Last summer Miss D. L. Reynolds kindly organized an excursion of ten, all told, to discuss her recent paper on “The Eastern End of the Newry Igneous Complex”(Quart. Journ. Geol. Soc., xc, 1934, p. 585). We were introduced in most helpful fashion to both field exposures and microscope slices. In some particulars, differences of interpretation arose; and at the conclusion I circulated a brief memorandum. This by request I now offer, with trifling changes, for publication. Page and figure references, unless otherwise defined, apply to Miss Reynolds's paper.