Clays And Shales Of Michigan Their Properties And Uses By H Ries Accompanied By Four Plates And Six Figures

Author : Heinrich Ries
Publisher : Rarebooksclub.com
ISBN 13 : 9781230157603
Total Pages : 254 pages
Book Rating : 4.1/5 (576 download)

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Download or read book Clays and Shales of Michigan; Their Properties and Uses, by H. Ries, Accompanied by Four Plates and Six Figures written by Heinrich Ries and published by Rarebooksclub.com. This book was released on 2013-09 with total page 254 pages. Available in PDF, EPUB and Kindle. Book excerpt: This historic book may have numerous typos and missing text. Purchasers can usually download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1900 edition. Excerpt: ...elsewhere In this report and in Part I. remarkable, that an intensely iron spring may discharge its highly mineral waters at the edge of a very pure marl bed. The grass about the spring will be covered with oxidized iron showing a red slime or even a bog iron effect, but the marl itself is not influenced in the slightest. It will generally be noticed that marls with the highest organic content also contain the highest percentage of iron and alumina. Insoluble and soluble silica. The per cent of insoluble silica is traceable to several sources. First of all, nearly all beds contain fine quartz sand independent of the ordinary coarse drainage sand and pebbles that may be washed into the bed as already explained. This sand can sometimes be found to permeate the bed from top to bottom, even when the bed is thirty feet deep. If, however, there is a very even layer of the organic lining above referred to, the sand does not seem to penetrate as well, if at all. The sand will be found in the purest beds to vary from a fraction of a per cent to several per cent in amount. This is in the case of a comparatively pure marl. In case a clay has at any time mixed with the bed the content of insoluble silica will vary, but will remain larger together with other disturbing features, such as the increase in magnesia before mentioned. Sometimes such a condition will produce an increase in content of magnesia toward the bottom of the bed, while in a pure bed little if any regular variation of magnesia has been discoverable with increase in depth from which sample may have been taken. Soluble silica. The marl is intimately associated with the remains of plants, no matter how pure it may be or at what depth it may be sampled. The same may be said in regard to...