 | William Thomson Baron Kelvin, Peter Guthrie Tait - 1867 - 914 pągines
...gravity to manifest its claim, aii«l sink the heavier solid below the lighter liquid. This proof— must go on until the sunk portions of crust build up from the bottom a sufficiently close ribbed solid skeleton or frame, to allow fresh incrustations to remain bridging across the now... | |
 | 1869 - 668 pągines
...may have r. taincd from tlie eballhlm or Uie liquid in s >me places, or, at all evems, it maybe hell up by the viscidity of the liquid, until it has acquired some considerable thickness Miftioient, to allow gravity to manifest its claim, and sink the beavier solid below the lighter liqniit.... | |
 | 1869 - 1500 pągines
...have r tained from tlie ebulliiini of the liquid in s 'in.- places, or, at all events, it may be hel.l up by the viscidity of the liquid, until it has acquired...lighter liquid. This process must go on until the sunk pur; ions of crust build up from the bottom a sufficiently close-riblied solid skeleton or frame, to... | |
 | James Samuelson, William Crookes - 1876 - 606 pągines
...thickness of a few metres when the surface would be cool and the whole solid dense enough to sink. " This process must go on until the sunk portions of...build up from the bottom a sufficiently closeribbed skeleton or frame, to allow fresh incrustations to remain bridging across the now small areas of lava... | |
 | British Association for the Advancement of Science - 1877 - 826 pągines
...attempt to prove that they are of marine origin, Transactions of the Boyal Society for Feb. 1830, p. 81. on until the sunk portions of crust build up from the bottom a sufficiently cloaeribbed skeleton or frame to allow fresh incrustations to remain, bridging aeróse the now small... | |
 | William Thomson Baron Kelvin, Peter Guthrie Tait - 1883 - 564 pągines
...incrustation at the surface must commence. (ee.) It is probable that crust may thus form over wide extents of surface, and may be temporarily buoyed up by the...sunk portions of crust build up from the bottom a sufliciently close ribbed solid skeleton or frame, to allow fresh incrustations to remain bridging... | |
 | William Thomson Baron Kelvin - 1890 - 564 pągines
...Britiih Attociatio* Report for 1847. 31. It is probable that crust may thus form over wide extents of surface, and may be temporarily buoyed up by the...portions of crust build up from the bottom a sufficiently close ribbed solid skeleton or frame, to allow fresh incrustations to remain bridging across the now... | |
 | William Thomson Baron Kelvin - 1890 - 578 pągines
...Action," Britith Association Heportjor 1847. 31. It is probable that crust may thus form over wide extents of surface, and may be temporarily buoyed up by the...portions of crust build up from the bottom a sufficiently close ribbed solid skeleton or frame, to allow fresh incrustations to remain bridging across the now... | |
 | William Thomson Baron Kelvin - 1890 - 546 pągines
...thicknesses of a few metres, when the surface would be cool and the whole solid dense enough to sink. " This process must go on until the sunk portions of...build up from the bottom a sufficiently close-ribbed skeleton or frame to allow fresh incrustations to remain, bridging across the now small areas of lava... | |
 | William Thomson Baron Kelvin - 1894 - 624 pągines
...thicknesses of a few metres, when the surface would be cool and the whole solid dense enough to sink. " This process must go on until the sunk portions of...build up from the bottom a sufficiently close-ribbed skeleton or frame to allow fresh incrustations to remain, bridging across the now small areas of lava... | |
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... in some places, or, at all events, it may be held up by the viscidity of the liquid; until it has acquired some considerable thickness sufficient to allow gravity to manifest its claim, and sink the heavier solid below the lighter liquid. This process... 
