bluuebunny/crossref_metadata_2025_split huggingface dataset:
Því flýgur krákan víða
Authors: Halldórsson Ólafur 
Published: March 2024

In the Arnamagnean Collection in Copenhagen there are two vellum leaves, AM 687b 4to, the remnants of a book of song (free organum for 2 and 3 voices). The manuscript is written by an Icelander. Its first known owner was Porleifur Bjornsson, minister at Reykhólar (16th century). Fol. lv—2v contain scores, but on Fol. lr there are eight riddles, three verses and one Pula (fragment?), written in the 16th century. These rhymes are printed here in orthography of the manuscript, but riddles nr.1—7 have previously been printed (inexactly) from a copy by Hallgrímur Scheving (JS 289 8vo) in Islenzkar gátur (Icelandic Riddles), collected by Jón Árnason, Copenhagen 1887, and riddle nr. 4 also in Almanak hins íslenzka pjóðvinafelags 1876.It is clear from errors owing to misreadings that the writer of 687b has copied the riddles from a book, and from the beginnings of nr. 6: Hverr er sá inn priði (Who is the third one), nr. 7: Hverr er sá inn ellejti (Who is the eleventh one) and nr. 8: Mggr er sá inn nítiándi (The nineteenth is a son) it may be deduced that they come from a collection of riddles. The riddles are in the Ijóðaháttr metre but the lines are unusually long and all the stanzas are more than 6 lines (9, 12 and 15). They contain a few words that are either rare or otherwise unknown in Icelandic and a few with unusual meanings: 2.9 rauf, fem. ó-stem, used tomean the same as Da. røv, Sw. rov. — 2.10 hjassi, masc. an-stem, meaning the same as Da. isse, Sw. hjásse; this is also found in rímur. — 3.7 sauðafeitt, where feitt is obviously the same as Da. fat, Sw. Dial. fatt, Old Sw. ulla fætter, ought to be "'fætt in Icelandic, here used to mean uncombed wool or a sheep's woolen coat. — 4.6 knapaldr, neutr., unknown from other sources, here probably used for a block of wood. — 6.2 pari (or parri), masc. an-stem, the same as Sw. tarre. — 8.4 vígnýra, neutr., thesame word as Old Gotlandic 'vigniauri', i. e. testicle. The solution of the riddles is: No. 1: a steelyard. — No. 2: a mouldfor forging nails. — No. 3: wool combs. — No. 4: a footstool. — No. 5: a pot-hook. — No. 6: a bell clapper. — No. 7: a fish-hook, probably one with a bent stem. — No. 8: a stalk of angelica. Dating the riddles is problematic, but in all probability they are fromthe 12th or 13th century. They have probably been written down in the same place as the verses, which are of different ages, no. 9 probably oldest and no. 12 youngest. East Nordic words suggest that the riddles have not been composed in Iceland and che verses are obviously not Icelandic. The author does not feel competent to pronounce whether the riddles and the verses were composed in the eastern part of Norway, or perhaps in Sweden. In the above-mentioned work by Jón Árnason the riddles no. 1060, 535 and 777 are orally transmitted fragments derived from the riddles here numbered 3, 5 and 8.
Um hljóðdvöl í íslenzku
Authors: Sigmundsson Svavar 
Published: March 2024

Previously it was believed that Jón Arason (died 1550) was the last Icelandic poet to observe the old rules of quantity, but Stefán Karlsson has pointed out that as late as 1643 poetry was being written in the old manner.
The difference in length between í and i, for example, was secondary, the main difference being that í was tense, whereas i was lax. The first stage in this development was that + tense: -r tense lost its significance, and + length: -j- length became the deciding factor both for the old lax vowels and all diphthongs. In modern Icelandic there is no phonetic difference between long and short vowels, whereas such a difference does exist in modern Faroese.
In Icelandic diplomas from ca. 1300—1450 there are many examples of doubled intervocalic consonants, mostly following a lax vowel (for example sammann), and following diphthongs, most often ei (nteittaði); the same phenomenon is present in Norwegian diplomas from the same time, although in the Icelandic // appears only sproradically for / (Steffán), whereas the Norwegian has many examples of this. In the oldest of these diplomas there are also many examples of uncertainty as to whether the tensity of a vowel should be indicated by doubling it or by adding a diacritical mark over it, and in the case of the length of a consonant, whether to double it: máálum, naat, setu, snori, aara instead of málum, nátt, settu, Snorri, Ara. Examples of this uncertainty also occur in modern Icelandic (orusta : orrusta). Diphthongization of e began already in the 13th century, that of <* around 1400, whereas diphthongization of á and ó \s not observed in writing before the 15th and 16th centuries. At the same time, or perhaps somewhat later, lax vowels became long before short consonants. The unstressed vowels i and u were first written e and o, since they corresponded to e and 6. When e became a diphthong, i was written when unstressed, and by analogy, u. Somewhat different was the development of foreign loanwords: Ádam and (.va. Delabialization of y and ý is more recent, beginning around or after 1500, but examples of a difference between y and i are still to be found in the ballad book of Gissur Sveinsson (born 1604). Delabialization of y in the diphthong ey, however, began already in the first half of the 14th century. The corresponding development in the other Scandinavian languages is also mentioned.
Seismic Measurements on The Faeroe Island, 1970
Authors: Casten Uwe 
Published: March 2024

