James Hutton 15965 221852898 2008-06-26T11:24:56Z 83.105.70.249 /* Evolution */ Minor grammatical change - rearrangement of words to remove split infinitive. {{Infobox Scientist |name = |box_width = |image =James Hutton.jpg |image_width =150px |caption = James Hutton, painted by [[Abner Lowe]] |birth_date = [[14 June]] [[1726]] |birth_place = [[Edinburgh]] |death_date =[[26 March]] [[1797]] |death_place = |residence = |citizenship = |nationality = [[Scotland|Scottish]] |ethnicity = |field = [[geology]] |work_institutions = |alma_mater = |doctoral_advisor = |doctoral_students = |known_for = [[geology]] |author_abbrev_bot = |author_abbrev_zoo = |influences = |influenced = |prizes = |religion = |footnotes = |signature = }} '''James Hutton''' ([[3 June]] [[1726]] [[Old Style|OS]] <small>([[14 June]] [[1726]] [[New Style|NS]])</small> [[Edinburgh]] — [[26 March]] [[1797]]) was a [[Scotland|Scottish]] [[geologist]], [[Natural history|naturalist]], [[chemist]] and [[experiment]]al [[Agriculture|farmer]]. He is considered the [[father of]] modern [[geology]].<ref name="MillennialPlaque">{{cite web |url= http://www.ed.ac.uk/explore/people/plaques/jameshutton.html |title= Millennial Plaques: James Hutton |author= [[University of Edinburgh]] |publisher= (Hutton's [http://www.ed.ac.uk/explore/people/plaques/ Millennial Plaque], which reads, “In honour of James Hutton 1726-1797 [[Geologist]], [[chemist]], [[Natural history|naturalist]], [[father of]] modern [[geology]], [[alumnus]] of the University,” is located at the main entrance of the [[King's Buildings|Grant Institute]]) }}</ref><ref name="Denby">{{cite web |url= http://www.newyorker.com/archive/2004/10/11/041011crat_atlarge |title= Northern Lights: How modern life emerged from eighteenth-century Edinburgh |author= David Denby |format= [[html]] |work= [[The New Yorker]] |publisher= Review of [[James Buchan]]'s ''Crowded With Genius (Capital of the Mind'' in the [[United Kingdom|UK]]) |date= [[11 October]] [[2004]] |quote= In 1770, James Hutton, an [[experiment]]al [[Agriculture|farmer]] and the owner of a [[sal ammoniac]] works, began poking into the peculiar shapes and textures of the [[Salisbury Crags]], the looming, irregular rock formations in [[Edinburgh]]. Hutton noticed something astonishing—[[fossil]]ized fish remains embedded in the rock. The remains suggested that [[Volcano|volcanic activity]] had raised the mass from some depth in the sea. In 1785, he delivered a lecture to the [[Royal Society of Edinburgh]], which included the remarkable statement that “with respect to human observation, this world has neither a beginning nor an end.” Coolly discarding [[Young Earth creationism|Biblical accounts of creation]], the book that he eventually published, “The Theory of the Earth,” helped establish the foundations of modern [[geology]]. }}</ref> His theories of geology and [[Geologic time scale|geologic time]],<ref name="VestigeProspectAMNH">{{cite web |url= http://www.amnh.org/education/resources/rfl/web/essaybooks/earth/p_hutton.html |title= James Hutton: The Founder of Modern Geology |author= [[American Museum of Natural History]] |work= Earth: Inside and Out |date= 2000 |quote= The result, therefore, of this physical enquiry,” Hutton concluded, “is that we find no vestige of a beginning, no prospect of an end. }}</ref> also called [[deep time]],<ref name="TaylorReviewBaxter">{{cite web |url= http://findarticles.com/p/articles/mi_hb3498/is_200609/ai_n18326057 |title= ''Ages in Chaos: James Hutton and the Discovery of Deep Time'' |author= Kenneth L. Taylor |work= [[The Historian]] ([[Abstract (summary)|abstract]]) |publisher= [[Book review]] of [[Stephen Baxter]], ISBN 0-7653-1238-7 |date= September 2006 |quote= }}</ref> came to be included in theories which were called [[plutonism]] and [[Uniformitarianism (science)|uniformitarianism]]. ==Early life and