II.—Cyclones and Climate

1919 ◽  
Vol 6 (4) ◽  
pp. 158-162
Author(s):  
R. Mountford Deeley

From time to time I have been given an opportunity to discuss in the Geological Magazine the question of the cause or causes of climatic variations. The subject is one of deep interest to the geologist. Even Lyell, in the first edition of his Principles of Geology, gave a good deal of space to it, but contented himself with merely pointing out that variations in the distribution of the land would lead to changes in the climate. He wisely limited himself to this aspect of the question, for, at that time, the directions of the winds in middle latitudes were not such as meteorological theory would have led us to expect.

1935 ◽  
Vol 72 (4) ◽  
pp. 184-189 ◽  
Author(s):  
L. F. Spath

One of the problems left unsolved in my “Revision of the Jurassic Cephalopod Fauna of Kachh” consisted of the determination of the exact age of certain Jurassic beds that had yielded (in addition to ammonites) species of Trigonia. Among these, T. smeei J. de C. Sowerby is of unusual, general interest; and, as readers of the Geological Magazine may remember, this species has been the subject of much controversy. It was one of the species whose “morphological position, viewed from the evolutionary standpoint”, caused them to be described as Cretaceous. Thanks to the continued researches of Mr. J. H. Smith, of Bhuj, who has been good enough to send me new collections from various critical sections in Kachh, I am now in a position to add to the evidence for a Jurassic age of a number of these species of Trigonia. If it be asked why, in a work on cephalopods, I have gone out of my way to express scepticism regarding the use of species of Trigonia for correlation, I can only say that this genus happened to be represented among the ammonite material sent to me. There is no reason, so far as I can see, why Trigonia should not be quite as useful for zonal purposes as ammonites. I have been equally sceptical about Stolley’s work on belemnites. But in either case I will leave the results to speak for themselves. It seems to me that if Upper Oxfordian species like Trigonia smeei and such allies as T. tenuis, T. tra-peziformis, T. remota Kitchin, not to mention the associated Astarte, Gervillia, Cucullaea, Exogyra, etc., could be claimed to be of Cretaceous age by one of the most eminent authorities, then it is time to remind the general palaeontologist again of what workers on ammonites have realized long ago.


PEDIATRICS ◽  
1973 ◽  
Vol 52 (3) ◽  
pp. 462-463
Author(s):  
Randolph K. Byers

To Dr. Zisman: Dr. R. K. Byers, after noting that your questions "are ones to which there are probably no generally accepted answers" answered them as follows: Answer to Question 1: This depends on the habits of the operating physician. Personally, I use a good deal of local anesthetic, probably in 90% of the cases in which puncture is done for I think it is easier to do a lumbar puncture if the subject is unaware of the time that the needle is being stuck in his back.


1875 ◽  
Vol 2 (4) ◽  
pp. 168-172
Author(s):  
J. R. Dakyns

The publication in the Number of the Geological Magazine for November, 1874, of Mr. Goodchild's ingenious Drift theory leads me to make a few remarks on the subject.


1889 ◽  
Vol 6 (5) ◽  
pp. 211-214
Author(s):  
Robert Chalmers

A Paper on the Glaciation of Eastern Canada by the writer will shortly appear in the Canadian Record of Science, Montreal. It is intended to be a condensed statement of the principal facts hitherto collected on this interesting subject, with references to the reports and publications in which details are given. The following is an abstract which I send to the Geological Magazine in advance. The subject is regarded as an important one, and has occupied the attention of geologists for many years, as Eastern Canada is the battle ground, so to speak, of the advocates of the rival theories of continental glaciation and floating ice. The results thus far obtained from a somewhat careful study of its glacial phenomena, however, point to conclusions which are at variance with those held by extreme glacialists, and show that the theory of local glaciers upon the more elevated portions of the country and icebergs or floating ice striating the lower coastal areas during the Post-Tertiary submergence of these, as maintained by Sir William Dawson, will serve to explain all the observed phenomena.


Author(s):  
Andrew Stewart

This chapter discusses how there was a good deal of confusion about what strategy to follow in defending East Africa. The thinking of the few politicians interested in the subject, and within the regional governments, was flawed, with the dangers misunderstood or overlooked. Successive British governments showed no real sense of recognizing that this could be an important wartime hub for raw materials and training. These significant failings were compounded by the failure of senior military officers to make a compelling argument about Italian intentions and the potential challenge these presented. While the Chiefs of Staff in London were right to assume that Mussolini would focus on Egypt, due to the vital importance attached to controlling the Suez Canal, they were wrong to conclude that he would enter the war at the first opportunity.