Skjálvtafrøðiligar dýpdarkanningar vóru gjørdar í samvinnu við laarda háskúlan í Hambung (Institut fiir die Physik des Erdkórpers) á rygginum millum Føroya og íslands í døgunum 9. til 14. juli 1970. Við tveggja-skipaháttinum vóru skjálvtafrøðiligar afturvarp- og brotmátingar gjørdar á sjónum. 1 Streymoy fylgdu 4 landstøðir við spreingingunum á sjónum. Uppsetingar av skjálvtaritunum frá landstøð nr. 2 eru sýndar. Einans ein Lind kundi verða rannsakað við at bera saman skjálvtafrøðiligu viðburðirnar. Snarleikin 6,1 (5,6 • 5,7) km/s er ein P^bylgjiu-snarleiiki og 3,4 km/s ein S-bylgju-snarleiki. Teir eru at vísa seg snarleikar hjá undirstøðinum undir basaltgrýti Føroya.
Fólkanøvn í Norðoya sýslu 1801
Authors: Jákupsstovu Jákup í 
Published: March 2024

I seinastu grein (Fólkanøvn í Eysturoyar sýslu 1801. Fróðskaparrit 19. bók, 1971) varð gjørt upp, at hagartil vóru kannað nøvn á 4.620 fólkum av landsins íbúgvatali 1801 tilsamans 5.265 fólkum
»Tey írestandi 645 fólk verða at f inna í Norðoya sýslu....«
Hetta er kortini lættari sagt enn gjørt. Anton Degn skjalavørður endar sítt avrit av manntalslistanum fyri Norðoya sýslu við hesum dómi: »De daarligst og mest ufuldstændigt affattede af alle Folketællingslisterne 1801«, og í hesum eigur hann allan rætt.
Mórena á Borðoyarvík, súm bendir á eitt millumbil í glersetingini har norðuri
Authors: Rasmussen Jóannes 
Published: March 2024

The present article deals wlth a glaoial deposit facing the coast of Borðoyarvík near Klakksvík. The deposit consists of till, separated into an upper and a lower part by intercalated, thin lenticular layers of fine, slightly stratified, firm clay or sand. The upper till frequently contains shingle and pebbles which are not to be seen in the lower till. The intercalated clay bed contains remnants of wood, probably driftwood (Picea or Larix). Furthermore there are marane diatoms (Paralia), pollen of Empetrumand Gramineae in great number, some pollen grains of birch and a few pollen grains of pine and hazel. The wood has been radiocarbon dated to > 30.000 years. The upper till shows a retreat and later advance of the ice front. The clay bed, probably of interglacial origin, is secondarily deposited.
Glacial striae, roches moutonnees and ice movements on Suðuroy (Faeroe Islands)
Authors: Jørgensen Gunni , Rasmussen Jóannes 
Published: March 2024

