Ankole Folk Tales

Africa ◽  
1951 ◽  
Vol 21 (1) ◽  
pp. 32-40 ◽  
Author(s):  
F. Lukyn Williams

Opening ParagraphAnkole is a district in the south-west of the Uganda Protectorate. Its inhabitants, as a result of fifty years of British administration, are being gradually welded together into one people, the Banyankole. There are, however, two distinct ethnic groups in the country: the Bantu aborigines who till the soil and the cattlekeeping Bahima. The latter were Hamitic invaders from the north, who brought with them their own long-horned cattle, easily distinguishable from the small shorthorned zebu type found already in the country. Their one aim in life was and is the well-being of their herds.

Africa ◽  
1958 ◽  
Vol 28 (2) ◽  
pp. 135-147
Author(s):  
Wolf Leslau

Opening ParagraphMoča is a dialect of the Kafa cluster, in the south-west of Ethiopia. It is spoken in the province of Ilubabor, to the west of Kafa, extending north across the river Baro. The language is called Šäkka by the Moča themselves; the term Moča is used by the Galla and by the Europeans.The dialects of the Kafa cluster are: Kafa spoken in the province of Kafa, between the rivers Omo and Goǧeb to the north and the Gimira tribes to the south; Boša (or Garo) spoken to the north of the river Goǧeb, and west of Omo; and Moča.


2020 ◽  
Vol 35 (2) ◽  
pp. 386-394
Author(s):  
O. M. Kazymir ◽  
I. A. Hotun

The excavations headed by O. P. Motsa of the settlement on the bank of the river Nyvka in Sofiivska Borshchahivka in the western suburb of Kiev provided the representative collection, containing a number of items, quite rare, and even unique in the South Rus lands. One of them is the bronze pin with a total length of about 10 cm casted in two-sided form with a top in the form of duck. The researchers consider the pins, as a part of the costume, attributed to the Baltic and Finnish-Ugric population, which surrounded the North Rus lands and partially was a part of the Old Rus state. Initially, through contacts with the latter, these items got to Novgorod and other destinations (in Chersonese, for example, according to experts, such things serve as an indicator of ties with suppliers of northern fur). The pin from the Sofiyivska Borshchahivka settlement obviously represents a further development of the shape of these decorations: in its upper part above three petals with inserted rings there is a three-dimensional figure of a duck with its head pointing back. Analysis of literature allows trace the usage of a small group of similar ear-picks and pins with figures of a rooster, a dog etc. — species that have long been valued by various ethnic groups. The decoration from Sofiyivska Borshchahivka reflects the level of development of medieval metal-plastics, shows the cultural ties (especially along with other items presented on the site which tend to the specified region), acts as an indicator of both the high well-being of the population of medieval settlement structures and not yet exhausted information opportunities of the latter.


1969 ◽  
Vol 32 (3) ◽  
pp. 496-526 ◽  
Author(s):  
H. T. Norris

The gibla, the south-west of Mauritania, is a monotonous region of gum acacia trees, baobabs, ‘dead’ dunes, and hillocks. This ‘backwood’ is the last refuge of Znāga Berber, once spoken far to the north in whole regions of the Western Sahara. A number of short poems, a cycle of folk-tales, and a handful of masterpieces of extended odes in praise of the Prophet—some 200 years old and written in Arabic script—this is the meagre literary legacy of a proud and cherished tradition.


1932 ◽  
Vol 69 (5) ◽  
pp. 209-233 ◽  
Author(s):  
G. D. Osborne

THE Carlingford-Barnave district falls within the boundaries of Sheet 71 of the Ordnance Survey of Ireland, and forms part of a broad promontory lying between Carlingford Lough on the north-east and Dundalk Bay on the south-west. The greater part of this promontory is made up of an igneous complex of Tertiary age which has invaded the Silurian slates and quartzites and the Carboniferous Limestone Series. This complex has not yet been investigated in detail, but for the purposes of the present paper certain references to it are necessary, and these are made below. The prevalence of hybrid-relations and contamination-effects between the basic and acid igneous rocks of the region is a very marked feature, and because of this it has been difficult at times to decide which types have been responsible for the various stages of the metamorphism.


1907 ◽  
Vol 7 (1) ◽  
pp. 22-31 ◽  
Author(s):  
R. Tanner Hewlett ◽  
George S. Barton

In view of the importance of a pure milk supply, we considered that it might be of interest to examine chemically, microscopically, and bacteriologically, a number of specimens of milk coming into the Metropolis for which purpose we decided to select samples from the various counties, the milk of which is consigned to London. We found that milk so consigned comes from about twenty-six counties extending from Derby in the North, to Hampshire and Devonshire in the South and South-West, and from Hereford in the West, to Norfolk in the East.


1954 ◽  
Vol 49 ◽  
pp. 267-291
Author(s):  
Elizabeth B. Wace

The Cyclopean Terrace Building lies to the north-west of the Lion Gate on the northern end of the Panagia Ridge and faces almost due west across the valley of the Kephissos and modern main road from Corinth to Argos. It lies just below the 200 m. contour line, and one terrace below the houses excavated in 1950–51 by Dr. Papadimitriou and Mr. Petsas to the east at the same end of the ridge. The area contains a complex of buildings, both successive and contemporary, and in view of the discovery of structures both to the south-west and, by the Greek Archaeological Service, to the north-east it is likely that this whole slope was covered by a portion of the outer town of Mycenae. This report will deal only with the structure to which the name Cyclopean Terrace Building was originally given, the so-called ‘North Megaron’, supported by the heavy main terrace wall.The excavation of this structure was begun in 1923. The main terrace wall was cleared and two L.H. IIIC burials discovered in the top of the fill in the south room. In 1950 it was decided to attempt to clear this building entirely in an endeavour to find out its date and purpose. The clearing was not, however, substantially completed until the close of the 1953 excavation season, and this report presents the available evidence for the date as determined by the pottery found beneath the building; the purpose is still a matter for study, though various tentative conclusions can be put forward.


