' Letters to Sir Joseph Williamson (Camden Soc., 1874), i.
Williamson (Proc. Roy.
-A Williamson, Journeys in North China, Manchuria and Eastern Mongolia (2 vols., London, 1870); S.
ALEXANDER WILLIAM WILLIAMSON (1824-1904), English chemist, was born at Wandsworth, London, on the 1st of May 18 24.
For his work on etherification Williamson in 1862 received a Royal medal from the Royal Society, of which he became a fellow in 1855, and which he served as foreign secretary from 1873 to 1889.
The older histories of the colony are: Hugh Williamson, History of North Carolina (2 vols.
TAYLOR, a town in Williamson county, Texas, U.S.A., about 35 m.
Williamson as professor of chemistry at University College, London.
Williamson showed how alcohol and ether were to be regarded as derived from water by substituting one or both hydrogen atoms by the ethyl group; he derived acids and the acid anhydrides from the same type; and from a comparison of many inorganic and the simple organic compounds he concluded that this notion of a " water-type " clarified, in no small measure, the conception of the structure of compounds.
The city has, besides, numerous fine office buildings, including that of the Society for Savings (an institution in which each depositor is virtually a stockholder), the Citizens', Rose, Williamson, Rockefeller, New England and Garfield buildings; and several beautiful churches, notably the Roman Catholic and Trinity cathedrals, the First Presbyterian ("Old Stone"), the Second Presbyterian, the First Methodist and Plymouth (Congregational) churches.
GEORGETOWN, a city and the county-seat of Williamson county, Texas, U.S.A., on the San Gabriel river, about 25 m.
The Williamson artisan school is entirely supported by an endowment.
Williamson in 1850.
Williamson (Journeys in North China, i.
There are several varieties of grasshopper mice (Orychomys), white-footed mice (Peromyscus), harvest mice (Reithrodontomys), rice-rats (Oryzomys), wood-rats (Neotoma), voles (Microtus), &c. Bats inhabit caves in Burnet, Williamson, Lampasas, Gillespie and other counties.
C. Williamson, by his study of the structure of the plants of the coalmeasures, opened up a new line of research which has been followed by Bertrand Renault, D.
FRANKLIN, a town and the county-seat of Williamson county, Tennessee, U.S.A., in the central part of the state, on the Harpeth river, and about 20 m.
C. Williamson, Francia (1900).
C. Williamson and F.
C. Williamson (best known as a botanist) in Pritchard's Infusoria, in 1861.
C. Williamson, "The Rotifera" in A.
John Williamson Nevin >>
This has been so since the famous law case of Williamson v.
Williamson in the principal square of Walsall.
In 1907 (according to state authorities) coal was produced in 52 counties, Williamson, Sangamon, St Clair, Macoupin and Madison giving the largest yield.
Williamson, Journeys in North China (London, 1870), S.
Williamson, Ann., 1852, 81, p. 77).
Williamson and F.
Yet in this area, according to the investigations of Mr Williamson (Report of the Scottish Fishery Board for 1898), nearly 500 millions of plaice eggs are naturally produced in one spawning season.
The governors of the state have been as follows: - William King Democrat William Durkee Williamson (acting) Benjamin Ames (acting) .
Williamson, History of the State of Maine (Hallowell, 1832); J.
JOHN WILLIAMSON NEVIN (1803-1886), American theologian and educationalist, was born on Herron's Branch, near Shippensburg, Franklin county, Pennsylvania, on the 20th of February 1803.
He was a descendant of Hugh Williamson of North Carolina, and was of Scotch blood and Presbyterian training.
See Theodore Appel, The Life and Work of John Williamson Nevin (Philadelphia, 1889), containing Nevin's more important articles.
Calcified specimens are especially characteristic of the British Carboniferous formation; their preservation is equally perfect with that of the silicified fossils, and their investigation by Witham, Binney, Williamson and others has proved no less fertile.
The investigations of Nathorst, Williamson and others have shown that a very large proportion of the casts and impressions attributed to Algae had in all probability a totally different origin.
Spherical sacs, bearing forked spines, described by Williamson under the name of Zygosporites, are frequent, usually in an isolated state.
The anatomical structure of all parts of the plant is now known, in various Calamarieae, thanks more especially to the work of Williamson in England and of Renault in France.
Size.) After Williamson (Scott, " Studies").
Williamson thoroughly worked out, in petrified specimens, the organization of a cone which he named Bowmanites Dawsoni; it was subsequently demonstrated by Zeiller that this fructification belonged to a Sphenophyllum, the cones of the well known species S.
The type of fructification described by Williamson and now named Sphenophyllum Dawsoni consists of long cylindrical cones, in external habit not unlike those of some Calamarieae.
Affinities to any members of the group, and the view, of which Williamson was the chief advocate, that they form a homogeneous Cryptogamic family, is now fully established.
Primary phloem can be recognized with certainty in favourable cases, the question of the formation of secondary phloem by the cambium is not yet fully cleared up. In the Lepidodendron fuliginosum of Williamson, shown by its leaf-bases to have been a Lepidophloios, the secondary wood is very irregular, and consists largely of parenchyma.
The structure of a Bothrodendron has recently been investigated and proves to be identical with that of the petrified stem which Williamson named Lepidodendron mundum.
Grievii, of Williamson, from the Lower Carboniferous of Scotland.
The curious, transversely-ribbed fossils known as Sternbergia or Artisia have proved to be casts of the medullary cavity of Cordaiteae; their true nature was first demonstrated by Williamson in 1850.
Williamson was the first to express the opinion that the Bennettitean flowers known as Williamsonia were borne on the trunks which terminated in a crown of pinnate fronds of the type long known as Zamites gigas; this view was regarded by Saporta and others as incorrect, and the nature of the Bennettitean foliage was left an open question.
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