About: Playfair cipher is a research topic. Over the lifetime, 257 publications have been published within this topic receiving 1965 citations. The topic is also known as: Playfair system.
TL;DR: The history of the later portion of James Hutton's great work on the theory of the Earth is a perplexing question as discussed by the authors, and we do not know why his friends did not publish it.
Abstract: AS we learn from Sir Archibald Geikie in his interesting preface, the history of the later portion of James Hutton's great work on the “Theory of the Earth” is a perplexing question. In 1795 the well-known two volumes appeared, containing the first and second parts, but the title-page bears the words “in four parts.” Of those two the first is little more than a reprint of the essay on the same subject read to the Royal Society of Edinburgh in 1785. The second part, dealing with the operation of natural causes on the surface of the globe—or dynamical geology, as it is now sometimes called—was new matter. These volumes are without preface or preliminary sketch, so that no clue is given to the plan of the remainder of the work, while the fact that Hutton ends his second volume with an elaborate summary suggests that he contemplated a pause of some duration before issuing the remainder. At his death, in 1797, the third volume, according to Playfair, was practically complete; and we do not know why his friends did not publish it. Perhaps, as Sir A. Geikie suggests, they waited for certain illustrations, which Mr. John Clerk, Hutton's great friend, had promised to furnish. Gaps are left for these in the text; but, at any rate, Playfair and Lord Webb Seymour quote from the manuscript in a paper on Glen Tilt, read to the Royal Society of Edinburgh in 1814. It was then lost sight of—the earlier portion, including three chapters, has vanished; the other was a parting gift from Lord Webb Seymour to Leonard Horner, and was presented by him to the Geological Society of London in 1856. In its charge it has remained, forgotten by most of the Fellows, till Sir Archibald Geikie urged its publication on the Council, promising to take upon himself the laborious task of editing. Needless to say, this has been admirably done. The manuscript is printed as though it had followed on the preceding volumes. A few small lacunae or matters needing explanation are dealt with in explanatory notes, which are models of terseness and a great help to the reader, who, in addition, has to thank the editor for an index, not only to this volume, but also to the two others. Theory of the Earth with Proofs and Illustrations. In four parts. By James Hutton, M.D. and F.R.S.E. Vol. iii. Edited by Sir Archibald Geikie, D.C.L., F.R.S. (Geological Society, Burlington House, 1899.)
TL;DR: Jameson's System of Mineralogy as mentioned in this paper was the first attempt to explain the formation of the earth's crust and was published in Edinburgh in 1808 and published in London in 1816.
Abstract: Robert Jameson (1774–1854) was a renowned geologist who held the chair of natural history at Edinburgh from 1804 until his death. A pupil of Gottlob Werner at Freiberg, he was in turn one of Charles Darwin's teachers. Originally a follower of Werner's influential theory of Neptunism to explain the formation of the earth's crust, and an opponent of Hutton and Playfair, he was later won over by the idea that the earth was formed by natural processes over geological time. He was a controversial writer, accused of bias towards those who shared his Wernerian sympathies such as Cuvier, while attacking Playfair, Hutton and Lyell. He built up an enormous collection of geological specimens, which provided the evidence for his System of Mineralogy, first published in 1808 and here reprinted from the second edition of 1816. Volume 1 deals with what Jameson terms 'earthy minerals', including diamonds, rubies and feldspar.
TL;DR: A detailed architectural history of Edinburgh can be found in this article, which amalgamates the city's three main characteristics - a dramatic natural setting, an old town which evolved over several centuries and the Georgian "new town" which was conceived and built between 1766 and 1840.
Abstract: This architectural history of Edinburgh amalgamates the city's three main characteristics - a dramatic natural setting, an "old town" which evolved over several centuries and the Georgian "new town" which was conceived and built between 1766 and 1840. The book begins with the original proposals to build the New Town and ends a hundred years later with the death of William Playfair in the year of the completion of the National Gallery. It features period photographs of the city in the '50s by the late Sir Edwin Smith.
TL;DR: For example, the authors pointed out that as long as the science of the past is interpreted as being nothing more than ideas and knowledge about the external world of nature, its social and institutional aspects will continue to be disregarded.
Abstract: For obvious reasons the political and social effects of the French Revolution on Britain remain perpetually fascinating to political and social historians. Yet with the exception of the radical minister and natural philosopher Joseph Priestley, its influence on British scientists and institutions devoted to science has not received the attention it deserves. The reason for this neglect is clear: as long as the science of the past is interpreted as being nothing more than ideas and knowledge about the external world of nature then its social and institutional aspects will continue to be disregarded. If, however, past science is viewed as an activity which was socially organized and countenanced, we may expect it to have shown sensitivity in various degrees to some of the diverse elements in its social environment.