II.—The Dolomite Reefs of the South Tyrol and Venetia. Contribution to the History of the Formation of the Alps. (Die Dolomit - Riffe von Süd-Tyrol und Venetia. Beiträge zur Bildungsgeschichte der Alpen. Von Edmond Mojsisovics von Mojsvár.) With a Map, in 6 Sheets, of the Tyrolese Venetian Alps, 30 Photographs, and 110 Woodcuts; pp. 552.

1879 ◽  
Vol 6 (09) ◽  
pp. 428
Author(s):  
H.
Keyword(s):  
1894 ◽  
Vol 1 (2) ◽  
pp. 49-60 ◽  
Author(s):  
Maria M. Ogilvie

The Raibl period was the natural sequel of the variable and unequal movements which prevailed over Alpine areasinPermian and pre-Raibl Triassic time. Many basins formerly open were then enclosed; rauchwackes and beds of dolomite and gypsum were interbedded with fossiliferous deposits. Whereas,insome places, the dolomitic nature of the deposit is confined to special horizons, in the South Tyrol “Dolomites” it may almost be said to reign throughout. This makes it all but impossible to say when Schlern dolomite ends and Raibl beds begin. in the present incomplete state of our knowledge with regard to the heteropism of the Raibl series throughout the whole Alps, I have judged it best to begin the Raibl horizon at any particular place with the first appearance of a distinctly Raibl fauna, even although that fauna may not have been proved to correspond to the acknowledged lowest fauna of Raibl age in distant parts of the Alps.To return for a moment to the succession of Schlern dolomite upon the Cassian beds of Enneberg, I found that, where Schlern dolomite rests on Cipit limestones, it has at its base a conglomeratic appearance, as if Cipit blocks had been imbedded in a beautifully fine white or reddish dolomitic mud, instead of the dingy brown and black tufaceous sediments. This is the case in several places, e.g. upon Pordoi and Sella Jochs, where there is no evidence of unconformity. Again, where the dolomite succeeds the thin-bedded marls and limestones of Cassian age, it does so conformably; but one and the same bed is at some parts calcareous and fossiliferous, at other parts dolomitic and unfossiliferous. Seeing that this holds good at various horizons in Lower as well as Middle Trias over the whole area of South Tyrol, we need f in d nothing remarkable in it from the point of view of the stratigraphical succession. Indeed, I have only mentioned these observations as an indication of the particular mode of transition from conditions of deposition favourable for the Cassian fauna to those in which the Raibl fauna was enabled to make an occasional appearance in the South Tyrol dolomites. At a very little distance above the base of Schlern dolomite all signs of Coral life disappear, and the deposit looks a homogeneous rock, although always retaining local variation in the degree of its dolomitism. At this stage the rock often shows typical Oolite structure. As regards the presence or want of stratification, it has as little to do with the question of the Coral Keef origin of the dolomite as the amount of magnesic salts in the rock—stratification is present and absent in one and the same “Keef.”


Antiquity ◽  
1960 ◽  
Vol 34 (135) ◽  
pp. 191-200 ◽  
Author(s):  
Werner Krämer

Only a few decades after the conquest of Gaul by Caesar the power of the free Celtic tribes in central Europe collapsed as a consequence of their finding themselves placed, during the course of the 1st century B.C., in an insecure position between the Romans and the Germans pressing down from the North. The victorious Alpine campaign of Drusus and Tiberius in 15 B.C. sealed the fate of, among others, the Vindelicians who occupied the south German area north of the Alps as far as the Danube. Here, still today, mighty hillforts bear witness to the power of those nameless Celtic chieftains who caused them to be erected. Contemporary literary sources tell all too little about the history of this area and about the cultural connections of its inhabitants before the Roman occupation. Therefore modern research relied upon Caesar’s description of the Gallic tribes in drawing parallels between the large late La Tène hillforts in central Europe and the city-like tribal centres of the Gauls in France, which Caesar called ‘oppida’ or even ‘urbes’.


1996 ◽  
Vol 15 (1) ◽  
pp. 68-75 ◽  
Author(s):  
Mary Creese

Maria Ogilvie Gordon, honorary member of the Vienna Geological Society and the London Geological Society's 1932 Lyell Medalist, was one of the most outstanding of Britain's early women field geologists. Her work, begun in 1891 and continued until the early 1930's, was carried out in the Dolomites of the South Tyrol, and focused primarily on the unravelling of the tectonic history of the region. Her publications were substantial, many appearing in Austrian journals. She had, in addition, what amounted to a second career as a civic and social leader, particularly in matters relating to the advancement of women and the welfare of children and young people.


1947 ◽  
Vol 37 (1-2) ◽  
pp. 39-46 ◽  
Author(s):  
R. M. Dawkins

The famous Varangian corps of mercenary soldiers in the service of the emperors of Byzantium is well known in its earlier days to have been recruited from the Scandinavian north. Forging their way from their own inhospitable lands the Northmen, first of all from Sweden, reached the Volga and the lands even to. the south of the Caspian; later by the ‘East Way’, called also the ‘Varangian Way’, they came down through Russia by way of the Dnieper and the Black Sea to Constantinople, first as pirates, then as traders, and finally as the most trusted guards of the imperial person. Later again they ventured on the all-sea route, the ‘West Way’, and also opened a path across Europe, either over the Alps or by way of Provence, and so through Italy: this was the ‘Southern Way’, otherwise called the ‘Way by Rome’ But in the eleventh century, in the first half of which Harald Hardrada, the most famous of all the Varangians, was in the imperial service, there was a certain change; recruits began to come increasingly from England.The first actual mention of the English name seems to be in a bull issued by the Emperor Alexios in 1088 to Christodoulos, the Abbot of the Monastery on Patmos.


2020 ◽  
Vol 6 (3) ◽  
pp. 21-51
Author(s):  
Debashree Mukherjee

In 1939, at the height of her stardom, the actress Shanta Apte went on a spectacular hunger strike in protest against her employers at Prabhat Studios in Poona, India. The following year, Apte wrote a harsh polemic against the extractive nature of the film industry. In Jaau Mi Cinemaat? (Should I Join the Movies?, 1940), she highlighted the durational depletion of the human body that is specific to acting work. This article interrogates these two unprecedented cultural events—a strike and a book—opening them up toward a history of embodiment as production experience. It embeds Apte's emphasis on exhaustion within contemporaneous debates on female stardom, industrial fatigue, and the status of cinema as work. Reading Apte's remarkable activism as theory from the South helps us rethink the meanings of embodiment, labor, materiality, inequality, resistance, and human-object relations in cinema.


Author(s):  
A.V. Plyusnin ◽  
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R.R. Ibragimov ◽  
M.I. Gyokche ◽  
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...  
Keyword(s):  

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