1313.) M. De Luc, on Geological Phenomena. mountains in Somersetshire, named the Mendip-hills. I ascended these hills by the remarkable cleft called Chedder-cliffs, in which I pointed out indisputable proofs of a fracture, with angular motions, different in its opposite sides; and in particular I mentioned the openings of three caverns, at different levels, on these sides, relating what a well-informed inhabitant of the country had described to me of the interior form of these caverns. After wards I described the top of these hills, on which the lime-stone strata are bassetting-out: then I came to a great intersection of these hills, near the town of Wells, in which intersection is the opening of a famous cavern named Wookey-hole; whence, as well as at the foot of Cheddercliffs, issues a clear stream of water; a proof that there are in these hills large reservoirs, where the waters, muddy when they enter the crevices of the surface in time of rain, deposit their sedi. ments. I went some way in that cavern with the guide who is accustomed to attend the curious, and he gave me the same description of the internal parts of the hill, as I had heard at Chedder-cliffs; for he told me that these caverns also were interrupted by great faults, branching off in various directions; and he gave ine a proof that all these caverns communicated to one another from Wookey-hole to Chedder-cliffs; that a dog, entering at the former, and losing its way to return, had come out some days after at Chedder cliffs, quite emaciated. After having related all these circumstances, I came at p. 429 of the same volame, to shew that these caverns, in our continents, demonstrated the pre-existence of cavities in the globe. It is impossible to doubt that these caverns have been produced by some catastrophes of the strata, that catastrophe must have been occasioned either by the subsidence of the parts now the lowest, as in my system; or by the lifting up of the parts now the highest, which appears to be Mr. Farey's sense, when he speaks of lifts in Derbyshire. But, whatever be the case in this last respect, I decided that absolute dilemma, by the following peremptory argument. If the highest parts had been raised, there could not have existed any vacancy in the mass thus lifted up; since the pressure exercised from below, would have been communicated In succession to every part of the mass. Whereas, in the subsidence of the strata, there must haye remained vacancies with 1 23 all the characters observed in our caverns, in the manner which I have explained. In a journey after this, proceeding from Totness, along the river Dart, I described the singular changes, at the same level, between the lime-stone and the schisti, with grey-wacke; the former of which, in that country, are called slate; and the latter, dun-stone. Such a situation of strata, so different in their kinds, cannot have any other cause they catastrophes. I stopped at Buckfastleigh, a small town, situated in a dale, behind a small insulated hill, which attracted my attention; for I saw it consisting, on one side, of lime-stone strata, much broken; and on the opposite side, of slate and dun-stone. In walking quite around this hill, I met with a gentleman of the place, whom I found kindly disposed to answer my questions; his informations are related from page 104, of the second volume of my Travels in England; therefore I shall only give a short account of them. Having inquired of him, whether that mixture of different kinds of strata extended to a great distance, he answered me: "That in this country every thing indicated that there had been some great revolution, which had produced, not merely external disorder, but also great effects in the external parts of the ground." He then informed me, that in the mass of the calcareous strata, in parts where, being too deep, they did not appear externally, there were many caverns, of which he gave me the following particulars:-"They are divided into diferent chambers, adorned with pillars of sta lactites. It is very dangerous to proceed far in these caverns, con account of fissures so deep, that, if a large stone is thrown down them, it is heard for some time to strike against the sides, after which the noise generally dies away; but in some chasms, where, after some time, the stone can still be heard to reach the bottom, the sound is that of faling into water." This is again a phenomenon of the caverns of our Continents, which cannot be explained but by the subsidence of the broken strata, occasioned by previously existing cavities in the globe. This gentleman told me farther: "That these caverns communicated with each other by passages, more or less wide, forming a kind of subterranean labyrinth, where no body darst venture far, and of which, therefore, the extent remained uknown.' unknown." As an instance of this, he related to me, " that some time before, when he had been out shooting, one of his dogs, pursuing a rabbit, had entered a hole in a rock; that he waited for him, and called him a long time, but in vain; so that he had concluded him actually lost in some cavern: however, after some days, the dog returned home, but excessively lean and almost dying; so that, though much care was taken of him, it was a great while before he recovered." This is the same case as the dog in the caverns of the Meudip hills, and shows precisely the nature of those caverns. 