career== James Hutton was born in [[Edinburgh]] on [[3 June]] [[1726]] as one of five children of a merchant who was Edinburgh City Treasurer, but died when James was still young. Hutton's mother had him educated at the [[Royal High School (Edinburgh)|High School of Edinburgh]] where he was particularly interested in mathematics and chemistry, then when he was 14 he attended the [[University of Edinburgh]] as a "student of humanity". He was apprenticed to a lawyer when he was 17, but took more interest in chemical experiments than legal work and at the age of 18 became a [[physician]]'s assistant as well as attending lectures in medicine at the University of Edinburgh. After three years he studied the subject in [[Paris]], then in 1749 took the degree of [[Doctor of Medicine]] at [[Leiden|Leyden]] with a thesis on [[Circulatory system|blood circulation]].<ref name=bio2>{{cite web |url=http://www.james-hutton.org/One/Biography/02.htm |title=Early Years |accessdate=2008-04-11 |publisher=James Hutton.org}}</ref> Around 1747 he had a son by a Miss Edington, and though he gave his child James Smeaton Hutton financial assistance, he had little to do with the boy who went on to become a post-office clerk in [[London]].<ref name=bio4>{{cite web |url=http://www.james-hutton.org/One/Biography/04.htm |title=Settled and Unsettled |accessdate=2008-04-11 |publisher=James Hutton.org}}</ref> After his degree Hutton returned to London, then in the summer of 1750 at the age of 24 went back to Edinburgh and resumed chemical experiments with close friend, James Davie. Their work on production of [[ammonium chloride|sal ammoniac]] from [[soot]] led to their partnership in a profitable chemical works,<ref name=bio3>{{cite web |url=http://www.james-hutton.org/One/Biography/03.htm |title=Thoughts of Settling in the World |accessdate=2008-04-11 |publisher=James Hutton.org}}</ref> manufacturing the crystalline salt which was used for dyeing, metalworking and as smelling salts and previously was available only from natural sources and had to be imported from [[Egypt]]. Hutton owned and rented out properties in Edinburgh, employing a factor to manage this business.<ref name=ent1>{{cite web |url=http://www.james-hutton.org/One/Entrepreneur/Frameset.htm |title=Business and Related Interests |accessdate=2008-04-11 |publisher=James Hutton.org}}</ref> ===Farming and geology=== Hutton inherited from his father the [[Berwickshire]] farms of ''Slighhouses'', a lowland farm which had been in the family since 1713, and the hill farm of ''Nether Monynut''.<ref name=ag1>{{cite web |url=http://www.james-hutton.org/One/Agronomy/Frameset.htm |title=James Hutton the Farmer |accessdate=2008-04-11 |publisher=James Hutton.org}}</ref> In the early 1750s he moved to ''Slighhouses'' and set about making improvements, introducing farming practices from other parts of Britain and experimenting with plant and animal husbandry.<ref name=ag3>{{cite web |url=http://www.james-hutton.org/One/Agronomy/03.htm |title=Return to Slighhouses and Farm Improvement |accessdate=2008-04-11 |publisher=James Hutton.org}}</ref> He recorded his ideas and innovations in an unpublished treatise on ''The Elements of Agriculture''.<ref name=ag6>{{cite web |url=http://www.james-hutton.org/One/Agronomy/06.htm |title=The Elements of Agriculture |accessdate=2008-04-11 |publisher=James Hutton.org}}</ref> This developed his interest in [[meteorology]] and [[geology]],<ref name=ag3/> and by 1753 he had "become very fond of studying the surface of the earth, and was looking with anxious curiosity into every pit or ditch or bed of a river that fell in his way”. Work in clearing and draining his farm provided ample opportunities, and he noticed that “a vast proportion of the present rocks are composed of materials afforded by the destruction of bodies, animal, vegetable and mineral, of more ancient formation”. His theoretical ideas began to come together in 1760, and while his farming activities continued, in 1764 he went on a geological tour of the north of Scotland with George Maxwell-Clerk.