1888 ◽  
Vol 5 (9) ◽  
pp. 408-414
Author(s):  
A. Irving

Considering the interest that has been awakened of late in the Bagshot Beds of the London Basin, and the paucity of good sections open to the light of day exhibiting any considerable vertical range of those beds, it has occurred to me that a fuller description of these Finchampstead sections may be of sufficient interest to students of Tertiary geology to justify its appearance in the pages of the Geological Magazine. In the task we have before us of attempting to workout the old physical geography of the Lower Thames Basin in later Eocene times, every contribution of facts (by no means the easiest part of inductive science) must be welcome to students of the subject. The problem was sketched in its outlines and bequeathed to his successors by the versatile mind of the late Prof. John Phillips, F.R.S. “In considering these remarkable strata (he says, of the London Bagshot Beds), which were accumulated in a period so near, geologically speaking, to our own, we are presented with problems of great interest, which, if they can be solved, will have more than local application.


1891 ◽  
Vol 8 (10) ◽  
pp. 456-458 ◽  
Author(s):  
A. J. Jukes-Browne

Until recently no outcrop of the Vectian or Lower Greensand was known to occur between Lulworth on the coast of Dorset and the neighbourhood of Devizes in Wiltshire. It was supposed that, with the exception of a small area of Wealden in the Vale of Wardour, the whole of the Lower Cretaceous Series in Dorset and South Wilts was concealed and buried beneath the overlapping Upper Cretaceous strata. A recent examination of this district however has revealed two areas where the Vectian sands emerge from beneath the Gault. One of these has already been indicated in the pages of the Geological Magazine; the other is the subject of the present communication.


1958 ◽  
Vol 14 (4) ◽  
pp. 399-410
Author(s):  
L. Nicolau D’olwer
Keyword(s):  

Dr. Silvio Zavala is to be congratulated on his draft chapter dealing with the history and influence of religion in the New World. The topic covers the planting of Christianity on American soil and, under its influence, the birth of a new society that was to be Christian in its institutions, in its culture, and, for several centuries, in all outward manifestations of its thought. In summarizing so broad a subject in few pages, Dr. Zavala leads us to ponder many extremely important points. The pages that follow are the product of a good deal of thinking, with regard both to the provisional text and to the subject in general. What a pity that meditation does not always succeed in fully clarifying our ideas and in completely dispelling our doubts!


Author(s):  
Jay Parini

Nobody just walks into a classroom and begins to teach without some consideration of self-presentation, much as nobody sits down to write a poem, an essay, or a novel without considering the voice behind the words, its tone and texture, and the traditions of writing within a particular genre. Voice is everything in literature, playing in the mind of the writer, the ear of the reader; the search for authenticity in that voice is the writer’s work of a lifetime. What I want to suggest here is that teachers, like writers, also need to invent and cultivate a voice, one that serves their personal needs as well as the material at hand, one that feels authentic. It should also take into account the nature of the students who are being addressed, their background in the subject and their disposition as a class, which is not always easy to gauge. It takes a good deal of time, as well as experimentation, to find this voice, in teaching as in writing. For the most part, the invention of a teaching persona is a fairly conscious act. Teachers who are unconscious of their teaching self might get lucky; that is, they might adopt or adapt something familiar—a manner, a voice—that actually works in the classroom from the beginning. Dumb luck happens. But most of the successful teachers I have known have been deeply aware that their selfpresentation involves, or has involved at some point, the donning of a mask. This taking on of a mask, or persona (from the Latin word implying that a voice is something discovered by “sounding through” a mask, as in per/sona), is no simple process. It involves artifice, and the art of teaching is no less complicated than any other art form. It is not something “natural,” i.e., “found in nature.” A beginning teacher will have to try on countless masks before finding one that fits, that seems appropriate, that works to organize and embody a teaching voice. In most cases, a teacher will have a whole closet full of masks to try on for size.


2019 ◽  
pp. 86-110
Author(s):  
Martin George ◽  
Antonia Layard

In 1925, England enacted substantial legislation that recast the existing Land Law, and which provided the framework on which modern Land Law was developed for more than seventy-five years. The essential framework remained intact until the enactment of the Land Registration Act 2002, which replaced, and substantially modified, the Land Registration Act 1925. But while the Land Registration Act 2002 is expected to be an important piece of legislation relating to land ownership in England, the 1925 legislation will still provide a good deal of the theoretical underpinning of the subject. This chapter discusses the main strategies of the Land Registration Act 1925, focusing on its effect on unregistered land. It first describes Land Law after 1925 before turning to legal estates, legal interests in land, equitable rights, land charges registration under the Land Charges Act 1925, unregistrable interests, and classification of interests.


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