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An important area of Antal Grassalkovich I's (1694–1771) art patronage was the erection of ecclesiastic buildings. Máriabesnyő is particularly significant, for it did not only become a popular place of pilgrimage in the region owing to a votive statue, but it also became the burial place of the founder since it was close to his mansion in Gödöllő. A sofar unknown 18th century pictorial source of the Besnyő convent was found in the Capuchin archives in Vienna, which calls for a revision of the building phases of the baroque monastery. The ink and wash drawing by a hand of little talent shows the building complex from two directions on the basis of on-the-spot observation. The monastery was built in three major phases. After the foundation, first the small Loretto Chapel was erected (with the monks' crypt under it) using the mediaeval ruins (1759–1762) together with the dwelling(s) of the hermits, which were either three small hermitages or a part of the groundfloor section of today's western wing. The convent was built on the plans of master builder János Mayrhoffer of Pest in the second phase (1763–1767); its U-shape enclosed a court with the Chapel on the fourth side. The monastery consists of one-storey wings. The oratory is in the southern, the refectory in the eastern wing. On the gable of the southern end of the latter a sun dial was made in 1765 as the Historia Domus registered, on the basis of which the baroque veduta must be dated to 1765/1766 (since the church, the southern corridor and the sacristy are still missing). On the eastern side of the monastery a hanging garden was created with cellars under it. The church with two vault sections and chancel was built on the western side of the Loretto Chapel in 1768–1771 with a portico in front and an undercroft and the crypt of the Grassalkovich family. Mayrhoffer's plan survives in Gyula Wälder's 20th century copy; it contains part of the groundplans of the three levels. The Historia Domus claims that a painter of Pest Ferenc Winkler painted a picture of the Virgin of Besnyő for the cloisters, and he is named as the decorator of the corner tower at the southeastern end of the hanging garden.

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Acta Geologica Hungarica
Authors: Tibor Zelenka, Endre Balázs, Kadosa Balogh, János Kiss, and at. al.

Surface Neogene volcanics in Hungary are abundantly documented in the literature, but buried volcanic structures are little known. Early burial of the volcanic centers beneath latest Miocene to Pliocene sediments preserved much of their original relief, permitting their classification into genetic types. More than two-thirds of Hungary is covered by thick Neogene and Quaternary sediments, below which buried volcanic eruptive centers and the extent of their products may only be recognized by complex geologic-geophysical methods. Our study is based on the data of several thousand wells, more than 60,000 km of seismic sections, as well as airborne and surface geophysical (gravimetric, magnetic, electromagnetic, radiometric) data. Results of chemical, mineralogical studies and K/Ar dating of deep cores were also included. The data were evaluated in terms of the regional deep structure of the Carpathian-Balkan region, the Miocene evolution of which was determined by the position, movement and welding of individual microplates. Integration of all available data reveals that the Miocene volcanic centers are concentrated near microplate boundaries. In the volcanic centers the lavas and pyroclastic deposits far exceed 50 m in thickness. The data show that the buried volcanic rocks below the Transdanubian region (Little Hungarian Plain and Somogy-Baranya Hills), the Danube-Tisza Interfluve and the Great Hungarian Plain extend over a much larger area than do the outcropping volcanoes in Northern Hungary (from the Visegrád to the Tokaj Mts). In the southern part of Transdanubia (W. Hungary) a major calcalkaline, rhyolitic, ignimbritic event took place early, in Eggenburgian and Ottnangian (Early Miocene) times. The centers and tuff sheets of this volcanic event can be traced from the Mecsek Mts to the Salgótarján Basin, the southwestern Bükk Basin and the central part of the Great Hungarian Plain. This event was followed by andesitic volcanism. The rhyolite and dacite volcanic centers of Karpatian age are predominantly situated in Transdanubia, whereas the Badenian (Mid-Miocene) andesite and dacite series of large stratovolcanoes are buried below southern Transdanubia, the Danube-Tisza Interfluve and the Great Hungarian Plain. In Sarmatian and early Pannonian (Late Miocene) times, pyroclastic sheets several thousand meters thick and lava domes were formed; they are predominantly rhyolitic, subordinately andesitic and dacitic, and are situated in the eastern part of the Great Hungarian Plain (Nyírség).  With the end of microplate motion, as the plate consolidated in the late Miocene, thick but areally restricted alkali-trachite (Little Hungarian Plain) and alkali-basalt lava domes and tuff craters formed in the Little Hungarian Plain, Transdanubia and the Danube-Tisza Interfluve.

