The century dictionary and cyclopedia, a work of universal reference in all departments of knowledge with a new atlas of the world . of being isochro-nous ; the property of a pendulum by which itperforms its vibrations in equal times. isochronon (i-sokro-non), H. [< Gr. laoxpovov,neut. of laoxpovog,^ equal in time: see isochro-nous.] An equal time-keeper; a clock designedto keep perfectly accui-ate time. isochronous (i-sokro-nus), a. [< Gr. laSxpomg,equal in age or time, < laog, equal, + xp^^od _ time: see chronic] Same as isochronal. isochronously (i-sokro-nus-U), adv. Same asisochro
The century dictionary and cyclopedia, a work of universal reference in all departments of knowledge with a new atlas of the world . of being isochro-nous ; the property of a pendulum by which itperforms its vibrations in equal times. isochronon (i-sokro-non), H. [< Gr. laoxpovov,neut. of laoxpovog,^ equal in time: see isochro-nous.] An equal time-keeper; a clock designedto keep perfectly accui-ate time. isochronous (i-sokro-nus), a. [< Gr. laSxpomg,equal in age or time, < laog, equal, + xp^^od _ time: see chronic] Same as isochronal. isochronously (i-sokro-nus-U), adv. Same asisochronalli/. isochroous (i-sokro-us), a. [< Gr. laoxpoog, like-colored, < laog, equal, + ;tp()a, color.] Being ofthe same color throughout; whole-colored. isoclinal (i-so-klinal), a. and h. [As isocline +-al.] I. a. Of eqiial inclination: applied ingeology to strata which incline or dip in thesame direction. See monoclinal. The flexures are often so rapid that after denudation ofthe tops of the arches the strata are isoclinal, or appear tobe dipping .all in the same direction. A. Geikie, Text Book of Geology, p. 930 isoclinal. Isoclinal Lines for 1890. Isoclinal lines, in mofinetigm, lines drawn upon a mapthrough p*tints at all of which the dip of the needle is «. Same as isncHne. The directions of the isogonals, isoclinals, and lines ofequal horizontal force have been found. Nature, XXXIX (iso-klin), n. [< Gv. iang, equal, +K/.ivcn; ineliue: see cline.^ In geoL, a fold inwhich the strata are so appressed that the limbsor flanks (the parts on each side of the axis ofthe fold) are isoclinal, or dip in the same direc-tion. See monocUiie. Also called overturn, oroverturned (i-so-klinik), a. and «. [< isocline +-(<•.] Same as isoclinal. The wodinic lines of the globe run round the earth likethe parallels of latitude, but are irregular in form. S. P. Ttiompson, Elect, and Mag., p. 117. The whole region . . wo
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