U radu se istražuje usmena književnost Bistre, opisuju se vrste i oblici koji se pojavljuju, kao i teme i motivi koji prevladavaju u kazivanjima prema dostupnim izvorima. Istraživanje je pokazalo da ...se usmena književnost bistranskoga kraja ponajviše temelji na usmenoj lirici, folklornom kazalištu i usmenoj predaji što su tijekom terenskoga istraživanja 1970-ih godina zabilježili istraživači Instituta za etnologiju i folkloristiku (tada: Institut za narodnu umjetnost). Komparativna je analiza pokazala da se pojedine teme i motivi u zapisanim pjesmama iz drugih krajeva pojavljuju u bistranskim inačicama usmene lirike. U istraživanjima folklornoga kazališta zabilježene su dramske scene mahom vezane uz vjerske blagdane, pokladne maškare i svadbene običaje, dok su u usmenoj predaji zabilježeni zapisi o Seljačkoj buni, kmetovima i feudalcima i liku Matije Gupca. U današnje se vrijeme očuvanjem i promicanjem bistranske usmene tradicije bave članovi Kulturno-umjetničkoga društva „Bistra“, Udruga „Ekomuzej Bistra“, kao i druge bistranske udruge, mještani i istraživači.
The paper explores oral literature of Bistra, describes the types and forms that appear, as well as the themes and motifs that prevail in narrations according to available sources. The research showed that oral literature of the Bistra region is mostly based on oral lyrics, folklore theater and oral tradition, which was recorded during field research in the 1970s by researchers at the Institute of Ethnology and Folklore Research (then: Institute of Folk Art). Comparative analysis has shown that certain themes and motifs in written poems from other regions appear in Bistran versions of oral lyrics. Within the research of folklore theater, dramatic scenes were recorded, mostly related to religious holidays, carnival masquerades and wedding customs, while oral tradition contains records of the Peasant uprising 1573, serfs and feudal lords and the figure of Matija Gubec. Nowadays, members of the Cultural and Artistic Society "Bistra", the Association "Ecomuseum Bistra", as well as other Bistra associations, locals and researchers are involved in preserving, and promoting Bistra oral tradition.
The borders of the cadastral municipalities that are still valid today are, in many cases, based on much older landowners’ borders of feudal lordships. Thus, in central Slovenia, in the forests below ...Mount Krim, we find the old boundary marks representing today’s cadastral municipality of Preserje, based on the former border between the Carthusia Bistra and the Ig estate from 1726. The main purpose of this paper is to present the current state of the preserved boundary marks along this border. The preserved boundary marks are about 80 cm high, have carved sequential letters, the year 1726 and coats of arms of the Carthusia Bistra and the earls Engelshaus (the owners of the Ig estate at that time). In 1748, this boundary was adopted as the boundary between the Notranjska (Inner) and the Gorenjska (Upper) districts of the Carniola region in the Habsburg Monarchy. As part of the Franciscan cadastral survey in 1823, this border was used as the border of cadastral municipalities, and it has retained this role until today. On the Franciscan cadastral maps, we find eleven locations numbered with the year 1726 and the consecutive letter from B to M. Today, at these locations, we can still find two original boundary marks decorated with coats of arms and the year 1726, two destroyed original boundary marks and three probably later replaced boundary marks without inscriptions and coats of arms. We also examined locations on the even older eastern border of the Carthusia Bistra, on which today mainly only post-war trigonometric points of lower orders can be found; only on the Smrekovec hill under Rakitna did we find another older boundary mark without additional inscriptions or coats of arms.
