construction rate and sequence. It was found out that the process of secondary humidification of the slope is directly related to the progress of works. The recorded increase of marl water content was on average 1.2% and the average decrease of uniaxial compressive strength was 28 %. RÉSUMÉ Au suivi des conditions de sols de fondation et des ouvrages ancres dans les marnes sensibles a l'humidite de la partie nord-est de la Slovenie, des questions sont posees de savoir si les parametres de resistance de la roche, suffisants et de qualite, obtenus a partir des recherches, sont surestimes, dans quelle mesure a l'arriere-pays les conditions suite a l'excavation sont egales aux conditions en phase de recherches, et de quelle maniere le taux de construction ou de l'excavation de la roche agissent sur la condition entiere et la modification des parametres de resistance. -
Tipi Hidrografskih Območij V Gričevjih Severovzhodne Slovenije Glede Na Značilnosti Reliefa in Prsti
giss15_2020_gis 09-10.qxd 28.8.2020 7:55 Page 53 Modeliranje pokrajine, 53–71, Ljubljana 2020 TIPI HIDROGRAFSKIH OBMOČIJ V GRIČEVJIH SEVEROVZHODNE SLOVENIJE GLEDE NA ZNAČILNOSTI RELIEFA IN PRSTI dr. Mauro Hrvatin, dr. Manca Volk Bahun ZRC SAZU, Geografski inštitut Antona Melika [email protected], ORCID: https://orcid.org/0000-0002-6021-8736 [email protected], ORCID: https://orcid.org/0000-0003-4720-9541 dr. Dénes Lóczy University of Pécs, Faculty of Sciences, Institute of Geography and Earth Sciences [email protected], ORCID: https://orcid.org/0000-0002-2542-6775 DOI: https://doi.org/10.3986/9789610504696_04 UDK: 911.2:556.166(497.41) 551.4:556.166(497.41) IZVLEČEK Tipi hidrografskih območij v gričevjih severovzhodne Slovenije glede na značilnosti reliefa in prsti Nadzor nad poplavami je učinkovitejši, če vodo zadržujemo že v povirjih, s čimer preprečimo prehitro in neobvladljiv o stekanje vode v nižje dele porečja. Sodobno integrirano in trajnostno upravljanje s porečji zahteva ponovno ovrednotenje obstoječih ukrepov za zmanjševanje prehitrega odtoka vode in preprečeva- nje poplav. Ti obsegajo tradicionalne in sodobne pristope. V prispevku smo glede na reliefne in pedološke razmere z razvrščanjem v skupine določili sedem tipov hidrografskih območij v gričevjih severovzhodne Slovenije. Za vsako skupino hidrografskih območij so značilne svojevrstne odtočne razmere, ki pomem- bno vplivajo na pogostost in obseg poplav. KLJUČNE BESEDE relief, prst, poplava, geografski informacijski sistem, razvrščanje v skupine, gričevje, Slovenija ABSTRACT Types of hydrographic areas in the low hills of northeastern Slovenia according to the landscape and soil characteristics Flood control can be more efficient if it retains runoff in the higher sections of watersheds before concen- tration of runoff increases to an extent where inundations cannot be prevented. -
Case Study Slovenia
TOWN Small and medium sized towns in their functional territorial context Applied Research 2013/1/23 Case Study Report | Slovenia Version 05/09/2013 ESPON 2013 1 This report presents the interim results of an Applied Research Project conducted within the framework of the ESPON 2013 Programme, partly financed by the European Regional Development Fund. The partnership behind the ESPON Programme consists of the EU Commission and the Member States of the EU27, plus Iceland, Liechtenstein, Norway and Switzerland. Each partner is represented in the ESPON Monitoring Committee. This report does not necessarily reflect the opinion of the members of the Monitoring Committee. Information on the ESPON Programme and projects can be found on www.espon.eu The web site provides the possibility to download and examine the most recent documents produced by finalised and ongoing ESPON projects. This basic report exists only in an electronic version. © ESPON & University of Leuven, 2013. Printing, reproduction or quotation is authorised provided the source is acknowledged and a copy is forwarded to the ESPON Coordination Unit in Luxembourg. List of authors Nataša Pichler-Milanović, University of Ljubljana, Faculty of Civil and Geodetic Engineering, Ljubljana, Slovenia Samo Drobne, University of Ljubljana, Faculty of Civil and Geodetic Engineering, Ljubljana, Slovenia Miha Konjar, University of Ljubljana, Faculty of Civil and Geodetic Engineering, Ljubljana, Slovenia © Institute UL-FGG d.o.o, Jamova 2, SI-1001 Ljubljana, Slovenia ESPON 2013 i Table of contents -
Kmečko Življenje V Zgornjesavski Dolini V 18. in 19. Stoletju, 495–512 2016
