scholarly journals I.—Note on the Discovery of Bos Primigenius in the Lower Boulder-clay of Scotland

1868 ◽  
Vol 5 (51) ◽  
pp. 393-395
Author(s):  
James Geikie
Keyword(s):  
The Other ◽  
Imperfect State ◽  
Boulder Clay ◽  
Core Measures ◽  
Outer Curve

It Will interest some of your readers to hear that remains of Bos primigenius have recently been obtained from the true till or lower Boulder-clay of Scotland. The specimens hitherto found appear to have come either from the fine Glacial brick-clays, which are posterior in date to the larger portion of our Boulder-clay, or from deposits of still later age. A few days ago I heard that the navvies employed in making the new “Crofthead and Kilmarnock Extension Railway” had come upon what was described to me as a “wounderful big bull's head.” I lost no time in visiting the locality, and saw the fossil in the possession of Mr. John Strain, C.E., who allowed me to examine it, and was afterwards kind enough to accompany me to the railway cutting in order to point out the exact spot from which the relic was taken. The skull is in rather an imperfect state, and only one of the horn-cores remains, the other having been broken off near the base. The perfect core measures 31 inches in length along the outer curve, and gives at its base a circumferences of 14 inches. The breadth of the forehead between the horns is 10 inches. From the character of the flat forehead, from the origin of the cores, and from the direction and curvature of the remaining one, there can be no doubt that the skull is that of Bos primigenius.

Aristotle's Wondering Children

Politeia ◽  
2019 ◽  
Vol 1 (3) ◽  
pp. 68-81
Author(s):  
Ioannis Alysandratos ◽  
Dimitra Balla ◽  
Despina Konstantinidi ◽  
Panagiotis Thanassas ◽  
Keyword(s):  
Moral Status ◽  
Philosophy Of Education ◽  
Ancient Philosophy ◽  
The Other ◽  
Human Beings ◽  
Human Flourishing ◽  
Systematic Account ◽  
Imperfect State ◽  
The One ◽  
Shed Light

Wonder is undoubtedly a term that floats around in today’s academic discussion both on ancient philosophy and on philosophy of education. Back in the 4th century B.C., Aristotle underlined the fact that philosophy begins in wonder (θαυμάζειν), without being very specific about the conditions and the effects of its emergence. He focused a great deal on children’s education, emphasizing its fundamental role in human beings’ moral fulfillment, though he never provided a systematic account of children’s moral status. The aim of this paper is to examine, on the one hand, if, to what extent, and under what conditions, Aristotle allows for philosophical wonder to emerge in children’s souls, and, on the other hand, how his approach to education may shed light to the link between wonder and the ultimate moral end, i.e. human flourishing. We will, thus, 1) try to offer a unified outlook of the philosopher’s views on children’s special cognitive and moral state, and 2) illustrate how wonder contributes in overcoming their imperfect state of being.

scholarly journals II.—On the Collocation of the Strata at Roswell Hole, near Ely

1868 ◽  
Vol 5 (50) ◽  
pp. 347-349
Author(s):  
Harry G. Seeley
Keyword(s):  
The Other ◽  
Boulder Clay ◽  
Geological Magazine

In the Geological Magazine, 1864, Vol. I. p. 150, and 1865, Vol. II. p. 529, two papers of mine appeared upon the strata at Ely. In them, as briefly as might be, are given the sequence of the beds from the Chalk to the Kimmeridge-clay, and the relations of these beds to the Boulder-clay and Kimmeridge-clay on the other side of the pit, where, on all hands, it is allowed to be in situ.

scholarly journals III. On Preglacial (?) Drift in Queen's County, Ireland

1865 ◽  
Vol 2 (16) ◽  
pp. 442-443
Author(s):  
G. Henry Kinahan
Keyword(s):  
Outer Margin ◽  
The Other ◽  
Coal Measure ◽  
Boulder Clay

‘The Coal-measure hills that form the outer margin of the Castlecomer table-land are generally covered with local drift; but the drift on nearly all the other Coal-measure hills is largely composed of limestone, even on the top of hills 700 feet high. What is most remarkable, however, is that in some places there are valleys and plains not more than 400 feet above the sea without a particle of limestone-drift on them, while hills in their vicinity are covered with it’.In sinking the various pits in the Queen's County Collieries, a Stratified Drift was found under some of this Boulder-clay. When the place was visited, none of these sections could be examined; but fortunately a record of each was kept in the ‘bore-books’ that are in the possession of the different agents and proprietors.

