Some Remains (hitherto unpublished) of Joseph Butler, LL.D.

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A long argument took place, in which Butler supported the claims of reason, while Byrom defended the claims of authority. Byrom dined with Butler 14 Feb. In August Wesley had an interview with Butler. They had caused scandal, and the bishop probably felt it a duty to remonstrate. Wesley declined to give any promise Tyerman's Life of Wesley , i. At Bristol, Butler made the acquaintance of Josiah Tucker, afterwards the well-known dean of Gloucester. Butler made Tucker his domestic chaplain, and gave him a prebend in the cathedral.

Tucker tells us that Butler used to walk for hours in the garden behind his palace at night, and upon one such occasion suddenly asked his chaplain whether public bodies might not go mad as well as individuals, adding that nothing else could account for most of the transactions in history Tucker's Humble Address and earnest Appeal to the Landed Interest , p. On the death of Archbishop Potter in an offer of the primacy was made to Butler, who had in been made clerk of the closet to the king on the death of Egerton, bishop of Hereford.

Hearing, however, that his uncle had a chance of the archbishopric, he came up to town prepared to advance 20, l. In the bishopric of Durham was offered to Butler. It was proposed to him that the lord-lieutenancy of the county, previously attached to the bishopric, should be given to a layman, and that the deanery of St. Paul's to be vacated by him should be conferred upon Secker on condition that Butler should give the stall at Durham vacated by Secker to Dr.

Butler declined to allow the dignity of the see to be diminished by the separation of the lord-lieutenancy, or to agree to a contract which he thought simoniacal. He was accordingly appointed to the bishopric unconditionally. The arrangement, however, as to Chapman and Secker was carried into effect.

The lord-lieutenancy was not separated from the bishopric till the next vacancy. A plan for establishing bishops in the American colonies was suggested at this time by Butler Annual Register , , p. It came to nothing, but was noticed in a later controversy between Secker and a Dr. Mayhew, of Boston, in A contemporary reference is made in R. He delivered a charge in printed in his works.

He speaks incidentally of the influence of outward form in strengthening the beliefs, superstitions, and religions of heathens, Mahommedans, and Catholics. This pamphlet was republished with Blackburne's name by R. It is only worth notice as partly accounting for the report afterwards spread, that Butler had died a catholic.

Another circumstance which aroused the suspicions of his contemporaries was his erection in the chapel of his palace at Bristol of a slab of black marble over the altar, with an inlaid cross of white marble. It remained till the destruction of the palace in the Bristol riots of Secker on 23 May said that he regretted the cross, but emphatically denied the truth of the rumour.

Other letters appeared in the same paper, showing only that the writers were determined to believe, though without a tittle of evidence. Secker in a letter of 21 July replied, exposing sufficiently the utter groundlessness of the statement. A full account is given in the notes to Halifax's preface to Butler's Works , i. Butler does not appear to have taken any part in politics.

He had, however, a house at Hampstead, which had once belonged to Sir Henry Vane. The house was sold upon his death see Park's Hampstead , p. During his short tenure of the see of Durham, Butler showed great liberality, received the principal gentry three times a week, subscribed liberally to charities, and visited his clergy. The story was told that, in answer to some application for a subscription, he asked his steward how much money he had in the house.

Butler's health was failing, and his physicians sent him to Bristol and afterwards to Bath, where he died on 16 June He was buried in the cathedral at Bristol. The last tells Secker that Butler was constantly talking of writing to his old friend, even when unable to express himself clearly. By his will he left l. The balance of his estate after various bequests, including l. Bartlett , Forster, and now standing in the little room within my library at Hampstead, be burnt, without being read by any one, as soon as may be after my decease.

One portrait of Bishop Butler is in the Newcastle Infirmary, and was taken during his last illness. It is engraved in the Oxford edition of his works. Butler's position in contemporary speculation was unique. The deist controversy, which culminated about , is throughout in his mind, though he designedly abstains from special references.

The method of abstract metaphysical reasoning applied by his early friend Clarke both to ethical and theological speculations had led to a system which tended to reduce the historical element of belief to a secondary position or to eliminate it entirely. Butler, while admitting the validity of Clarke's reasoning, adopts the different method of appealing to observation of facts Preface to Sermons , p.

In this he follows Shaftesbury the only writer to whom he explicitly refers , who had endeavoured to show the general harmony between virtue and happiness; but he tries to fill a gap in Shaftesbury's argument by showing the natural supremacy of conscience, and therefore the existence of moral obligation, even where self-interest is opposed to conscience. The main result of the sermons is therefore the psychological system, in which the conscience is represented as holding a supreme position by its own self-evidencing authority among the various faculties which constitute human nature; while other passions, and in particular self-love and benevolence, are independent but subordinate.

The psychology, though somewhat perplexed, shows remarkable acuteness, and the argument that self-love, instead of being the sole or supreme faculty, really presupposes the existence of co-ordinate passions, is especially noteworthy. Butler greatly influenced the common-sense school of Hutcheson and his followers, who are also allied to Shaftesbury; and his influence upon Hume is perceptible, especially in Hume's admission of independent benevolent impulses, in connection with a utilitarian principle which had generally been interpreted as leading to pure egoism.

This leads to a consideration of the problem of free will and necessity, while the second part argues for the conformity between the doctrine thus taught by fact and the nature of the christian revelation. The impressiveness of Butler's argument, the candour of his reasonings, and the vigour and originality of his thought have been denied by no one. It is remarkable, indeed, that the greatest theological work of the time, and one of the most original of any time, produced little contemporary controversy. Locke, wherein his sentiments relating to personal identity are cleared up from some mistakes of the Rev.

This is a sequel to a vindication of Locke against Bishop Browne, and includes an answer to Andrew Baxter. These pamphlets are worthless. To some thinkers he appears as the most profound apologist of christian theology, while others have held that his argument leads to scepticism, because, while conclusive against the optimism of the deists, it really shows only that the difficulties in revealed theology are equalled by the difficulties of natural religion.