2016 1.01 Izvirni znanstveni članek UDK 304.3(497.452)''17/18'' 323.3:63-051(497.452)''17/18' Prejeto: 1. 6. 2016 Alenka Kačičnik Gabrič dr., višja arhivistka, Arhiv Republike Slovenije, Zvezdarska 1, SI–1000 Ljubljana E-pošta: [email protected] Kmečko življenje v Zgornjesavski dolini v 18. in 19. stoletju IZVLEČEK Območje Zgornjesavske doline je precej obsežno in raznoliko, v njen okvir pa po Gamsovi pokrajinsko-ekološki členitvi spada alpska dolina, po kateri teče Sava Dolinka. Pričujoči članek na osnovi podatkov v starih zemljiških evidencah obravnava območje od Bele Peči do Jesenic, ki ga je v preteklosti močno zaznamovalo rudarjenje in do danes pustilo trajni pečat. Zemlja je za osnovno kmetijsko dejavnost slabo rodovitna in najbolj primerna za živinorejo, mikroklimatske razmere pa se od ene do druge katastrske občine nekoliko razlikujejo. Klima je povsod bolj ali manj visokogorska in kmetijski pridelavi dokaj neprijazna. V preteklosti pa je tistim, ki so živeli v visokogorskih predelih območja, življenje oteževala tudi geografska odmaknjenost. KLJUČNE BESEDE Zgornjesavska dolina, kmečko življenje, Bela Peč, Rateče, Podkoren, Dovje, Hrušica, Jesenice, Kranjska Gora, Planina, Gozd ABSTRACT RURAL LIFE IN THE UPPER SAVA VALLEY IN THE 18TH AND 19TH CENTURIES The area of the Upper Sava Valley is a vast and diverse one and, according to the Gams’s landscape-ecological clas- sification, also includes the alpine valley of the Sava Dolinka River. Drawing on old land records, the paper at hand discusses the area stretching from Bela Peč to Jesenice, which was once strongly affected by the mining industry, with its traces still visible today. -
The British, Kugy, and Western Slovenia
182 The British, Kugy, and Western Slovenia Ksenija Rozman Plates 69-72 The Julian Alps, the Sava valley, the surroundings of the lakes at Bled and Bohin;, Lake Cerknica, the city of Ljubljana and the Postojna caves are areas which the British have been visiting for centuries-fust as scientists, later also as travellers and mountaineers, and today mainly as tourists. All these areas are readily accessible by organized motor co'ach tours which start from Bled, Bohinj and Kran;ska gora. This territory, once part of the multi-national Austrian empire, now is the western part of the republic of Slovenia, one of the six constituent republics of Yugoslavia. The highest mountain in Yugoslavia, Triglav (2863m), lies in Slovenia. Dr Julius Kugy once asked France Avein, the Slovenian moun taineer, climber and professor of electrical engineering, what part of the Julian Alps he liked the best. Avein decided on the western Julian Alps, but Kugy demurred; 'That's all right, my dear Avein, it's beautiful! But the eastern part has the Triglav. The Triglav is not a mountain, the Triglav is a realm.'l Forests, mountains, mountain flora, meadows, rivers and lakes are all naturally constituent parts of the globe-but so many prominent Britons have wri~ten so much in praise of Slovenia and its people that even the best educated European could hardly fail to take heed and to be flattered. Sir Humphry Davy, and after him Josiah Gilbert and GC Churchill thought that the valley of the Sava river was the most beautiful valley in Europe. -
App. E1.1 - the Earthquake of 25 May 1448 in Catalonia
"A Basic European Earthquake Catalogue and a Database for the evaluation of long-term seismicity and seismic hazard" (BEECD) App. E1.1 - The earthquake of 25 May 1448 in Catalonia study by Salicrú i Lluch R., 1995. The 1448 earthquake in Catalonia. Some effects and local reactions. Annali di Geofisica, 38, pp. 503-513 short comment by V. Castelli For this earthquake the BEECD WF contains the following entry, coming from the input PEC MEM83. The root is to be considered "hidden" among the references supplied by this PEC. Ds Ye Mo Da Ho Mi Ax R Rc Nmo Ix Io Lat Lon Mm MEM83 1448 05 24 01 30 CARDEDEU.B HID 3C - 0 80 41.633 02.333 - This earthquake has been recently studied by Salicrú i Lluch (1995). Brief analysis of the sources used by the study The study starts from a summary of the available dataset, collected by the leading Catalan seismological compilation (Fontserè and Iglésies, 1971) and consisting of "several contemporary chronistic and narrative sources from Barcelona [...] Perpinyà [...] Vic [...] and Girona [...]". The study then goes on to improve this reasonably good, but uneven dataset by adding new, unpublished contemporary sources and giving a new interpretation of a document already known to Fontserè and Iglésies (1971), which connected it to an earthquake occurred in September 1450. The study shows that it was written on July 1450 and could therefore be related to the previous event. The new data come from the episcopal archives of Barcelona and the central archives of the Aragonese kingdom (ACA, 1453; Acords, 1424-1451; ADV, 1450; Dietari, 1411-1458; ADB, 1448-1453; Jornades, 1411-1484; Revista, 1881).