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The burial site and fragments of the tomb of Queen Gertrude of Andechs-Meran, first wife of King Andrew II (1205–1235) and a victim of assassination in 1213, were discovered during the excavations carried out in the Cistercian church of Pilis between 1967 and 1982. Her tomb was found along the central axis of the church, in the crossing. The present study, which includes the complete catalogue of the known fragments, attempts to establish the typology, iconography, and stylistic context of the artwork. New reconstructions are proposed for the two short sides of the sarcophagus-shaped tomb, which each bore distinct forms: one contained a wide, shallow niche, while the other depicted two standing figures under a double arcade. The figural ornaments on the sides of the tomb and the gisant with angels on the lid occupy an important place in the history of funerary art. In fact, the tomb displays one of the first examples of this type of decoration. The seated figures on the side relief probably represent the choir of saints in heaven, who provided companionship for the soul of the deceased queen. Gertrude herself is represented not only on top of the tomb, but also appears as a donor in one of the reliefs.

Stylistic analysis of the figures proves that their master came from the workshop responsible for the Last Judgment and Callixtus portals of the cathedral of Reims. He must have left the workshop around 1220, before the portals were completed and installed in the façade of the northern transept. At about this time, Villard de Honnecourt also embarked on his travels that took him from Reims to Hungary. The style of Gertrude’s tomb bears similarities to the Villard’s drawings, even if we do not wish to attribute the sculptures to him. A team of masons from Reims also arrived in Pannonhalma during this time frame and worked on the abbey church there. Their most important work in Pannonhalma is the southern portal of the new church, the Porta Speciosa. The complicated nature of these construction histories reminds us of the need for caution when attributing one work of art to one person.

Both Gertrude’s tomb and the Porta Speciosa are prime examples of the cultural and artistic period that began in the late 12th century, when the Kingdom of Hungary was a leader in the region in the reception of French Gothic.

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A magyar jogban a halottakon végezhető, de nem temetési beavatkozásokról csak az egészségügyi jog szól, így egyéb tudományos célú vizsgálatok sem lennének elvileg lehetségesek. Ebben kizárólag a nemzetközi múzeumi etikai kódex érvényesül. Sok kultúra ezt halottgyalázásnak tekinti. A halottgyalázás kriminális formáin túl az orvosi eljárás (kutatás és gyakorlás) is alkalmas lehet arra, hogy a holttest méltóságának sérelmét jelentse. Ennek ellensúlyozása, hogy a post mortem beavatkozásokhoz az érintett vagy hozzátartozói beleegyezése szükséges. A dolgozat a magyar szabályozást mutatja be, amelyben a halottat betegnek tekintjük, a holttest vonatkozásában a betegjogok speciális érvényesülése történik. A jog a boncolást illetően számos jogot ad a hozzátartozónak, és az anatómiai oktatást is szabályozza. A szervnyerés során az opting-out elvét érvényesíti, tiltakozást csak a betegtől fogad el. Szigorúan védi az elhunyt egészségügyi adatait, de nem korlátozza a hozzátartozók érdekérvényesítését. A képzés és továbbképzés csekély figyelmet fordít ezekre a kérdésekre, a szabályozás pedig nem felel meg a jelenkor elvárásainak és lehetőségeinek, ezért célszerű lenne újragondolni a probléma teljes spektrumát. Orv. Hetil., 2012, 153, 330–338.

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4291/2010. számú ügyben.] [Hungarian] 8 Government decree No. 145/1999 (X. 1.) regarding law No. 43 of 1999 on cemeteries and on burial procedures

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. Gargett, R. H. (1989) Grave shortcomings: The evidence for Neanderthal burial. Current Anthropology , 30, 157-190. Grave shortcomings: The evidence for Neanderthal burial. Current Anthropology

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, A., Wall, S. and Westberg, M. (2014): Lichens from the Vadstena Monastery churchyard — the burial place of Erik Acharius. — Graphis Scripta 26 (1–2): 34–39. Westberg M. Lichens

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, J. (1971): Greek Burial Customs. London. Greek Burial Customs. Naber, S. A. (1983): Observationes criticae in Aristophanem

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Painted dedication to Genius and a relief depicting aquila from a sanctuary in Sopianae

(Appendix to the study: Painted depiction of Genius of Sopianae by Anita Kirchhof)

Acta Archaeologica Academiae Scientiarum Hungaricae
Authors: Boglárka Fábián and Ádám Szabó

burials: the II burial chamber)] SpecN 20 ( 2006 ) 49 – 102 . UbiEratLupa = O. Harl – F. Harl : Forschungsgesellschaft Wiener Stadtarchäologie . Datenbank zur Erfassung römischer Steindenkmäler: Vámos 2008 = P. Vámos

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Arias-Garralda 1996 = P. Arias— M. D. Garralda : Mesolithic burials in Los Canes cave (Asturias, Spain). Human Evolution 11 (1996) 129–138. Garralda M

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