Mon′o‐clin″ic (?), a. [Mono- + Gr. � to incline.] (Crystallog.) Having one oblique intersection; — said of that system of crystallization in which the vertical axis is inclined to one, but at right angles to the other, lateral axis. See Crystallization.
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Webster's Dictionary 1913
Webster's Revised Unabridged Dictionary, C. & G. Merriam Co., 1913.