<ref name=geo1>{{cite web |url=http://www.james-hutton.org/One/Geology/Frameset.htm |title=Farming and Hutton the Geologist |accessdate=2008-04-11 |publisher=James Hutton.org}}</ref> ===Edinburgh and canal building=== In 1768 Hutton returned to [[Edinburgh]], letting his farms to tenants but continuing to take an interest in farm improvements and research which included experiments carried out at ''Slighhouses''. He developed a red dye made from the roots of the [[madder]] plant.<ref name=ag5>{{cite web |url=http://www.james-hutton.org/One/Agronomy/05.htm |title=Return to Edinburgh |accessdate=2008-04-11 |publisher=James Hutton.org}}</ref> He had a house built in 1770 at St John’s Hill, Edinburgh, overlooking [[Salisbury Crags]].<ref name=ag5/> He was one of the most influential participants in the [[Scottish Enlightenment]], and fell in with numerous first-class minds in the sciences including [[John Playfair]], philosopher [[David Hume]] and economist [[Adam Smith]].<ref name=soc1>{{cite web |url=http://www.james-hutton.org/One/SocialContext/Frameset.htm |title=Hutton’s Contemporaries and The Scottish Enlightenment |accessdate=2008-04-11 |publisher=James Hutton.org}}</ref> He was a particularly close friend of [[Joseph Black]], and the two of them together with Adam Smith founded the ''Oyster Club'' for weekly meetings, with Hutton and Black finding a venue which turned out to have rather disreputable associations.<ref name=soc1>{{cite web |url=http://www.james-hutton.org/One/SocialContext/02.htm |title=The Oyster Club |accessdate=2008-04-11 |publisher=James Hutton.org}}</ref> Between 1767 and 1774 Hutton had considerable close involvement with the construction of the [[Forth and Clyde canal]], making full use of his geological knowledge, both as a shareholder and as a member of the committee of management, and attended meetings including extended site inspections of all the works. In 1777 he published a pamphlet on ''Considerations on the Nature, Quality and Distinctions of Coal and Culm'' which successfully helped to obtain relief from excise duty on carrying small coal.<ref name=ent2>{{cite web |url=http://www.james-hutton.org/One/Entrepreneur/02.htm |title=The Forth and Clyde Canal |accessdate=2008-04-11 |publisher=James Hutton.org}}</ref> ==Theory of rock formations== Hutton hit on a variety of ideas to explain the [[rock formations]] he saw around him, but according to Playfair he "was in no haste to publish his theory; for he was one of those who are much more delighted with the contemplation of truth, than with the praise of having discovered it”. After some 25 years of work,<ref name=geo3>{{cite web |url=http://www.james-hutton.org/One/Geology/03.htm |title=The Theory of the Earth |accessdate=2008-04-11 |publisher=James Hutton.org}}</ref> his ''Theory of the Earth; or an Investigation of the Laws observable in the Composition, Dissolution, and Restoration of Land upon the Globe'' was read to meetings of the [[Royal Society of Edinburgh]] in two parts, the first by his friend [[Joseph Black]] on [[7 March]] [[1785]], and the second by himself on [[4 April]] [[1785]]. Hutton subsequently read an abstract of his dissertation ''Concerning the System of the Earth, its Duration and Stability'' to Society meeting on [[4 July]] [[1785]],<ref name=TOE/> which he had printed and circulated privately.<ref name=abstract/> In it, he outlined his theory as follows; {{quotation|The solid parts of the present land appear in general, to have been composed of the productions of the sea, and of other materials similar to those now found upon the shores. Hence we find reason to conclude:<br> 1st, That the land on which we rest is not simple and original, but that it is a composition, and had been formed by the operation of second causes.