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Image from page 806 of "Inglenook, The (1907)" (1907) by Internet Archive Book Images

<b>Identifier</b>: inglenook19079126bret <b>Title</b>: <a href="https://www.flickr.com/photos/internetarchivebookimages/tags/bookidinglenook19079126bret">Inglenook, The (1907)</a> <b>Year</b>: <a href="https://www.flickr.com/photos/internetarchivebookimages/tags/bookyear1907">1907</a> (<a href="https://www.flickr.com/photos/internetarchivebookimages/tags/bookdecade1900">1900s</a>) <b>Authors</b>: <a href="https://www.flickr.com/photos/internetarchivebookimages/tags/bookauthorBrethren_Publishing_House">Brethren Publishing House</a> <b>Subjects</b>: <a href="https://www.flickr.com/photos/internetarchivebookimages/tags/booksubjectChurch_of_the_Brethren__Periodicals">Church of the Brethren--Periodicals</a> <b>Publisher</b>: <a href="https://www.flickr.com/photos/internetarchivebookimages/tags/bookpublisherElgin__Ill____Brethren_Publishing_House">Elgin, Ill. : Brethren Publishing House</a> <b>Contributing Library</b>: <a href="https://www.flickr.com/photos/internetarchivebookimages/tags/bookcontributorBridgewater_College__Alexander_Mack_Memorial_Library">Bridgewater College, Alexander Mack Memorial Library</a> <b>Digitizing Sponsor</b>: <a href="https://www.flickr.com/photos/internetarchivebookimages/tags/booksponsorLYRASIS_members_and_Sloan_Foundation">LYRASIS members and Sloan Foundation</a> <b>View Book Page</b>: <a href="https://archive.org/stream/inglenook19079126bret/inglenook19079126bret#page/n806/mode/1up" rel="nofollow">Book Viewer</a> <b>About This Book</b>: <a href="https://archive.org/details/inglenook19079126bret" rel="nofollow">Catalog Entry</a> <b>View All Images</b>: <a href="https://www.flickr.com/photos/internetarchivebookimages/tags/bookidinglenook19079126bret">All Images From Book</a> Click here to <a href="https://archive.org/stream/inglenook19079126bret/inglenook19079126bret#page/n806/mode/1up" rel="nofollow"><b>view book online</b></a> to see this illustration in context in a browseable online version of this book. <b>Text Appearing Before Image:</b> <i>ent may apply forsome locality, perhaps, but not for every place for ithas been determined by experiment that the growthvaries according to the strength of the lime-water andthe rapidity of evaporation. Horace Hovev has de- volume or flow of the trickling water is so small andthe evaporation great enough that the greater partof the lime in solution is deposited before the waterflowing on the outside arrives at the tip. Some sta-lactites have the same diameter throughout. If morethan about two or three feet long, their formationcan be accounted for in the following way: the rateof deposit is the same everywhere as the trickling orrunning water flows down the form on the exterior.The cylindrical forms varying from one to thirty-six inches in length are formed usually in a differentway. These are hollow or tubular and have grownfrom their interiors. When the drop of water firsttrickles througli the roof of the cavern and evaporates,cr_\-stals of lime-carbonate are deposited. Since, while</i> <b>Text Appearing After Image:</b> <i>termined by actual experiment that in WyandotteCave stalactites increase one inch and stalagmites one-fourth inch in twenty-five years. In Howes Cave,N. Y.. he removed a stalagmite in 1874. Six year^later the newly formed stone image was measured.It was thirteen inches thick and four and one-halfinches high. So the rate in that locality is fairlyrapid. The pendent shafts of the Cathedral Spiresin the Cave of the Winds are about three or fourfeet long. At the rate for the Wyandotte Cave theseshafts required about twelve hundred years to develop;at the rate for Howes Cave sixty-four years; acother rates often used to make estimates, from eigh-teen hundred to thirty-si.x hundred years. Whicn-ever rate is taken as a unit of measurment, theirdevelopment seems to be slow. It almost requiresan eflrort of the mind to appreciate fully the time re-quired to form stalactites or columns of calcium car-bonate being a few score feet long and fifteen ortwenty feet in circumference like those at Lura</i> <b>Note About Images</b> <i>Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.</i>
غار ویاندوت (به انگلیسی: Wyandotte Cave) در جنوب ایالت ایندیانا در آمریکا است جنسش از آهک بوده و معبرهای آن دارای پنج سطح می‌باشد و یکی از بزرگترین غارهای آمریکای شمالی به حساب می‌آید.در این غار یک کوه به ارتفاع ۵/۴۰ متر وجود دارد که یکی از بزرگترین ... Read further
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