Flestar ritgerðir um glersetingarjarðfrøði Føroya eru frá seinastu øld. Hildið verður at Føroyar vóru eitt glersetingarøki fyri seg, tí ísskøvur og seyðagrót vísa út í allar ættir, og einki ísborið fremmant grót er funnið í oyggjunum. ísskøvur eru ikki sæddar oman fyri 500 m og gitt varð ti, at ísurin hevði ikki rokkið longri upp. Kanningar seinastu árini hava víst, at ísurin í landsynning úr Føroyum hevur ligið um allan landgrunnin.
Greinin snýr seg um kanningar av ísgongdini í Suðuroy. Skøvut hella (ísskøvur) og avbrýndur klettur (seyðagrót) eru merkieftir ísi, har hann er farin um eitt landslag. ísgongdin í Suðuroy er vorðin kannað við at geva hesum merkjum gætur, og eru tær einstøku eygleiðingarnar av ísskøvum og seyðagróti settar upp í yvirliti. Ættin, sum nevnd er í sambandi við seyðgrót, er tann ættin, ísurin er gingin í. Úrslitið av kanningunum er, at Suðuroyggin í hvussu so er í seinastu ístíð hevur verið egið glersetingarøki, og at meginísmarkið, markið miilum ísin, sum gekk vestureftir og ísin sum gekk eystureftir, hevur ligið nær útímóti vesturstrondini. ísmarkið hevur ligið eitt sindur eystan fyrí vatnsmarkið, ið nú er; tað er á kortinum avmerkt sum feit reyð strika og ørvar vísa ísgongdina báðar vegir. Merki eftir aðrari ísgongd — frá einari eldri istíð — eru ikki sædd; tað verður tí hildið at ísurin gjøgnum alla ísøldina er farin um eitt landslag, sum líkt var landslagnum nú er. Sjá annars hjálagda kort yvir ísgongdina í Suðuroy.
Bygdekirken pá Færøyene sett fra Norge
Authors: Christie Håkon 
Published: March 2024

Víst hevur verið á, at føroyska bygdakirkjan í sniði minnir nógv um langkirkjur úr gróti, sum gjørdust rættuliga vanligar í Noregi eftir 1250. Múrurin og sóknarkirkjan í Kirkjubø eru av hesum slagi. Langkirkjur finnast sostatt í Føroyum í miðøld, men sambandið millum hesar kírkjur úr 13. øld og bygdakirkjurnar úr 19. øld er ikki eyðsæð. Rannsakaðu kirkjutoftirnar á Sandi vísató á hetta sambandið. Meðan báðar tær elstu kirkjurnar hava smalri kór, er triðja kirkjan úr seinmiðøld ein langkirkja við javnbreiðum kóri og kirkjurúmi. Á Sandi sæst siðurin at byggja langkirkjur úr viði sostatt at stava frá einum tíðarskeiði, tá enn var vanligt í Noregi at byggja slíkar kirkjur úr gróti. Í Noregi vórðu eisini langkirkjur úr viði bygdar í miðøld, og skilliga við grótkirkjunum sum fyrimynd. Hóast føroyska bygdakirkjan í byggihátti er skyld við norsku stavkirkjurnar, eru sermerki hennara runnin úr øðrum byggisiðum.
The autumn migration at Akraberg, Faroe Islands, 1982
Authors: Bloch Dorete , Sørensen Søren 
Published: March 2024

í tíðarskeiðinum 17/9 - 11/10 1982 varð roynd gjørd at hava fuglakanningarstøð á vitanum á Akrabergi (Mynd 1-4) við 1 eygleiðara. í hesum tíðarbili vórðu sædd 101 sløg (App. 1). Eygleiddir vórðu fuglar, ið ferðaðust um hav og land, og eisini fuglar, sum støðgaðu á. Av sjófugli, ið regluliga flytur um okkara leiðir, var mest til av havhesti (í mesta lagi sæddir 18.000/tíma), næst var rita (2000/tíma) og súla (50/tíma), App. 1). Allir kjógvarnir og serstakliga nakað av dimmum havskrápi sóust á havætt. Smáflokkar av ymiskum gásasløgum og somuleiðis smyril vórðu sæddir (Talva 4). Av vaðfugli var bara tjaldursgrælingur í meingi (Talva 5). Av smáfugli vóru títlingur og grátítlingur teir, ið mest var til av (Mynd 6), meðan talið av steinstólpu minkaði, sum frá leið (Mynd 7). Helmingurin av teimum sæddu sløgunum verður hildin at vera fuglar, ið bendir eru av leið úr Skandinavia, Stóra Bretlandi, og sløg, ið búleika eystari á (Mynd 8-9). Av eysturlendskum sløgum sóust m.o. reyðtítlingur (nýtt slag), dvørgspurvur (nýtt slag), ural-ljómari (App. 2). Tað, ið rakt varð við av fugli á Akrabergi, samsvaraði væl við tað, ið sást á Fair Isle sama tíðarskeið. Av hesum sæst, at Akraberg er eitt sera væl hóskandi stað at hava fuglastøð á.
Vágamálføri
Authors: Petersen Hjalmar P. 
Published: March 2024