...in central Slovenia, in the forests below mountain Krim, we still find old boundary marks representing today's cadastral municipality of Preserje, which are based on the formei^ borde}" between ...the Bistra Carthusian monastery and the Ig estate from 1726. In 1748, this boundary was adopted as the boundary between the Notranjska (Inner) and the Gorenjska (Upper) districts of the Carniola region in the Habsburg Monarchy. On the Franciscan cadastral maps, we found eleven locations marked with 1726 and letters fiom В to M. Today, at these locations, we still find two original, two destroyed original boundary marks and three late}" replaced boundary marks without any inscriptions or coats of arms. V članku predstavljamo zgodovinski oris obravnavane meje in mej nib kamnov, ki smo ga pripravili na podlagi sistematičnega pregleda starejših zemljiškokatastrskih náčrtov, terenskih preverb in literature. Arhiv RS: signatura PE, ki jo razložimo na primeru SI AS 176/A/A133/g/A15 (https://vac. sjas.gov.si/vac/search/details?id=233458), kjer SI AS 176 označuje franciscejski kataster za Kranjsko, oznaka SI AS 181 pa reambulančni kataster za Kranjsko. Kot bo razvidno iz rezultátov, smo na terenu na nekaterih potencialnih lokacijah mejnikov našli starejše kamnite mejnike, naravne skale ali pa le presečišča nekdanjih poti. 3 ZGODOVINA MEJNIH SPOROV MED KARTUZIJO BISTRO IN IŽANSKIMI GOSPODI Za razumevanje zgodovinskega konteksta poteka obravnavanih mej katastrskih občín pa tudi starih označb na najdenih mejnih kamnih je treba poznati zgodovinski razvoj lastniške oziroma parcelne strukture obravnavanega območja. Leta 1782 pa ga je v okviru svojih reform ukinil cesar Jožef II., ki je bil zaslužen tudi za jožefinsko katastrsko izmēro. Nemško ime Freudenthal, ki se je uveljavilo v 17. stoletju, je nastalo iz latinskega opisnega poimenovanja »vesele oziroma prijetne doline v Borovnici« in tudi samega poimenovanja Borovnice, za katero že v 14. stoletju zasledimo razli čičo Freudnicz (Kobe, 1961; Mlinarič, 2001, str. 23). Prvi obranjeni opis meje kartuzije Bistra je iz leta 1264: začela se je pri nekdanji skali nad vodo na sotočju Ljubijanice in Borovniščice, potem je tekla ob bregu Ljubijanice do Podpeči, potem mimo vasi Kamnik pod Krimom v smeri današnje Rakitne, od tu proti zahodu do Cerknice in nato naravnost proti severozahodu к mejni crti, ki je ločevala območje oglejskega patriarha od ozemlja koroškega vojvode, do Logatca, nato do planine »Brekovica«1, s te planine pa preko grebenov do gore nad vasjo Tunjca2 in končno severozahodno od Vrhnike do združitve z izhodiščno točko (Kobe, 1961; Mlinarič, 2001, str. 37) (slika 4).
Boreholes Badel-1 and Badel-2, located in Sesvete near Zagreb, were drilled through 71.50 and 84.40 m of Quaternary sediments, respectively. Within these sediments, the occurrence of earthy aggregate ...and 1-2 mm nodules of the deep blue coloured mineral vivianite was observed. Interpretation of the depositional environment, provenance of the sediments and vivianite occurrence was based on sedimentological, mineralogical and palynological analyses. Three different facies within the alluvial environments were interpreted: 1) gravels and sands typical of alluvial environments 2) structureless beds of silts and clays deposited in oxbow lakes, marshes and floodplains 3) chaotic sediments deposited in the upper part of the alluvial fan. Macroscopically, an earthy aggregate is essentially an occurrence of flattened vivianite crystals grouped in clusters. The studied sediments are the product of intensive weathering of different types of rocks from Medvednica Mt. with a prevalence of green-schists. Rocks from Medvednica Mt. as the source of ferrous iron (Fe^sup 2+^) and phosphorus (P), and reductive depositional environments can indicate conditions for genesis of vivianite.
Projekt Ekomuzej Bistra zamišljen je kao integrirani projekt kojemu je svrha da na temelju ekomuzejskih postulata omogući održivo i participativno upravljanje cjelokupnom baštinom bistranskog kraja ...te da ujedno potakne razvoj kulturnih i turističkih sadržaja na području sjeverozapadnog dijela Zagrebačke županije, duž obronaka Medvednice – od sljemenskog vrha do lijeve obale rijeke Krapine na zapadu. Općina Bistra je 2014. uvrstila projekt Ekomuzeja Bistra u strateške razvojne projekte Općine Bistra te u Bazu projekata Zagrebačke županije, a 2016., na inicijativu dr. sc. Klementine Batine, osnovana je udruga Ekomuzej Bistra s ciljem zaštite, istraživanja i prezentiranja cjelokupne baštine Bistre radi održavanja kontinuiteta lokalnog identiteta te podizanja kvalitete života i održivog razvoja lokalne zajednice