It is a retort, not an explanation, and therefore sceptical in essence. Mill 's Autobiography , p. A similar view is stated by Mr. James Martineau , who says Studies of Christianity , p. These, together with the correspondence with Clarke, form Butler's works. The first collected edition was published at Edinburgh in I keep my private Journal distinct from the above.

With respect to the land Planariae , unquestionably they are not molluscous animals. I read your letters last night, this morning I took a little walk; by a curious coincidence, I found a new white species of Planaria , and a new to me Vaginulus third species which I have found in S. America of Cuvier. Amongst the marine mollusques I have seen a good many genera, and at Rio found one quite new one. With respect to the December letter, I am very glad to hear the four casks arrived safe; since which time you have received another cargo, with the bird skins about which you did not understand me.

Have any of the B. Ayrean seeds produced plants? From the Falklands I acknowledged a box and letter from you; with the letter were a few seeds from Patagonia. At present I have specimens enough to make a heavy cargo, but shall wait as much longer as possible, because opportunities are not now so good as before. You tell me you like hearing how I am going on and what doing, and you well may imagine how much I enjoy speaking to any one upon subjects which I am always thinking about, but never have any one to talk to [about].

After leaving the Falklands we proceeded to the Rio S. Cruz, following up the river till within twenty miles of the Cordilleras. Unfortunately want of provisions compelled us to return. This expedition was most important to me as it was a transverse section of the great Patagonian formation. I conjecture an accurate examination of fossils may possibly determine the point that the main bed is somewhere about the Miocene period using Mr.

Lyell's expression ; I judge from what I have seen of the present shells of Patagonia. This bed contains an enormous field of lava. This is of some interest, as being a rude approximation to the age of the volcanic part of the great range of the Andes. Long before this it existed as a slate and porphyritic line of hills. I have collected a tolerable quantity of information respecting the period and forms of elevations of these plains. I think these will be interesting to Mr. Lyell; I had deferred reading his third volume till my return: you may guess how much pleasure it gave.

I had my barometer with me, I only wish I had used it more in these plains. The valley of S. Cruz appears to me a very curious one; at first it quite baffled me. I believe I can show good reasons for supposing it to have been once a northern straits like to that of Magellan. When I return to England you will have some hard work in winnowing my Geology; what little I know I have learnt in such a curious fashion that I often feel very doubtful about the number of grains [of value?

Whatever number they may turn out, I have enjoyed extreme pleasure in collecting them. I have already seen enough to be convinced that the present families of corallines as arranged by Lamarck, Cuvier, etc. It appears that they are in the same state [in] which shells were when Linnaeus left them for Cuvier to rearrange. I do so wish I was a better hand at dissecting, I find I can do very little in the minute parts of structure; I am forced to take a very rough examination as a type for different classes of structure.

It is most extraordinary I can nowhere see in my books one single description of the polypus of any one coralline excepting Alcyonium Lobularia of Savigny. I found a curious little stony Cellaria 1 a new genus each cell provided with long toothed bristle, these are capable of various and rapid motions. This motion is often simultaneous, and can be produced by irritation. This fact, as far as I can see, is quite isolated in the history of zoophytes excepting the Flustra with an organ like a vulture's head ; it points out a much more intimate relation between the polypi than Lamarck is willing to allow.

I forgot whether I mentioned having seen something of the manner of propagation in that most ambiguous family, the corallines; I feel. Cellaria , a genus of Bryozoa, placed in the section Flustrina of the Suborder Chilostomata. The "gemmule" of a Halimeda contained several articulations united, ready to burst their envelope, and become attached to some basis. I believe in zoophytes universally the gemmule produces a single polypus, which afterwards or at the same time grows with its cell or single articulation. The Beagle left the Sts. Narborough call the west coast South Desolation, "because it is so desolate a land to behold.

An Englishman gave me three specimens of that very fine Lucanoidal insect which is described in the Camb. I find Chiloe is composed of lava and recent deposits. The lavas are curious from abounding in, or rather being in parts composed of pitchstone.

If we go to Chiloe in the summer, I shall reap an entomological harvest. I suppose the Botany both there and in Chili is well-known. I forgot to state that in the four cargoes of specimens there have been sent three square boxes, each containing four glass bottles. I mention this in case they should be stowed beneath geological specimens and thus escape your notice, perhaps some spirit may be wanted in them. If a box arrives from B.

Ayres with a Megatherium head the other unnumbered specimens, be kind enough to tell me, as I have strong fears for its safety. We arrived here the day before yesterday; the views of the distant mountains are most sublime and the climate delightful; after our long cruise in the damp gloomy climates of the south, to breathe a clear dry air and feel honest warm sunshine, and eat good fresh roast beef must be the summum bonum of human life.

I do not like the look of the rocks half so much as the beef, there is too much of those rather insipid ingredients, mica, quartz and feldspar. Our plans are at present undecided; there is a good deal of work to the south of Valparaiso and to the north an indefinite quantity.

I look forward to every part with interest. I have sent you in this letter a sad dose of egotism, but recollect I look up to you as my father in. Stephens Trans. Volume IV. Natural History, and a son may talk about himself to his father. In your paternal capacity as proproctor what a great deal of trouble you appear to have had. How turbulent Cambridge is become. Before this time it will have regained its tranquillity. I have a most schoolboy-like wish to be there, enjoying my holidays.

It is a most comfortable reflection to me, that a ship being made of wood and iron, cannot last for ever, and therefore this voyage must have an end. October 28th. This letter has been lying in my portfolio ever since July; I did not send it away because I did not think it worth the postage; it shall now go with a box of specimens. Shortly after arriving here I set out on a geological excursion, and had a very pleasant ramble about the base of the Andes.

The whole country appears composed of breccias and I imagine slates which universally have been modified and oftentimes completely altered by the action of fire. The varieties of porphyry thus produced are endless, but nowhere have I yet met with rocks which have flowed in a stream; dykes of greenstone are very numerous. Modern volcanic action is entirely shut up in the very central parts which cannot now be reached on account of the snow of the Cordilleras.

