scholarly journals ”Elveland” – Irony and Laughter as Power Media in Sea Sámi Folk-Song Tradition

Nordlit ◽  
2004 ◽  
Vol 8 (1) ◽  
pp. 47
Author(s):  
Lill Tove Fredriksen

The article is a literary analysis of the satirical Sámi folk-song ”Elveland”. The song about about the road man, forester and river attendant Elveland on the west side of the municipality of Porsanger was made in the beginning of the 1900s, as a form of revenge on the part of the local community because he would not let them cut as much firewood as they needed. With irony as an important device, the text serves as a meeting point for dialogues between different voices, and where power relations and the political nature of cultural identity is revealed.


1938 ◽  
Vol 18 (1) ◽  
pp. 68-74 ◽  
Author(s):  
Philip Corder ◽  
I. A. Richmond

The Roman Ermine Street, having crossed the Humber on the way to York from Lincoln, leaves Brough Haven on its west side, and the little town of Petuaria to the east. For the first half-mile northwards from the Haven its course is not certainly known: then, followed by the modern road, it runs northwards through South Cave towards Market Weighton. In the area thus traversed by the Roman road burials of the Roman age have already been noted in sufficient quantity to suggest an extensive cemetery. The interment which is the subject of the present note was found on 10th October 1936, when men laying pipes at right angles to the modern road, in the carriage-drive of Mr. J. G. Southam, having cut through some 4 ft. of blown sand, came upon a mass of mixed Roman pottery, dating from the late first to the fourth century A.D. Bones of pig, dog, sheep, and ox were also represented. Presently, at a depth of about 5 ft., something attracted closer attention. A layer of thin limestone slabs was found, covering two human skeletons, one lying a few feet from the west margin of the modern road, the other parallel with the road and some 8 ft. from its edge. The objects described below were found with the second skeleton, and the first to be discovered was submitted by Mr. Southam to Mr. T. Sheppard, F.S.A.Scot., Director of the Hull Museums, who visited the site with his staff. All that can be recorded of the circumstances of the discovery is contained in the observations then made, under difficult conditions. ‘Slabs of hard limestone’, it was reported, ‘taken from a local quarry of millepore oolite and forming the original Roman road, were distinctly visible beneath the present roadway—one of the few points where the precise site of the old road has been located. On the side of this… a burial-place has been constructed. What it was like originally it is difficult to say, beyond that a layer of thin … slabs of limestone occurred over the skeletons. This had probably been kept in place or supported by some structure of wood, as several large iron nails, some bent at right angles, were among the bones.’ If this were all that could be said about the burials, they would hardly merit a place in these pages. The chief interest of the record would be its apparent identification of the exact course of the Roman road at a point where this had hitherto been uncertain. Three objects associated with the second skeleton are, however, of exceptional interest.



Antiquity ◽  
1929 ◽  
Vol 3 (9) ◽  
pp. 49-59 ◽  
Author(s):  
O. G. S. Crawford

Probably not one in ten thousand of those who pass through the middle of Durrington Walls is aware of its existence. Though plainly visible when once pointed out, the earthen ramparts have been so greatly altered by ploughing as to be hardly recognizable, and the reconstruction of their orginal form is a very pretty exercise in field-archaeologyThe walls consists of a round enclosure, cut into two unequal parts by the road from Amesbury to Netheravon (Wilts), about a mile and a half north of Amesbury, on the west bank of the Avon. Woodhenge is only eighty yards to the south, close to and on the west side of the same road. The earthwork differs fundamentally from the ordinary defensive ‘camp’, for it encloses, not a hill-top but a coombe or hollow, and it has its ditch inside, not outside, the rampart. In this latter respect it resembles the circles at Avebury and Marden in Wilts, Knowlton in Dorset, Thornborough in Yorkshire, and Arbour Low in Derbyshire; though there are points of difference. In size, Durrington Walls compares closely with Avebury, whose great earthen circle is slightly smaller in diameter; rom east to west the internal area of the Walls is 1300feet across, and from north to south about 1160 feet. (The average diameter at Avebury is 1130 feet). Both too are within easy reach of a stream, the Avon being IOO yards from the eastern entrance of the Walls, and the Kennet 330 yards from the nearest point of the great circle at Avebury. The enclosure at Marden actually touches the banks of the Avon at a point higher up in its course.



