Self-Duality
92 9MA THEMA TICS: J. v. NE UMANN PR;OC. N. A. S. 13 Loc. cit. See also Zisman, "Comparison of the Statically and Seismologically Determined Elastic Constants of Rocks," Proc. Nat. Acad. Sci., 19, 680 (1933). 14 Harold Jeffreys, The Earth, Its Origin, History and Physical Constitution, 2nd ed., Cambridge (1928). a L. D. Leet, "Velocity of Elastic Waves in Granite and Norite," Physics, 4, 375 (1933). CONTINUOUS GEOMETRY By J. V. NEUMANN INSTITUTRE FOR ADVANCED STUDY, PRINCBTON, N. J. Communicated January 8, 1936 Introduction. 1. The classical axiomatic treatments of geometry are all based on the notions of points, lines and planes, the "undefined entities" of the axiomatization being either the two distinct classes of points and lines, or the three classes of points, lines and planes.I Thus the lowest- dimensional linear subspaces of the given space receive chief attention ab initio. The suggestion of replacing these distinct' classes of "undefined entities" by a unique class which consists of all linear subspaces of the given space, was first made by K. Menger.2 An essential part of his system was the axiomatic requirement of the existence of an integer-valued function (with any linear subspace as argument) which possesses the formal properties of linear dimensionality.8 These investigations were carried further by G. Bergmann,4 who replaced the explicit postulation of the existence of an integer-valued dimension function by axioms securing the existence of points and by certain requirements concerning the algebraic properties of points. Recently K. Menger has taken up the subject again, and has given a system of axioms in which the axioms on the algebraic properties of points are simpler than those in G.
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