See also:SIR See also:CHARLES See also:LYELL (1797-1875)
, See also:British geologist, was the eldest son of See also:Charles See also:Lyell of Kinnordy, See also:Forfarshire, and
was See also:born on the 14th of See also:November 1797, on the See also:family See also:estate in See also:Scotland
.
His See also:father (1767–1849) was known both as a botanist and as the translator of the Vita Nuova and the Convito of See also:Dante: the plant Lyellia was named after him
.
From his boyhood Lyell had a strong inclination for natural See also:history, especially See also:entomology, a See also:taste which he cultivated at Bartley See also:Lodge in the New See also:Forest, to which his family had removed soon after his See also:birth
.
In 1816 he entered See also:Exeter See also:College, See also:- OXFORD
- OXFORD, EARLS OF
- OXFORD, EDWARD DE VERE, 17TH EARL
- OXFORD, JOHN DE VERE, 13TH EARL OF (1443-1513)
- OXFORD, PROVISIONS OF
- OXFORD, ROBERT DE VERE, 9TH EARL OF (1362-1392)
- OXFORD, ROBERT HARLEY, 1ST
Oxford, where the lectures of Dr See also:Buckland first See also:drew his See also:attention to See also:geological study
.
After taking his degree of B.A. in 1819 (M.A. in 1821) he entered See also:Lincoln's See also:Inn, and in 1825, after a delay caused by chronic weakness of the eyes, he was called to the See also:bar, and went on the western See also:circuit for two years
.
During this See also:- TIME (0. Eng. Lima, cf. Icel. timi, Swed. timme, hour, Dan. time; from the root also seen in " tide," properly the time of between the flow and ebb of the sea, cf. O. Eng. getidan, to happen, " even-tide," &c.; it is not directly related to Lat. tempus)
- TIME, MEASUREMENT OF
- TIME, STANDARD
time he was slowly gravitating towards the See also:life of a student of See also:science
.
In 1819 he had been elected a See also:fellow of the Linnean and Geological See also:Societies, communicating his first See also:paper, " On a See also:Recent Formation of Fresh-See also:water See also:Limestone in Forfarshire," to the latter society in 1822, and acting as one of the honorary secretaries in 1823
.
In that See also:year he went to See also:France, with introductions to See also:Cuvier, See also:Humboldt and other men of science, and in 1824 made a geological tour in Scotland in See also:company with Dr Buckland
.
In 1826 he was elected a fellow of the Royal Society, from which in later years he received both the See also:Copley and Royal medals; and in 1827 he finally abandoned the legal profession, and devoted himself to See also:geology
.
At this time he had already begun to See also:plan his See also:chief See also:work, The Principles of Geology
.
The subsidiary See also:title, " An See also:Attempt to Explain the Former Changes of the See also:Earth's See also:Surface by Reference to Causes now in Operation," gives the keynote of the task to which Lyell devoted his life
.
A See also:journey with See also:Murchison in 1828 gave rise to See also:joint papers on the volcanic See also:district of See also:Auvergne and the See also:Tertiary formations of See also:Aix-en-See also:Provence
.
After parting with Murchison he studied the marine remains of the See also:Italian Tertiary Strata and then conceived the See also:idea of dividing this geological See also:system into three or four See also:groups, characterized by the proportion of recent to See also:extinct See also:species of shells
.
To these groups, after consulting Dr See also:Whewell as to the best nomenclature, he gave the names now universally adopted—See also:Eocene (See also:dawn of recent), See also:Miocene (less of recent), and See also:Pliocene (more of recent); and with the assistance of G
.
P
.
See also:Deshayes he drew See also:lip a table of shells in See also:illustration of this See also:classification
.
The first See also:volume of the Principles of Geology appeared in 1830, and the second in See also:January 1832
.
Received at first with some opposition, so far as its leading theory was concerned, the work had ultimately a See also:great success, and the two volumes had already reached a second edition in 1833 when the third, dealing with the successive formations of the earth's crust, was added
.
Between 183o and 1872 eleven See also:editions of this work were published, each so much enriched with new material and the results of riper thought as to See also:form a See also:complete history of the progress of geology during that See also:interval
.
Only a few days before his See also:death See also:Sir Charles finished revising the first volume of the 12th edition; the revision of the second volume was completed by his See also:nephew Mr (after-wards Sir) Leonard Lyell; and the work appeared in 1876
.
In See also:August 1838 Lyell published the Elements of Geology, which, from being originally an expansion of one See also:section of the Principles, became a See also:standard work on stratigraphical and palaeontological geology
.
This See also:book went through six editions in Lyell's lifetime (some intermediate editions being styled See also:Manual of Elementary Geology), and in 1871 a smaller work, the Student's Elements of Geology, was based upon it
.
His third great work, The Antiquity of See also:Man, appeared in 1863, and ran through three editions in one year
.
In this he gave a See also:general survey of the arguments for man's See also:early See also:appearance on the earth, derived from the discoveries of See also:flint implements in See also:post-Pliocene strata in the See also:Somme valley and elsewhere; he discussed also the deposits of the Glacial See also:epoch, and in the same volume he first gave in his See also:adhesion to See also:Darwin's theory of the origin of species
.
