Prispevek predstavlja dognanja interdisciplinarne raziskave človeških kostnih ostankov, odkritih leta 2011 na grobišču iz starejše železne dobe na Cesti Borisa Kidriča v Zagorju ob Savi. ...Študija je del obsežnejšega projekta osteoloških in izotopskih analiz kostnih ostankov iz bronaste in železne dobe (14–4. st. pr. n. št.) z območij Slovenije in Hrvaške.
Osteološka raziskava šestih oseb je pokazala, da gre za ostanke enega mlajšega odraslega moškega, enega zrelega odraslega moškega in dveh zrelih odraslih žensk ter dveh otrok nedoločljivega spola. Pri vseh šestih osebah so bile na kolagenu, pridobljenem iz kosti in/ali dentina, opravljene analize stabilnih izotopov ogljika in dušika. Na podlagi rezultatov lahko pri vseh osebah sklepamo na kopensko prehrano, ki vključuje živalske proteine (meso in/ali mlečne izdelke) in rastlinske sestavine tako iz rastlin C3 kot C4.
Željeznički promet i izgradnja željezničke infrastrukture odigrali su ključnu ulogu u razvoju industrije na prostoru Hrvatskog zagorja. Tijekom druge polovine 19. stoljeća željeznice je "odvozila" ...radnike iz Hvarskog zagorja u Zagreb. Nakon II. svjetskog rada željeznica "dovozi" radnike i sirovine u velike industrijske pogone na prostoru Hrvatskog zagorja. Ovaj rad daje historijsko-geografsku analizu razvoja industrije smještene uz željezničku infrastrukturu na prostoru Hrvatskog zagorja, analizirajući okolnosti nastavka, razvoj, okolnosti stagnacije te današnje stanje prostora i mogućnosti razvoja. U radu će biti obrad strok signeno 10 najvećih industrijskih kompleksa na prostoru općina Gornja Stubica, Konjščina, Bedekovčina, Hum na Sutli i Kumrovec te gradova Zabok, Oroslavje i Krapina smještenih uz
The goal of this paper is to, in way of interpreting the spirit of the place and using an interdisciplinary approach, present the history of one branch of the Galjuf family, which was seated at ...Vižovlje Manor in the west part of the Krapina-Zagorje County, several kilometers northwest of Veliko Trgovišće. In this sense, the paper is focused on the biographical data of those family members who were the owners of the manor. The social-architectural status of the manor in view of the terms dvorac and kurija is also discussed, since Croatian professional and scholarly literature has yet to precisely distinguish the meanings of these terms. The basic architectural elements of the manor are described, as are the changes during the observed period, with reference to the current scholarly knowledge about their appearance based on available historical sources. A significant source on social life in the manor and the changes that followed the social-economic developments of that time is the »Spomen-knjiga posjetilaca dvorca u Vižovlju« (Commemorative Visitor Book of Vižovje Manor), one of the rare preserved commemorative books from a Zagorje manor. It is also a paradigmatic portrayal of the life of Zagorje’s minor nobility in the late 18th and the 19th century.
Autori donose podatke o Slovencima u sjeverozapadnoj Hrvatskoj, odnosno Slovenaca na području Krapinsko – zagorske županije i Varaždinske županije. Istraživanje je provedeno u Državnom arhivu u ...Varaždinu i u Hrvatskom državnom arhivu. Autori predstavljaju rezultate o broju Slovenaca u Varaždinu i okolici i njihov utjecaj na kulturni i gospodarski život grada. U posljednjem poglavlju autori donosi rezultate polustrukturiranih intervjua s pripadnicima slovenske nacionalne manjine u Varaždinu i u Humu na Sutli i donose informacije o organizaciji slovenske nacionalne manjine u Varaždinu.
The Dinaridic metallogenic province is a part of the Alpine–Himalayan orogenic system, developed as a result of opening and closure of the Tethys Ocean by convergence of the African and Eurasian ...plates. The northern boundary of the Dinarides is related to the northern African margin (Adria–Apulia). The Tisia mega-unit, a small continental block, positioned between the Dinarides and the Carpathians, is genetically related to the South Eurasian edge.