<br> 2nd, That before the present land was made, there had subsisted a world composed of sea and land, in which were tides and currents, with such operations at the bottom of the sea as now take place. And,<br> Lastly, That while the present land was forming at the bottom of the ocean, the former land maintained plants and animals; at least the sea was than inhabited by animals, in a similar manner as it is at present.<br> Hence we are led to conclude, that the greater part of our land, if not the whole had been produced by operations natural to this globe; but that in order to make this land a permanent body, resisting the operations of the waters, two things had been required;<br> 1st, The consolidation of masses formed by collections of loose or incoherent materials;<br> 2ndly, The elevation of those consolidated masses from the bottom of the sea, the place where they were collected, to the stations in which they now remain above the level of the ocean.}} ===Search for examples=== [[Image:Hutton's-Section.jpg|thumb|right|''Hutton's Section'' Plaque, [[Salisbury Crags]], Edinburgh. Placed by [[Historic Scotland]].]] At [[Glen Tilt]] in the [[Cairngorms|Cairngorm mountains]] in the [[Scottish Highlands]], Hutton found [[granite]] penetrating [[metamorphic rock|metamorphic]] [[schist]]s, in a way which indicated that the granite had been [[molten]] at the time. This showed to him that granite formed from cooling of molten rock, not [[Precipitation (chemistry)|precipitation]] out of water as others at the time believed, and that the granite must be younger than the schists.<ref name="Macfarlane">{{cite web |url= http://findarticles.com/p/articles/mi_qa3724/is_200309/ai_n9253355 |title= Glimpses into the abyss of time |author= Robert Macfarlane |format= [[html]] |work= [[The Spectator]] |publisher= Review of Repcheck's ''The Man Who Found Time'' |date= [[13 September]] [[2003]] |quote= Hutton possessed an instinctive ability to reverse physical processes - to read landscapes backwards, as it were. Fingering the white quartz which seamed the grey granite boulders in a Scottish glen, for instance, he understood the confrontation that had once occurred between the two types of rock, and he perceived how, under fantastic pressure, the molten quartz had forced its way into the weaknesses in the mother granite. }}</ref><ref name=tilt>[http://www.scottishgeology.com/outandabout/classic_sites/locations/glen_tilt.html Scottish Geology - Glen Tilt]</ref> He went on to find a similar penetration of [[volcanic rock]] through [[sedimentary rock]] near the centre of [[Edinburgh]], at [[Salisbury Crags]],<ref name="Denby"/> adjoining [[Arthur's Seat, Edinburgh|Arthur's Seat]]: this is now known as Hutton's Section.<ref>[http://www.scottishgeology.com/outandabout/classic_sites/locations/huttons_section.html Scottish Geology - Hutton's Section]</ref><ref>[http://www.geos.ed.ac.uk/undergraduate/field/holyrood/huttonsloc.html Hutton's Section at Hoyrood Park]</ref> He found other examples on the [[Isle of Arran]] ([[Hutton's Unconformity]]) and in [[Galloway]].<ref name=tilt/> [[Image:Hutton Unconformity , Jedburgh.jpg|thumb|right|Hutton Unconformity at [[Jedburgh]]. Photograph (2003) below [[John Clerk of Eldin|Clerk of Eldin]] illustration (1787).]] In 1787 Hutton noted what is now known as the Hutton [[Unconformity#Angular unconformity|Unconformity]]<ref name="VestigeProspectAMNH"/> at Inchbonny,<ref name="Unconformity Jedburgh">{{cite web |url= http://www.jedburgh-online.org.uk/aroundjedburgh.asp |title= Jedburgh: Hutton's Unconformity |format= [[html]] |work= Jedburgh online |quote= Whilst visiting Allar's Mill on the Jed Water, Hutton was delighted to see horizontal bands of red sandstone lying 'unconformably' on top of near vertical and folded bands of rock. }}</ref> [[Jedburgh]], in layers of [[sedimentary rock]]. As shown in the illustrations here to the right, layers of grey [[shale]] in the lower layers of the cliff face are tilted almost vertically, immediately above which are horizontal layers of [[red sandstone]]. He found a similar formation at [[Siccar Point]] on the [[Berwickshire]] coast in 1788.