In the south of the R. Maypu I examined the Tertiary plains, already partially described by M. America as well as in Europe. I have been much interested by finding abundance of recent shells at an elevation of 1, feet; the country in many places is scattered over with shells but these are all littoral ones. So that I suppose the 1, feet elevation must be owing to a succession of small elevations such as in With these certain proofs of the recent residence of the ocean over all the lower parts of Chili, the outline of every view and the form of each valley possesses a high interest.

Has the action of running water or the sea formed this deep ravine? Gay," by Alex. Brongniart Ann. I have not sufficient arguments, but I do not believe that more than a small fraction of the height of the Andes has been formed within the Tertiary period. The conclusion of my excursion was very unfortunate, I became unwell and could hardly reach this place.

I have been in bed for the last month, but am now rapidly getting well. I had hoped during this time to have made a good collection of insects but it has been impossible: I regret the less because Chiloe fairly swarms with collectors; there are more naturalists in the country, than carpenters or shoemakers or any other honest trade. I have since heard from B. Ayres that it went to Liverpool by the brig Basingwaithe. If you have not received it, it is I think worth taking some trouble about.

In October two casks and a jar were sent by H. I have no doubt you have received them. With this letter I send a good many bird skins; in the same box with them, there is a paper parcel containing pill boxes with insects. The other pill boxes require no particular care. You will see in two of these boxes some dried Planariae terrestrial , the only method I have found of preserving them they are exceedingly brittle.

By examining the white species I understand some little of the internal structure. There are two small parcels of seeds. There are some plants which I hope may interest you, or at least those from Patagonia where I collected every one in flower. There is a bottle clumsily but I think securely corked containing water and gas from the hot baths of Cauquenes seated at foot of Andes and long celebrated for medicinal properties. I took pains in filling and securing both water and gas.

If you can find any one who likes to analyze them, I should think it would be worth the trouble.

I have not time at present to copy my few observations about the locality, etc. Will you tell me how the Arachnidae which I have sent home, for instance those from Rio, appear to be preserved. I have doubts whether it is worth while collecting them. We sail the day after to-morrow: our plans are at last limited and definite; I am delighted to say we have bid an eternal adieu to T.

The Beagle will not. Tres Montes; from which point we survey to the north. The Chonos Archipelago is delightfully unknown: fine deep inlets running into the Cordilleras-where we can steer by the light of a volcano. I do not know which part of the voyage now offers the most attractions. This is a shamefully untidy letter, but you must forgive me. I have just returned from Mendoza, having crossed the Cordilleras by two passes. This trip has added much to my knowledge of the geology of the country. Some of the facts, of the truth of which I in my own mind feel fully convinced, will appear to you quite absurd and incredible.

I will give a very short sketch of the structure of these huge mountains. In the Portillo pass the more southern one travellers have described the Cordilleras to consist of a double chain of nearly equal altitude separated by a considerable interval. This is the case; and the same structure extends to the northward to Uspallata; the little elevation of the eastern line here not more than 6,, feet.

To begin with the western and principal chain, we have, where the sections are best seen, an enormous mass of a porphyritic conglomerate resting on granite. This latter rock seems to form the nucleus of the whole mass, and is seen in the deep lateral valleys, injected amongst, upheaving, overturning in the most extraordinary manner, the overlying strata.

The stratification in all the mountains is beautifully distinct and from a variety in the colour can be seen at great distances. I cannot imagine any part of the world presenting a more extraordinary scene of the breaking up of the crust of the globe than the very central parts of the Andes. The upheaval has taken place by a great number of nearly N. I cannot tell you how I enjoyed some of these views-it is worth coming from England, once to feel such intense delight; at an elevation from 10 to 12, feet there is a transparency in the air,.

The formation I call Porphyritic Conglomerates is the most important and most developed one in Chili: from a great number of sections I find it a true coarse conglomerate or breccia, which by every step in a slow gradation passes into a fine claystone-porphyry; the pebbles and cement becoming porphyritic till at last all is blended in one compact rock.

The porphyries are excessively abundant in this chain. There are porphyries which have been injected from below amongst strata, and others ejected, which have flowed in streams; it is remarkable, and I could show specimens of this rock produced in these three methods, which cannot be distinguished. It is a great mistake considering the Cordilleras here as composed of rocks which have flowed in streams. In this range I nowhere saw a fragment, which I believe to have thus originated, although the road passes at no great distance from the active volcanoes. The porphyries, conglomerate, sandstone and quartzose sandstone and limestones alternate and pass into each other many times, overlying where not broken through by the granite clay-slate.

In the upper parts, the sandstone begins to alternate with gypsum, till at last we have this substance of a stupendous thickness. I really think the formation is in some places it varies much nearly 2, feet thick, it occurs often with a green epidote? The upper beds which form some of the higher pinnacles consist of layers of snow-white gypsum and red compact sandstone, from the thickness of paper to a few feet, alternating in an endless round.

The rock has a most curiously painted appearance. At the pass of the Peuquenes in this formation, where however a black rock like clay-slate, without many laminae, occurring with a pale limestone, has replaced the red sandstone, I found abundant impressions of shells. The elevation must be between 12 and 13, feet. A shell. Perhaps some good conchologist 1 will be able to give a guess, to what grand division of the formations of Europe these organic remains bear most resemblance.

They are exceedingly imperfect and few. It was late in the season and the situation particularly dangerous for snow-storms. I did not dare to delay, otherwise a grand harvest might have been reaped. So much for the western line; in the Portillo pass, proceeding eastward, we meet an immense mass of conglomerate, dipping to the west 45 deg, which rest on micaceous sandstone, etc. Now this conglomerate which reposes on and dips from the protogene 45 deg consists of the peculiar rocks of the first described chain, pebbles of the black rock with shells, green sandstone, etc.

It is hence manifest that the upheaval and deposition at least of part of the grand eastern chain is entirely posterior to the western. To the north in the Uspallata pass, we have also a fact of the same class. Bear this in mind: it will help to make you believe what follows. I have said the Uspallata range is geologically, although only 6,, feet, a continuation of the grand eastern chain.