1969 ◽  
Vol 19 ◽  
pp. 139-142 ◽  
Author(s):  
Theodora S. Mackay ◽  
Pierre A. Mackay

The following random lot of inscriptions was noted during three brief trips into the territory around Olba-Diocaesareia, in the spring of 1966, while we were guests at the British Institute of Archaeology at Ankara. These trips were part of a year of archaeological wandering made possible by the grant of the Olivia James Travelling Fellowship, administered by the Archaeological Institute of America.1. Seleuceia-Korykos: This inscription was discovered by the able and energetic curator of antiquities at Silifke, Mr. Mehmet Belen, to whose great kindness we owe our knowledge of it. It is cut on a rock face above some faint traces of an ancient road from Korasion to Korykos, which runs parallel to the modern coast road at this point. About 19 km. east of Silifke, the modern road turns north away from the shore, and runs inland along the west side of a seasonal watercourse called Kuru Dere, “dry river bed”. Just north of the gravel bank at the mouth of Kuru Dere, at a point where the rock wall cuts back from the west side of the road to form a very small tributary stream bed, there are faint traces of rock cut steps some 5 metres above the road. Above these, on the south side of the tributary stream bed, a roughly dressed rectangular panel, 0·80 × 0·45 m., has been cut into the rock.



1924 ◽  
Vol 61 (11) ◽  
pp. 513-515 ◽  
Author(s):  
Sidney Melmore

A Small quarry was opened about three years ago at Thwaite Head, which lies between the southern ends of Coniston Lake and Windermere. It is on the west side of the road between that hamlet and Hawkshead, and exposes a nearly vertical sill, 40 feet wide, running E.N.E.-W.S.W. in the Bannisdale slates. On the south side a series of joint-planes running parallel to the bedding of the slates and curving inwards at the top have split the igneous rock into flags, while in the body of the rock the jointing is much coarser, so that it is quarried in large blocks. Both the igneous rock and the slates are much decomposed and friable along the southern junction, and it is here a little galena is said to have been found when the quarry was first opened. This is not improbable, as the old Thwaite Head lead mine is situated not far off on the banks of Dale Park Beck.



1886 ◽  
Vol 7 ◽  
pp. 251-274
Author(s):  
L. R. Farnell

The questions concerning the art of Pergamon, its characteristics and later influence, depend partly for their solution on the reconstruction and explanation of the fragments in Berlin. Much progress has been made in the work during the last year. The discovery which decided what was the breadth of the staircase, and what were the figures which adorned the left wing and the left staircase wall, has been already mentioned in the Hellenic Journal. It is now officially stated that the staircase was on the west side of the altar, although Bohn, in his survey of the site, at first conceived that this was impossible. Assuming that this point is now settled, we may note what is certain, or probable, or what is merely conjectural, in the placing of the groups. We know that the wing on the left of the staircase, and the left staircase-wall, were occupied by the deities of the sea and their antagonists: by Triton, Amphitrite, Nereus, and others which we cannot name. Among them, also, we may perhaps discern the figure of Hephaestos, and in their vicinity we must suppose Poseidon. On the right wing of the staircase, and around the south-west corner, we have good reason for placing Dionysos, with Cybele and her attendant goddesses, although the order of the slabs on which these latter are found is not the same as was formerly supposed.



