FRASER, SIR WILLIAM AUGUSTUS, Bart. (1826-1898), English politician, author and collector, was born on the 10th of February 1826, the son of Sir James John Fraser, 3rd baronet, a colonel of the 7th Hussars, who had served on Wellington's staff at Waterloo. He was educated at Eton and at Christ Church, Oxford, entered the 1st Life Guards in 1847, but retired with a captain's rank in 1852. He then set about entering parliament, and the ups and downs of his political career were rather remarkable. He was returned for Barnstaple in 1852, but the election was declared void on account of bribery, and the constituency was disfranchised for two years. At the election of 1857 Sir William, who had meantime been defeated at Harwich, was again returned at Barnstaple. He was, however, defeated in 1859, but was elected in 1863 at Ludlow. This seat he held for only two years, when he was again defeated and did not re-enter parliament until 1874, when be was returned for Kidderminster, a constituency he represented for six years, when he retired. He was a familiar figure at the Carlton Club, always ready with a copious collection of anecdotes of Wellington, Disraeli and Napoleon III. He died on the 17th of August 1898. He was an assiduous collector of relics; and his library was sold for some L20,000. His own books comprise _Words on Wellington_ (1889), _Disraeli and his Day_ (1891), _Hic et Ubique_ (1893), _Napoleon III._ (1896) and the _Waterloo Ball_ (1897). FRASER, the chief river of British Columbia, Canada, rising in two branches among the Rocky Mountains near 52 deg. 45' N., 118 deg. 30' W. Length 740 m. It first flows N.W. for about 160 m., then rounds the head of the Cariboo Mountains, and flows directly S. for over 400 m. to Hope, where it again turns abruptly and flows W. for 80 m., falling into the Gulf of Georgia at New Westminster. After the junction of the two forks near its northern extremity, the first important tributary on its southern course is the Stuart, draining Lakes Stuart, Fraser and Francois. One hundred miles lower down the Quesnel, draining a large lake of the same name, flows in from the east at a town also so named. Farther on the Fraser receives from the west the Chilcotin, and at Lytton, about 180 m. from the sea, the Thompson, its largest tributary, flows in from the east, draining a series of mountain lakes, and receiving at Kamloops the North Thompson, which flows through deep and impassable canyons. Below Hope the Lillooet flows in from the north. The Fraser is a typical mountain stream, rapid and impetuous through all its length, and like most of its tributaries is in many parts not navigable even by canoes. On its southern course between Lytton and Yale, while bursting its way through the Coast Range, it flows through majestic canyons, which, like those of the Thompson, were the scene of many tragedies during the days of the gold-rush to the Cariboo district. At Yale, about 80 m. from its mouth,