then returned to Washington, resigned his seat, and entered the Union army as colonel of the 31st Illinois Volunteers, which he organized. He was regarded as one of the ablest officers who entered the army from civil life. In Grant’s campaigns terminating in the capture of Vicksburg, which city Logan’s division was the first to enter and of which he was military governor, he rose to the rank of major-general of volunteers; in November 1863 he succeeded Sherman in command of the XV. Army Corps; and after the death of McPherson he was in command of the Army of the Tennessee at the battle of Atlanta. When the war closed, Logan resumed his political career as a Republican, and was a member of the National House of Representatives from 1867 to 1871, and of the United States Senate from 1871 until 1877 and again from 1879 until his death, which took place at Washington, D.C., on the 26th of December 1886. He was always a violent partisan, and was identified with the radical wing of the Republican party. In 1868 he was one of the managers in the impeachment of President Johnson. His war record and his great personal following, especially in the Grand Army of the Republic, contributed to his nomination for Vice-President in 1884 on the ticket with James G. Blaine, but he was not elected. His impetuous oratory, popular on the platform, was less adapted to the halls of legislation. He was commander-in-chief of the Grand Army of the Republic from 1868 to 1871, and in this position successfully urged the observance of Memorial or Decoration Day, an idea which probably originated with him. He was the author of The Great Conspiracy: Its Origin and History (1886), a partisan account of the Civil War, and of The Volunteer Soldier of America (1887). There is a fine statue of him by St Gaudens in Chicago.
The best biography is that by George F. Dawson, The Life and Services of Gen. John A. Logan, as Soldier and Statesman (Chicago and New York, 1887).
LOGAN, SIR WILLIAM EDMOND (1798–1875), British geologist, was born in Montreal on the 20th of April 1798, of Scottish parents. He was educated partly in Montreal, and subsequently at the High School and university of Edinburgh, where Robert Jameson did much to excite his interest in geology. He was in a business house in London from 1817 to 1830. In 1831 he settled in Swansea to take charge of a colliery and some copper-smelting works, and here his interest in geology found abundant scope. He collected a great amount of information respecting the South Wales coal-field; and his data, which he had depicted on the 1-in. ordnance survey map, were generously placed at the disposal of the geological survey under Sir H. T. de la Beche and fully utilized. In 1840 Logan brought before the Geological Society of London his celebrated paper “On the character of the beds of clay lying immediately below the coal-seams of South Wales, and on the occurrence of coal-boulders in the Pennant Grit of that district.” He then pointed out that each coal-seam rests on an under-clay with rootlets of Stigmaria, and he expressed his opinion that the under-clay was the old soil in which grew the plants from which the coal was formed. To confirm this observation he visited America in 1841 and examined the coal-fields of Pennsylvania and Nova Scotia, where he found the under-clay almost invariably present beneath the seams of coal. In 1842 he was appointed to take charge of the newly established geological survey in Canada, and he continued as director until 1869. During the earlier years of the survey he had many difficulties to surmount and privations to undergo, but the work was carried on with great tact and energy, and he spared no pains to make his reports trustworthy. He described the Laurentian rocks of the Laurentian mountains in Canada and of the Adirondacks in the state of New York, pointing out that they comprised an immense series of crystalline rocks, gneiss, mica-schist, quartzite and limestone, more than 30,000 ft. in thickness. The series was rightly recognized as representing the oldest type of rocks on the globe, but it is now known to be a complex of highly altered sedimentary and intrusive rocks; and the supposed oldest known fossil, the Eozoon described by Sir J. W. Dawson, is now regarded as a mineral structure. Logan was elected F.R.S. in 1851, and in 1856 was knighted. In the same year he was awarded the Wollaston medal by the Geological Society of London for his researches on the coal-strata, and for his excellent geological map of Canada. After his retirement in 1869, he returned to England, and eventually settled in South Wales. He died at Castle Malgwyn in Pembrokeshire, on the 22nd of June 1875.
See the Life, by B. J. Harrington (1883). (H. B. Wo.)
LOGAN, a city and the county-seat of Cache county, Utah, U.S.A., on the Logan river, about 70 m. N. of Salt Lake City. Pop. (1900) 5451 (1440 foreign-born); (1910) 7522. It is served by the Oregon Short Line railroad. It lies at the mouth of Logan Cañon, about 4500 ft. above the sea, and commands magnificent views of the Wasatch Mountains and the fertile Cache Valley. At Logan is a temple of the Latter-Day Saints (or Mormons), built in 1883, and the city is the seat of the Agricultural College of Utah, of Brigham Young College, and of New Jersey Academy (1878), erected by the women of the Synod of New Jersey and managed by the Woman’s Board of Home Missions of the Presbyterian Church. The Agricultural College was founded in 1888 and opened in 1890; an agricultural experiment station is connected with it and the institution comprises schools of agriculture, domestic science and arts, commerce, mechanic arts and general science. Six experiment stations in different parts of the state and a central experimental farm near St George, Washington county, were in 1908 under the direction of the experiment station in Logan. Brigham Young College was endowed by Brigham Young in 1877 and was opened in 1878; it offers courses in the arts, theology, civil engineering, music, physical culture, domestic science, nurse training and manual training. Logan has various manufactures, and is the trade centre for a fertile farming region. The municipality owns and operates its water works and its electric lighting plant. Logan was settled in 1859 and first incorporated in 1866.
LOGANSPORT, a city and the county-seat of Cass county,
Indiana, U.S.A., on the Wabash river, at the mouth of the Eel
river, about 67 m. N. by W. of Indianapolis and 117 m. S. by
E. of Chicago. Pop. (1900) 16,204, of whom 1432 were foreign-born,
(1910 census) 19,050. It is served by six divisions
of the Pittsburg, Cincinnati, Chicago & St Louis, two divisions
of the Vandalia (Pennsylvania Lines), and the Wabash railways,
and by electric interurban lines. The city is the seat of the
Northern Indiana Hospital for the Insane (1888), and has a
public library, and a hospital (conducted by the Sisters of St
Joseph). Among the principal buildings are the court house,
a Masonic temple, an Odd Fellows’ temple, and buildings of
the Order of Elks, of the Knights of Pythias, and of the fraternal
order of Eagles. Situated in the centre of a rich agricultural
region, Logansport is one of the most important grain and produce
markets in the state. The Wabash and the Eel rivers provide
good water power, and the city has various manufactures,
besides the railway repair shops of the Vandalia and of the
Pittsburg, Cincinnati, Chicago & St Louis railways. The value
of the city’s factory product increased from $2,100,394 in 1900
to $2,955,921 in 1905, or 40.7%. Limestone, for use in the
manufacture of iron, is quarried in the vicinity. The city owns
and operates the water works and the electric-lighting plant.
Logansport was platted in 1828, was probably named in honour
of a Shawnee chief, Captain Logan (d. 1812), became the county-seat
of Cass county in 1829, and was chartered as a city in
1838.
LOGAR, a river and valley of Afghanistan. The Logar river
drains a wide tract of country, rising in the southern slopes of the
Sanglakh range and receiving affluents from the Kharwar hills,
N.E. of Ghazni. It joins the Kabul river a few miles below the
city of Kabul. The Logar valley, which is watered by its southern
affluents, is rich and beautiful, about 40 m. long by 12 wide,
and highly irrigated throughout. Lying in the vicinity of the
capital, the district contributes largely to its food-supply. The
valley was traversed in 1879 by a brigade under Sir F. (afterwards
Lord) Roberts.
