In members of the same class the average amount of change during long and equal periods of time, may, perhaps, be the same, but as the accumulation of the long-enduring formations depends upon great masses having been deposited on areas while subsiding, our formations have been almost necessarily accumulated at wide and irregularly intermittent intervals; consequently, the amount of change exhibited (embedded in consecutive formations) is not equal; each formation does not mark a new and complete act of creations but only an occasional scene, taken almost at hazard, in a slowly changing drama ...
1 comment:
Um, MJ? Can I get a rosetta stone here?
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