Bathurst, John

New Brunswick s bedrock geology is well mapped and largely well understood. Because of NB s mineral wealth, a great deal of mineral exploration work has been carried out since the 1950s. The bedrock in NB is also diverse in age. The oldest Precambrian rocks can be found in the Saint John area, whereas some of the younger ones, in the form or Triassic basalts, occupy more than half of the Island of Grand Manan. Most of NB s rocks are of Middle Paleozoic age. The triangle between Moncton, Fredericton, and Bathurst is occupied by a thick sequence of Carboniferous rocks that host... 

McCutcheon, S.R., Walker, J.A. 2001. Voicanogenic massive suiphide deposits of the Bathurst Mining Camp Geoiogicai Association of Canada-Mineraiogicai Association of Canada, Joint annuai meeting, St. John s, Newfoundiand, Guidebook for Field trip B7, 89. 

The first person to study the new or post-Aristotelian chemistry in Oxford, however, seems to have been Dr Thomas Willis of Christ Church, who had, with his friends Ralph Bathurst and John Lydall, studied Chymistry in Peckewater Inne chamber in the late 1640s.Yet more of Willis anon. And then came Dr (later Sir) William Petty. Following the radical reorganisation of Oxford after the capture of King Charles I and the end of the first cycle of civil wars in the late 1640s, many new faces were intruded into the University by Parliament, to replace Royalist dons who would not forswear their loyalty to His Majesty and were thus ejected from their posts in 1648. To put it plainly. 

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