Pseudomorphs of pyrrhotine after pyrite in the Ballachulish slates

1950 ◽  
Vol 29 (210) ◽  
pp. 234-238 ◽  
Author(s):  
Henrich Neumann
Keyword(s):  
Single Crystals ◽  
The Other ◽  
The South ◽  
The North ◽  
Loch Leven ◽  
Other Hand ◽  
Dark Colour ◽  
South Shore ◽  
North And South

The Ballachulish slates, exposed to the north and south of Loch Leven in Argyllshire, contain, in most places, cubes of pyrite up to half an inch in diameter. During a visit to the area in the spring of 1949 the writer's attention was attracted by the dark colour of the 'pyrite' cubes in the North Ballaehulish slate quarry a little more than a mile east of Onich. On examination these proved to consist of a mass of haphazardly orientated crystals of pyrrhotine with irregular outlines. Slates collected from the main working quarry on the south shore of Loch Leven, on the other hand, contain cubes which are single crystals of unaltered pyrite.

Attitudes to reform: political parties in Ulster and the Irish land bill of 1881

1985 ◽  
Vol 24 (95) ◽  
pp. 327-340
Author(s):  
Francis Thompson
Keyword(s):  
Political Parties ◽  
Detailed Examination ◽  
The Other ◽  
The South ◽  
The North ◽  
Other Hand ◽  
Previous Decade ◽  
History Of

The Irish land act of 1881, it is generally agreed, was a victory for the Land League and Parnell, and nationalist policy with regard to the act and the attitude of southern tenants towards it have been many times subjected to detailed examination by historians of this period. In these analyses of the events of 1880–81, however, little reference is normally made to the part played by the different parties and interests in the north of the country. It is often assumed, for example, that the Ulster tenants held aloof from the campaign for reform, lending no more than occasional vocal support to the agitational efforts of tenants in the south and west. Indeed, they were later excoriated by William O'Brien, Michael Davitt and others not only for giving no support to the land movement but also for sabotaging Parnell's policy of testing the 1881 act by precipitately rushing into the land courts to take advantage of the new legislation: ‘that hard-fisted body of men, having done nothing themselves to win the act, thought of nothing but turning it to their own immediate use, and repudiating any solidarity with the southern and western rebels to whom they really owed it’. If, however, northern tenants were harshly judged by nationalist politicians in the years after 1881, the part played by the northern political parties in the history of the land bill has been either ignored or misunderstood by historians since that time. The Ulster liberals, for example, are rarely mentioned, the implication being that they made no contribution to the act even though it implemented almost exactly the programme on which they had been campaigning for much of the previous decade. The northern conservatives, on the other hand, are commonly seen as leading opponents of the bill, more intransigent than their party colleagues in the south, ‘quick to denounce any weakening of the opposition’ to reform, and ‘determined to keep the tory party up to the mark in defending the landlord interest’

scholarly journals THE SOUTH-EASTERN BORDER REGION OF THE HITTITE STATE

2016 ◽  
pp. 19-30
Author(s):  
ROBERT GHAZARYAN
Keyword(s):  
Border Region ◽  
The Other ◽  
The South ◽  
The North ◽  
Other Hand ◽  
Euphrates Valley ◽  
Important Position ◽  
The One ◽  
The Right ◽  
Armenian Highland

Tegarama was one of the eastern lands of the Hittite Kingdom. In the geographic sense it is part of the Armenian Highland that is why its history is of special interest to us. Taking into account the fact that the Armenian people had considerable ethnic ties with the Upper Euphrates region, specialists have traditionally tended to identify “Home of Torgom” in the Trans Euphrates region together with the city Tegarama (Assyrian Til-Garimmu) mentioned from the 2nd millennium BC. “Home of Torgom” literally repeats Bet-Togarma mentioned in the Bible. The study of the history of the country of Tegarama is also important because in Armenian historiography, starting from Movses Khorenatsi, Armenian ancestor Hayk is called “Son of Torgom”, and the Armenian people - “People of Torgom”. Most of the researchers located Tegarama in the place of the present settlement Gyurun. By comparing the “Cappadocian”, Hittite and Assyrian sources, Tegarama can be located in the Upper Euphrates valley, on the right bank of the river, to the north of Kargamis, to the west of Isuwa, to the south of Upper Land and to the east of Kanes. The territory of Tegarama was not far from Nesa - one of the initial centers of the Hittites; and it was also one of the initial places of inhabitance of the Hittites. Tegarama also occupied a strategically important position. On the one hand it bordered on the country of Mitanni, on the other hand - on Isuwa. Thus, the country of Tegarama occupied a significant geographic position: on the one hand roads led from here to other western districts of the Armenian Highland, to Tsopk, and on the other hand - to Northern Syria and Northern Mesopotamia. It was also one of the spiritual centers of Hatti.