It has its nucleus of granite, consists of grand beds of various crystalline rocks, which I can feel no doubt are subaqueous lavas alternating with sandstone, conglomerates and white aluminous beds like decomposed feldspar with many other curious varieties of sedimentary deposits. These lavas and sandstones alterate very many times, and are quite conformable one to the other. During two days of careful examination I said to myself at least fifty times, how exactly like only rather harder these beds are to those of the upper Tertiary strata of Patagonia, Chiloe and Concepcion, without the possible identity ever having occurred to me.

At last there was no resisting the conclusion. I could not expect shells, for they never occur in this formation; but lignite or carbonaceous shale ought to be found. I had previously been exceedingly puzzled by meeting in the sandstone, thin layers. Some of these genera are mentioned by Darwin Geol. I strongly suspect the underlying granite has altered such beds into this pitchstone. The silicified wood particularly characteristic was yet absent. The conviction that I was on the Tertiary strata was so strong by this time in my mind, that on the third day in the midst of lavas and [?

How do you think I succeeded? In an escarpement of compact greenish sandstone, I found a small wood of petrified trees in a vertical position, or rather the strata were inclined about deg to one point and the trees 70 deg to the opposite one. That is, they were before the tilt truly vertical. The sandstone consists of many layers, and is marked by the concentric lines of the bark I have specimens ; 11 are perfectly silicified and resemble the dicotyledonous wood which I have found at Chiloe and Concepcion; 1 the others I only know to be trees from the analogy of form and position; they consist of snow-white columns like Lot's wife of coarsely crystalline carb.

The largest shaft is 7 feet. They are all close together, within yards, and about the same level: nowhere else could I find any. It cannot be doubted that the layers of fine sandstone have quietly been deposited between a clump of trees which were fixed by their roots. The sandstone rests on lava, is covered by a great bed apparently about 1, feet thick of black augitic lava, and over this there are at least 5 grand alternations of such rocks and aqueous sedimentary deposits, amounting in thickness to several thousand feet.

I am quite afraid of the only conclusion which I can draw from this fact, namely that there must have been a depression in the surface of the land to that amount. But neglecting this consideration, it was a most satisfactory support of my presumption of the Tertiary I mean by Tertiary, that the shells of the period were closely allied, or some identical, to those which now live, as in the lower beds of Patagonia age of this eastern chain.

A great part of the proof must remain upon my ipse dixit of a mineralogical resemblance with those beds whose age is known, and the character of which resemblance. Specimens of the silicified wood were examined by Robert Brown, and determined by him as coniferous, "partaking of the characters of the Araucarian tribe, with some curious points of affinity with the yew.

I hardly expect you to believe me, when it is a consequence of this view that granite, which forms peaks of a height probably of 14, feet, has been fluid in the Tertiary period; that strata of that period are altered by its heat, and are traversed by dykes from the mass. That these strata have also probably undergone an immense depression, that they are now inclined at high angles and form regular or complicated anticlinal lines.

To complete the climax and seal your disbelief, these same sedimentary strata and lavas are traversed by very numerous , true metallic veins of iron, copper, arsenic, silver and gold, and these can be traced to the underlying granite. A gold mine has been worked close to the clump of silicified trees. If when you see my specimens, sections and account, you should think that there is pretty strong presumptive evidence of the above facts, it appears very important; for the structure, and size of this chain will bear comparison with any in the world, and that this all should have been produced in so very recent a period is indeed wonderful.

In my own mind I am quite convinced of the reality of this. I can anyhow most conscientiously say that no previously formed conjecture warped my judgment. As I have described so did I actually observe the facts. But I will have some mercy and end this most lengthy account of my geological trip. On some of the large patches of perpetual snow, I found the famous red snow of the Arctic countries; I send with this letter my observations and a piece of paper on which I tried to dry some specimens. If the fact is new and you think it worth while, either yourself examine them or send them to whoever has described the specimens from the north and publish a notice in any of the periodicals.

I also send a small bottle with two lizards, one of them is viviparous as you will see by the accompanying notice. Gay-a French naturalist-has already published in one of the newspapers of this country a similar statement and probably has forwarded to Paris some account; as the fact appears singular would it not be worth while to hand over the specimens to some good lizardologist and comparative anatomist to publish an account of their internal structure?

Do what you think fit. This letter will go with a cargo of specimens from Coquimbo. I shall write to let you know when they are sent off. In the box there are two bags of seeds, one [from the] valleys of the Cordilleras 5,, feet high, the soil and climate exceedingly dry, soil very light and stony, extremes in temperature; the other chiefly from the dry sandy Traversia of Mendoza 3, feet more or less. If some of the bushes should grow but not be healthy, try a slight sprinkling of salt and saltpetre.

The plain is saliferous. All the flowers in the Cordilleras appear to be autumnal flowerers-they were all in blow and seed, many of them very pretty. I gathered them as I rode along on the hill sides. If they will but choose to come up, I have no doubt many would be great rarities. In the Mendoza bag there are the seeds or berries of what appears to be a small potato plant with a whitish flower. They grow many leagues from where any habitation could ever have existed owing to absence of water.

Amongst the Chonos dried plants, you will see a fine specimen of the wild potato, growing under a most opposite climate, and unquestionably a true wild potato. It must be a distinct species from that of the Lower Cordilleras one. Perhaps as with the banana, distinct species are now not to be distinguished in their varieties produced by cultivation. I cannot copy out the few remarks about the Chonos potato. With the specimens there is a bundle of old papers and notebooks. Will you take care of them; in case I should lose my notes, these might be useful.

I do not send home any insects because they must be troublesome to you, and now so little more of the voyage remains unfinished I can well take charge of them. In two or three days I set out for Coquimbo by land; the Beagle calls for me in the beginning of June. So that I have six weeks more to enjoy geologising over these curious mountains of Chili.

There is at present a bloody revolution in Peru. The Commodore has gone there, and in the hurry has carried our letters with him; perhaps amongst them there will be one from you. I wish I had the old Commodore here, I would shake some consideration for others into his old body. From Coquimbo you will again hear from me. This is the last letter which I shall ever write to you from the shores of America, and for this reason I send it. In a few days time the Beagle will sail for the Galapagos Islands.

