The London, Edinburgh and Dublin Philosophical Magazine and Journal of ScienceTaylor & Francis, 1875 |
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Common terms and phrases
acid Ångström anhydrous aniline appears aurora axis bands binomial body boron bright brine calculated calorimeter carbon cent centims chloride circuit coil colour constant containing cooled corresponding crater cryohydrate crystals curve determined diameter diamond diffused direction discharge disk distance effect electromotive force elements equal equation error eruption experiments extra current flame force freezing-mixture give given glass graphite grms hydrate hydrogen iron Leyden jar light lines liquid magnetic magnetic moment means measured metal method metres millim molecules NaCl needle observed obtained ogive paper pencil phenomena Phil placed plate platinum polarized poles portion position produced quantity ratio represent resistance S. P. WOODWARD salt saturated separated silicon slit solid solidified solution specific gravity specific heat spectra spectroscope spectrum substance surface Table temperature tion tube vapour vibrations vis viva water of crystallization wave-lengths weight
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Page 33 - I have heard of thee by the hearing of the ear : But now mine eye seeth thee. Wherefore I abhor myself, and repent in dust and ashes.
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Page 416 - The value of this work is almost inestimable. There can be no question that the amount of time and labour bestowed on it is enormous. . . . There is certainly no Metallurgical Treatise in the language calculated to prove of such general utility.
Page 160 - THE ANNALS AND MAGAZINE OF NATURAL HISTORY, INCLUDING ZOOLOGY, BOTANY, AND GEOLOGY. MONTHLY, PRICE 2s.
Page 73 - By W. Topley, Esq., FGS, Geological Survey of England. The author referred to many instances in which beds have unequal development, being much thicker in some places than in others ; and the main object of his paper was to show that such thickening and thinning of beds has an important effect in producing the apparent dip of overlying beds.
Page 479 - Cyrena fluminalls occurs in them. The author regards them as deposits from a great expanse of fresh water kept back by a barrier of polar ice descending far towards the south. In its greatest extension this ice-barrier would produce the crushing of the bed-rock ; and as it retreated, the water coming down from the higher ground in the south would cover a continually increasing surface. 4. " On the Microscopic Structure and Composition of British Carboniferous Dolerites.
Page 480 - ... proportions, just as is known to be the case in imperfectly fused slags. He maintains that there is an absolute identity of composition, structure, and mode of occurrence in these eruptive rocks of very widely separated geological periods, and that therefore they should be placed in one group. 5. " Additional Remarks on Boulders, with a particular reference to a group of very large and far-travelled erratics in Llanarmon parish, Denbighshire.