Provider: - Institution: - Data provided by Europeana Collections- Monumentul este realizat din piatră și bucăți de piatră prinse cu ciment. Este alcătuit dintr-o bază, în două trepte, și un obelisc ...format din trei trepte. Pe partea superioară, încheiată cu reprezentarea unei piramide de dimensiuni mici, este fixată o cruce. Separarea între treptele de mijloc și superioară ale obeliscului s-a realizat printr-o cornișă de dimensiuni reduse. Pe toate cele trei trepte (nivele) ale obeliscului sunt incizate nume de eroi. Pe treapta de mijloc numele de eroi sunt dispuse pe două rânduri și sunt despărțite printr-o linie incizată. Întreaga compoziție se caracterizează prin simplitate. Înălțime (h) monument: 2,97m.- Mențiuni despre monument: Stare bună de conservare.- Inscripții pe monument: „SCUMPILOR NOȘTRI EROI DIN DEDA-BISTRA GĂLĂOAIA 1914-1919” NUME DE EROI (36)- All metadata published by Europeana are available free of restriction under the Creative Commons CC0 1.0 Universal Public Domain Dedication. However, Europeana requests that you actively acknowledge and give attribution to all metadata sources including Europeana
Scarce basin remnants of Cretaceous synorogenic sediments exposed in the Medvednica, Ivanščica, Žumberak Mts. and Samobor Hills of northern Croatia record the early orogenic history of the NW ...Dinarides. The provenance of sandstones from five clastic formations (Oštrc, Bistra, Kravljak, Vivodina and Glog) which cover a time span from Early to late Late Cretaceous was studied by combining petrography, whole-rock geochemistry, heavy mineral chemistry and detrital zircon fission track dating. These sediments record at least two major regional thermotectonic events which correlate well with those affecting both the Alps and the Tisza-Dacia unit to the north and east, and the central Dinaride region to the south. Short zircon fission track lag times in Barremian to Albian sediments indicate that continental fragments of the distal Adria plate margin underwent relatively fast, synsedimentary exhumation in the Early Cretaceous. Moreover, a clear dominance of Campanian zircon cooling ages (80–73 Ma) in Maastrichtian sandstones indicates detritus deriving from the erosion of newly and rapidly exhumed basement units which had undergone Late Cretaceous metamorphism in the Eastern Alps and/or the Tisza-Dacia region. Probably, the rapid Maastrichtian erosion generating metamorphic detritus occurred to a great extent on neighbouring Austroalpine basement units, and/or on the upper plate Tisza-Dacia unit during the subduction stage or the initial stages of the continent–continent collision with Adria. Development of the accretionary wedge probably resulted in a renewed availability of ophiolites for erosion within small and/or dynamically changing catchments, which can be deduced from the notable differences in reconstructed source lithologies for the coeval Glog and Vivodina formations. Combined evidence from sedimentary provenance indicators precludes the Dinaride (Adriatic) basement as a significant source for the Maastrichtian sediments.
Bistra Marului and Sucu rivers spring from Tarcu Mountains and are tributaries of the accumulation lake of Poiana Marului, being the main rivers transporting significant quantities of water to the ...lake. In order to perform an analysis from a morphometric point of view of the hydrographical network within the hydrographical basins of the two rivers, we have used the Horton - Strahler classification system, because, having a genetic basis, this classification system allows a comparative analysis of the hydrographical basins. By using this classification system, we have noticed that the two rivers have the same order and we have proved, what has already been known as a general rule, that the hydrographical basins with the same order, that are located in similar physical and geographical conditions, have on average approximately the same size of the reception basin surfaces, of the water flows, of the average slopes, of the course lengths etc. Moreover, we have proved that the two hydrographical basins have approximately the same shape and that the floods that they may generate are approximately identical as magnitude and manifestation. PUBLICATION ABSTRACT
Pri podvodnem pregledu struge potoka Bistra na Ljubljanskem barju so bili na območju ledine Mali Otavnik odkriti ostanki koliščarske naselbine iz zgodnje bronaste dobe. V plasti peska z ...organskim deritom, ki se je odložila v okolici lesenih pilotov, so bili dokumentirani odlomki keramičnih posod, kamniti odbitki in orodja ter številni neobdelani kostni ostanki živali. Med kera-miko izstopajo fragmenti skodel in vrčka iz fine sive keramike z okrasom vtisnjene vrvice ter bolj številni grobi trebušasti lonci z lijakastim vratom. Naselbina, ki jo radiokarbonska analiza datira med konec 21. in začetek 18. stoletja pr. n. št., leži na skrajnem zahodnem robu razprostranjenosti pramenaste keramike in dopolnjuje fragmentarno poznavanje zadnje faze kolišč na Ljubljanskem barju. V poglobljenem delu struge vzporedno z ostanki kolišča so bili poleg keramike, sorodne tisti iz okolice pilotov, sekire iz jelenjega roga in harpune iz roga kaprida, odkriti tudi odlomki maloštevilnih posod s primerjavami v naselbinskih in grobnih kontekstih med osrednjo Slovenijo, Krasom, Istro in Liko. Slednji morda predstavljajo sledove mlajše faze poselitve iz končnega dela zgodnje bronaste dobe ali srednje bronaste dobe.
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