I look forward with joy and interest to this, both as being somewhat nearer to England and for the sake of having a good look at an active volcano. Although we have seen lava in abundance, I have never yet beheld the crater. I sent by H. Conway two large boxes of specimens.

The Conway sailed the latter end of June. With them were letters for you, since that time I have travelled by land from Valparaiso to Copiapo and seen something more of the Cordilleras. Some of my geological views have been, subsequently to the last letter, altered. I believe the upper mass of strata is not so very modern as I supposed. This last journey has explained to me much of the ancient history of the Cordilleras. I feel sure they formerly consisted of a chain of volcanoes from which enormous streams of lava were poured forth at the bottom of the sea.

These alternate with sedimentary beds to a vast thickness; at a subsequent period these volcanoes must have formed islands, from which have been produced strata of several thousand feet thick of coarse conglomerate. The alternations of compact crystalline rocks I cannot doubt subaqueous lavas , and sedimentary beds, now upheaved fractured and indurated, form the main range of the Andes. The formation was produced at the time when ammonites, gryphites, oysters, Pecten, Mytilus , etc.

In the central parts of Chili the structure of the lower beds is rendered very obscure by the metamorphic action which has rendered even the coarsest conglomerates porphyritic. The Cordilleras of the Andes so worthy of admiration from the grandeur of their dimensions, rise in dignity when it is considered that since the period of ammonites, they have. The geology of these mountains pleased me in one respect; when reading Lyell, it had always struck me that if the crust of the world goes on changing in a circle, there ought to be somewhere found formations which, having the age of the great European Secondary beds, should possess the structure of Tertiary rocks or those formed amidst islands and in limited basins.

Now the alternations of lava and coarse sediment which form the upper parts of the Andes, correspond exactly to what would accumulate under such circumstances. In consequence of this, I can only very roughly separate into three divisions the varying strata perhaps 8, feet thick which compose these mountains. I am afraid you will tell me to learn my ABC to know quartz from feldspar before I indulge in such speculations. I lately got hold of a report on M.

Dessalines D'Orbigny's labours in S. America; 1 I experienced rather a debasing degree of vexation to find he has described the Geology of the Pampas, and that I have had some hard riding for nothing, it was however gratifying that my conclusions are the same, as far as I can collect, with his results. It is also capital that the whole of Bolivia will be described. I hope to be able to connect his geology of that country with mine of Chili. After leaving Copiapo, we touched at Iquique.

I visited but do not quite understand the position of the nitrate of soda beds. Here in Peru, from the state of anarchy, I can make no expedition. I hear from home, that my brother is going to send me a box with books, and a letter from you. It is very unfortunate that I cannot receive this before we reach Sydney, even if it ever gets safely so far. I shall not have another opportunity for many months of again writing to you.

Will you have the charity to send me one more letter as soon as this reaches you directed to the C. Your letters besides affording me the greatest delight always give me a fresh stimulus for exertion. Excuse this geological prosy letter, and farewell till you hear from me at Sydney, and see me in the autumn of The Beagle arrived at Falmouth on Sunday evening, and I reached home late last night.

My head is quite confused with so much delight, but I cannot allow my sisters to tell you first how happy I am to see all my dear friends again. I am obliged to return in three or four days to London, where the Beagle will be paid off, and then I shall pay Shrewsbury a longer visit. I am most anxious once again to see Maer, and all its inhabitants, so that in the course of two or three weeks, I hope in person to thank you, as being my first Lord of the Admiralty.

Believe me your most affectionate nephew,. I suppose you will be in Hart St. I write because I cannot avoid wishing to be the first person to tell Mrs. Lyell and yourself, that I have the very good, and shortly since [i. The lady is my cousin Miss Emma Wedgwood, the sister of Hensleigh Wedgwood, and of the elder brother who married my sister, so we are connected by manifold ties, besides on my part, by the most sincere. The date of his arrival in Shrewsbury was, therefore, October 4th, as given in the Life and Letters , I.

The entries in his Diary are:— October 2, Took leave of my home. October 4, Reached Shrewsbury after absence of 5 years and 2 days. I determined when last at Maer to try my chance, but I hardly expected such good fortune would turn up for me. I shall be in town in the middle or latter end of the ensuing week. But I deeply feel your kindness and friendship towards me, which in truth I may say, has been one chief source of happiness to me, ever since my return to England: so you must excuse me.

I am well sure that Mrs. Lyell, who has sympathy for every one near her, will give me her hearty congratulations. I cannot tell you how much I enjoyed my Maer visit,—I felt in anticipation my future tranquil life: how I do hope you may be as happy as I know I shall be: but it frightens me, as often as I think of what a family you have been one of. I was thinking this morning how it came, that I, who am fond of talking and am scarcely ever out of spirits, should so entirely rest my notions of happiness on quietness, and a good deal of solitude: but I believe the explanation is very simple and I mention it because it will give you hopes, that I shall gradually grow less of a brute, it is that during the five years of my voyage and indeed I may add these two last which from the active manner in which they have been passed, may be said to be the commencement of my real life, the whole of my pleasure was derived from what passed in my mind, while admiring views by myself, travelling across the wild deserts or glorious forests or pacing the deck of the poor little Beagle at night.

Excuse this much egotism,— I give it you because I think you will humanize me, and soon teach me there is greater happiness than building theories and accumulating facts in silence and solitude. My own dearest. Darwin was married on January 29th, see Life and Letters , I. The present letter was written the day after he had become engaged.

Emma, I earnestly pray, you may never regret the great, and I will add very good, deed, you are to perform on the Tuesday: my own dear future wife, God bless you The Lyells called on me to-day after church; as Lyell was so full of geology he was obliged to disgorge,—and I dine there on Tuesday for an especial confidence.