scholarly journals IV.—On the Formation of the “Rock-Basin” of Lough Corrib, County Galway

1866 ◽  
Vol 3 (29) ◽  
pp. 489-495 ◽  
Author(s):  
G. H. Kinahan
Keyword(s):  
Metamorphic Rock ◽  
The Other ◽  
Metamorphic Rocks ◽  
Northern Portion ◽  
Boulder Clay

Lough Corrib is a long irregular lake of various widths, but having a general bearing of about N.W. and S.E. Its N.W. portion is in a granite and metamorphic rock country, while the rest of it overlies Carboniferous rocks, principally limestone. The northern portion is deep, the southern shallow, and through the whole of it are scattered numerous islands which, in the former part, are generally composed of Boulder-clay, while those in the latter portion are nearly always rock. Its known natural outlets are two, one being over the barrier of metamorphic rocks at Galway (U on Map, Pl. XIX), and the other subterranean passage south of Castlegar (T on Map, Pl. XIX). On all sides of the lake are rocks extending under it, or, to use Professor Ramsay's term, it lies in a “Rock-basin.” What excavated this Rock-basin? I propose in this paper to consider.

I.—On the Sands and Gravels Intercalated in the Boulder-clay

1891 ◽  
Vol 8 (8) ◽  
pp. 337-348
Author(s):  
G. W. Bulman
Keyword(s):  
Ice Sheets ◽  
The Other ◽  
Cold Period ◽  
Glacial Geology ◽  
Boulder Clay ◽  
The One

The interpretation of the sands and gravels intercalated in the glacial drift is one of the most interesting problems in glacial geology. Do they, on the one hand, represent the deposits of one or more mild intervals alternating with periods of intense cold; or were they, on the other, laid down during one continuous cold period marked by such slight oscillations as can be shown to occur in connection with existing glaciers and ice-sheets?

The Gravels of Little Hayes, and the Age of the Crouch Valley, South-East Essex

1926 ◽  
Vol 63 (6) ◽  
pp. 273-275 ◽  
Author(s):  
J. W. Gregory
Keyword(s):  
The Other ◽  
Geological Survey ◽  
The South ◽  
Railway Station ◽  
Small Patch ◽  
North West ◽  
Previous Note ◽  
Boulder Clay ◽  
The One

The rarity of drifts in the Crouch Valley has been often remarked. The only river gravel marked in it on the Geological Survey Map, sheet I N.E., is a small patch at Little Hayes, a couple of hundred yards north of the Crouch, and 1¼ miles S.S.W. from Woodham Ferrers railway station. In the Evolution of the Essex Rivers (1922, p. 47), an analysis of the five chief constituents, based on a collection made by Mr. H. J. Nicholson, recorded some Jurassic sandstones which I regarded as probably derived from the boulder clay on hills about three miles north and north-west. A visit to the pit last year in order to obtain larger specimens of the Jurassic material yielded various cherts; one is a typical Rhaxella chert, which has not been previously recorded so far to the south-east. A thin bedded oolitic chert, which was different to any that I knew, was submitted to Mr. H. C. Sargent with the inquiry whether it might be one of the Carboniferous cherts of the Midlands. Mr. Sargent identified some of the inclusions as silicified oolitic grains, and rejected the rock as Midland Carboniferous. The specimens and slides were also kindly examined by Professor Boswell, who showed them to Mr. E. T. Dumble for comparison with the Rhaxella chert found by him in the Crag; they also did not know any similar rock. The specimens were then sent to Dr. Morley Davies, who confirmed the identity of the one specimen with the ordinary Oxford-Buckingham Rhaxella chert, and has, in the previous note, described the other as a Rhaxella chert in which the spicules are the nuclei of oolitic grains.

IV.—Report on the Drift at Moel Tryfaen

1900 ◽  
Vol 7 (3) ◽  
pp. 115-123 ◽  
Author(s):  
E. Greenly
Keyword(s):  
Scientific Work ◽  
The Other ◽  
Rock Surface ◽  
Boulder Clay ◽  
High Level ◽  
Short Time

