The North American Review, Volume 96Jared Sparks, James Russell Lowell, Edward Everett, Henry Cabot Lodge O. Everett, 1863 Vols. 227-230, no. 2 include: Stuff and nonsense, v. 5-6, no. 8, Jan. 1929-Aug. 1930. |
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Page 24
... Forbes calls dirt - bands . These bands are not , as he thinks , the effect of unequal disintegration of certain parts of the glacier ; they attach to the interstices of the beds , which gain the surface in the order of their succession ...
... Forbes calls dirt - bands . These bands are not , as he thinks , the effect of unequal disintegration of certain parts of the glacier ; they attach to the interstices of the beds , which gain the surface in the order of their succession ...
Page 32
... Forbes concluded that the ice was a viscous mass , urged onward by the mutual pressure of its parts . There has been much dispute as to what constitutes the theory of Mr. Forbes ; but , if we understand his writings , it is that the ...
... Forbes concluded that the ice was a viscous mass , urged onward by the mutual pressure of its parts . There has been much dispute as to what constitutes the theory of Mr. Forbes ; but , if we understand his writings , it is that the ...
Page 43
... Forbes commenced his measurements in 1842 , and , by taking the result of a few days only , actually observed the quicker central flow before Mr. Agassiz did . The results of Mr. Agassiz were , however , published before those of Mr. Forbes ...
... Forbes commenced his measurements in 1842 , and , by taking the result of a few days only , actually observed the quicker central flow before Mr. Agassiz did . The results of Mr. Agassiz were , however , published before those of Mr. Forbes ...
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