I was quite ashamed of myself to-day, for we talked for half an hour, unsophisticated geology, with poor Mrs. Lyell sitting by, a monument of patience. I want practice in ill-treatment the female sex,—I did not observe Lyell had any compunction; I hope to harden my conscience in time: few husbands seem to find it difficult to effect this. Since my return I have taken several looks, as you will readily believe, into the drawing- room; I suppose my taste [for] harmonious colours is already deteriorated, for I declare the room begins to look less ugly.

I take so much pleasure in the house, 1 I declare I am just like a great overgrown child with a new toy; but then, not like a real child, I long to have a co-partner and possessor. The following passage is taken from the MS. Darwin's lifetime:—. You all know your mother, and what a good mother she has ever been to all of you. She has been my greatest blessing, and I can declare that in my whole life I have never heard her utter one word I would rather have been unsaid. She has never failed in kindest sympathy towards me, and has borne with the utmost patience my frequent complaints of ill-health and discomfort.

I do not believe she has ever missed an opportunity of doing a kind action to any one near her. I marvel at my good fortune that she, so infinitely my superior in every single moral quality, consented to be my wife. She has been my wise adviser and cheerful comforter throughout life, which without her would have been during a very long period a miserable one from ill-health.

She has earned the love of every soul near her.

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We are indebted, for this information, to Mr. Wheatley, of the Society of Arts. Lyell started on his first visit to the United States in July, , and was absent thirteen months. Darwin returned to London July 23rd, , after a prolonged absence; he may, therefore, have missed seeing Lyell.

Assuming the date to be correct, it would seem that the plan of living in the country was formed a year before it was actually carried out. I have no doubt that your father did rightly in persuading you to stay [at Shrewsbury], but we were much disappointed in not seeing you before our start for a year's absence. I cannot tell you how often since your long illness I have missed the friendly intercourse which we had so frequently before, and on which I built more than ever after your marriage.

It will not happen easily that twice in one's life, even in the large world of London, a congenial soul so occupied with precisely the same pursuits and with an independence enabling him to pursue them will fall so nearly in my way, and to have had it snatched from me with the prospect of your residence somewhat far off is a privation I feel as a very great one.

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I hope you will not, like Herschell, get far off from a railway. You must have been surprised at not having heard sooner about the house. Emma and I only returned yesterday afternoon from sleeping there. I will give you in detail, as my father would like, my opinion on it-Emma's slightly differs. This is bad, as the drive from [ i.

I calculate we are two hours going from London Bridge. Village about forty houses with old walnut trees in the middle where stands an old flint church and the lanes meet. Inhabitants very respectable-infant school-grown up people great musicians-all touch their hats as in Wales and sit at their open doors in the evening; no high road leads through the village.

The little pot-house. There are butcher and baker and post-office.

CONTENTS OF VOLUME I.

A carrier goes weekly to London and calls anywhere for anything in London and takes anything anywhere. On the road [from London] to the village, on a fine day the scenery is absolutely beautiful: from close to our house the view is very distant and rather beautiful, but the house being situated on a rather high tableland has somewhat of a desolate air.

There is a most beautiful old farm-house, with great thatched barns and old stumps of oak trees, like that of Skelton, one field off. The charm of the place to me is that almost every field is intersected as alas is ours by one or more foot-paths. I never saw so many walks in any other county. The country is extraordinarily rural and quiet with narrow lanes and high hedges and hardly any ruts. It is really surprising to think London is only 16 miles off.

The house stands very badly, close to a tiny lane and near another man's field. Our field is 15 acres and flat, looking into flat-bottomed valleys on both sides, but no view from the drawing- room, which faces due south, except on our flat field and bits of rather ugly distant horizon.

Close in front there are some old very productive cherry trees, walnut trees, yew, Spanish chestnut, pear, old larch, Scotch fir and silver fir and old mulberry trees, [which] make rather a pretty group. They give the ground an old look, but from not flourishing much they also give it rather a desolate look. There are quinces and medlars and plums with plenty of fruit, and Morello cherries; but few apples. The purple magnolia flowers against the house. There is a really fine beech in view in our hedge.

The kitchen garden is a detestable slip and the soil looks wretched from the quantity of chalk flints, but I really believe it is productive. The hedges grow well all round our field, and it is a noted piece of hayland. This year the crop was bad, but was bought, as it stood, for 2 pounds per acre-that is 30 pounds—the purchaser getting it in. Last year it was sold for 45 pounds-no manure was put on in the interval.

Does not this sound well? Ask my father. Does the mulberry and magnolia show it is not very cold in winter, which I fear is the case? Tell Susan it is 9 miles from Knole Park and 6 from Westerham, at which places I hear the scenery is beautiful. There are many very odd. House ugly, looks neither old nor new-walls two feet thick-windows rather small-lower story rather low. Capital study 18 x Dining-room 21 x Drawing-room can easily be added to: is 21 x Three stories, plenty of bedrooms. We could hold the Hensleighs and you and Susan and Erasmus all together.

House in good repair. Cresy a few years ago laid out for the owner 1, pounds and made a new roof. Water-pipes over house-two bath-rooms-pretty good offices and good stable-yard, etc. I believe the price is about 2, pounds, and I have no doubt I shall get it for one year on lease first to try, so that I shall do nothing to the house at first last owner kept three cows, one horse, and one donkey, and sold some hay annually from one field.

I have no doubt if we complete the purchase I shall at least save 1, pounds over Westcroft, or any other house we have seen. Emma was at first a good deal disappointed, and at the country round the house; the day was gloomy and cold with N. She likes the actual field and house better than I; the house is just situated as she likes for retirement, not too near or too far from other houses, but she thinks the country looks desolate.

I think all chalk countries do, but I am used to Cambridgeshire, which is ten times worse. Emma is rapidly coming round. She was dreadfully bad with toothache and headache in the evening and Friday, but in coming back yesterday she was so delighted with the scenery for the first few miles from Down, that it has worked a great change in her. We go there again the first fine day Emma is able, and we then finally settle what to do. Darwin's papers after the publication of the Life and Letters. It gives the impression that he intended to write a natural history diary after the manner of Gilbert White, but there is no evidence that this was actually the case.

