The process of rapid superficial humifaction which takes place. here, is to be attributed doubtless to the temperature being so much higher than in the temperate zones, where a corresponding degree of decomposition would be the work of years.

From these delusions to those still more fashionable deceptions, practised by the whole tribe of magnetisers, the transition is very natural.

But being chiefly sections of younger rocks than ours, the Austrian diagrams exhibit a more disturbed surface, so far as regards faults and slips, snapped anticlinals, upshoved synclinals, lapped folds, […]

By the Stigiall flode, And the stremes wode Of Cochitos bottumles well; […]