VI.—British Association for the Advancement of Science, Bournemouth, 1919

1919 ◽  
Vol 6 (12) ◽  
pp. 551-563
Author(s):  
J. W. Evans

Another direction in which the work of the Survey could with advantage be extended is in the execution of deep borings on carefully thought-out schemes by which a maximum of information could be obtained. Both in Holland and Germany borings have been carried out to discover the nature of the older rocks beneath the Secondary and Tertiary strata, and Professor Watts, in his Presidental Address to the Geological Society in 1912 (Proc. Geol. Soc., pp. lxxx–xc), has dwelt on the importance of exploring systematically the region beneath the wide spread of the younger rocks that covers such a great extent of the East and South of England. Professor Boulton, my predecessor in this Chair, has endorsed this appeal, but nothing has been done or is apparently likely to be done in this direction. It seems extraordinary that no co-ordinated effort should have been made to ascertain the character and potentiality of this almost unknown land that lies close beneath our feet and is the continuation of the older rocks of the west and north to which we owe so much of our mineral wealth. It is true that borings have been put down by private enterprise, but, being directed only by the hope of private gain and by rival interests, they have been carried out on no settled plan, and the results and sometimes the very existence of the borings have been kept secret. The natural consequences of this procedure have been the maximum of expense and the minimum of useful information.

1981 ◽  
Vol 19 (1) ◽  
pp. 173-182 ◽  
Author(s):  
Varda Eker

Corruption is a wide-spread phenomenon in the developing world. The term is usually reserved for ‘the practice of using the power of office for making private gain in breach of laws and regulations nominally in force’, or as more flamboyantly defined by M. McMullan, ‘a public official is corrupt if he accepts money…for doing something that he is under duty to do anyway, that he is under duty not to do, or to exercise a legitimate discretion for improper reasons’.1 Corruption is thus a description of activites emanating from and related to officialdom. Irregular activities among private individuals are a matter of private enterprise. They are not usually classified as corruption, but as straightforward theft, fraud, embezzlement, and the like.


1899 ◽  
Vol 6 (11) ◽  
pp. 501-505
Author(s):  
W. Boyd Dawkins

The discovery of a coalfield in 1890 at Dover, in a boring at the foot of Shakespeare Cliff, has been already brought before the British Association by the author at Cardiff in 1892, and is so well known that it is unnecessary to enter into details other than the following. The Carboniferous shales and sandstones contain twelve seams of coal, amounting to a total thickness of 23 feet 5 inches. These occur at a depth of 1,100 feet 6 inches below Ordnance datum, and have been penetrated to a depth of 1,064 feet 6 inches, or 2,177 feet 6 inches from the surface. They are identical, as I have shown elsewhere, with the rich and valuable coalfields of Somersetshire on the west, and of France and Belgium on the east


1907 ◽  
Vol 4 (2) ◽  
pp. 49-58
Author(s):  
William Whitaker

Among the many distinguished geologists and men of science whom one has been accustomed to meet, year after year, at the gatherings of the Geological Society, the British Association, and the Geologists’ Association during the past forty years, none has, by good camaraderie and hard work both in the field and study, established a better claim to our warm personal regard and esteem than Mr. Whitaker, whose portrait we present to our readers this month.


1914 ◽  
Vol 1 (2) ◽  
pp. 69-73
Author(s):  
R. M. Deeley

In 1866 I communicated a paper to the Geological Society of London on the Pleistocene Succession in the Trent Basin. The boulderclays and outwash deposits of this district are of two distinct kinds, the one containing rocks from the west and north-west, and the other boulders etc., from the east or north-east of the district. In all cases, except where they have been ploughed up and re-arranged by the ice itself, the drifts containing westerly rocks only are the lowest, and the drifts with easterly rocks have been spread over them. We thus have two distinct ice-flows to deal with.


1904 ◽  
Vol 1 (4) ◽  
pp. 166-172
Author(s):  
Alexander Ievixg

Mr. Alexander Somervail has been so good as to send me lately a paper read by him before Section C of the British Association at Southport, September, 1903, and printed in the Geological Magazine, Dec. IV, Vol. X, No. 472, October, 1903. The paper contains certain criticisms on the published work of Professor Hull, F.R.S., and myself among the Bed Rocks of the South Devon coast, with especial reference to “ the Base of the Keuper iu South Devon.” I desire to reply here to Mr. Somervail, and in so doing shall have to refer frequently to the three papers of my own published in the Quarterly Journal of the Geological Society in the years 1888, 1892, 1893, and to the paper by Professor Hull in the same Journal in the year 1892. For the sake of convenience and brevity I will refer to these papers by certain letters, as below.


2010 ◽  
Vol 37 (1) ◽  
pp. 39-57 ◽  
Author(s):  
P. G. Moore

Insights gained into the activities of the West of Scotland Regional Dredging Committee of the British Association for the Advancement of Science (BAAS): a committee comprising the Reverend Dr Charles Popham Miles (Chairman), Dr Robert Kaye Greville, Professor John Hutton Balfour and Thomas Campbell Eyton, are presented. Based particularly on previously unreported correspondence between Miles and Balfour, and between Greville and Balfour that is housed in the archives of the Royal Botanic Garden Edinburgh, the backgrounds of these persons (like their shared religious leanings) are illuminated and their practical experiences of dredging in the Firth of Clyde, notably in Lamlash Bay (Isle of Arran), brought into focus. Economic aspects relating to the costs of dredging, the finances of participants and the adequacy of the initial BAAS grant are highlighted and other social aspects commented upon. There is no known surviving contemporary account of the interactions between this network of BAAS dredging committee members, so this correspondence seemingly remains, to date, the only information that is available as primary sources.


1874 ◽  
Vol 1 (9) ◽  
pp. 404-411 ◽  
Author(s):  
R. J. Lechmere Guppy

In the Geological Magazine (Vol IV. p. 496) I have given some notes on West Indian Geology, with descriptions of a few new species of fossils. The notes were intended, in part, as supplementary to the papers published in the Journal of the Geological Society, and in the Geological Magazine, on the Geology and Palaeontology of the West Indies, and in part to exhibit an improved classification of the Caribean upper and middle Tertiaries.


1872 ◽  
Vol 9 (100) ◽  
pp. 433-441 ◽  
Author(s):  
Henry Woodward

When I first drew attention to this genus at the Bath Meeting of the British Association in 1864, only one nearly perfect specimen was known. Mr. Salter was acquainted with this form, so long ago as 1857, and referred to it, among other new and undescribed Crustacea, in a paper “On some New Palæozoic Star-fishes” found at Leintwardine, Shropshire, under the name of Limuloides. Portions of several others had also been met with, to which Mr. Salter attached MS. names in (the Museum of Practical Geology, Jermyn-street, but they have not been heretofore described. The most perfect of these Limuloid forms was described by me in a paper read before the Geological Society in June, 1865.3 (See Plate X. Fig. 1.)


1864 ◽  
Vol 1 (3) ◽  
pp. 102-106 ◽  
Author(s):  
T. Rupert Jones

Dr. Duncan'S researches on the Palæontology of the West Indies have so much enhanced the value of any fossils found in those islands, that I do not hesitate to make a few remarks on some Orbitoides contained in a piece of Antiguan ‘Chert’, given many years ago, by Dr. Nugent, to the Geological Society, and to which Mr. H. M. Jenkins, Assistant-Secretary G.S., some months since directed my attention; and also on some specimens of fossiliferous flint and limestone from Jamaica.


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