The geology of the Dinarides is constrained by the Alpine Wilson cycle. The major stages of the cycle are: (a) Permian early intra-continental rifting; (b) Triassic advanced rifting; (c) Jurassic oceanization; (d) Cretaceous subduction; (e) Paleogene collision; and (f) Neogene post-collision and extension followed by orogenic collapse. Each stage creates characteristic ore deposits related to the specific geological environments. Stage (a) bears hydrothermal siderite–barite–polysulphide deposits, epigenetic sedimentary uranium deposits, red bed-type, sabkha-type copper and barite deposits and evaporites. Stage (b) favored SEDEX and hydrothermal iron–polysulphide–barite–mercury and MVT deposits. Stage (c) developed chromites, asbestos, talc and magnesite deposits. The spatial position of stage (d) remains poorly constrained. The Southern Tisia unit might be a possible candidate for the Tethyan active continental margin with the Cretaceous subduction zone positioned beneath. Absence of voluminous subduction-related magmatism and mineral deposits, however, favors subduction within the Vardar zone (the easternmost Dinarides), adjoined to the Serbomacedonian ensialic terrain with its large Cu-porphyry deposits. Stage (e) was a prelude to the prolific phase (f) with its numerous hydrothermal Pb, Zn and Sb deposits that mostly occur in the western Vardar zone. The geology and metallogeny of Southern Tisia, with medium/high grade metamorphics, I-type, S-type granites, resembles the Middle Austro-Alpine unit, formed during the main Carboniferous collisional stage.
This contribution provides a review of the metallogenic characteristics of the Northwestern and Central Dinarides and Southern Tisia mega-units, based on recently-gained knowledge on the regional geology, petrology and genesis of mineral deposits. Establishment of the plate tectonic model several decades ago greatly contributed to an integrated interpretation of ore deposit genesis. In turn, basic research in the field of ore genesis generated new data that can be used to improve the plate tectonic model.
The Macelj formation is an informal Eggenburgian-early Ottnangian lithostratigraphic unit that is established in the area of the Hrvatsko Zagorje Basin, which represented a marginal zone of the Early ...Miocene Central Paratethys Sea. Modern studies, as a part of the Geologic Map of the Republic of Croatia 1:50 000 project, yielded new data that improves the knowledge of the depositional and stratigraphic characteristics of the formation. The sedimentological research within this study was focused on the two older lithostratigraphic units of the Macelj formation: the Vučji Jarek member and the Čemernica member. The Vučji Jarek mb. is represented by three facies. The Facies of horizontally bedded sandstones is characterized by mostly medium-grained, moderately sorted sandstones that reflect deposition on the foreshore to the upper shoreface. The facies of horizontally and cross-bedded glauconitic sandstones is composed of fine- to coarsegrained, well-sorted sandstones that indicate foreshore to shoreface deposition under tidal influence. The Facies of horizontally and cross-bedded pyroclastics consists of tuff, pumice, lapilli and large blocks, showing a chaotic structure in places. Deposition occurred at the shoreface under tidal influence. The Čemernica mb. is represented by the Facies of structureless clayey-silty sands that are poorly sorted and bioturbated, and indicates deposition below the fairweather wavebase, in the offshore-transition zone. Deposits of the members include marine macro- and microfossil associations. K-Ar dating of separated glauconite mineral fractions yielded an early Eggenburgian age for the Vučji Jarek mb. glauconitic sandstones (19.2±0.64 Ma) which is in accordance with biostratigraphical analyses. Sedimentological characteristics of the Eggenburgian Macelj fm., especially those that reflect the tidal influence, fit the general characteristics of the Central Paratethys Sea in the Early Miocene.
