The Quarterly Review, Volumes 262-263William Gifford, Sir John Taylor Coleridge, John Gibson Lockhart, Whitwell Elwin, William Macpherson, John Murray, William Smith, George Walter Prothero, Rowland Edmund Prothero (Baron Ernle) John Murray, 1934 |
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Page 276
... direction if deviation of any kind can be averted . When frequent turns are unavoidable , however , any idea of direction is inevitably lost to the utter stranger - or would be were he subject to human limitations - and one has only to ...
... direction if deviation of any kind can be averted . When frequent turns are unavoidable , however , any idea of direction is inevitably lost to the utter stranger - or would be were he subject to human limitations - and one has only to ...
Page 38
... direction in 1820 and at the same intervals until 1894. It is unnecessary , perhaps , to compare the epoch , at every stage , but , in the Northern Hemisphere , the first maximum of the earthquake period occurred in 1810-11 and the last ...
... direction in 1820 and at the same intervals until 1894. It is unnecessary , perhaps , to compare the epoch , at every stage , but , in the Northern Hemisphere , the first maximum of the earthquake period occurred in 1810-11 and the last ...
Page 39
... direction as during the principal earthquake , and retard them if it were on the point of slipping in the opposite direction . In other words , if the initial movement were to be continued , the epochs of the 42 - minute period would ...
... direction as during the principal earthquake , and retard them if it were on the point of slipping in the opposite direction . In other words , if the initial movement were to be continued , the epochs of the 42 - minute period would ...
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