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Updated: August 22, 2026
The primitive limestone presents spacious caverns as well as transition limestone,* and that which is exclusively called secondary. In the transition limestone we remark the caverns of Elbingerode, of Rubeland, and of Scharzfeld, in the Hartz; those of the Salzfluhe in the Grisons; and, according to Mr.
Here I took a narrow path through the woods, and after following a tediously long road over the hills, reached Elbingerode, where I spent the night, and left the next morning for Blankenburg. I happened to take the wrong road, however, and went through Rubeland, a little village in the valley of the Bode.
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