BUCKINGHAMSHIRE, EARLS OF. The first earl of Buckinghamshire (to be distinguished from the earls of Buckingham, q.v.) was John Hobart (c. 1694-1756), a descendant of Sir Henry Hobart (d. 1625), attorney-general and chief justice of the common pleas under James I., who was made a baronet in 1611, and who was the great-grandson of Sir James Hobart (d. 1507), attorney-general to Henry VII. The Hobarts had been settled in Norfolk and Suffolk for many years, when in 1728 John Hobart, who was a son of Sir Henry Hobart, the 4th baronet (d. 1698), was created Baron Hobart of Blickling. In 1740 Hobart became lord-lieutenant of Norfolk and in 1746 earl of Buckinghamshire, his sister, Henrietta Howard, countess of Suffolk, being the mistress of George II. He died on the 22nd of September 1756, and was succeeded as 2nd earl[[1]] by his eldest son John (1723-1793), who was member of parliament for Norwich and comptroller of the royal household before his accession to the title. From 1762 to 1766 he was ambassador to Russia, and from 1776 to 1780 lord-lieutenant of Ireland, but he was hardly equal to the exceptional difficulties with which he had to deal in the latter position. He died without sons at Blickling Hall, Norfolk, on the 3rd of August 1793, when his half-brother George (c. 1730-1804), became 3rd earl. Blickling Hall and his Norfolk estates, however, passed to his daughter, Henrietta (1762-1805), the wife of William Kerr, afterwards 6th marquess of Lothian.
Robert Hobart, 4th earl of Buckinghamshire (1760-1816), the eldest son of the 3rd earl, was born on the 6th of May 1760. He was a soldier, and then a member of both the English and the Irish Houses of Commons; from 1789 to 1793 he was chief secretary to the lord-lieutenant of Ireland, exerting his influence in this country to prevent any concessions to the Roman Catholics. In 1793, being known by the courtesy title of Lord Hobart, he was sent to Madras as governor, but in 1798, after serious differences between himself and the governor-general of India, Sir John Shore, afterwards Lord Teignmouth, he was recalled. Returning to British politics, Hobart was called up to the House of Lords in 1798 (succeeding to the earldom of Buckinghamshire in 1804); he favoured the union between England and Ireland; from March 1801 to May 1804 he was secretary for war and the colonies (his family name being taken for Hobart Town in Tasmania), and in 1805 he became chancellor of the duchy of Lancaster under Pitt. For a short time he was joint postmaster-general, and from 1812 until his death on the 4th of February 1816 he was president of the Board of Control, a post for which his Indian experience had fitted him.
The 4th earl left no sons, and his titles passed to his nephew, George Robert Hobart (1789-1849), a son of George Vere Hobart (1761-1802), lieutenant-governor of Grenada. In 1824 the 5th earl inherited the Buckinghamshire estates of the Hampden family and took the name of Hampden, his ancestor, Sir John Hobart, 3rd baronet, having married Mary Hampden about 1655. On his death in February 1849 his brother, Augustus Edward Hobart (1793-1884), who took the name of Hobart-Hampden in 1878, became 6th earl. His two sons, Vere Henry, Lord Hobart (1818-1875), governor of Madras from 1872, and Frederick John Hobart (1821-1875), predeceased him, and when the 6th earl died he was succeeded by his grandson, Sidney Carr Hobart-Hampden (b. 1860), who became 7th earl of Buckinghamshire, and who added to his name that of Mercer-Henderson. Another of the 6th earl's sons was Augustus Charles Hobart-Hampden, generally known as Hobart Pasha (q.v.).
See Lord Hobart's Essays and Miscellaneous Writings, edited with biography by Lady Hobart (1885).
[1] Until 1784, when George Grenville, Earl Temple, was created marquess of Buckingham, the 2nd earl of Buckinghamshire always signed himself "Buckingham"; his contemporaries knew him by this name, and hence a certain amount of confusion has arisen.
BUCKINGHAMSHIRE (abbreviated Bucks) a south midland county of England, bounded N. by Northamptonshire, E. by Bedfordshire, Hertfordshire and Middlesex, S. for a short distance by Surrey, and by Berkshire, and W. by Oxfordshire. Its area is 743.2 sq. m. The county is divided between the basins of the rivers Ouse and Thames. The first in its uppermost course forms part of the north-western boundary, passes the towns of Buckingham, Stony Stratford, Wolverton, Newport Pagnell and Olney, and before quitting the county forms a short stretch of the north-eastern boundary. The principal tributary it receives within the county is the Ouzel. The Thames forms the entire southern boundary; and of its tributaries Buckinghamshire includes the upper part of the Thames. To the north-west of Buckingham, and both east and west of the Ouzel, the land rises in gentle undulations to a height of nearly 500 ft., and north of the Thames valley a few nearly isolated hills stand boldly, such as Brill Hill and Muswell Hill, each over 600 ft., but the hilliest
part of the county is the south, which is occupied by part of the Chiltern system, the general direction of which is from south-west to north-east. The crest-line of these hills crosses the county at its narrowest point, along a line, above the towns of Prince's Risborough and Wendover, not exceeding 11 m. in length. This line divides the county into two parts of quite different physical character; for to the south almost the whole land is hilly (the longer slope of the Chiltern system lying in this direction), well wooded, and pleasantly diversified with narrow vales. The chief of these are watered by the Wye, Misbourne and Chess streams. The beech tree is predominant in the woods, in so much that William Camden, writing c. 1585, supposed the county to take name from this feature (A.S. boc, beech). In the south a remnant of ancient forest is preserved as public ground under the name of Burnham Beeches. The Chilterns reach a height of nearly 900 ft. within the county.
