MAKE A MEME View Large Image The Quarterly journal of the Geological Society of London (12513261734).jpg 1872 <br> OLDHAM AND MAHET CACHAE EAETHQTJAKE <br> 267 <br> And where apertures are provided at the same moment almost <br> by the earth-fissures the rising liquids ...
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Keywords: The Quarterly journal of the Geological Society of London (12513261734).jpg 1872 <br> OLDHAM AND MAHET CACHAE EAETHQTJAKE <br> 267 <br> And where apertures are provided at the same moment almost <br> by the earth-fissures the rising liquids will through these find <br> easy vent <br> As respects the height in the fissures //' to which the water of <br> the water-bearing or ooze-bed o o can rise when the mass C is <br> Fig 5 ” Diagram iUustrathig the Rise of Water in tJie Fissures <br> pressed down upon it by the vertical component of the wave-motion <br> if V the maximum velocity of the wave-particle which is in the <br> contrary direction impressed upon the mass C Avhose weight is <br> W then the impressed work accumulated in C is <br> TJ ” 1 _ V2 ˘ <br> '7 <br> and as the mass C is not free to move in the direction B A the <br> horizontal component of the wave's motion whose wave-path is <br> A B makes the angle B with the horizon ; i e 6 is its angle of <br> emergence <br> Then in the vertical the impressed work is <br> but <br> V2 <br> V sm df 2g h or h i ” <br> h being the height due to the velocity in the vertical <br> Hence the minimum height to which the water from the ooze- <br> bed will be raised by the depression of the mass C is 7i in feet <br> provided there is enough water in the ooze-bed and that the latter <br> is easily compressible <br> This is on the assumption that the specific gravity of the mass C <br> is the same as that of water ; but as dense earth is about sp gr 1-92 <br> so the actual minimum height of water-rise in the fissure /' will be <br> 1-92 7i <br> We have no information as to either the wave-velocity or the angle <br> of emergence for any locality in this Cachar earthquake If how- <br> ever we assume the velocity in the vertical component to be 30 feet <br> v2 34985276 108770 51125 Page 267 Text v 28 http //www biodiversitylibrary org/page/34985276 1872 Geological Society of London Biodiversity Heritage Library The Quarterly journal of the Geological Society of London v 28 1872 Geology Periodicals Smithsonian Libraries bhl page 34985276 dc identifier http //biodiversitylibrary org/page/34985276 smithsonian libraries Information field Flickr posted date ISOdate 2014-02-14 Check categories 2015 August 26 CC-BY-2 0 BioDivLibrary https //flickr com/photos/61021753 N02/12513261734 2015-08-27 10 00 29 cc-by-2 0 PD-old-70-1923 The Quarterly journal of the Geological Society of London 1872 Photos uploaded from Flickr by Fæ using a script
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