ors, and made Mr. Bessemer possible, has contributed a large part toward making the world what it is. That it is not perfect, and has from time to time to be supplemented to meet the constantly developing wants of society, does not detract from its real value, or from the fact that whatever is brought in in addition to it is closely connected with it, and largely dependent upon it for the power to perfect itself. It was supplemented in the middle ages by something very like the manual training-schools, in the shape of the guilds, and the systems of apprenticeship and journeymen; and it is the workmen, who have deliberately cast these systems away, and are decrying all distinctions founded on excellence, and not the advocates of the old education, that have made the new training-schools necessary.
Contributions to the Tertiary Geology and Paleontology of the United-States. By Angelo Heilprin, Professor of Invertebrate Paleontology at the Academy of Natural Sciences of Philadelphia. Philadelphia: Published by the Author. 1884. Pp. 117.
Professor Heilprin has, in the present volume, made a valuable addition to the literature on this subject.
Besides offering a general systematic review and analysis of the formation taken as a whole, a concise statement is given of the geology of the tertiary period in all of those States of the Atlantic and Gulf border where the formation has been determined; each of these States is separately considered.
The second division of the book treats of the relative ages and classification of the post-eocene tertiary deposits of the Atlantic slope; and contains carefully prepared faunal lists of Maryland, Virginia, and North and South Carolina.
The other divisions of the volume relate respectively to the stratigraphical evidence afforded by the tertiary fossils of the peninsula of Maryland; to the occurrence of nummulitic deposits in Florida, and the association of nummulites with a freshwater fauna; a comparison of the tertiary mollusca of the Southeastern United States and Western Europe in relation to the determination of identical forms, and to the age of the Tejon rocks of California, and the occurrence of ammonitic remains in tertiary deposits. A map accompanies the volume.
The whole work bears the mark of careful study and research, and will undoubtedly greatly assist the labor of future workers in this field.
Annual Address. By C. V. Riley, as President of the Entomological Society-of Washington for 1884. Pp. 10.
The society had just closed its first year when this address was delivered (March 18, 1885). The address notices some of the more striking entomological events of the year, and brings forward some general observations that are suggestive. With reference to the Entomological Division of the Agricultural Department, of which Dr. Riley is the head, no one more fully than himself appreciates how far it falls short of his own ideal and of the necessities of the country, or "how difficult it is to build up to that ideal under the unfortunate political unscientific atmosphere that pervades the department. . . . It was to get away from official surroundings, away from the work of the United States entomologist, that the members of the division decided to join in the organization of this society. It was still more to get acquainted with those of kindred tastes outside the department, in Baltimore and elsewhere, as well as in Washington, and to cultivate social intercourse and interchange of views and experience." The various branches of the science are well represented in the society and in the various collections in Washington.
The Climatic Treatment of Disease: Western North Carolina as a Health Resort. By Henry O. Marcy. Pp. 24.
The former subject mentioned in the title is considered in the first fourteen pages of this pamphlet. Concerning the second subject, we have a description of the triangular region between the Blue Ridge and the Smoky Mountains of Northern North Carolina, where, within an area of fifty miles, there are twenty peaks over six thousand feet high; nine tenths of the entire district is an unbroken, primeval forest of the largest growth, chiefly of decidu-