The dialect of Vágar and Mykines (hence VM) is spoken on the westernmost islands of the Faroc Islands. Earlier works on dialects - e.g.- Fterøsk Anthologi (1891) - regard it as a part of the dialect in Suðurstreymoy. In my opinion it better taken as a genuine dialect. The reasons are: diftongization and glide insertion in the structures 1) a/æ-a > ei:a (hagan), 2) ú-a > áu-a (fáa)and3)ø-a>>'w:-a(kvøða).(The IPA script is used in the article itself). Some other minor phonological features speak against grouping VM with Suðurstreymoy, especially the pronunciation of Old Norse ó as /eu:/ rather than /áu:/ as in Suðurstreymoy. More important - together with the diftongization an glide insertion - is, that VM has one special intonation sct called drynjing.The tone of a word at the end of a phrase is approximately as high as the tone on the following syllable. This intonation set has although nothing to do with the musical accent in Norwegian, Swedish and in Danish dialects. The drynjing is one of the reasons for very clearly articulated vowels at theend of a word. This has, in turn influence on the morphology, compare Suðurstreymoy ein stórir vinir (nom. sg. mask.), tann góðe vinirin (nom. sg. mask.), leir góðe vinirnir (nom., akk. pl. mask.), eg vende (pret. 1. p. sg. ind.) vit vende (pret. 1. p. pl. ind.) and Vágar/Mykines ein stórur vinur, tann góói vinurin, teir góðu vinirnir, eg vendi, vit vendu. VM and Suðurstreymoy has thus different ways of expressing the content of some bound morphemes. Thedialect of Vágar and Mykines do not soften plosives between vowels and at the end of a word as in Suðurstreymoy, e.g. VM tak(a): Suðurstreymoy tag(a). Wíthin the area there are no mentionable differences, and the only change I have observed is that the younger generation do not have glide insertion and diftongization in word of the kvøða-typc. Older texts (Svabo towards the end of 1800) fails to quote this diftongization and in the fúa-type. There is a possibility, that they were not presentin the dialect at that time, but Svabo also fails to quote diftongization in words of the hagan-type. It is only seen in hypercorrect writing with original Faroes ey /ey) form Old Norse au. This makes you think, that he deliberately is avoiding all.the diftongizations whatever his reasons may be. One observation I made, listening to the tapes, was a spirant g in lagdur. This can be the ON pronunciation of the g-sound in a protected phonological environment an just in one family, or an innovation. Following the development of the dialect from Svabo until today, there are rather few changes in morphology and phonology. One change seen durng the last years in VM is when youngsters confuse nom. and akk. pl. definite eg sú bátarnar > eg sá bátarnir. This can be due to radio and television, which is very mush under influence of the Suðurstreymoy dialect, or just an inner change taking place in the morphology, so that the system gets »simpler«.
Holocene Tephra Layers in the Faroe Islands
Authors: Dugmore Andrew J. , Newton Anthony J. 
Published: March 2024

Evidence of at least five silicic and one basaltic tephra layers of Holocene age have been found in the Faroe Islands. All these tephras are likely to have originated in Iceland. In addition, historical records suggest fallout may have occurred after three recent eruptions of Katla in 1625 AD, 1660 AD, 1755 AD, but this has yet to be confirmed with finds of tephra. The one basaltic layer currently known in Faroe is called the Saksunarvatn tephra, and was deposited about 9100 BP. It forms an important regional isochrone, that is present throughout the north-east Atlantic region. We report new geochemical data on the Saksunarvatn tephra from the type site, and an older silicic tephra designated L3574. While the identity of the two youngest Holocene silicic tephras found in Faroe remains uncertain, we present geochemical data on two mid-Holocene silicic tephras which identifies them as the Icelandic tephras H-4 (3800 BP) and H-S (3500 BP).
Heltn
Authors: Weyhe Eivind 
Published: March 2024