24 Remarks on Mr. Farey's Notation of Musical Intervals. [Feb. 1, In the same part of my Travels, I described many other phænomena which I recommend to the attention of M. Farey, as they led me to the following conclusion, (repeated in many parts of my Travels, after similar descriptions :) "That no doubt can remain, that all the strata of that country have undergone subsidences, with angular motions of their parts divided by fractures; and that the low space through which the Dart now winds, is the part where this subsidence was the greatest." J. A. DE Luc. Windsor. To the Editor of the Monthly Magazine, I SIR, N reply to an inquiry that night well be made, respecting the utility and superiority of the notation of musical intervals chosen by Mr. John Farey, that gentleman remarks, that logarithms represent ratios " only when an indefinitely great number of places of figures are used, the least or the greatest musical intervals, those having the most simple ratios (as 1:2) having just as long a sound and complicated a common logarithm as the largest, most incommensurate, or complicated ratio." Now, I wish to ask the ingenious Mr. Farey, what he means, in this sentence, by a long sound; and next, what the length of a sound has to do with musical intervals? By the length of a sound, is generally understood its duration, or the length of time, which it continues audible; and the most ignorant in harmonics will admit, that an interval is the same whether the two sounds which form or constitute that interval, continue audible for one minute, for half an hour, or for any portion of time whatever. As Mr. John Farey writes for the public, your readers have a right to expect that he will descend" to give some explanation. Notwithstanding Mr. F.'s former en deavours at explanation, I remain one of the many who cannot perceive the superiority of the notation which he has derived from the manuscripts in the Royal Institution. I still think, with Lord Stanhope and the author of the Retrospect (vol. iv. p. 4, 1809), that his way of expressing an interval by Σ. f. and m. is as unnecessary as to express the number 8691 by 8000+600+3 score +2 dozen+7. If any of your readers have reasons for holding a different opinion of Mr. Farey's would-be-thought improvement in the calculation of intervals, they would afford me, and others, much pleasure by making those reasons public. Mr. Liston indeed calls the notation ingenious, but no-where employs it in his large folio of 144 pages, wholly. on musical intervals, entitled an "Essay on Perfect Intonation;" 1812. There is another practice of Mr. Farey's which, I am pleased to observe, is as little followed by respectable writers as the preceding. The practice to which I allude is the needless, or worse than needless, introduction of such words as the following, for which he seems to entertain a father's fondness: "Douzeave, quatorzeave, siezave, dixseptave, dixneuf ave, vingtunave, vingtduxave, vingtquatreave, cinquarteneufave." Philos. Mag. No. 170, &c.-Are these terms French or English? If French, why should we prefer French words to Latin or Italian ? Italian terms, it would appear, should have the preference, on account of that language being so much connected with music, and being, in the judgment of the great Dryden, the most musical of all languages, living or dead. If he is desirous to Frenchify our musical terms and to press the French cardinal numbers into his service, let him do so uni. formly, and write huitave instead of octave, &c. Perhaps, however, he may aspire to the reputation of a Hudibras, who "Could coin or counterfeit New words, with little or no wit, superparticular, subsuperparticular, sesquialterate, subsesquialterate, superpartient, subsuperpartient, submultiplex, superparticular," &c. &c. in Eu clid's Section of the Canon, and in some old and useless Treatises on Music. Mr. Farey's term douzeave, if I understand him, denotes a system in which there are eleven sounds differing in pitch, be LWEC tween any given sound, as C and its octave. Now a-days, when we have so many scales, as Hawkes', Loeschman's, Dr. R. Smith's, Liston's, &c. some new terms may be useful; but I do not like that they should be more than half French; nor do I approve of their having the termination in ave, because octave and septave, two established terms, are not employed to express that the interval 1:2 or viii. has so many different sounds between the two that constitute that interval as to divide it into eight or seven smaller intervals, but they are employed according to the musical degrees, -according to the literal names of the terminating sounds of the interval. The nomenclature of no science is so much 10 need of reformation as that of music, and, the longer Mr. F. may persist in the use of his mongrel names, the more will reformation be necessary: it will make hin the jest of the learned, though he may become the wonder of the ignorant. April 29, 1812. A. BODORGAN. To the Editor of the Monthly Magazine, SIR, SORRY ORRY I am to