Geology.—The northern half of the county is occupied by Jurassic strata, in the southern half Cretaceous rocks predominate except in the south-eastern corner, where they are covered by Tertiary beds. Thus the oldest rocks are in the north, succeeded continuously by younger strata to the south; the general dip of all the rocks is south-easterly. A few patches of Upper Lias Clay appear near the northern boundary near Grafton Regis and Castle Thorpe, and again in the valley of the Ouse near Stoke Goldington and Weston Underwood. The Oolitic series is represented by the Great Oolite, with limestones in the upper part, much quarried for building stones at Westbury, Thornborough, Brock, Whittlewood Forest, &c.; the lower portions are more argillaceous. The Forest Marble is seen about Thornton as a thin bed of clay with an oyster-bearing limestone at the base. Next above is the Cornbrash, a series of rubbly and occasionally hard limestones and thin clays. The outcrop runs by Tingwick, Buckingham, Berehampton and Newport Pagnell, it is quarried at Wolverton and elsewhere for road metal. Inliers of these rocks occur at Marsh Gibbon and Stan Hill. The Oxford Clay and Kimmeridge Clay, with the Gault, lie in the vale of Aylesbury. The clay is covered by numerous outliers of Portland, Purbeck and Lower Greensand beds. The Portland beds are sandy below, calcareous above; the outcrop follows the normal direction in the county, from south-west to north-east, from Thame through Aylesbury; they are quarried at several places for building stone and fossils are abundant. The Hartwell Clay is in the Lower Portland. Freshwater Purbeck beds lie below the Portland and Lower Greensand beds; they cap the ridge between Oving and Whitchurch. Glass-making sands have been worked from the Lower Greensand at Hartwell, and phosphatic nodules from the same beds at Brickhill as well as from the Gault at Towersey. A broad band of Gault, a bluish clay, extends from Towersey across the county in a north-easterly direction. Resting upon the Gault is the Upper Greensand; at the junction of the two formations numerous springs arise, a circumstance which has no doubt determined the site of several villages. The Chalk rises abruptly from the low lying argillaceous plain to form the Chiltern Hills. The form of the whole of the hilly district round Chesham, High Wycombe and the Chalfonts is determined by the Chalk. Reading beds, mottled clays and sands, repose upon the Chalk at Woburn, Barnham, Fulmer and Denham, and these are in turn covered by the London Clay, which is exposed on the slopes about Stoke Common and Iver. Between the Tertiary-capped Chalk plateau and the Thames, a gentler slope, covered with alluvial gravel and brick earth, reaches down to the river. Thick deposits of plateau gravel cover most of the high ground in the southern corner of the county, while much of the northern part is obscured by glacial clays and gravels.
Industries.—The agricultural capacities of the soil vary greatly in different localities. On the lower lands, especially in the Vale of Aylesbury, about the headwaters of the Thame, it is extremely fertile; while on the hills it is usually poor and thin. The proportion of cultivated land is high, being about 83% of the whole. Of this a large and growing portion is in permanent pasture; cattle and sheep being reared in great numbers for the London markets, to which also are sent quantities of ducks, for which the district round Aylesbury is famous. Wheat and oats are the principal grain crops, though both decrease in importance. Turnips and swedes for the cattle are the chief green crops; and dairy-farming is largely practised. There is no general manufacturing industry, but a considerable amount of lace-making and straw-plaiting is carried on locally; and at High Wycombe and in its neighbourhood there is a thriving trade in various articles of turnery, such as chairs and bowls, from beech and other hard woods. The introduction of lace-making in this and neighbouring counties is attributed to Flemish, and later to French immigrants, but also to Catharine of Aragon during her residence (c. 1532) at Ampthill. Down to the later part of the 19th century a general holiday celebrated by lace-makers on the 25th of November was known as "Cattarn's Day."
Communications.—The main line of the London & North-Western railway crosses the north-east part of the county. Bletchley is an important junction on this system, branches diverging east to Fenny Stratford, Bedford and Cambridge, and west to Oxford and Banbury, Buckingham being served by the western branch. There is also a branch from Cheddington to Aylesbury. The Metropolitan-Great Central joint line serves Amersham, Chesham (by a branch), and Aylesbury, joining the North-Western Oxford branch at Verney Junction; this line is used by the Great Central railway, the main line of which continues north-westward from Quainton Road. A light railway connects this station with the large village of Brill to the south-west. The Great Central and the Great Western companies jointly own a line passing through Beaconsfield, High Wycombe, and Prince's Risborough, which is connected northward with the Great Central system. Before the opening of this line in 1906 the Great Western branch from Maidenhead to Oxford was the only line serving High Wycombe and Prince's Risborough, from which there are branches to Watlington and Aylesbury. The main line of this company crosses the extreme south of the county by Slough and Taplow. The Grand Junction Canal, reaching the valley of the Ouse by way of the Ouzel valley from the south, has branches to Aylesbury and to Buckingham. Except the Thames none of the rivers in the county is continuously navigable.