Ultramafic cumulate rocks represent the rarest allochthonous fragments of the Mesozoic oceanic lithosphere observed today in the Upper Jurassic to Lower Cretaceous mélange of Mt. Kalnik, located in ...the SW part of the Zagorje-Mid-Transdanubian Zone (ZMTDZ). Poikilitic heteroadcumulate ultramafic rocks of Mt. Kalnik are represented by amphibole lherzolites/harzburgites and plagioclase lherzolites. Both were formed by in-situ processes within a magma chamber following the general crystallization sequence of: Al-chromite → Mg-rich olivine → enstatite ± augite → Ca-amphibole (pargasite ± edenite ± magnesiohornblende) → Ca-plagioclase (An82.6_87.4). Cumulate minerals are spinel and olivine as well as orthopyroxene and clinopyroxene which are usually enclosed in intercumulate phases such as amphibole and/or plagioclase that render an interstitial mesostasis. Rocks' textural characteristics, mineral crystallization order and their phase chemistry are all suggestive of low-pressure sub-solidus crystallization in an open system. The low Ti content in augite and scant HFSE abundances suggest the studied rocks may have formed from a depleted mantle source. In addition to the medium to high degree of partial melting of the source, the parental process that gave rise to the Mt. Kalnik ultramafic cumulates also included a low degree of fractional crystallization. The segregation of oxidized Al-chromite and oikocrysts of pargasite and edenite in an early crystallization stage illustrates the formation of a cumulate sequence from volatile-rich magmas. These magmas usually have a high oxidation potential and are exclusively found in intra-oceanic subduction zones, predominantly in island arcs. The overall whole-rock geochemistry e.g. (Nb/La)n = 0.25-0.34; (Ti/Gd)n = 0.49-0.89; (Th/Nb)n = 5.29-8.63; (La/Lu)cn = 0.57-0.68 together with a record of Ca-rich plagioclase (up to An87.4) and low Ti clinopyroxene (≤0.54 wt%) corroborate the supra-subduction tholeiitic nature of the magma source. Ultramafic cumulates from the ophiolitic mélange of Mts. Kalnik and Medvednica show common genetic features and geotectonic provenance. Comparison with analogous ultramafic lithotypes of the north-eastern segment of the ZMTDZ (the Szarvaskö Complex, Hungary), the ultramafic cumulates of Mts. Kalnik and Medvednica portray some subtle differences that may indicate their distinctive geotectonic provenance. Mts. Kalnik and Medvednica ultramafic cumulates represent the vestiges of a single Upper Jurassic intra-oceanic arc system formed in the western branch of the Meliata-Maliak segment of the Neotethyan oceanic realm.
Puran se na širem području Hrvatskog zagorja uzgaja od 16. stoljeća. Nakon otkrića Novog svijeta vjerojatno je iz Srednje Amerike brodovima stigao u Europu, najvjerojatnije u Španjolsku, zatim u ...Englesku pa u Njemačku i Italiju, odakle se proširio i u naše krajeve. S vremenom se udomaćio, nije se križao s drugim pasminama pa je specifičan uzgoj u malim jatima koja su veći dio života provela na otvorenom u prirodi skupljajući hranu uvjetovao razvoj specifičnih morfoloških i fizioloških svojstava. Utjecao je na kvalitetu mesa, po čemu je zagorski puran poznat te se smatra specijalnom pasminom u gospodarskom smislu, a u uz to ima i veliko značenje kao vrijedan element biološke raznolikosti Hrvatske. U prošlosti se ova izvorna pasmina peradi slabo izučavala, tek nešto prije drugog svjetskog rata, iako je tada predstavljala značajan izvozni proizvod tradicionalnog uzgoja u zemlje zapadne Europe. Od drugog svjetskog rata do sredine devedesetih godina prošloga stoljeća zagorski puran gotovo je izumro i nestao. Svojom inicijativom i stručnošću, koncem devedesetih godina prošloga i početkom ovoga stoljeća spasili su ga pojedini entuzijasti i stručnjaci Agronomskog fakulteta u Zagrebu. Od tada se zagorski puran ozbiljnije istražuje, podupire i promovira, iako mu broj jedinki još uvijek varira na godišnjoj razini. U svakom je slučaju spašen, čak je u nekim inicijativama povremeno bio i ozbiljna robna marka kojoj, na kraju se pokazalo, treba stabilnost i kontinuitet uzgoja. Ovaj rad prikazuje stanje i gospodarske perspektive zagorskog purana u Varaždinskoj županiji.