witness such a mistake relative to rice bread; and, in order to prevent farther imposition on your readers, be pleased to insert a few remarks: philosophers say, Look before you leap, which " F. S. S." has certainly omitted to do; for in the first place he, probably like Colonel Johnes, doubted the truth of its marvellous effects when he read of them, and he most likely set out with a mind filled with prejudice against rice; or, what is still more probable, he is a rice contractor for the British army in Portugal, or a regrater of bread corn, and is fearful of diminishing its consumption, as well as increasing the demand for rice. In the second place, he will recol lect that rice is like most other things, composed of good and bad, and most likely be procured very bad rice, on purpose to endeavour to frustrate Colonel Johnes's well-meant intentions. Exclusive of that gentleman's recoinmendation, in your Magazine for June, there was another under the signature of "Philanthropist," in the number for May; nor is this all, for I have seen it (with mine own eyes) recommended in twelve Magazines, which I could and would specify were it necessary, exclusive of several country and London Newspapers; and what, sir, have they all been " deceived by their servants!" for they were all under signatures. MONTHLY MAG. No. 237. Now, to a moral certainty, (which some folks say is no certainty at all) I have not been deluded by my servants, for, none can I afford to keep; lastly, as to its extreme unwholesomeness, I can only say that, I have eaten freely of it, and never felt any of the injurious effects; and, if it is so very unwholesome, how comes it to be used so much in our boarding-schools as it is, for puddings, &c. Again, I am acquainted with a very worthy gentlewoman, mistress of a small family of children, who have eaten ricebread for the last nine months, which I am sure would not have been the case, had it been judged in any degree inju rious to the health. S. LUKE. Newbury. To the Editor of the Monthly Magazine. sin, THE HE liberality which first induced you to afford me an opportunity of submitting to an impartial public, through the medium of your highly valuable publication, my claim to be considered the actual inventor of the improvements on the piano-forte, for which Mr. Loeschman obtained a patent, will, I trust, be extended, to allow me, for a moment, to trespass further on the patience of your numerous readers, whilst I briefly offer a few remarks on the conduct of the two gentlemen Mr. L. mentioned in his reply to mine of February last. In these Mr. L. made a feeble attempt to invalidate my statements, and to remove the impression they were calculated to make on the public mind, by endeavouring to establish two points: First, that he was under no obligation whatever for any assistance from me in the construction of his instrument, either scientific, original, or mechanical; for, at the period when he first requested my attention, "though he had not one completed, yet he had many in hand with six pedals."-Secondly, That all the sci entific knowledge I pretended to have afforded him, as something exclusively my own, was to be found in Kercher's and Dr. Smith's Harmonics; though he omitted to inform your readers at what part of either of these authors' works, the knowledge in question is to be found; and stating that, "it was from repeated interviews with an HonourableGentleman and Dr. Kemp, he was induced and enabled to perfect his invention." My circumstantial refutation of all these particulars, by a full detail of facts, dates, and an explicit statement of the information E 1 26 Meteorological Report at Carlisle, for 1812. information I actually afforded Mr. Loeschman, through your kind indulgence, appeared in your Magazine for June last. And I flatter myself, I must have fully substantiated my claim, and satisfied your readers of the veracity of all my respective statements. And, so conclusive, so unanswerable, were these statements, that Mr. Loeschman has never since ventured the slightest animadversion on any one of my charges or observations. That Mr. Loeschman should introduce the name of Dr. Kemp, and allude to an Honourable Gentleman, in the hope of prejudicing the public by their united respectability against crediting my single assertion, is not at all surprising; but, that these gentlemen should seem by their tacit acquiescence to give currency to his misrepresentations, is what indeed does surprise me! Particularly, as soon as I had read Mr. Loeschman's answer to my statements, and found their names implicated as supporting his misrepresentations, I waited upon Dr. Kemp and requested a few minutes' conversation with him; bot received for answer, "he was so much en [Feb. 1, gaged, he could not see me." In consequence, I communicated my business by letter, requesting he would have the goodness to inform me what instructions he had afforded Mr. L. in the construction of his six-pedal instrument, and at what time. Though this was at the beginning of April, I have never yet received any answer. About the same time, I also addressed a letter to the Honourable George Pomeroy, the gentleman to whom Mr. Loeschman alludes. It was delivered at his residence to a person who promised to give it him the moment he returned. The contents was similar to the one addressed to Dr. Kemp, but I have not been favoured with any reply. I, therefore, thus publicly call upon the Hon. George Pomeroy and Dr. Kemp, either to disavow all participation in Mr. Loeschman's misrepresentations, or to substantiate by indubitable evidence, that, previous to October 1808, they furnished Mr. Loeschman with the precise instructions which enabled him to construct his "six-pedal patent pianoforte." THOMAS GRENVILLE. No. 24, Store-street, Dec. 2, 1812. For the Monthly Magazine. 