May 15th. On the road to Down from Keston. The water all percolates straight downwards.

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Ascertain average depth of wells, inclination of strata, and springs. Does the water from this country crop out in springs in Holmsdale or in the valley of the Thames? Examine the fine springs in Holmsdale. The valleys on this platform sloping northward, but exceedingly even, generally run north and south; their sides near the summits generally become suddenly more abrupt, and are fringed with narrow strips, or, as they are here called, "shaws" of wood, sometimes merely by hedgerows run wild.

The sudden steepness may generally be perceived, as just before ascending to Cudham Wood, and at Green Hill, where one of the lanes crosses these valleys. These valleys are in all probability ancient sea-bays, and I have sometimes speculated whether this sudden steepening of the sides does not mark the edges of vertical cliffs formed when these valleys were filled with sea-water, as would naturally happen in strata such as the chalk.

In most countries the roads and footpaths ascend along the bottoms of valleys, but here this is scarcely ever the case. All the villages and most of the ancient houses are on the platforms or narrow strips of flat land between the parallel valleys. Is this owing to the summits having existed from the most ancient times as open downs and the valleys having been filled up with brushwood?

I have no evidence of this, but it is certain that most of the farmhouses on the flat land are very ancient.

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There is one peculiarity which would help to determine the footpaths to run along the summits instead of the bottom of the valleys, in that these latter in the middle are generally covered, even far more thickly than the general surface, with broken flints. This bed of flints, which gradually thins away on each side, can be seen from a long distance in a newly ploughed or fallow field as a whitish band. Every stone which ever rolls after heavy rain or from the kick of an animal, ever so little, all tend to the bottom of the valleys; but whether this is sufficient to account for their number I have sometimes doubted, and have been inclined to apply to the case Lyell's theory of solution by rain-water, etc.

The flat summit-land is covered with a bed of stiff red clay, from a few feet in thickness to as much, I believe, as twenty feet: this [bed], though lying immediately on the chalk, and abounding with great, irregularly shaped, unrolled flints, often with the colour and appearance of huge bones, which were originally embedded in the chalk, contains not a particle of carbonate of lime. This bed of red clay lies on a very irregular surface, and often descends into deep round wells, the origin of which has been explained by Lyell.

In these cavities are patches of sand like sea-sand, and like the sand which alternates with the great beds of small pebbles derived from the wear-and-tear of chalk-flints, which form Keston, Hayes and Addington Commons. Near Down a rounded chalk-flint is a rarity, though some few do occur; and I have not yet seen a stone of distant origin, which makes a difference-at least to geological eyes-in the very aspect of the country, compared with all the northern counties.

The chalk-flints decay externally, which, according to Berzelius Edin. New Phil. Journal , late number , is owing to the flints containing a small proportion of alkali; but, besides this external decay, the whole body is affected by exposure of a few years, so that they will not break with clean faces for building. This bed of red clay, which renders the country very slippery in the winter months from October to April, does not cover the sides of the valleys; these, when ploughed, show the white chalk, which tint shades away lower in the valley, as insensibly as a colour laid on by a painter's brush.

Nearly all the land is ploughed, and is often left fallow, which gives the country a naked red look, or not unfrequently white, from a covering of chalk laid on by the farmers. Nobody seems at all aware on what principle fresh chalk laid on land abounding with lime does it any good. This, however, is said to have been the practice of the country ever since the period of the Romans, and at present the many white pits on the hill sides, which so frequently afford a picturesque contrast with the overhanging yew trees, are all quarried for this purpose. The number of different kinds of bushes in the hedgerows, entwined by traveller's joy and the bryonies, is conspicuous compared with the hedges of the northern counties.

March 25th [? A few days later some of the copses were beautifully enlivened by Ranunculus auricomus , wood anemones, and a white Stellaria. Again, subsequently, large areas were brilliantly blue with bluebells. The flowers are here very beautiful, and the number of flowers; [and] the darkness of the blue of the common little Polygala almost equals it to an alpine gentian. There are large tracts of woodland, [cut down] about once every ten years; some of these enclosures seem to be very ancient.

On the south side of Cudham Wood a beech hedge has grown to Brobdignagian size, with several of the huge branches crossing each other and firmly grafted together. Larks abound here, and their songs sound most agreeably on all sides; nightingales are common. Judging from an odd cooing note, something like the purring of a cat, doves are very common in the woods. June 25th. This humming is rather deeper than the humming overhead, which has been continuous and loud during all these last hot days over almost every field. The labourers here say it is made by "air-bees," and one man, seeing a wild bee in a flower different from the hive kind, remarked: "That, no doubt, is an air-bee.

Huxley's obituary notice of Charles Darwin has appeared. We would venture to recommend it to our readers as the best possible introduction to these pages. There is, however, one small point in which we differ from Mr. In discussing the growth of Mr. Darwin's evolutionary views, Mr. Huxley quotes from the autobiography 2 a passage in which the writer describes the deep impression made on his mind by certain groups of facts observed in South America.

Huxley goes on: "The facts to which reference is here made were, without doubt, eminently fitted to attract the attention of a philosophical thinker; but, until the relations of the existing with the extinct species, and of the species of the different geographical areas with one another, were determined with some exactness, they afforded but an unsafe foundation for speculation.

It was not possible that this determination should have been effected before the return of the Beagle to England; and thus the date 3 which Darwin writing in assigns to the dawn of the new light which was rising in his mind, becomes intelligible. Life and Letters , I. Some account of the origin of his evolutionary views is given in a letter to Jenyns Blomefield , Life and Letters , II.

The date in question is July , when he "opened first note-book on Transmutation of Species. He wrote in his "Journal," page , "My attention was first thoroughly aroused, by comparing together the numerous specimens shot by myself and several other parties on board," etc. We agree with Mr. Huxley that is the date of the "new light which was rising in his mind.

We do not see that Mr. Huxley's supposition as to the effect of the determination of species, etc. Huxley quotes a letter from Darwin to Zacharias, "But I did not become convinced that species were mutable until, I think, two or three years [after ] had elapsed" see Letter This passage, which it must be remembered was written in , is all but irreconcilable with the direct evidence of the note-book.