<ref>[http://www.snh.org.uk/publications/on-line/geology/elothian_borders/hutton.asp Hutton's Unconformity]</ref> Hutton reasoned that there must have been several cycles, each involving [[deposition]] on the [[seabed]], uplift with tilting and [[erosion]] then undersea again for further layers to be deposited, and there could have been many cycles before over an extremely long history. In a 1788 paper he presented at the [[Royal Society of Edinburgh]],<ref name="VestigeProspectAMNH"/> Hutton remarked, "we find no vestige of a beginning, no prospect of an end." (This memorable line<ref name="VestigeProspectAMNH"/><ref name="KS Thomson">{{cite web |url= http://www.americanscientist.org/template/AssetDetail/assetid/14681;jsessionid=baa9... |title= Vestiges of James Hutton |author= Keith Stewart Thomson |format= [[html]] |work= [[American Scientist]] online, V. 89 #3 p. 212, May/June 2001 {{doi|10.1511/2001.3.212}} |quote= It is ironic that Hutton, the man whose prose style is usually dismissed as unreadable, should have coined one of the most memorable, and indeed lyrical, sentences in all science: "(in geology) we find no vestige of a beginning,—no prospect of an end." In those simple words, Hutton framed a concept that no one had previously contemplated, that the rocks making up the earth today have not, after all, been here since Creation. }}</ref><ref name="Lyrics">{{cite web |url= http://www.altmusic.ru/bands/BadReligion/NoControl.html |title= Lyrics, No Control |author= [[Greg Graffin]] |format= [[html]] |work= [[No Control (Bad Religion album)]] |date= 1989 |quote= there's no vestige of a beginning, no prospect of an end (Hutton, 1795) }}</ref> was quoted in the 1989 song “[[No Control (Bad Religion album)|No Control]]” by songwriter and [[professor]] [[Greg Graffin]].) Hutton brought [[James Hall, 4th Baronet|James Hall]] and [[John Playfair]] to see the strata in 1788. Playfair later commented about the experience, "the mind seemed to grow giddy by looking so far into the abyss of time."<ref name="Playfair RSE">{{cite web |url= http://findarticles.com/p/articles/mi_m1134/is_5_108/ai_54830705 |title= Hutton's Unconformity |author= [[John Playfair]] |format= [[html]] |work= Transactions of the [[Royal Society of Edinburgh]], vol. V, pt. III, 1805, quoted in [[Natural History (magazine)|Natural History]], June 1999 |quote= }}</ref> ==Publication== Though Hutton circulated privately a printed version of the abstract of his Theory (''Concerning the System of the Earth, its Duration, and Stability'') which he read at a meeting of the [[Royal Society of Edinburgh]] on [[4 July]] [[1785]],<ref name=abstract>[http://www.uwmc.uwc.edu/geography/hutton/Abstract-facsimile/abstract1.htm ''Concerning the System of the Earth''] abstract</ref> the theory as read at the [[7 March]] [[1785]] and [[4 April]] [[1785]] meetings did not appear in print until 1788. It was titled ''Theory of the Earth; or an Investigation of the Laws observable in the Composition, Dissolution, and Restoration of Land upon the Globe'' and appeared in ''Transactions of the Royal Society of Edinburgh'', vol. I, Part II, pp.209-304, plates I and II, published 1788.