1813.] Remarks on the Weather at Carlisle, in 1812. experienced a dead calm. The range of the thermometer, this month, gives the excessive variation of forty degrees. February was most unseasonably mild, and extremely wet. The average temperature 41° 05, and density 29-53 inches, are in unison with the quantity of rain, 4.62 inches. The surrounding mountains were sometimes covered with snow. March. The average temperature of this month 36°-65, is 40-4 lower than that of the last, and nearly as low as January, excepting one mild day (28th,) the weather was throughout extremely cold. Much snow fell here, and in the surrounding country it was drifted to an immense depth. Not a mild shower of rain fell; the quantity 2.75 inches, is sleet and meited snow. Two brilliant parhelia were observed here from eight o'clock till near eleven on the morning of the 9th; the sun was in the centre, and the parhelia on each side, distant about twenty-five degrees, in a line exactly parallel to the horizon; the sky, during this period, was streaked with horizontal lines of thin white vapour; the parhelia were tinged with prismatic colours, like those of the rainbow. Barometer at the time S0 37, and rising. April. The weather continued with unabated severity during the whole of this month. The highest degree of the thermometer 51°, and the average for the whole month 40°-97, are unprecedented here; the snow which fell frequently covered the ground, and a great quantity lay on the neighbouring mountains. On the 26th we had a loud peal of thunder, and a heavy shower of hail. May. The first week was extremely cold and ungenial; between the 7th and 8th we experienced an increase of 37o of temperature. The weather afterwards was seasonable and pleasant, with light showers, till the middle of the month, when it again became cold and very drouglity, which continued till the 23d. The remainder was exceedingly fine, with refreshing showers, when vegetation began to make rapid progress. June. The former half of this month was temperate, but very droughty, not a drop of rain having fallen. The latter part was wet, gloomy, and exceedingly cold for the season; the rain which fell was generally mixed with hail. On the 17th and 25th we had some peals of thunder. The great quantity of snow which fell in March, and drifted on the sides of the mountains in this neighbour 27 hood, was not all dissolved before the end of this month. July. The greatest height of the thermometer this month 68°, and the aver age 56°-8, are unusually low for the season. The weather was invariably cold; from the 3d till the 19th it was very dry, with parching northerly winds. August. The weather during this month was also cold for the season; the average temperature 57°.3 is only half a degree higher than that of the pre. ceding month. The quantity of rain 2.58 inches, fell chiefly in moderate showers. On the 3d we had some peals of thunder; and on the night of the 18th, and the following morning, distant thunder, with incessant gleams of lightning. September was fair and seasonable tilt the 9th; the remainder of the month was often showery and drizzling, and rather unfavourable for the harvest. In the latter part of the month, the temperature was very variable; on the morning of the 29th we had a hoar-frost, when ice was observed. October. The weather during this month, though moist and gloomy, was not marked by violent winds, or heavy rains, yet the barometer continued unusually low, the average being 29.4. On the 19th, the mercury sunk to 28.13, and, excepting on the 15th of December, 1809, when it was 28.06, is the lowest ever observed here. November. The 7th, 8th, 19th, 20th, 21st, and 22d, were severe frost; on the 21st the thermometer was 12o below the freezing point. The rest of the month was moist and drizzling, and at times rather stormy. On the 17th, snow was observed on the mountains. December. The first six days were very mild and moist; on the 7th, a severe, but dry and pleasant frost, commenced, which continued without intermission till the 16th, when that and the two following days were rather stormy, with showers of snow. On the 22d, upwards of three inches depth of snow fell. The weather continued varying between frost and thaw from the 16th till the 28th, when the snow was all dissolved. The last four days of the month were ex. tremely mild and stormy. In the Monthly Magazine for February 1800, page 10, will be found a suinmary of the temperature, density, aud quantity of rain at Carlisle for the eight preceding years, Perhaps it may not be uninteresting to bring into one point E2. of |