J2merican Geological Society. • Lssociation of £Merican Geologists. Ed

J2merican Geological Society. 219 But if the fire be placed at the lower extremity of a vertical tube Or Chan- nel leading out of the apartment, the rarifaction of the gas by heal: Causes it to expand within the tube, and the column within being lighter than the corresponding column without, the former is forced up by the colder air which rushes in to maintain the equilibrium. This is precisely the action of a common chimney, which may be termed a self-acting ventilator of the most perfect kind. Two circumstances are requisite to render the chimney effective, first the fire should be so nearly beneath it, that it may become heated; and secondly, there must be some other openings in the apartment for the admission of air; the latter are usually found in sufficient abundance in the crevices of the doors and windows, and the former is attained by making the fire in the fire.place, or in a stove connected with the chimney or pipe. Unless both these conditions are satisfied, neither a fire nor a large light should be kept burning in the apartment. The dangerarising from carbonic gas is somewhat increased by its pecu- liar preliminary efli~cts; when a person is in an apartment in which it is generated and gradually diffused, as from burning coals, or a light, theming- ling of successive portions of it with the air produces a gentle lethargy, which is so tar from being unpleasant, that the subject is inclined to resist any attempt to arouse him, and if not forcibly rescued will speedily sink into the repose of death. In cases of suspended animation from this cause, life may often be restored by timely application of cold water to the lace, ex- posure to a current of fresh air, or fanning, with the occasional application of spirits of hartshorne or camphor to the nostrils, the camphor in particular I have seen used with excellent effect. C. Physical Science. •~lssociation of £merican Geologists. At a meeting held at the rooms of the Franklin Institute in the City of Philadelphia, on the ~d of April, 1840, the following gentlemen were present, viz: Edward Hitchcock, Amherst, Mass.; Lewis C. Beck, New Brunswick, N. J.; Henry D. Rogers, Philadelphia; Lardner Vanuxem, Bristol, Pa.; William W. Mather, Brooklyn, Ct.; Walter R. Johnson and Fimothy A. Conrad, Philadelphia; Ebenezer Emmons and James Hall, Albany, N~ Y.; Charles B. Trego, James (3. Booth, M. H. Boy~, R. E. Rogers~ and Alex- ander McKinley, Philadelphia; C. B. Haydon, Smithfield, Va.; Richard C. Taylor, Philadelphia; Douglass Houghton anti Bela Hubbard, Detroit, Michigan. Prof. HITeItCOCK was appointed Chairma% and Prof. L. C. BECK, Secretary. It was then unanimously resolved to organize an Association to be called " The Association of ¢2rnerican Geologists." After the transaction of business relating to the election of additional members, the time and place for holding the next Annual meeting, &c., several communications were made to the Association and discussions had thereon. The following is a brief abstract of these proceedings. First Day.--Specimens were laid on the table, of quartz, phosphate and carbonate of lime, having a fused appearanc% occurring in St. Lawrence county, N. Y.~ and some views were olt~red concerning the causes which have given rise to it. Remarks having been made on this subject by several ~ Phgsical Science. other members, it was referred for a full report at the next meeting of the Association. Specimens were next presented, of the sandstones of Massachusetts, ex- hibiting the fossil footmarks, so called, and some observations made in regard to them. This subject was of so much interest as to induce the As- sociation to appoint a committee to visit the localities and to report their conclusions at the next meeting. After this, followed a discussion on the subject of Diluvial Action, in which several members took part. Information was communicated concerning the diluvial grooves or scratches which are observed in the valleys of the Hudson, Ohio, and Mississippi,--the polished limestones of Western New York,--tbe erratic blocks tbund in New York, Pennsylvania~ &c., and several points were suggested for tuture investigation. Second Day.--The lirst business was a lecture on some parts of the Geolo- gy of the state of New Jersey. Upon this, remarks were offered by several members; after which there was presented to tile Association, An outline of the Geology of the state of Michigan. The remaining part of the day was spent in free conversation on various geological sub- jects. Third Day.