Rebel Retirement in the North through Discordant Exit Networks

2021 ◽  
pp. 118-143
Author(s):  
Rumela Sen
Keyword(s):  
The Other ◽  
Grassroots Organizations ◽  
Gray Zone ◽  
The South ◽  
The North ◽  
Other Hand ◽  
Land Relations ◽  
State Agents ◽  
The One

This chapter shows how weak grassroots organizations in the gray zone of state-insurgency interface led to scrawny informal exit networks in the North, discouraging rebel retirement and restricting their reintegration. The differences with the South stem from the secret and semi-secret ties that northern rebels build with state agents like police, politicians, and bureaucracy on the one hand and various nonstate agents like mafias and businesses on the other hand. These ties, alongside distinctive caste/class dynamics and land relations in the North, induces dominance of perverse criminality and spews intense militancy in the North, which vitiates the gray zone of state-insurgency interface.

The Problem of Failure in American History

2020 ◽  
pp. 249-264
Keyword(s):  
African American ◽  
Civil War ◽  
American History ◽  
The Other ◽  
Shared Understanding ◽  
The South ◽  
The Past ◽  
The North ◽  
To Come ◽  
North And South

C. Vann Woodward’s lecture compares two commemorations of the Civil War fifty years apart, one in 1911 and the other in 1961. The first one reflected sectional reunification predicated on a shared understanding of the tragic nature of war but also a sense that the conflict had solved the problem of sectional animosity. In so doing Woodward notes that whites in the North and South could only accomplish this by excluding meaningful African-American participation. The lecture then outlines the cycles of Reconstruction historiography, and looks at the dual psychological traumas the North and South experienced in the aftermath of Reconstruction. Woodward maintains that after the North emerged victorious from the war it failed to live up to its ideals, leaving wracked guilt, self-criticism, and remorse. The South emerged with a predilection for extortion, indignation, and extreme bellicosity, consistently blaming its own weaknesses on Reconstruction. Woodward suggests that historians should act as therapists, enabling the nation to come to terms with the psychological traumas triggered by the past.

I 10, 10-11: Casa Degli Amanti

1997 ◽  
Author(s):  
Roger Ling ◽  
Paul Arthur ◽  
Georgia Clarke ◽  
Estelle Lazer ◽  
Lesley A. Ling ◽  
...  
Keyword(s):  
The Other ◽  
Central Axis ◽  
The South ◽  
The West ◽  
The North ◽  
Small Window ◽  
South West ◽  
Dining Room ◽  
North Wall ◽  
North And South

The casa degli amanti (house of the lovers), at the south-west corner of the insula, falls into two fairly distinct halves: the atrium complex, oriented on the street to the west, and the peristyle with its surrounding rooms, oriented on the street to the south and on the property boundary to the east. In the atrium complex, the atrium is misplaced to the south of the central axis, allowing space for two large rooms to the north, one of which was possibly a shop or workshop (5.50 m. × 4.70 m.), with a separate entry from the street (I 10, 10), while the other (5.80 m. × 4.50 m.), decorated with mythological wallpaintings and provided with a wide opening on to the peristyle, must have been a dining-room or oecus (room 8). Each of these had a segmental vault rising from a height of about 3.50 m. at the spring to slightly over 4 m. at the crown. In the first the vault is missing, but the holes for some of its timbers are visible in the east wall and a groove along the north wall marks the seating for the planking attached to them; at a higher level, in the north and south walls, are the remains of beam-holes for the joists of the upper floor or attic (see below). The arrangements in room 8 are now obscured by the modern vault constructed to provide a surface for the reassembled fragments of the ceiling-paintings; but the shape of the vault is confirmed by the surviving plaster of the lunettes, while a beam-hole for the lowest of the vault-timbers is visible above the corner of the western lunette in an early photograph (Superintendency neg. C 1944). The shop I 10, 10 had a small window high in the street wall to the south of Its entrance; whether there were any additional windows above the entrance, it is impossible to say, since this part of the wall is a modern reconstruction. Room 8 was lit by a splayed window cut in the angle of the vault and the eastern lunette, opening into the upper storey of the peristyle.

scholarly journals XII. On a tendency observed in Sun-spots to change alternately from the one solar hemisphere to the other

1873 ◽  
Vol 21 (139-147) ◽  
pp. 399-402
Keyword(s):  
The Other ◽  
The South ◽  
The North ◽  
Other Hand ◽  
Spot Activity ◽  
Sun Spots ◽  
The One

1. Hitherto in our reductions we have summed up the spotted areas of the various groups occurring on the sun’s surface on any day, and have regarded their sum as a representation of the spot-activity for that day. It has occurred to us to see what result we should obtain by taking instead for each day the excess of the spotted area in the one solar hemisphere above that in the other. 2. On adopting this method, it soon became evident that during periods of great disturbance there is a tendency in spots to change alternately from the north or positive to the south or negative hemisphere, and vice versâ , the period of such change being about 25 days. When, on the other hand, the solar disturbance is inconsiderable, the spots do not present any such systematic oscillation.

