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Updated: May 28, 2025
C.2: Woolwich and Reading series: Argile plastique and lignite. C.3: Thanet sands: Sables de Bracheux. That gypsum has been selected by almost all Continental geologists as affording the best line of demarkation between the Middle and Lower Tertiary, or, in other words, between the Lower Miocene and Eocene formations.
Men worked and played and gambled and drank and joked and carried on the light-hearted, jolly existence of the camps just about the same as ever. Outside a few principals like Morton and his immediate satellites, there was no accurate demarkation between the desperadoes and the miners. Indeed, no one was ever quite sure of where his next neighbour's sympathies lay.
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