~The meeting was opened by some remarks on the apparent Stratification of Serpentine. A locality was referred to in the state of Pennsylvania where that rock exhibits the appearance of being regularly stratified. Several members presented facts concernirtg other localities bearing upon the question of the origin, whether strictly intrusive or meta- morphic, of certain belts of Serpentine. A statement was made in regard to the frequent occurrence of Fossil Infusoria in ahnost every town in New England in which primary rocks prevail. Amember remarked that aitevthe most diligent search he had been unable to detect them in the Cretaceous Groop. After remarks by several other members, the conclusion was, that so tar as Fossil Infusoria are known in this country, they are confined to the primary formations. A notice was next presented of the occurrence of the Native Black Perox- ide of copper on the shores of Lake Superior. This was tbllowed by remarks upon the copper ores of New Jersey. Some observations were then made regarding the Coal Fields of Penn- sylvania, particularly with reference to certain changes in the chemical. composition of the coal as we proceed from the east to the west. State- ments corroborating the general correctness of the views presented, and ex- tending the same to Ohio and Illinois, were made by other members. Some suggestions were next ofl~ered concerning the fertilizing properties of Mica. These led to some remarks on the cause of the fertilizing powers of the green sand, the peroxide of iron, &e.~when it was Resolved, that the subject of Mineral Manures be open for discussion at the next meeting, and that the members be requested to note all such facts as may contribute to its elucidation. Professor Silliman was then unanimously elected chairman for the next meeting, and the present chairman was requested to open that meeting with an address. The secretary was requested to prepare an abstract of the proceedings of this Session of the Association for publication in the American Journal of Science, and in the Journal of the Franklin Institute; when, after the usual resolution of thanks, the Association adjourned to meet in Philadelphia oa the first Monday" in hpril~ 1841. Lzwls C. B~.oK~ &oratory, ~I i~e~ription of an Optical Machine exhibited b~l Ma. R~. Rol~.It~s;of l~fan. chester, to the members of the British ./t~oociation~ at the meetCn$ of that body in Dubli% in the ~/ea~ 183~. .... ig. ~ 5, r , / ~ t • / • | s° ~1 i i ,i . 4 ~ t I e r x I I i / ~-- -- -~. _-~__~ i i i I d i i .... 1 a~ is the base plate, to which a plate b, and an upright arm c, connected with each other at the top by a cross.piece d9 are bolted~ forming ~ogether the frame of tile machine. 19" 2"22 Physical ~cience. e is a shaft, to which rotary motion may be given by the handlefl or by tt strap from a steam engine,'passing over a pulley g,~h, a toothed wheel gearing into i, a pinion on the shaft j,~k, a wheel on the same snalt gearing into !, an intermediate wheel that takes into the pinion ra, on the spindle n, ~to one end of which is secured a plate o, dovetailed on its face to receive and hold a card firmly, whilst the spindle revolves rapidly. To one end of the shaft j, is attached a plate p, and to this is riveted a disc r, of thin sheet iron, which, when the machine is in motion revolves freely within a flanch on the plate b. (This flanch is merely to prevent acci- dents to persons who may be about the machine.) In the plate b, opposite the centre of the spindle n, is a circular aperture s, about ~r of an inch diameter, and opposite to this aperture there is an oblong hole in the disc v, about an inch long in the direction of the disc~s diameter, and ~r of an inch broad. After the machine had been briefly explained to the section, it was placed in an anti.room where it remained during the meeting of the Association, that the members might have an opportunity of witnessing the phenomenon presented by it. For this purpose a card 5 inches long by £ inches broad, on the front of which was printed, Ill. I;oberts's • iaehine, which renders objects visible while revolving 40,000 times a minute, was examined by Dr. Dalton, Jan. 9, 1S35. was fixed to the face of the disc o, as the subject to be read while revolving rapidly. NoTz~Several hundreds of these cards were distributed, having printed on the reverse the following explanation. "When afirebrand is whirled in the dark, round a eentrein a plane per- pendicular to the eye of the spectator, it presents the appearance of a luminous circle. "From this fact it has been infered that the impression on the retina, made by the luminous body in its passage through every point of the cirel% remains until the body has completed a revolution.

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