Úrtak
Orðið heltn er ikki til sum felagsnavn í nútíðar føroyskum. Men tað er varðveitt sum navnliður í føroyskum staðanøvnum. Í greinini verður víst á, hvar í landinum navnið finst, og hvørjar formar tað kann hava. Borið verður saman við fornnorrønt, norskt og íslendskt, og ljóðligar og formligar málbroytingar verða umrøddar.
Abstract
In modern Faroese the word heltn does not exist as a common noun. It is however preserved as an element in Faroese placenames. The article indicates where in the Faroes the name is to be found and the different forms it can take. Comparison is made with Old Norse, Norwegian and Icelandic, and phonetic as well as morphological changes are discussed.
Constructing identities in children’s cultures of consumption
Authors: Hayfield Erica A. , Davies John , Marsden David 
Published: March 2024

Úrtak
Børn í vesturheiminum, eisini í føroyum, gerast meira og meira framkomin og vand sum brúkarar. Kortini er vitanin um, hvussu børn sjálv uppliva og samskifta umnýtslu í teirra mentanum, sera avmarkað. Hetta er fyrst og fremst orsakað av, at tað er sjón ar horn ið hjá teimum vaksnu, sum er grundarlagið, tá ið børn verða granskað. Í hesari grein verður tískil roynt at lýsa úr sjónarhorninum hjá børnum, hvønn leiklut nýtsla hevur, tá ið samleikin hjá børnum verður skapaður. Greinin hevurstøði í einari etnografiskari kanning, sum varð gjørd í Skotlandi, og úrslitini verða nýtt til at vísa á øki sum kundi verið áhugaverd at granska í Føroyum.
Abstract
Children in the Western world, including the Faroe Islands, are increasingly sophisticated consumers. Yet, little is known about how children themselves experience and mediate consumption in their cultures. The reason for this is primarily grounded in the adult-centric approach which has traditionally been applied in research with children. Therefore, this paper attempts tounderstand what role consumption plays in the con struction of identity among children from a child-centric perspective. The paper draws on an ethnographic study conducted in Scotland and uses these findings to map out some areas which usefully could be explored in the Faroese context.
Solitary ascidians (Tunicata, Ascidiacea and Sorberacea) of the Faroes
Authors: Ámundur  
Published: March 2024

Úrtak
Allir teir støku sjóbjølgarnir, sum vóru innsavnaðir undir BIOFAR-verkætlanini eru rannsakaðir og navngreindir til lægstu møguligu flokkingarskipan. Innan BIOFAR verkætlanin byrjaði í 1987, vóru 24 sløg av stakum sjóbjølg um staðfest innan fyri 200 fjórðinga sjómarkið. Eftir BIOFAR er talið økt til 36. Stakir sjóbjølgar eru staðfestir í 17 prosent av støðunum (225 av tilsamans1325). Tólv eru staðfestir fyri fyrstu ferð: Ascidia mentula Müller, 1776, Styela atlantica (Van Name, 1912), Styela similis Monniot, 1970, Styela theeli Ärnbäck-Christie-Linde, 1921, Cnemidocarpa mollispina Ärnbäck-Christie-Linde, 1922, Cnemi do carpamortenseni Hartmeyer, 1912, Polycarpa porculus Monniot C. and Monniot F., 1979, Molgula herdmani Bjerkan, 1905, Molgula mira (Ärnbäck, 1931), Molgula occulta Kuppfer, 1875, Eugyra islandica Millar, 1974, og Asajirus arcticus (Hartmeyer, 1923). Slektirnar Cnemidocarpa og Asajirus eru staðfestar fyri fyrstu ferð á økinum.
Abstract
All the solitary ascidian material collected during the BIOFAR programme has been worked through and identified to lowest possibly taxomomic level. Before the BIOFAR programme star ted in 1987, twenty four solitary ascidian species had been recorded within the Faroese Exclusive Eco nomic Zone (EEZ). The BIOFAR sampling has in creased this number to thirty six. Solitary ascidians are recorded at 17% of the stations (225 out of 1325). Twelve species were recorded for the first time:Ascidia mentula Müller, 1776; Styela atlantica (Van Name, 1912); Styela similis Monniot, 1970; Styela theeli Ärnbäck-Christie-Linde, 1921; Cnemidocarpa mollispina Ärnbäck-Christie-Linde, 1922; Cnemidocarpa mortenseni Hartmeyer, 1912; Polycarpa porculus Monniot C. and Monniot F., 1979; Molgula herdmani Bjerkan, 1905; Molgula mira (Ärnbäck, 1931); Molgulaocculta Kuppfer, 1875; Eugyra islandica Millar, 1974; and Asajirus arcticus (Hartmeyer, 1923). Two genera, Cnemidocarpa and Asajirus, are recorded for the first time in the area.
Distribution of Woodlice (Isopoda: Oniscoidea) in the Faroe Islands
Authors: Hansen Janus , Jensen Jens-Kjeld 
Published: March 2024