Starinar ◽  
2013 ◽  
pp. 269-286
Author(s):  
Perica Spehar ◽  
Natasa Miladinovic-Radmilovic ◽  
Sonja Stamenkovic

In 2012, in the village Davidovac situated in south Serbia, 9.5 km south-west from Vranje, archaeological investigations were conducted on the site Crkviste. The remains of the smaller bronze-age settlement were discovered, above which a late antique horizon was later formed. Apart from modest remains of a bronze-age house and pits, a late antique necropolis was also excavated, of which two vaulted tombs and nine graves were inspected during this campaign. During the excavation of the northern sector of the site Davidovac-Crkviste the north-eastern periphery of the necropolis is detected. Graves 1-3, 5 and 6 are situated on the north?eastern borderline of necropolis, while the position of the tombs and the remaining four graves (4, 7-9) in their vicinity point that the necropolis was further spreading to the west and to the south?west, occupying the mount on which the church of St. George and modern graveyard are situated nowadays. All graves are oriented in the direction SW-NE, with the deviance between 3? and 17?, in four cases toward the south and in seven cases toward the north, while the largest part of those deviations is between 3? and 8?. Few small finds from the layer above the graves can in some way enable the determination of their dating. Those are two roman coins, one from the reign of emperor Valens (364-378), as well as the fibula of the type Viminacium-Novae which is chronologically tied to a longer period from the middle of the 5th to the middle of the 6th century, although there are some geographically close analogies dated to the end of the 4th or the beginning of the 5th century. Analogies for the tombs from Davidovac can be found on numerous sites, like in Sirmium as well as in Macvanska Mitrovica, where they are dated to the 4th-5th century. Similar situation was detected in Viminacium, former capital of the roman province of Upper Moesia. In ancient Naissus, on the site of Jagodin Mala, simple rectangular tombs were distributed in rows, while the complex painted tombs with Christian motifs were also found and dated by the coins to the period from the 4th to the 6th century. Also, in Kolovrat near Prijepolje simple vaulted tombs with walled dromos were excavated. During the excavations on the nearby site Davidovac-Gradiste, 39 graves of type Mala Kopasnica-Sase dated to the 2nd-3rd century were found, as well as 67 cist graves, which were dated by the coins of Constantius II, jewellery and buckles to the second half of the 4th or the first half of the 5th century. Based on all above mentioned it can be concluded that during the period from the 2nd to the 6th century in this area existed a roman and late antique settlement and several necropolises, formed along an important ancient road Via militaris, traced at the length of over 130 m in the direction NE-SW. Data gained with the anthropological analyses of 10 skeletons from the site Davidovac-Crkviste don't give enough information for a conclusion about the paleo-demographical structure of the population that lived here during late antiquity. Important results about the paleo-pathological changes, which do not occur often on archaeological sites, as well as the clearer picture about this population in total, will be acquired after the osteological material from the site Davidovac-Gradiste is statistically analysed.


1981 ◽  
Vol 106 ◽  
pp. 69-75
Author(s):  
I Parsons

A series of smal! volcanic centres cut Ordovician turbidites of Formation A in the southem part of Johannes V. Jensen Land between Midtkap and Frigg Fjord (Map 2). Their general location and main rock types were described by Soper et al. (1980) and their nomenclature is adopted here for fig. 22 with the addition of the small pipe B2. A further small intrusion, south-west of Frigg Fjord, was described by Pedersen (1980). The centres lie 5-10 km south of, and parallel to, the important Harder Fjord fault zone (fig. 22) which traverses the southern part of the North Greenland fold belt and shows substantial downthrow to the south (Higgins et al., this report).


2014 ◽  
Vol 31 (1) ◽  
pp. 61-68 ◽  
Author(s):  
Samuli Helama ◽  
Jari Holopainen ◽  
Mauri Timonen ◽  
Kari Mielikäinen

Abstract A near-millennial tree-ring chronology (AD 1147-2000) is presented for south-west Finland and analyzed using dendroclimatic methods. This is a composite chronology comprising samples both from standing pine trees (Pinus sylvestris L.) and subfossil trunks as recovered from the lake sediments, with a total sample size of 189 tree-ring sample series. The series were dendrochronologically cross-dated to exact calendar years to portray variability in tree-ring widths on inter-annual and longer scales. Al though the studied chronology correlates statistically significantly with other long tree-ring width chronologies from Finland over their common period (AD 1520-1993), the south-west chronology did not exhibit similarly strong mid-summer temperature or spring/early-summer precipitation signals in comparison to published chronologies. On the other hand, the south-west chronology showed highest correlations to the North Atlantic Oscillation indices in winter/spring months, this association following a dendroclimatic feature common to pine chronologies over the region and adjacent areas. Paleoclimatic comparison showed that tree-rings had varied similarly to central European spring temperatures. It is postulated that the collected and dated tree-ring material could be studied for wood surface reflectance (blue channel light intensity) and stable isotopes, which both have recently shown to correlate notably well with summer temperatures.


Author(s):  
Paul D. Escott

This chapter emphasizes the analysis of the wartime forces in both sections that affected unity or division. It raises questions about the roots of the large amount of internal violence or irregular warfare in the South. For the North, it probes the nature of nationalism and asks about that section’s social, political, and religious divisions. Factors affecting both the Republican and the Democratic Parties of the North deserve new attention, as do the role of women in both sections, ethnic groups in the North especially, and the impact of emancipation and racism.


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