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See also: south-eastern county of Scotland, bounded N. by the Firth of Forth, N.E. by the See also: North See also: Sea, E., S.E. and S. by See also: Berwickshire, and S.W. and W. by See also: Edinburghshire
.
It covers an See also: area of 171,o11 acres, or 267 sq. m
.
Its sea-See also: coast See also: measures 41 M
.
The See also: Bass See also: Rock and Fidra Isle belong'to the See also: shire; and there are numerous rocks and reefs off the See also: shore, especially between See also: Dunbar and Gullane See also: Bay
.
Broadly speaking, the See also: northern See also: half of the shire slopes gently to the coast, and the See also: southern half is hilly
.
Several of the peaks of the Lammermuirs exceed 1500 ft., and the more level See also: tract is broken by Traprain See also: Law (724) in the parish of Prestonkirk, North See also: Berwick Law (612), and Garleton See also: Hill (590) to the north of the county
See also: town
.
The only important See also: river is the See also: Tyne, which rises to the south-See also: east of Borthwick in See also: Mid-See also: Lothian, and, taking a generally north-easterly direction, reaches the sea just beyond the See also: park of Tynninghame See also: House, after a course of 28 m., for the first 7 M. of which it belongs to its See also: parent shire
.
It is noted for a very See also: fine variety of See also: trout, and See also: salmon are sometimes taken below the linn at East Linton
.
The Whiteadder rises in the parish of Whittingehame, but, flowing towards the south-east, leaves the shire and at last joins the See also: Tweed near Berwick
.
There are no natural lakes, but in the parish of Stenton is found Pressmennan Loch, an artificial See also: sheet of See also: water of somewhat See also: serpentine shape, about 2 M. in length, with a width of some 400 yds., which was constructed in 1819 by damming up the See also: ravine in which it lies
.
The See also: banks are wooded and picturesque, and the water abounds with trout
.
Geology.—The higher ground in the south, including the Lammermuir Hills, is formed by shales, greywackes and grits of Ordovician and See also: Silurian age; a narrow See also: belt of the former lying on the north-western See also: side of the latter, the strike being S.W. to N.E
.
The granitic mass of Priestlaw and other felsitic rocks have been intruded into these strata . TheSee also: lower Old Red See also: Sandstone has not been observed in this county, but the younger sandstones and conglomerates fill up See also: ancient depressions in the Silurian and Ordovician, such as that See also: running northward from Oldhamstocks towards Dunbar and the valley of Lauderdale
.
A faulted-in tract of the same formation, about 1 m. in breadth, runs westward from Dunbar to near See also: Gifford
.
Carboniferous rocks See also: form the See also: remainder of the county
.
The Calciferous Sandstone series, shales,'thin limestones and sandstones, is exposed on the south-eastern coast; but between Gifford and North Berwick and from Aberlady to Dunbar it is represented by a See also: great thickness of volcanic rocks consisting of tuffs and coarse breccias in the lower beds, and of porphyritic and andesitic lavas above
.
These rocks are well exposed on the coast, in the Garleton Hills and Traprain Law; the latter and North Berwick Law are volcanic
and North Berwick
.
The shire is under school-See also: board jurisdiction, and besides high See also: schools at See also: Haddington and North Berwick, some of the elementary schools See also: earn grants for higher See also: education
.
The county council spends a proportion of the " See also: residue " See also: grant in supporting
See also: short courses of instruction in technical subjects (chiefly See also: agriculture), in experiments in the feeding of cattle and the growing of crops, and in defraying the travelling expenses of technical students
.
See also: History.—Of the Celts, who were probably the earliest in-habitants, traces are found in a few place names and circular camps (in the parishes of Garvald and Whittinghame) and hill forts (in the parish of Bolton)
.
After the See also: Roman occupation, of which few traces remain, the See also: district formed See also: part of the Saxon See also: kingdom of Northumbria until ror8, when it was joined to Scotland by See also: Malcolm II
.
It was comparatively prosperous till the See also: wars of See also: Bruce and See also: Baliol, but from that See also: period down to the union of the kingdoms it suffered from its nearness to the Border and from See also: civil strife
.
The last battles fought in the county were those of Dunbar (1650) and See also: Prestonpans (1745)
.
See J . See also: Miller, History of Haddington (1844); D
.
Croal, Sketches of East Lothian (Haddington, 1873); See also: John Martine, Reminiscences of the County of Haddington (Haddington, 1890, 1894); Dr
See also: Wallace See also: James, Writs and Charters of Haddington (Haddington, 1898)
.
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