scholarly journals II.—The Perched Blocks of Norber Brow and their Levels Relative to their Place of Origin

1891 ◽  
Vol 8 (7) ◽  
pp. 291-292
Author(s):  
T. Mellard Reade

In a recent excursion the Liverpool Geological Society visited Norber Brow, near Austwick, to inspect the celebrated perched blocks of Silurian rock lying upon the Carboniferous limestone plateau. The visit was made in very appropriate weather during a storm of hail which added a weird element to the scene and heightened by contrast the blackness of the Silurian blocks. Since returning home I have re-read Prof. McKenny Hughes' interesting paper on the subject, and find that generally speaking my notes and measurements are in accord with his. The angularity of the perched blocks, so different to the rounded and striated erratics of the Boulder Clay Plains of Lancashire and Cheshire, and the absence of Boulder Clay, is very striking, and inevitably suggests their transportal by glacier ice probably at the last phase of the glacial period.

1889 ◽  
Vol 10 ◽  
pp. 231-242 ◽  
Author(s):  
Jane E. Harrison

The subject of the exploits of Theseus as seen on Greek vase-paintings has recently been treated by Professor Milani in a long and interesting paper in the Museo Italiano di antichità classica (iii. 1, p. 236). I propose therefore to set aside all general consideration of the myth and its typography, and to confine myself to the discussion and elucidation of two hitherto unpublished vases (plates I., II.), one of them included in Professor Milani's list, one entirely unknown to him, and both, as I hope to show, having strong claims on the attention of archaeologists. They are (1) a red-figured vase, which for convenience sake I shall call from its owner the Tricoupi cylix; (2) the fragments of a red-figured cylix from the De Luynes collection in the Bibliothèque Nationale, Paris.1. The Tricoupi cylix, plate I. When I was in Athens in the spring of 1888, Miss Tricoupi with her accustomed kindness, so familiar to all visitors to Athens, allowed me to examine at my leisure her brother's collection of antiquities. I found to my surprise that it contained a vase which I have reason to believe is from the hand of Duris, and of which, so far as I am aware, no mention has been made in the numerous discussions of vases dealing with the exploits of Theseus, and which therefore, I suppose to be entirely unknown. I record here my grateful thanks to Miss Tricoupi for her kind permission to publish the vase, and for her goodness in facilitating its exact reproduction. The drawing from which plate I. is facsimiled was made for me by M. Gilliéron under my own personal supervision, and I can therefore vouch for its perfect accuracy. I was specially anxious to secure its.immediate publication as, though the vase is at present in such safe hands, the security of antiquities in private collections is always precarious.


1914 ◽  
Vol 1 (4) ◽  
pp. 434-438 ◽  
Author(s):  
W. G. Clarke

In former parts of these “Proceedings” Dr. W. Allen Sturge, M.V.O., has put forward views concerning the striæ on surface implements, views which are so opposed to the canons of geology and archæology, and involve so great an upheaval of accepted beliefs, that but for the skill with which the facts and conclusions were marshalled, they would not have received a moment's consideration. Few archæologists have the material on which to form a reliable judgment, and fewer still are prepared to accept the upheaval of current views rendered necessary by the adoption of the theory that minor glaciations occurred after the deposition of the chalky boulder clay. Even more revolutionary was the view as to the occurrence of a glacial period at all and this was strenuously fought for many years, and even now is by no means accepted by all geologists. The drift deposits were referred to by old writers as “Extraneous Rubbish,” and were sometimes divided into Diluvium and Alluvium. It was not until 1840, when Agassiz read his paper before the Geological Society on “Glaciers, and the Evidence of their having once existed in Scotland, Ireland, and England,” that this momentous explanation of a vast and difficult problem was given to geologists, and years elapsed before it was generally accepted.


