XXVII. The Inner Earth

GA 97/1906-04-21/p004 ·1906-04-21 · English MediumMedium alignmentSome paragraph re-numbering between this translation and the German original — the locus may slip by a paragraph or two.
Record: listeners' notes. Written from listeners' notes, summaries, or memory rather than a shorthand transcript. The wording is the note-taker's as much as Steiner's: weigh a single striking phrase here far more cautiously than the same phrase in a stenographic volume, and do not rest an argument on one word. Evidence: «Notizen von einunddreißig Einzelvorträgen mit sechs Fragenbeantwortungen» (Notes of thirty-one single lectures with six question-answerings). Rudolf Steiner Verlag Gesamtverzeichnis 2022, volume subtitle. The translation is the maintainer's, not a published one.

Let me first of all remind you that present-day people have only managed to penetrate the outer shell of the earth to a very small depth. They have gone scarcely beyond a depth of 2,000 metres. Everything else, everything beyond this, is beyond their limits of penetration. And they would really be utterly surprised, perhaps even confused, if they did succeed in learning more about the deeper layers of this our earth. They would be confused because they would find things there that show only the faintest similarity to those we know on the earth's surface. They would not have words to describe most of them, for the states of matter inside the earth are indeed utterly different from anything we know up here. They would be utterly amazed to find that the metal which corresponds to our silver is liquid like mercury down there. And the same holds true for the other metals and the minerals.

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