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Updated: June 15, 2025
It is believed that chalk-beds still forming in some of our present seas may form one continuous mass dating back to earliest geologic ages. On the other hand, rocks different in character maybe formed at the same time in regions not far apart say a sandstone along shore, a coral limestone farther seaward, and a chalk-bed beyond.
"A French-chalk mine," said he, "would not be a bad thing, but I hoped that you had struck a bed of mineral gutta-percha. That would be a grand find." But the chalk-bed was at last passed, and we began again to bring up nothing but common earth. "I suppose," said my optimist to me, one morning, "that you must soon come to water, and if you do I hope it will be hot water." "Hot water!" I exclaimed.
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