In August, 1898, it became known that what is perhaps the clearest and most instructive section in the famous high-level drift deposits at Moel Tryfaen must in a short time be swept away in the course of the quarrying operations. There are two slate quarries on Moel Tryfaen, the “Alexandra” and the “Moel Tryfaen” Quarries, excavated in the same line of strike of the slates. Gradually expanding, they had approached each other so nearly as to leave a narrow bank between them with no more than a yard or two of uncut turf upon it. Now the drift sections thus in danger of destruction are exceedingly important for the following reasons: (1) They are at right angles to the strike of the slates, and thus display the character of the underlying rock surface; (2) they show the nature and position of the junction of the shelly sands and gravels with the overlying Boulder-clay; (3) the false bedding and other structures in the sands and gravels are best seen along them; (4) they have been more accessible than the other sections in the quarries. A Committee was therefore appointed to preserve, by photography, supplemented by a written report, an impartial record of the phenomena displayed in these sections. The Committee have much pleasure in acknowledging their obligations to Mr. Menzies, the manager of the Alexandra Quarry, who, with a large-minded appreciation of scientific work for which geologists cannot be too grateful, offered to suspend operations in that part of the quarry for three months, besides showing the Committee every hospitality and facilitating their work by all means in his power.

Stromatoporoids from the Famennian (Devonian) Wabamun Formation, Normandville oilfield, north–central Alberta, Canada

1988 ◽  
Vol 62 (03) ◽  
pp. 411-419 ◽  
Author(s):  
Colin W. Stearn
Keyword(s):  
Patch Reef ◽  
Abundant Species ◽  
The Other ◽  
North Central ◽  
Biotic Crisis

Stromatoporoids are the principal framebuilding organisms in the patch reef that is part of the reservoir of the Normandville field. The reef is 10 m thick and 1.5 km2in area and demonstrates that stromatoporoids retained their ability to build reefal edifices into Famennian time despite the biotic crisis at the close of Frasnian time. The fauna is dominated by labechiids but includes three non-labechiid species. The most abundant species isStylostroma sinense(Dong) butLabechia palliseriStearn is also common. Both these species are highly variable and are described in terms of multiple phases that occur in a single skeleton. The other species described areClathrostromacf.C. jukkenseYavorsky,Gerronostromasp. (a columnar species), andStromatoporasp. The fauna belongs in Famennian/Strunian assemblage 2 as defined by Stearn et al. (1988).

D. The Line Spectrum of Pulsating Variable Stars

1967 ◽  
Vol 28 ◽  
pp. 207-244
Author(s):  
R. P. Kraft
Keyword(s):  
Variable Stars ◽  
The Other ◽  
Line Spectrum ◽  
Afternoon Session ◽  
Empirical Information ◽  
Pulsating Variable Stars ◽  
Almost Continuous ◽  
Informal Approach

(Ed. note:Encouraged by the success of the more informal approach in Christy's presentation, we tried an even more extreme experiment in this session, I-D. In essence, Kraft held the floor continuously all morning, and for the hour and a half afternoon session, serving as a combined Summary-Introductory speaker and a marathon-moderator of a running discussion on the line spectrum of cepheids. There was almost continuous interruption of his presentation; and most points raised from the floor were followed through in detail, no matter how digressive to the main presentation. This approach turned out to be much too extreme. It is wearing on the speaker, and the other members of the symposium feel more like an audience and less like participants in a dissective discussion. Because Kraft presented a compendious collection of empirical information, and, based on it, an exceedingly novel series of suggestions on the cepheid problem, these defects were probably aggravated by the first and alleviated by the second. I am much indebted to Kraft for working with me on a preliminary editing, to try to delete the side-excursions and to retain coherence about the main points. As usual, however, all responsibility for defects in final editing is wholly my own.)

C. The Continuous Spectrum of Pulsating Variable Stars

1967 ◽  
Vol 28 ◽  
pp. 177-206
Author(s):  
J. B. Oke ◽  
C. A. Whitney
Keyword(s):  
Continuous Spectrum ◽  
Variable Stars ◽  
Velocity Fields ◽  
The Other ◽  
Line Spectrum ◽  
Direct Information ◽  
Thermodynamic Structure ◽  
Diagnostic Interpretation ◽  
Pulsating Variable Stars ◽  
The Continuum

Pecker:The topic to be considered today is the continuous spectrum of certain stars, whose variability we attribute to a pulsation of some part of their structure. Obviously, this continuous spectrum provides a test of the pulsation theory to the extent that the continuum is completely and accurately observed and that we can analyse it to infer the structure of the star producing it. The continuum is one of the two possible spectral observations; the other is the line spectrum. It is obvious that from studies of the continuum alone, we obtain no direct information on the velocity fields in the star. We obtain information only on the thermodynamic structure of the photospheric layers of these stars–the photospheric layers being defined as those from which the observed continuum directly arises. So the problems arising in a study of the continuum are of two general kinds: completeness of observation, and adequacy of diagnostic interpretation. I will make a few comments on these, then turn the meeting over to Oke and Whitney.

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