o cover t during times of tranquility, suc t toprofound internal forces as here.

    It ers t ton ional insights.

    From looking at  soil ed by t particles of tinually ed elses naturalconclusion tually be e smoot everyional process, some form of rene, t created neo keep taintops,  been deposited during floods, but ains t it  created neinents and t up mountain c is not too muco say t geologists grasp tions of t for te tectonics. Above all, on’s ted  Earts of time, far more ts o transform utterly our understanding of th.

    In 1785, ton ivemeetings of ty of Edinburg attracted almost no notice at all. It’s not o see  to his audience:

    In ted; for, after tuated by , it is by tion of tter of t titutes trinsic in relation to t violent fracture and divulsion; but till to seek; andit appears not in t is not every fracture and dislocation of tances of mineral veins,are found.

    Needless to say, almost no one in test idea . Encouraged by o expand ouc someumble onto clarity in a more expansive format, ton spent t ten yearspreparing wo volumes in 1795.

    togeto nearly a t pessimistic friends  from anyted ed of quotations from Frencill in the original French.

    A ticing t it  publisil 1899, more turyafter ton’s deat all.

    ton’s trong candidate for t read important book in science(or at least  so many otestgeologist of tury and a man t.

    Luckily ton ics atty of Edinburg only e silken prose but—to many years at ton’s elboually understood on rying