<ref name=TOE>[http://www.uwmc.uwc.edu/geography/hutton/hutton.htm ''Theory of the Earth''] full text (1788 version)</ref> Following criticism, especially [[Richard Kirwan]]'s, who thought him [[atheist]] and not logical, among other things,<ref name=TOE/> Hutton published a two volume version of his theory in 1795,<ref name="TheoryEarthGutenbergVolONE">{{gutenberg|no=12861|name=Theory of the Earth, Volume 1}}</ref><ref name="TheoryEarthGutenbergVolTWO">{{gutenberg|no=14179|name=Theory of the Earth, Volume 2}}</ref> consisting of the 1788 version of his theory (with slight additions) along with a lot of material drawn from shorter papers Hutton already had to hand on various subjects such as the origin of granite. It included a review of alternative theories, such as those of [[Thomas Burnet]] and [[Georges-Louis Leclerc, Comte de Buffon]]. The whole was entitled ''An Investigation of the Principles of Knowledge and of the Progress of Reason, from Sense to Science and Philosophy'' when the third volume was completed in 1794.<ref name="Pearson">{{cite web |url= http://thedispersalofdarwin.blogspot.com/2007/06/more-on-james-hutton.html |title= In Retrospect |author= Paul N. Pearson |format= [[html]] |work= [[Nature (journal)|Nature]] [http://www.nature.com/nature/journal/v425/n6959/index.html V. 425 #6959, p. 665] |publisher= Comments on Hutton's 3-volume 1794 work, ''An Investigation of the Principles of Knowledge and of the Progress of Reason, from Sense to Science and Philosophy'' |date= [[16 October]] [[2003]] |quote= }}</ref> Its 2,138 pages prompted Playfair to remark that “The great size of the book, and the obscurity which may justly be objected to many parts of it, have probably prevented it from being received as it deserves.” ==Opposing theories== His new theories placed him into opposition with the then-popular [[Neptunism|Neptunist]] theories of [[Abraham Gottlob Werner]], that all rocks had precipitated out of a single enormous flood. Hutton proposed that the [[interior of the Earth]] was hot, and that this heat was the engine which drove the creation of new rock: land was eroded by air and water and deposited as layers in the sea; heat then consolidated the [[sediment]] into stone, and uplifted it into new lands. This theory was dubbed "[[Plutonism|Plutonist]]" in contrast to the flood-oriented theory. As well as combating the Neptunists, he also opened up the concept of [[deep time]] for scientific purposes, in opposition to [[Catastrophism]]. Rather than accepting that the earth was no more than a few thousand years old, he maintained that the [[Age of the planet Earth|Earth must be much older]], with a history extending indefinitely into the distant past.<ref name="Macfarlane"/> His main line of argument was that the tremendous displacements and changes he was seeing did not happen in a short period of time by means of catastrophe, but that processes still happening on the Earth in the present day had caused them. As these processes were very gradual, the Earth needed to be ancient, in order to allow time for the changes. Before long, scientific inquiries provoked by his claims had pushed back the age of the earth into the millions of years &ndash; still too short when compared with what is known in the 21st century, but a distinct improvement. ==Acceptance of geological theories== The prose of ''Principles of Knowledge'' was so obscure, in fact, that it also impeded the acceptance of Hutton's geological theories. Restatements of his geological ideas (though not his thoughts on evolution) by [[John Playfair]] in 1802 and then [[Charles Lyell]] in the 1830s removed this hindrance. If anything, Hutton's ideas were eventually accepted too well. At least some of the initial resistance to modern scientific ideas like [[plate tectonics]] and asteroid strikes causing mass extinctions can be attributed to too-strict adherence to [[Uniformitarianism (science)|uniformitarianism]]. ==Other contributions== ===Meteorology=== It was not merely the earth to which Hutton directed his attention. He had long studied the changes of the [[Earth's atmosphere|atmosphere]]. The