A See also:fourth edition appeared in 1873
.
In 1831–1833 Lyell was See also:professor of geology at See also:- KING
- KING (O. Eng. cyning, abbreviated into cyng, cing; cf. O. H. G. chun- kuning, chun- kunig, M.H.G. kiinic, kiinec, kiinc, Mod. Ger. Konig, O. Norse konungr, kongr, Swed. konung, kung)
- KING [OF OCKHAM], PETER KING, 1ST BARON (1669-1734)
- KING, CHARLES WILLIAM (1818-1888)
- KING, CLARENCE (1842–1901)
- KING, EDWARD (1612–1637)
- KING, EDWARD (1829–1910)
- KING, HENRY (1591-1669)
- KING, RUFUS (1755–1827)
- KING, THOMAS (1730–1805)
- KING, WILLIAM (1650-1729)
- KING, WILLIAM (1663–1712)
King's College, See also:London, and delivered while there a course of lectures, whieh became the See also:foundation of the Elements of Geology
.
In 1832 hemarried See also:Mary (1809–1873) eldest daughter of Leonard See also:Horner (q.v.), and she became thenceforward associated with him in all his work, and by her social qualities making his See also:home a centre of attraction
.
In 1834 he made an excursion to See also:Denmark and See also:Sweden, the result of which was his Bakerian lecture to the Royal Society " On the Proofs of the See also:gradual Rising of See also:Land in certain Parts of Sweden." He also brought before the Geological Society a paper " On the Cretaceous and Tertiary Strata of Seeland and Moen." In 1835 he became See also:president of the Geological Society
.
In 1837 he was again in See also:Norway and Denmark, and in 1841 he spent a year in travelling through the See also:United States, See also:Canada and Nova See also:Scotia
.
This last journey, together with a second one to See also:America in 1845, resulted not only in papers, but also in two See also:works not exclusively geological, Travels in See also:North America (1845) and A Second Visit to the United States (1849)
.
During these journeys he estimated the See also:rate of recession of the falls of See also:Niagara, the See also:annual See also:average See also:accumulation of alluvial See also:matter in the See also:delta of the See also:Mississippi, and studied those See also:vegetable accumulations in the " Great See also:Dismal Swamp " of See also:Virginia, which he afterwards used in illustrating the formation of beds of See also:coal
.
He also studied the coal-formations in Nova Scotia, and discovered in company with Dr (afterwards Sir J
.
W.) See also:Dawson (q.v.) of See also:Montreal, the earliest known landshell, Pupa vetusta, in the hollow See also:stem of a Sigillaria
.
In bringing a knowledge of See also:European geology to See also:bear upon the extended formations of North America Lyell rendered immense service
.
Having visited See also:Madeira and See also:Teneriffe in company with G
.
Hartung, he accumulated much valuable See also:evidence on the See also:age and deposition of See also:lava-beds and the formation of volcanic cones
.
He also revisited See also:Sicily in 1858, when he made such observations upon the structure of See also:Etna as refuted the theory of " craters of See also:elevation " upheld by Von See also:Buch and See also:Elie de See also:Beaumont (see Phil
.
Trans., 1859)
.
Lyell was knighted in 1848, and was created a See also:baronet in 1864, in which year he was president of the British Association at See also:Bath
.
He was elected corresponding member of the See also:French See also:Institute and of the Royal See also:Academy of Sciences at See also:Berlin, and was created a See also:knight of the Prussian See also:- ORDER
- ORDER (through Fr. ordre, for earlier ordene, from Lat. ordo, ordinis, rank, service, arrangement; the ultimate source is generally taken to be the root seen in Lat. oriri, rise, arise, begin; cf. " origin ")
- ORDER, HOLY
Order of Merit
.
During the later years of his life his sight, always weak, failed him altogether
.
He died on the 22nd of See also:February 1875, and was buried in See also:Westminster See also:Abbey
.
Among his characteristics were his great thirst for knowledge, his perfect fairness and See also:sound See also:judgment; while the extreme freshness of his mind enabled him to accept and appreciate the work of younger men
.
The LYELL See also:MEDAL, established in 1875 under the will of Sir Charles Lyell, is See also:cast in See also:bronze and is to be awarded annually (or from time to time) by the See also:Council of the Geological Society
.
The medallist may be of any See also:country or either See also:sex
.
Not less than one-third of the annual See also:interest of a sum of £2000 is to be awarded with the medal; the remaining interest, known as the LYELL GEOLOGICAL FUND, is to be given in one or more portions at the discretion of the Council for the encouragement of geological science
.
See Life, Letters and See also:Journals of Sir Charles Lyell, See also:Bart., edited by his See also:sister-in-See also:law, Mrs Lyell (2 vols., 1881) ; Charles Lyell and See also:Modern Geology, by T
.
G
.
See also:Bonney (1895)
.
(H
.
B
.
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