Cilj rada je, u smislu interpretacije duha mjesta (genius loci), interdisciplinarnim
pristupom, prikazati povijest jedne grane obitelji Galjuf, koja je u razdoblju
od druge polovice XVIII. do početka ...XX. st. kao svoje sjedište imala dvorac
Vižovlje, koji se nalazi na zapadnom dijelu Krapinsko-zagorske županije,
nekoliko kilometara sjeverozapadno od Velikoga Trgovišća. U tom smislu, rad se
fokusirao na biografske podatke onih članova obitelji koji su bili vlasnici
dvorca. Problematiziran je i društveno-graditeljski status dvorca, na relaciji
dvorac–kurija, budući da ni stručno-znanstvena literatura nije uspostavila
jasne granice u određenju samih pojmova. Prikazani su osnovni arhitektonski
elementi dvorca, njegove mijene tijekom promatranoga razdoblja, uz osvrt na
sadašnje znanstvene spoznaje o njegovu izgledu temeljem dostupnih povijesnih
izvora. Govoreći o društvenom životu u dvorcu i mijenama koje su pratile
tadašnja društveno-ekonomska kretanja, važan izvor predstavlja Spomen-knjiga
posjetilaca dvorca u Vižovlju, kao jedna od rijetkih sačuvanih spomen-knjiga
zagorskih kurija i dvoraca, a koja je ujedno i paradigmatični prikaz života
zagorskoga sitnog plemstva kraja XVIII. i XIX. st.
The
goal of this paper is to, in way of interpreting the spirit of the place and
using an interdisciplinary approach, present the history of one branch of the
Galjuf family, which was seated at Vižovlje Manor in the west part of the
Krapina-Zagorje County, several kilometers northwest of Veliko Trgovišće. In
this sense, the paper is focused on the biographical data of those family
members who were the owners of the manor. The social-architectural status of
the manor in view of the terms dvorac and kurija is also discussed, since
Croatian professional and scholarly literature has yet to precisely distinguish
the meanings of these terms. The basic architectural elements of the manor are
described, as are the changes during the observed period, with reference to the
current scholarly knowledge about their appearance based on available
historical sources. A significant source on social life in the manor and the
changes that followed the social-economic developments of that time is the
»Spomen-knjiga posjetilaca dvorca u Vižovlju« (Commemorative Visitor Book of
Vižovje Manor), one of the rare preserved commemorative books from a Zagorje
manor. It is also a paradigmatic portrayal of the life of Zagorje’s minor
nobility in the late 18th and the 19th century.
Istraživanje vaskularne flore provedeno je na dijelu južnih padina planine Ivanščice iznad grada Zlatara u listopadu 2022. godine. Zabilježeno je ukupno 85 svojti vaskularne flore unutar 47 porodica. ...S obzirom na broj svojti najzastupljenije su bile porodice Rosaceae, Asteraceae te Aspleniaceae, Fabaceae, Fagaceae i Lamiaceae. Biljne svojte su s obzirom na životni oblik uglavnom hemikriptofiti (35,7 %) i fanerofiti (33,3 %), dok su terofiti najmanje zastupljeni (6,0 %). Na temelju Ellenbergovih indikatorskih vrijednosti zabilježenim vrstama pogoduju staništa umjerene vlažnosti te kisela tla umjereno bogata humusom. Prema Crvenoj knjizi vaskularne flore Hrvatske na istraživanom području rastu jedna osjetljiva (Taxus baccata L.) i jedna gotovo ugrožena vrsta (Cyclamen purpurascens Mill.), a zabilježene su i dvije invazivne vrste (Robinia pesudoacacia L. i Erigeron annuus (L.) Desf). Rezultati ukazuju da su staništa na južnim padinama Ivanščice karakterizirana velikom raznolikošću biljnih vrsta, stoga su u svrhu njihova očuvanja nužna daljnja istraživanja.
The research of vascular flora was conducted on the part of the southern slope of Ivanščica near the town of Zlatar in October 2022. A total of 85 taxa of vascular flora belonging to 47 families were recorded. The most abundant families were Rosaceae, Asteraceae, Aspleniaceae, Fabaceae, Fagaceae and Lamiaceae. According to Ellenberg’s indicator values, specific habitat conditions, characterized by moderately wet and moderately acidic soil with a moderate amount of humus favor the development of different plant life forms. Out of the total recorded plant taxa, hemicryptophytes make up 35.7 %, followed by phanerophytes (33.3 %), while therophytes are the least represented with 6.0 %. According to their status in the Red List of Croatian vascular flora, one vulnerable (Taxus baccata L.) and one nearly threatened (Cyclamen purpurascens Mill.) plant species were found. Two invasive plant species were also recorded (Robinia pesudoacacia L. and Erigeron annuus (L.) Desf). The results indicate that the habitats on the southern slopes of Ivanščica are characterized by great diversity of plant species, therefore further research is necessary for their preservation.
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