IV.—The Post-Pleistocene Flora and Fauna of Central England

1910 ◽  
Vol 7 (12) ◽  
pp. 542-553
Author(s):  
A. R. Horwood
Keyword(s):  
Fresh Water ◽  
The Other ◽  
Central Position ◽  
The South ◽  
Alluvial Deposits ◽  
Drainage Systems ◽  
River Drainage ◽  
The North ◽  
The One ◽  
North And South

The central position of Leicestershire gives it not only a peculiar relationship in regard to river-drainage, streams radiating from its plateau-frontier on the one hand to the north, flowing into the Humber, and on the other to the south into the Bristol Channel, separated alone by a now comparatively insignificant divide in the neighbourhood of Lutterworth. Also the very fact that this divide is given, by the otherwise lowland character of the tract to the north and south, a barrier-like aspect, renders it highly probable that the flora and fauna in this basin-like area is more or less homogeneous. That it has been uniform in character, no doubt from pre-Glacial times, when doubtless the existing drainage systems (though probably still more ancient fundamentally) received their most recent stamp, having been little modified (except in depth or width) during Glacial or later times. For this purpose we must needs summarize all that is known as to the occurrence of plants or land and fresh water Mollusca in post-Pleistocene alluvial deposits.

The General Oceanography of the Strait of Belle Isle

1954 ◽  
Vol 11 (3) ◽  
pp. 198-260 ◽  
Author(s):  
A. G. Huntsman ◽  
W. B. Bailey ◽  
H. B. Hachey
Keyword(s):  
Shallow Water ◽  
The South ◽  
Hydrographic Data ◽  
Arctic Water ◽  
Tidal Period ◽  
North Shore ◽  
The North ◽  
Labrador Current ◽  
South Shore ◽  
North And South

Hydrographic data for late August, 1923, show for the Strait (a) progressive inward movement on the north side of Arctic or sub-Arctic water, (b) progressive outward movement on the south side of Gulf water and (c) a dominant outward flow with evidence of a previous dominant inward flow. Time differences suggest tidal causes for the marked temperature and salinity changes. Current measurements for a double tidal period indicate residual trends of nine and eight miles per day in opposite directions on the north and south sides of the Strait. Inside, the Esquiman Channel shows two contra-clockwise eddies north and south of the Mekattina Bank. In addition, hydrographic data show a strong northeasterly movement along the Newfoundland shore and a weaker southwesterly one along the opposite Quebec shore.Planktonic animals indicate the water movements, Mertensia, Acartia spiniremis, Themisto, Pseudalibrotus and Oikopleura vanhöffeni surviving to various degrees in the water from the Labrador Current that reaches the centre of the Gulf along the north shore of the Strait and Channel. Other forms characterize the warm shallow water along the Newfoundland shore inside the Strait and show its movement outward to the east coast of Newfoundland. The Greenland seal fishery of winter reflects the inward movement from the Labrador Current. Cod and herring fisheries invade this cool water of the north shore only locally in summer with access of warmer water from the south shore. Lobsters and cunners are very abundant in, but particularly confined to, the warm shallow water mentioned above.

The Position of Kajkavian in the South Slavic Dialect Continuum in Light of Old Accentual Isoglosses

2017 ◽  
Vol 62 (1) ◽  
Author(s):  
Mate Kapović
Keyword(s):  
The Other ◽  
The South ◽  
North West ◽  
Slavic Languages ◽  
The North ◽  
Other Hand

SummaryAll South Slavic languages, from Bulgaria in the South-East to Slovenia in the North-West, are part of a dialect continuum. This paper outlines the position of what is traditionally called Kajkavian in that continuum in light of old accentual isoglosses. Kajkavian shares several old prosodic-phonological isoglosses with Slovene (such as the rise of the neocircumflex), while on the other hand it is connected with Western Štokavian and Čakavian through some morphological-categorial accentual isoglosses (like the innovative accent of the infinitive and

Geologie des confins des provinces d'Alicante et de Murcie (Espagne)

1966 ◽  
Vol S7-VIII (1) ◽  
pp. 80-86 ◽  
Author(s):  
Jacques Azema
Keyword(s):  
The Other ◽  
The South ◽  
Structural Units ◽  
Space And Time ◽  
The North ◽  
Other Hand ◽  
Dual Evolution

Abstract Within the Alicante and Murcia provinces (Spain) the superposition of two large structural units can be seen: the Prebetic autochthonous complex in the north and the Subbetic allochthonous complex in the south. The autochthonous complex reflects a dual evolution in space and time which is expressed in the Tertiary as two provinces--the Prebetic of Alicante and the western Prebetic--and in the Jurassic and Cretaceous by the development of a north to south facies differentiation. The Subbetic domain on the other hand represents homogeneous sedimentation and constitutes a single paleogeographic unit. The Subbetic rests unconformably on southern formations of the Prebetic, its maximum observable displacement being on the order of 15-20 km.

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