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stitution of the earth, or deranging the sister planets : moreover, the cause must be transitory, and one which, having acted its part once, may not have had occasion to repeat it in the long period of five thousand years. Any supposeable cause that would not fulfil these conditions, is insufficient for our purpose.

• Would a comet fulfil them? Much would depend on its bulk and distance. It would not fulfil them if we suppose a comet, large in comparison of the earth, to move in a line joining the centres of the two bodies, so as to produce a direct shock; but, if we suppose one of suitable dimensions to move in such a direction as would allow it only to graze the earth, it is not impossible that the shock of this body, a body, such as we require, out of the solar system, might produce the degree and kind of derangement which we are attempting to account for ; I mean, a great temporary derangement on the surface of the earth, unaccompanied by any material change of its planetary motion. Euler, who, in a treatise entitled “ De periculo a nimiâ comete appropinquatione metuendo,has investigated the changes that would be made in the elements of the earth’s orbit by a comet, its equal in bulk, coming almost in contact with it, finds that the attraction of such a comet would indeed alter the length of our year, but only by the addition of seven hours. The maximum effect resulting from the comet's attraction at the time of its passage, would be greater than we should be led to infer from the total result of its at. traction, after its final departure ; for the changes occasioned during its approach, would be in a great measure undone during its retreat: but, even at their maximum, they would not be very great; because, from the rapidity of the comet's motion, time would be wanting to complete them. A comet grazing the earth would be incompetent, Euler says, to produce even a deluge of our continents, unless the shortness of its stay were compensated by a magnitude of volume, exceeding that upon which he has founded his calculation.

' I shall conclude by remarking, that if the hypothesis of a shock derived from the passage either of a comet or of one of those numerous, important, and long neglected bodies, often of great magnitude and velocity, which occasion meteors, and shower down stones upon the earth, would explain the phenomena of the deluge, (a point upon which I forbear to give any opinion), we need not be deterred from embracing that hypothesis, under an apprehension that there is in it any thing extravagant or absurd. In the limited period of a few centuries, there is little probability of the interference of two bodies so small in comparison with the immensity of space; but the number of these bodies is extremely great ; and it is therefore by no means improbable, says La Place, that such interference should take place in a vast number of years.

Essay III. On the Inequalities which existed on the Surfuce o the Earth previously to diluvian action, and on the Causes of these Inequalities.-After admitting, that irregular crystallization, partial deposition, subsidence, earthquakes and volcanoes, may have

had considerable influence in producing some of the inequalities on the earth's surface, the author is still disposed to attribute by far the greater number of them to the action of running water. The general occurrence of conglomerate and greywacké on the confines of primitive rocks, seems to indicate a deluge similar in kind, though, perhaps, not equal in extent, to that which determined the present outline of ihe earth. . These considerations, which are despatched with much brevity, might, perhaps, with more propriety, have been included in the preceding Essay.

Essays IV. & V. On Formations.--On the Order of Succession in Rocks.-In opposition to the popular Wernerian notions of formations, or series of rocks of alleged contemporaneous origin, the author contends, that neither the intermixture of their ingredients, nor their alternations of occurrence, sufficiently justifies the inference of the simultaneous production of mineral substances; for, rocks generally held to be of very different ages, of ten present intermixtures of their component parts, or pass

into one another, while such a mutual blending is frequently not discoverable in others that are reputed to be of the same age. Yet, when two substances are distinctly incorporated in the same mass, it is difficult to conceive of them as generated at different epochs. Examples are also cited of alternating substances which are not regarded as coeval, while those which are deemed coen val, do not always alternate. So many exceptions to the principle of universal and partial formations, are, moreover, adduced, and so many formidable difficulties stated against its probability, that it ought, in fairness, to be abandoned.

• Unable to connect similar rocks of distant countries, obliged to connect dissimilar ones in the same neighbourhood, can any one uphold the doctrine of Universal Formations ? Let him, who answers in the affirmative, reflect on the consequences which that doctrine involves. He must admit, that, when the particles of quartz, feldspar, and mica, which had heretofore arranged themselves so as to form granite, changed their mode of arrangement so as to form gneiss, that change was conveyed with the rapidity of an electric shock from one end of the world to the other; that the currents of different hemispheres had so equable a motion ; that the particles borne along by these currents were so equally assorted; that, within the tropics, and without, the same depositions began and ceased at the same moment; that similar pebbles were detached from their native rocks, at the poles and at the equator, by equal forces acting under the same circumstances; and were deposited and cemented by the same means, and at the same time. _All this he must admit, or reject in toto the doctrine of Universal Formations.'

With regard to the Order of Succession in rocks, too, the facts which the author brings forth from his ample stores, are

calculated to shake our faith in the commonly received notions of the Wernerian schooi. Even the precedence of genealogy assigned to granite jas been successfully controverted: for this rock has been found to aiternate with gneiss, with mica-siate, and with schistus; nay, kitas has been coserved passing into it, and dipping beneath it. In some cases, it rests on quartz, on hornstone, on siate: anc, in France, not untrequentiy, co lime. stone. Again, the term pindument xi has, it shond seem, been gratuitously predicated of a particuiar description of prinite; * for, by the terms of the proposition, the bottom of this formation has never been seen, and consequency we have no means of ascertaining whether it be fundamenui or not.' Tie tables of sections in Ebei'; work may suffice to ccnvince us, that equal uncertainty prevails with respect to the relative position of ctner rocks reputed primitive. Besides, in 1. Testevery country, we find what are terr.ed transition rocks in the n est of primitive districts, or tice tercih; while the line of demarcation between even the primary and secondary classes, is far less distinct than has been generally surposed.

