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 to say,most of time. In 1802, five years after ton’s deation of ttonian principles, entitled Illustrations of ttonian tefully received by took an active interest in geology,, to change. And how.
In ter of 1807, teen like-minded souls in London got toget tavern at Long Acre, in Covent Garden, to form a dining club to be called ty. to meet once a monto sions over a glass or t at a deliberately y fifteenso discourage tions soon becameapparent, titutional, ers, lemen, of course—and tening to eclipse tific society in try.
t til June, off to spend t people erestin minerals, you understand, or even academics for t part, but simply gentlemen ime to indulge a a more or less professional level. By 1830, the like again.
It is o imagine no geology excited teentury—positively grippedit—in a no science ever em, a plump and ponderous study of a type of rockcalled grey ant bestseller, racing tions, even t costeigrue tonian style, unreadable. (As even a Murcer conceded, it