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Nevertheless, this work is expensive, so in order to keep providing tliis resource, we liave taken steps to prevent abuse by commercial parties, including placing technical restrictions on automated querying. Striated Rock-Surface at Wasdale Crao (From a Photo- graph by Mr. From Laurentian to (Jarboniferous and Permian, from Trias to Cretaceous, and from Eocene to Quaternary, the geological series appears to be fairly represented, not in continents only but also to a considerable extent in the large continental islands such as Great Britain and New Zealand.We also ask that you: Make non-commercial use of the files We designed Google Book Search for use by individuals, and we request that you use these files for personal, non-commercial purposes. Now this is certainly fi-ot what we should expect if the present continental areas had, at different epochs, risen out of the deep oceans. If oceanic and continental areas are interchangeable, it can only be because the very same causes (whatever they may be) that produce elevations and subsidences in the one produce them also in the other, and at first sight it appears probable that this would be the case. But a still greater difficulty remains to be considered. Hairy Saki \ V {YTGOi'Be Xes* Travels on the Amazon) Fachig 173 38. Lemurine Night Monkey (From Flower and Lydekker's Work) 173 40. Mr, Jukes-Browne, however, does not hold the view that they have been thus denuded, for he approvingly quotes Mr. In order to account for the actual contours of the ocean on this theory, we must suppose that, during subsidence, all the mountain ranges, peaks, valleys, and precipices were reduced to an almost uniform level surface by marine denudation, which, unless the process of subsi- dence were incredibly slow, seems most improbable.

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In order to make the subjects discussed more interest- ing to the general reader, I have, wherever possible, in- troduced copious illustrations, and this has led me in many cases so to modify and enlarge the original article as to render it a new piece of work. The p ERBf ANENCE OF Oc EANic Basins {Nc Uu Tol Science^ August, 1892). Our Molten Globe {Fortnightly Review, November, 1892) 40 IV. Erratic Blocks and Ice- sheets {Fortnig My Review, November, 1893) ... Flowers and Forests of the Far West {Fortnightly Review, December, 1891) 213 ANIMAL DISTRIBUTION. (3) The remarkable parallelism and com- pleteness of the series of geological formations in all the best known continents and larger continental islands, indicating that none of them have first risen from the ocean floor during any portion of known geological history, a conclusion enforced by the absence from any of them of that general deposit of oceanic ooze at some definite horizon, which would be at once the result and the proof of any such tremendous episode in their past history.STUDIES SCIENTIFIC , STUDIES// SCIENTIFIC ftp SOCIAL * -• BY ALFRED RUSSEL ^ALLACE LL. I have ventured to call them " Studies," because the larger part of them deal with problems in which I have been specially interested, and to the comprehension and solution of which I have devoted much time and thought. with any general interchange of oceanic and continental areas, or which render it exceedingly difficult to under- stand how such interchange could have been brought about.Many of these problems are connected with the modem theory of evolution, others with important geological and physical theories, others again with educational, political, or social questions. The Gorge of the Aar and its Teachings (Fortnightly Review, August, 1896) 129 DESCRIPTIVE ZOOLOGY. Monkeys : their Affinities and Distribution {Contem- porary Review, December, 1881) 146 Vm. These phenomena are : — (1) The enormous dis- proportion between the mean height of the land and the mean depth of the ocean, which would render it very- difficult for new land to reach the surface till long after the total submergence of the sinking continent.Usage guidelines Google is proud to partner with libraries to digitize public domain materials and make them widely accessible. Rock Groovings near Barmouth (From an unknown friend) 71 16. It is, that on all the present continents we nd either the same or a closely parallel series of geological formations, from the most ancient to the most recent.Public domain books belong to the public and we are merely their custodians. Rock Groovinos at Barmouth (From a Photograph by Mr. Not only do we find Palaeozoic, Mesozoic, and Cainozoic rocks everywhere present, but, in proportion as the con- tinents are explored geologically, we find a tolerably complete series of the chief formations.Public domain books are our gateways to the past, representing a wealth of history, culture and knowledge that's often difficult to discover. Boulder Clay on Chalk, Flamborouoh Head (From a Photograph by Mr. Boulder Clay on Upper Oolite, Yorkshire (From Photo- graph by Mr. A Scandinavian Boulder pound in Yorkshire (From Photograph by Mr. Silurian Erratic on Limestone, Ingleborough (From Photograph by Mr. thousands of feet, rarely exhibit any difference of level on the land surface, owing to the fact that subaerial denuda- tion has kept pace with slow and intermittent elevation.

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