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Updated: May 12, 2025
They said that each belonged mainly to the Old Red Sandstone period; that the cavern fronts rose in innumerable and wonderfully regular strata high in the air, each stratum about five frog-spans thick, and that in the present discovery lay an overpowering refutation of all received geology; for between every two layers of Old Red Sandstone reposed a thin layer of decomposed limestone; so instead of there having been but one Old Red Sandstone period there had certainly been not less than a hundred and seventy-five!
They said that each belonged mainly to the Old Red Sandstone period; that the cavern fronts rose in innumerable and wonderfully regular strata high in the air, each stratum about five frog-spans thick, and that in the present discovery lay an overpowering refutation of all received geology; for between every two layers of Old Red Sandstone reposed a thin layer of decomposed limestone; so instead of there having been but one Old Red Sandstone period there had certainly been not less than a hundred and seventy-five!
It was a vast round flattish mass, ten frog-spans in diameter and five or six high. Professor Snail put on his spectacles and examined it all around, and then climbed up and inspected the top. He said: "The result of my perlustration and perscontation of this isoperimetrical protuberance is a belief at it is one of those rare and wonderful creation left by the Mound Builders.
It was a vast round flattish mass, ten frog-spans in diameter and five or six high. Professor Snail put on his spectacles and examined it all around, and then climbed up and inspected the top. He said: "The result of my perlustration and perscontation of this isoperimetrical protuberance is a belief that it is one of those rare and wonderful creations left by the Mound Builders.
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