Author(s):  
Robert M. Lombardo

This chapter examines the activities of organized crime in Chicago after 1950, with particular emphasis on the Chicago Outfit. It begins with a discussion of the Outfit's takeover of all illegal gambling in Chicago as well as its connection with Chicago mayor Ed Kelly and the political protection given to vice activities in Chicago. It then considers the often confusing relationship between the Outfit and narcotic trafficking, along with the role that African Americans played in Outfit activities, including policy gambling and the distribution of heroin in the black community. It also reviews the history of the West Side Bloc, a group of elected public officials who supported the efforts of organized crime in Chicago, and how it contributed to the rise of racket subcultures in Chicago's “street crew” neighborhoods. The chapter concludes with an assessment of government efforts against organized crime, noting that one of the reasons for the existence of organized crime was the failure of local municipalities and the national government to take effective enforcement action against it.



1966 ◽  
Vol 34 ◽  
pp. 56-67
Author(s):  
J. M. Reynolds

The following group of inscriptions includes some unpublished texts found recently during the South Etruria survey and a few published ones in which additional or improved readings can be offered as a result of re-examination. Most of them are tombstones of essentially local significance, but nos. 1 and 4 from Tomba di Nerone, 5 from Casale Spizzichino and 20 from Filissano are of greater importance and interest.I. Sites on or near the Via Cassia.1. Travertine tombstone, damaged at the upper right corner (0·52 × 0·98 × 0·12), with schematic gable and acroteria above and a lightly and crudely incised wreath in the gable; inscribed on the exposed face, whose surface is damaged. Built into the wall of the drive leading to Via Cassia 901, which lies on the west side of the road a short distance beyond Tomba di Nerone. Recent building development revealed drainage cuniculi and other elements of a Roman building, and along the ancient road frontage there were several graves and remains of at least one mausoleum. It is very likely that some or all of the texts (nos. 1–4) were found locally.



2019 ◽  
pp. 217-260
Author(s):  
Jesse E. Hoffnung-Garskof

This chapter shows how a concert held on the West Side of Manhattan on New Year's Day 1897 served to unite and mobilize the networks that Rafael Serra and his allies had built over two decades. This was conducted in defense of a struggle against all privileges, and to celebrate, in the name of democracy and patriotic unity, the loyalty of that group to the party leader. As the war unfolded in Cuba, Figueroa and Serra engaged in a war of position, picking their near-term battles carefully in order to situate themselves advantageously for the coming struggle to preserve democratic values within the Cuban republic and for the political competitions that would follow. Supported by the men and women who gathered in the concert hall on New Year's Day, they were emerged victorious in one of the few open maneuvers in this long-simmering conflict. This chapter shows that the fact that Serra and Figueroa could still effectively maneuver within the Cuban Revolutionary Party, even after the death of Martí, sheds clear light on one of the major questions posed by this book. In short, the chapter considers what lasting impact the conflicts and alliances created within the Cuban Revolutionary Party in New York had on the evolution of Cuban politics after independence.



1869 ◽  
Vol 6 (62) ◽  
pp. 347-348
Author(s):  
H. C. Sorby

For a considerable time I have taken much interest in the question of the origin of the narrow and deep valleys in the Carboni-ferous Limestone district of Derbyshire, and have carefully recorded whatever seemed to explain their formation. So far I have never met with more striking facts than those to be seen in Deep Dale, about three miles in a direct line E.S.E. from Buxton. I estimate the depth of the valley at about 100 feet, and its width at from 100 to 200 yards. At a distance of about a mile from the Bakewell road there is a cavern, which is especially conspicuous on the east side. Its entrance is about 6 feet high, 20 feet broad, and 40 feet above the bottom of the valley. It extends nearly horizontally for about 30 yards, and then descends to a lower level, where I did not further examine it. On looking from the entrance to the opposite side of the dale I was surprised to see what appears to be a continuation of the same cavern. The entrance on that side is at about 80 feet above the valley, and is so much blocked up with detritus that one can only examine it for a space of 10 yards. Taking, however, all the facts into consideration, it appears to me that at a very remote period a subterranean stream flowed continuously along these two caverns, from west to east. There is abundance of suitable gather ground on the west side which even now has no well-marked surface drainage, and from which much of the water probably escapes by a subterranean course, ending in the large spring in the main valley, by the road-side below Kingsterndale.



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