He had not yet attained to a clear idea of Natural Selection, and therefore his views may not have had, even to himself, the irresistible convincing power they afterwards gained; but that he was, in the ordinary sense of the word, convinced of the truth of the doctrine of evolution we cannot doubt. He thought it "almost useless" to try to prove the truth of evolution until the cause of change was discovered.

And it is natural that in later life he should have felt that conviction was wanting till that cause was made out. We know that in he wrote the first sketch of his theory, and that it was greatly amplified in So that, at the date of the first letters of this chapter, we know that he had a working hypothesis of evolution which did not differ in essentials from that given in the Origin of Species. To realise the amount of work that was in progress during the period covered by Chapter II.

Thus to quote a story of Lord Avebury's one of Mr. Darwin's children is said to have asked, in regard to a neighbour, "Then where does he do his barnacles? Sir Joseph Hooker, to whom the first letter in this chapter is addressed, was good enough to supply a note on the origin of his intimacy with Mr. Darwin, and this is published in the Life and Letters. Darwin's letters to Sir Joseph have supplied. See also Nature , , June 22nd, page , where some reminiscences are published, which formed part of Sir Joseph's speech at the unveiling of Darwin's statue in the Oxford Museum.

But it should not be forgotten that, quite apart from this, science owes much to this memorable friendship, since without Hooker's aid Darwin's great work would hardly have been carried out on the botanical side. And Sir Joseph did far more than supply knowledge and guidance in technical matters: Darwin owed to him a sympathetic and inspiriting comradeship which cheered and refreshed him to the end of his life.

A sentence from a letter to Hooker written in shows, quite as well as more serious utterances, how quickly the acquaintance grew into friendship. What a good thing is community of tastes! I feel as if I had known you for fifty years. Darwin wrote: "Your letter has cheered me, and the world does not look a quarter so black this morning as it did when I wrote before. Your friendly words are worth their weight in gold. I must write to thank you for your last letter, and to tell you how much all your views and facts interest me. I must be allowed to put my own interpretation on what you say of "not being a good arranger of extended views"-which is, that you do not indulge in the loose speculations so easily started by every smatterer and wandering collector.

I look at a strong tendency to generalise as an entire evil. What you say of Mr. Brown is humiliating; I had suspected it, but would not allow myself to believe in such heresy. Fitz-Roy gave him a rap in his preface, 1 and made him very indignant, but it seems a much harder one would not have been wasted. My cryptogamic collection was sent. In the preface to the Surveying Voyages of the "Adventure" and the "Beagle," , forming Volume I of the work, which includes the later voyage of the Beagle , Captain Fitz-Roy wrote March, : "Captain King took great pains in forming and preserving a botanical collection, aided by a person embarked solely for that purpose.

He placed this collection in the British Museum, and was led to expect that a first- rate botanist would have examined and described it; but he has been disappointed. I do not believe he has yet published an account, but he wrote to me some year ago that he had described [the specimens] and mislaid all his descriptions. Would it not be well for you to put yourself in communication with him, as otherwise something will perhaps be twice laboured over?

My best though poor collection of the cryptogams was from the Chonos Islands. Would you kindly observe one little fact for me, whether any species of plant, peculiar to any island, as Galapagos, St. Helena, or New Zealand, where there are no large quadrupeds, have hooked seeds-such hooks as, if observed here, would be thought with justness to be adapted to catch into wool of animals.

Would you further oblige me some time by informing me though I forget this will certainly appear in your Antarctic Flora whether in islands like St. Helena, Galapagos, and New Zealand, the number of families and genera are large compared with the number of species, as happens in coral islands, and as, I believe, in the extreme Arctic land. Certainly this is the case with marine shells in extreme Arctic seas. Do you suppose the fewness of species in proportion to number of large groups in coral islets is owing to the chance of seeds from all orders getting drifted to such new spots, as I have supposed.

Did you collect sea-shells in Kerguelen-land? I should like to know their character. Your interesting letters tempt me to be very unreasonable in asking you questions; but you must not give yourself any trouble about them, for I know how fully and worthily you are employed.

Besides a general interest about the southern lands, I have been now ever since my return engaged in a very presumptuous work, and I know no one individual who would not say a very foolish one. I was so struck with the distribution of the Galapagos organisms, etc. I have read heaps of agricultural and horticultural books, and have never ceased collecting facts. At last gleams of light have come, and I am almost convinced. The rest of the letter has been previously published in Life and Letters , II.

Some Remains (Hitherto Unpublished) of Joseph Butler, LL.D. (Paperback)

Heaven forfend me from Lamarck nonsense of a "tendency to progression," "adaptations from the slow willing of animals," etc.! But the conclusions I am led to are not widely different from his; though the means of change are wholly so. I think I have found out here's presumption! You will now groan, and think to yourself, "on what a man have I been wasting my time and writing to. What a curious, wonderful case is that of the Lycopodium! I suppose you would hardly have expected them to be more varying than a phanerogamic plant.

I trust you will work the case out, and, even if unsupported, publish it, for you can surely do this with due caution. I have heard of some analogous facts, though on the smallest scale, in certain insects being more variable in one district than in another, and I think the same holds with some land-shells. By a strange chance I had noted to ask you in this letter an analogous question, with respect to genera, in lieu of individual species,—that is, whether you know of any case of a genus with most of its species being variable say Rubus in one continent, having another set of species in another continent non-variable, or not in so marked a manner.

Herbert 3 incidentally mentioned in a letter to me that the heaths at the Cape of Good Hope were very variable, whilst in Europe they are? In some genera of insects the variability appears to be common. Sir J. Hooker wrote, November 8, "I am firmly convinced but not enough to print it that L. Selago varies in Van Diemen's Land into L. Two more different species as they have hitherto been thought , per se cannot be conceived, but nowhere else do they vary into one another, nor does Selago vary at all in England.

No doubt Dean Herbert, the horticulturist. See Life and Letters , I. In shells, I hope hereafter to get much light on this question through fossils.