• It is said in the Wernerian theory, that, after the formation of all other strata, an immense delure suddenly occurred, and as suddenly retired, leaving, behind it, those scatteresi bummocks of focze trap, winich have, for some years, so great.y engiged the attention of geologists, The proots of this catastrocne, we are in urbed, are to be found in the great elevation which these rocks occasionally attain: in their broken stratification ; in their unconformadie posture ; and in the nature of their materiais.

• But are trap-rocks real.y more elevated than others ? or their stratification more broken? It is time enough to consider inferences when we have establisited facts. — If the posture of trap is orten unconformable, so is that of granite, sienite, hornbiend rock, purpurry, primitive Feenstore. &c.

* Every rock without exception lies, sometimes, in a conformatie, sometimes in an unconformable posture: and perhaps the different members of the forz-trap formation, as orten exhibit a wint of conformity towards each other, as, towards the beds on which they repose. — As to the nature of its materials-many of them are precisely the same as those found in other formations. The oniy rocks which are cited as peculiar to, and characteristic of, the newest fiütz-trup, are basalt, wacke, greystone, porphyry-siate, and trap-tuif. I am not sure that I know what greystone is : the only locality given of it by Jameson, is Vesuvius, where it is said to form a portion of the unchanged rocks. The doctrine, that it beiongs to the tütz-trap, therefore, is founded on an assumption, that we have the means ce distinguishing, in volcanic countries, substances which have been changed by the volcano from those which have nct-an assumption somewhat gratuitous. The remaining substances, viz. basist, wicht,

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porphyry-slate, and trap-tuff, are certainly not peculiar to this formation; as in England, Scotland, and Ireland, they are often found in terstratified with other formations much older. There is reason to suspect that, in Germany, trap-rocks of very different eras have been referred to the same era, and that much of that which has been supposed the newest flötz-trap in Scotland, and which ought, therefore, to be more modern than the beds of the basin of Paris, is coeval with red sandstone, mountain-limestone, and coal.

Essay VI. & VII. On the Properties of Rocks, as connected with their respective Ages. - On the History of Strata, as deduced from their Fossil Contents.The properties of rocks which are here considered, are their ingredients, structure, specific gravity, consolidation, stratification, posture with regard to the horizon, relative posture to one another, dip and direction, altitude, contained metals, and fossils. On cach of these heads the author offers some pertinent remarks; but which our limits will not not permit us to particularize. It is of importance, however, to notice, that the supposed relation between the age of a rock and the fossils which it contains, is often fallacious; and that the various facts which have now been collected concerning the interesting phenomena of organic relics, demonstrate the inaccuracy of some of the opinions which have been adopted by geologists of the first reputation.

Essay VIII. On Mineral l'eins. --According to our author's views, fissures have been produced principally by shrinkage; but others may have been caused, or enlarged, by the contraction of an adjoining mass, by the shock of an earthquake, or by failure of support, the erosion of subterranean waters occasioning subsidence. These fissures, or chasms, when filled with mineral matter, are called veins. Mr Greenough makes some excellent observations on their varieties, anomalies, and probable indications, which cannot fail to interest both the speculative geologist and the practical miner: but, while he rejects both the Huttonian and Wernerian hypotheses, relative to their formation, he sheds little original light on this obscure subject.

On the whole, however, he possesses the rare merit of stating his facts and opinions in a clear and manly, yet modest and respectful manner, untrammelled by preconceived systems, and unseduced by the fascination of great names. Truth, and truth alone, appears to have been the object of his extensive travels, of years of unwearied study, and of the devotion of an ample fortune to the prosecution of his favourite investigations. Nor will such praiseworthy efforts be without their reward, since they must evidently tend to assuage the angry contentions of conflicting geologists, and to demonstrate the superior va

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lue of patient inquiry and research, over hasty generalizations, or the construction of assailable theories. The brevity of the work, too, is the more meritorious, when we consider not only the rarity of that quality in books of this description, but the vast, and, we believe we might say, unparalleled extent both of reading and research which have gone to its composition. The prodigious number and bulk of the publications on Mineralogy and Geology which have been given to the world within these thirty years, have not only put correct information beyond the reach of ordinary readers—but have made it difficult for geologists themselves, at once to extend their own observations, and to keep clearly in view all that has been done by their associates. The work before us not only contains an admirable digest and collation of the most authoritative statements and opinions on a great variety of important questions, but is eminently calculated, by the contradictions which it everywhere exhibits, to abate the confidence of narrow observers and rash theorists; and to inculcate the necessity of that patient industry and modest scepticism, by which alone the pursuits of Geology can ever attain to the dignity of a Science.

Art. V. 1. Safe Method for rendering Income arising from Per

sonal Property available to the Poor-Laws. Longman & Co.

1819. 2. Summary Review of the Report and Evidence relative to the

Poor-Laws. By S. W. Nicol. York. 3. Essay on the Practicability of Modifying the Poor-Laws.

Sherwood. 1819. 4. Considerations on the Poor-Laws. By John Davison, A. M.

Oxford.

Our ur readers, we fear, will require some apology for being

asked to look at any thing upon the Poor-Laws. No subject, we admit, can be more disagreeable, or more trite: But, unfortunately, it is the most important of all the important subjects which the distressed state of the country is now crowding upon our notice.

A pamphlet on the Poor-Laws generally contains some little piece of favourite nonsense, by which we are gravely told this enormous evil may be perfectly cured. The first gentleman recommends little gardens; the second cows; the third a village shop; the fourth a spade; the fifth Dr Bell, and so forth. E

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