same volume in which his ''Theory of the Earth'' appeared contained also a ''Theory of [[Rain]]''. He contended that the amount of moisture which the air can retain in [[solution]] increases with temperature, and, therefore, that on the mixture of two masses of air of different temperatures a portion of the moisture must be condensed and appear in visible form. He investigated the available data regarding [[rainfall]] and [[climate]] in different regions of the globe, and came to the conclusion that the rainfall is regulated by the [[humidity]] of the air on the one hand, and mixing of different [[air current]]s in the higher atmosphere on the other. ===Evolution=== Hutton also advocated uniformitarianism for living creatures too &ndash; [[evolution]], in [[evolutionism|a sense]] &ndash; and even suggested [[natural selection]] as a possible mechanism affecting them: :"...if an organised body is not in the situation and circumstances best adapted to its sustenance and propagation, then, in conceiving an indefinite variety among the individuals of that species, we must be assured, that, on the one hand, those which depart most from the best adapted constitution, will be the most liable to perish, while, on the other hand, those organised bodies, which most approach to the best constitution for the present circumstances, will be best adapted to continue, in preserving themselves and multiplying the individuals of their race." &ndash; ''Investigation of the Principles of Knowledge'', volume 2.<ref name="Pearson"/> Hutton gave the example that where dogs survived through "swiftness of foot and quickness of sight... the most defective in respect of those necessary qualities, would be the most subject to perish, and that those who employed them in greatest perfection... would be those who would remain, to preserve themselves, and to continue the race". Equally, if an acute [[sense of smell]] was "more necessary to the sustenance of the animal... the same principle [would] change the qualities of the animal, and.. produce a race of well scented hounds, instead of those who catch their prey by swiftness". The same "principle of variation" would influence "every species of plant, whether growing in a forest or a meadow". He came to his ideas as the result of experiments in [[Plant propagation|plant]] and [[animal breeding]], some of which he outlined in an unpublished manuscript, the ''Elements of Agriculture''. He distinguished between [[heritable variation]] as the result of breeding, and [[non-heritable variations]] caused by environmental differences such as soil and climate. Hutton saw his "principle of variation" as explaining the development of varieties, but rejected the idea of evolution originating species as a "romantic fantasy". As a [[deism|deist]], to him this mechanism allowed species to form varieties better adapted to particular conditions and was evidence of benevolent design in nature. Hutton's ideas on geology were clarified in [[Charles Lyell]]'s books, which [[Charles Darwin]] read with enthusiasm during his [[Second voyage of HMS Beagle|voyage on the Beagle]], and it remained to Darwin independently to develop the idea of [[natural selection]] to explain ''[[The Origin of Species]]'' and bring it to the forefront of public consciousness at the same time as providing the voluminous evidence necessary to win over the scientific community to the theory. ==Works == * 1785. ''Abstract of a Dissertation Read in the Royal Society of Edinburgh, Upon the Seventh of March, and Fourth of April, MDCCLXXXV, Concerning the System of the Earth, Its Duration, and Stability''. Edinburgh. 