Úrtak
Fýra sløg av gráum undir steini eru staðfest í Føroyum: Trichoniscus pusillus Brandt, 1833, Ligia oceanica (Linnaeus, 1767), Oniscus asellus Linnaeus, 1758 og Porcellio scaber Latreille, 1804. Í hesari kanning varð einki nýtt slag funnið. Á 48 støðum vórðu grá undir steini staðfest fyri fyrstu ferð, so saman við eldri kanningum eru tey nú staðfest á 59 støðum tilsamans.Hesi støð eru sett á kort. Orðskift verður um útbreiðsluna.
Abstract
A survey of woodlice has been conducted. Species found were: Trichoniscus pusillus Brandt, 1833, Ligia oceanica, Oniscus asellus Linnaeus, 1758 and Porcellio scaber Latreille, 1804, and no new species were found. We were able to document the presence of woodlice in 48 new locations, bringing the total to 59. The distribution found is discussed.
COVID-19 Awareness, Overview of Vaccines and Method of Medical Education Among Medical Faculty Students
Authors: KARATAŞ Mehmet , HEPKARŞI Sevinç , ÖZTÜRK Çağlanur 
Published: March 2024

Background: Medical faculty students symbolize a significant part of the health-care society and are remarkable members of the coronavirus disease 2019 (COVID-19) pandemic to response.
Aims: This study aimed to evaluate various factors associated with COVID-19 awareness, vaccine, and medical education during the pandemic among medical faculty students via surveys.
Study design: We conducted a prospective cross-sectional survey study about masks, distance and hygiene awareness, COVID-19 vaccination, and methods of medical education with medical faculty students (MFS).
Methods: A total of 322 medical faculty students answered the questionnaire forms. The questionnaire collected socio-demographic characteristics, COVID-19 Awareness, general willingness, attitude toward vaccination, and attitude toward educational models.
Results: The total awareness score (79.53±27.45) was determined as a high level of awareness among the participants. 4th grade MFS were found to be more sensitive to mask, hygiene, and total score awareness than in the 2nd grade (p= 0.03, p=0.006). There were no statistically significant differences between educational grades in general willingness and attitude towards vaccination. It was determined that the medical students in the last 3 years wanted face-to-face education statistically more than the MFS in the first 3 years (p=0.00).
Conclusion: The vast majority of the participants had a high level of knowledge about COVID-19. The majority of the study population is willing to be vaccinated whereas some populations are hesitant about vaccination. This information may be used in future immunization strategies to increase the vaccination rates and which educational methods to choose among this group of future medical professionals.
İbn-i Sînâ’nın El-Kânûn Fi’t-Tıbb Eserinde Ossa Cranii (Kafa Kemikleri)
Authors: ÖZDEN Hilmi , ORTADEVECİ Abdullah , AKBAŞ Yadigar 
Published: March 2024

Onuncu ve on birinci yüzyıllarda yaşamış Müslüman Türk ilim adamı olan İbn-i Sînâ dünya tıp tarihinde önemli bir yere sahiptir. Modern tıbbın temelleri de onun eserleri üzerine atılmıştır. İbn-i Sînâ’nın eserleri İslam dünyası ve Avrupa tıp tarihinde 11-17. yüzyıllar arasında çok etkili olmuştur. Avrupa’daki tıp alanındaki bilimsel gelişmeler ve tıp faaliyetleri İbn-i Sînâ'nın çalışmaları üzerinden hareket etmiştir. Yahut onun yoğun etkisi altında kalmıştır. En önemli eseri El-Kanun fi’t-Tıbb’da anatomiye ait birçok değerli bilgi bulunmaktadır.
Bu araştırmada İbn-i Sînâ'nın El-Kanun fi’t-Tıbb adlı eserinin anatomi bölümündeki kafa kemikleri incelenecektir. El-Kanun fi’t-Tıbb çevirisinde ise Osmanlı döneminde yapılan Tokadî Mustafa Efendi ile Cumhuriyet döneminde Esin Kahya’nın çalışmaları esas alınmıştır.