1913 ◽  
Vol 10 (4) ◽  
pp. 154-163 ◽  
Author(s):  
Henry Dewey

While mapping the Upper Devonian and Carboniferous Rocks in North Devon I took the opportunity of examining the raised beach of Barnstaple Bay and the deposits resting upon it. As a result of my observations I found that the sequence of these deposits is identical bed for bed with that of Cornwall, South Wales, and Southern Ireland, except that in place of the Boulder-clay there is in North Devon a bed of clay with striated stones which may not be of glacial origin. The position of the Boulder-clay over the ancient head, however, corresponds with the position of the bed of glaciated stones and indicates the infra-Glacial age of the ‘head’. The fact that the ‘head’ is contemporaneous with ‘Coombe Rock’ has been held by all geologists familiar with the subject. It is a fact of first-class importance with regard to the relationship of man to the Glacial period, for it proves that man existed before these Boulder-clays were deposited. The evidence is inferential and supplied by the occurrence of Palæolithic implements of Le Moustier type in the Coombe Rock of Southern England and France. Granting, then, that the Le Moustier period is infra-Glacial, it remains to be seen to what Palæolithic period the raised beach belongs. We will proceed to consider the evidence available up to date, commencing with a brief account of the raised beach of North Devon.


1870 ◽  
Vol 7 (67) ◽  
pp. 4-10
Author(s):  
John Rofe

Within the last few months considerable, interest has been revived on the question of the origin of certain small excavations or borings which have been found in limestone rocks in different localities in Sicily, France, England, and Wales. The first public notice of them in England was by Dr. Buckland, whose attention, when at a meeting of Geologists at Boulogne in 1839, was called to some borings which had been found in the under-surface of a ledge of Carboniferous Limestone rock in the Boulonnais. After this Dr. Buckland examined some similar borings which the Rev. N. Stapleton had observed near Tenby, and described both caseg, in a communication to the Geological Society in 1841. About the same time that Dr. Buckland was engaged with these excavations, M. Constant Prévost found some similar perforations on Monte Pelegrino, near Palermo. Mr. C. P. Jopling discovered them in Furness in 1843. M. Bouchard Chantereaux, who met with them in the Bois des Roches, in the Bas Boulonnais, has published a memoir on the subject, the result of many years observation, to which I shall have occasion again to refer. Mr. Pengelly met with them in many localities in the Torbay district. They were also found on Birkrigg Common by Miss E Hodgson, of Ulverston, and were described by her in vol. vii of The Geologist, p. 42.


Think India ◽  
2019 ◽  
Vol 22 (3) ◽  
pp. 72-83
Author(s):  
Tushar Kadian

Actually, basic needs postulates securing of the elementary conditions of existence to every human being. Despite of the practical and theoretical importance of the subject the greatest irony is non- availability of any universal preliminary definition of the concept of basic needs. Moreover, this becomes the reason for unpredictability of various political programmes aiming at providing basic needs to the people. The shift is necessary for development of this or any other conception. No labour reforms could be made in history till labours were treated as objects. Its only after they were started being treating as subjects, labour unions were allowed to represent themselves in strategy formulations that labour reforms could become a reality. The present research paper highlights the basic needs of Human Rights in life.


2018 ◽  
Vol 11 (2) ◽  
pp. 41-51 ◽  
Author(s):  
I. Ya. Lukasevich

The subject of the research is new tools for business financing using the initial coin offering (ICO) in the context of the development of cryptocurrencies and the blockchain technologies as their basis. The purpose of the work was to analyze the advantages and disadvantages of the ICO in comparison with traditional financial tools as well as prospects, limitations and problems of using digital financial tools. Conclusions are made in relation to possibilities, limitations and application areas of digital business financing tools, particularly in the real sector, taking into account the specifics of the Russian economy and legislation. It is shown that the main problems of using the digital financial tools are related to the economic sphere and caused by the lack of adequate approaches to evaluation of assets as well as the shortage of objective information. The problems and new tasks of corporate finance in the digital economy are defined.


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