30pp. * 1788. ''The Theory of Rain''. Transactions of the Royal Society of Edinburgh, vol. 1, Part 2, pp. 41-86. * 1788. ''Theory of the Earth; or an Investigation of the Laws observable in the Composition, Dissolution, and Restoration of Land upon the Globe''. Transactions of the Royal Society of Edinburgh, vol. 1, Part 2, pp. 209-304. * 1792. ''Dissertations on different subjects in natural philosophy.'' Edinburgh ; London : A. Strahan, and T. Cadell. * 1794. ''Observations on granite''. Transactions of the Royal Society of Edinburgh, vol. 3, pp. 77-81. * 1794. ''A dissertation upon the philosophy of light, heat, and fire.'' Edinburgh : Cadell, Junior, Davies. * 1794. ''An Investigation of the Principles of Knowledge and of the Progress of Reason, from Sense to Science and Philosophy''. Edinburgh : A. Strahan, and T. Cadell. * 1795. ''Theory of the Earth; with Proofs and Illustrations''. Edinburgh: William Creech. 2 vols. * 1797. ''Elements of Agriculture''. Unpublished Manuscript. * 1899. ''Theory of the Earth; with Proofs and Illustrations, vol III'', Edited by Sir Archibald Geikie. Geological Society, Burlington: House, London. ==References== {{reflist}} ;''Biographies<nowiki>:</nowiki>'' * Jack Repcheck: ''The Man Who Found Time: James Hutton and the Discovery of the Earth's Antiquity.'' [[London]] and [[Cambridge, Massachusetts]]: [[Simon & Schuster]] (2003). ISBN 0743231899 ([[United Kingdom|UK]]), ISBN 073820692X ([[United States|US]]). * [[Stephen Baxter]]: ''Ages in Chaos: James Hutton and the Discovery of Deep Time.'' [[New York City|New York]]: [[Tor Books]] (Forge [[imprint]]), 2004. ISBN 0-76531-238-7. Published in the [[United Kingdom|UK]] as ''Revolutions in the Earth: James Hutton and the True Age of the World.'' [[London]]: [[Weidenfeld & Nicolson]], 2003. ISBN 0-29782-975-0. ==See also== {{Commons|James Hutton}} *[[Geology of Scotland]] *[[Climate of Scotland]] *[[Nicholas Steno]] *[[Shen Kuo]] ==External links== *[http://www.james-hutton.org.uk/ James Hutton.org.uk], links to ''James Hutton — The Man'' and ''The James Hutton Trail''. *[http://www.1911encyclopedia.org/H/HU/HUTTON_JAMES.htm Biography of James Hutton (From: Encyclopaedia Britannica, 11th Ed., 1910-1911)] *[http://www.mala.bc.ca/~johnstoi/darwin/sect2.htm James Hutton and Uniformitarianism] (scroll down) *[http://www.uwmc.uwc.edu/geography/hutton/James%20Hutton%20grave.htm James Hutton's memorial in Greyfriars Kirkyard, Edinburgh] *[http://www.uwmc.uwc.edu/geography/hutton/hutton.htm First Publication of Theory of the Earth] *[http://strata.geol.sc.edu/terminology/unconformity.html Glossary] Definition and examples of [[unconformity]] *[http://www.ronaldbrucemeyer.com/rants/0603almanac.htm Accessible Historical Perspective on James Hutton] * {{gutenberg author| id=Hutton_James | name=James Hutton}} * {{MacTutor Biography|id=Hutton_James}} * {{worldcat id|id=lccn-n80-153739}} {{Persondata |NAME=Hutton, James |ALTERNATIVE NAMES= |SHORT DESCRIPTION=Scottish geologist |DATE OF BIRTH=[[14 June]] [[1726]] |PLACE OF BIRTH=[[Edinburgh]] |DATE OF DEATH=[[26 March]] [[1797]] |PLACE OF DEATH= }} {{Enlightenment}} {{DEFAULTSORT:Hutton, James}} [[Category:1726 births]] [[Category:1797 deaths]] [[Category:Charles Darwin]] [[Category:People from Edinburgh]] [[Category:Burials at Greyfriars Kirkyard]] [[Category:Royal High School alumni]] [[Category:Royal Society of Edinburgh]] [[Category:Scottish Enlightenment]] [[Category:Scottish geologists]] [[Category:Scottish meteorologists]] [[Category:Alumni of the University of Edinburgh]] [[Category:Leiden University]] [[Category:University of Paris alumni]] [[ca:James Hutton]] [[da:James Hutton]] [[de:James Hutton]] [[et:James Hutton]] [[es:James Hutton]] [[eo:James Hutton]] [[fr:James Hutton]] [[id:James Hutton]] [[it:James Hutton]] [[ka:ჯეიმზ ჰატონი]] [[lb:James Hutton]] [[hu:James Hutton]] [[nl:James Hutton]] [[ja:ジェームズ・ハットン]] [[no:James Hutton]] [[pl:James Hutton]] [[pt:James Hutton]] [[sco:James Hutton]] [[sk:James Hutton]] [[sl:James Hutton]] [[sr:Џејмс Хатон]] [[sv:James Hutton]] [[tr:James Hutton]]