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A stratum's upper surface was parallel to the horizon when formed, so every stratum except the lowest was bounded by two horizontal planes, and strata now vertical or inclined were once horizontal.
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Formalization: several. Exactly horizontal (false: clinoforms, cross-bedding) versus near-horizontal for most sediment (true).
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Strata were deposited horizontally; inclined strata were once horizontal
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Steno N, “De solido intra solidum naturaliter contento dissertationis prodromus”, Macmillan, New York (Univ. of Michigan Studies, Humanistic Series XI), English translation by John Garrett Winter, 1916 (1669); Prodromus, position of strata, p. 230. Scope: Sedimentary strata; original attitude of bedding.
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Steno N. De solido intra solidum naturaliter contento dissertationis prodromus. Macmillan, New York (Univ. of Michigan Studies, Humanistic Series XI), English translation by John Garrett Winter, 1916 (1669), 205-283
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Nicolaus Steno
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1669
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Winter's 1916 translation with Hobbs's foreword; the Latin original is in archive.org nicolaistenonisd00sten. The translation's year is 1916; the graph dates the claims to 1669.
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Public domain (1669; translation 1916).
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De solido intra solidum naturaliter contento dissertationis prodromus
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Reading copy of De solido intra solidum naturaliter contento dissertationis prodromus
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Page 230 of the reading copy; paragraph 612 of the normalised text 1669-steno.txt (sha256 ffd1648fdb362aea9dc6fd282f07770a1f6b4b1f2b4b87635f8d88f0a8d58dbb), produced by build/fetch.py and checked by build/check-quotes.mjs. The text itself is not committed.
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Hence it follows that strata either perpendicular to the horizon or inclined toward it, were at one time parallel to the horizon.
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Nicolaus Steno 1669 claim: Strata were deposited horizontally; inclined strata were once horizontal
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