Kirkcudbrightshire

The Stewartry of Kirkcudbright (Siorrachd Chille Chuithbheirt in ) or Kirkcudbrightshire, was formerly a of south-western. It was also known as East Galloway, forming the larger region with.

Kirkcudbrightshire bounded on the north and north-west by, on the west and southwest by , on the south and southeast by the and the , and on the east and northeast by. It included the small islands of and. It had an area of 575,565 acres (2,323 km&sup2;). That area is now part of the of, and is additionally administratively used for.

In, a natural son of Sir  "the Good", became  and received in perpetual fee the Crown lands between the  and the. He appointed a to collect his revenues and administer justice, and there thus arose the designation of the "Stewartry of Kirkcudbright". (see below)

Its designation as 'Kirkcudbrightshire' is therefore historically incorrect. The county is still called The Stewartry by its inhabitants and forms the Stewartry area of Dumfries and Galloway Council, represented by eight Stewartry councillors. Local administration of the district today is overseen by a Stewartry Area Manager, based in the county town of Kirkcudbright.

The name Kirkcudbrightshire as alternative to Stewartry of Kirkcudbright appears to have been invented by the in the.

Geography
The north-western part of the former county is rugged, wild and desolate.

In this quarter the principal mountains are 843 m (2764 ft), the highest in the south of Scotland, and the group of the, the chief peaks of which are  814 m (2669 ft),  807 m (2650 ft),  746 m (2446 feet) and  716 m (2350 feet). Towards the south-west the chief eminences are 717 (2350 ft),  676 m (2216 ft), and the bold mass of   711 m (2331 ft). In the south-east the only imposing height is Criffel 569 m (1868 ft). In the north rises the majestic hill of of  797 m (2614 ft), and close to the Ayrshire border is the  698 m (2290 feet). The southern section of the shire is mostly level or undulating, but characterised by picturesque scenery.

The shore is generally bold and rocky, indented by numerous estuaries forming natural harbours, which however are of little use for owing to the shallowness of the sea. Large stretches of sand are exposed in the Solway at low water and the rapid flow of the tide has often occasioned loss of life.

The number of "burns" and "waters" is remarkable, but their length seldom exceeds 7 or 8 miles (13 km). Among the longer rivers are the Cree, which rises in Loch Moan and reaches the sea near Creetown after a course of about 30 miles, during which it forms the boundary, at first of and then of ; the Dee or Black Water of Dee (so named from the peat by which it is coloured), which rises in Loch Dee and after a course mainly S.E. and finally S., enters the sea at  below, its length being nearly 36 miles (58 km); the Urr, rising in Loch Urr on the  border, falls into the sea a few miles south of  27 miles (43 km) from its source; the , rising on the confines of Ayrshire, flows mainly in a southerly direction and joins the Dee at the southern end of  after a course of 24 miles (39 km) through lovely scenery; and the Deugh which, rising on the northern flank of the Windy Standard, pursues an extraordinarily winding course of 20 miles (32 km) before reaching the Ken. The, during the last few miles of its flow, forms the boundary with Dumfriesshire, to which county it almost wholly belongs.

The lochs and mountain tarns are many and well-distributed; but except for Loch Ken, which is about 6 miles (10 km) long by half a mile (1 km) wide, few of them attain noteworthy dimensions. There are several passes in the hill regions, but the only well-known glen is Glen Trool, not far from the district of in Ayrshire, the fame of which rests partly on the romantic character of its scenery, which is very wild around Loch Trool, and more especially on its associations with. It was here that when most closely beset by his enemies, who had tracked him to his fastness by sleuth hounds, Bruce with the aid of a few faithful followers won a surprise victory over the English in which proved the turning-point of his fortunes.

Geology
and rocks are the most important in this county; they are thrown into oft-repeated folds with their axes lying in a northeast-southwest direction. The Ordovician rocks are graptolitic black shales and grits of Llandeilo and Caradoc age. They occupy all the northern part of the county north-west of a line which runs some 3 m. north of New Galloway and just south of the Rinns of Kells. South-east of this line graptolitic Silurian shales of Llandovery age prevail; they are found around Dalry, Creetown, New Galloway, Castle Douglas and Kirkcudbright.

Overlying the Llandovery beds on the south coast are strips of Wenlock rocks; they extend from Bridgehouse Bay to and are well exposed in Kirkcudbright Bay, and they can be traced farther round the coast between the granite and the younger rocks. rocks appear in small faulted tracts, unconformable on the Silurian, on the shores of the Solway Firth. They are best developed about Kirkbean, where they include a basal red followed by conglomerates, grits and cement stones of Calciferous  age.

Brick-red sandstones of age just come within the county on the W. side of the Nith at Dumfries. Volcanic necks occur in the Permian and basalt dikes penetrate the Silurian at Borgue, Kirkandrews, etc.

Most of the highest ground is formed by the masses of which have been intruded into the Ordovician and Silurian rocks; the Criffel mass lies about Dalbeattie and Bengairn, another mass extends east and west between the Cairnsmore of Fleet and Loch Ken, another lies northwest and southeast between Loch Doon and Loch Dee and a small mass forms the Cairnsmore of Carsphairn.

deposits occupy much of the low ground; the ice, having travelled in a southerly or south-easterly direction, has left abundant striae on the higher ground to indicate its course. Radiation of the ice streams took place from the heights of Merrick, Kells, etc; local moraines are found near Carsphairn and in the Deagh and Minnoch valleys. Glacial s of boulder clay lie in the vales of the Dee, Cree and Urr.

Climate and Agriculture
The climate and soil suit grass and green crops rather than grain. The annual rainfall averages 45.7 inches (1.16 m). The mean temperature for the year is 9 °C (48 °F); for 4 January 4°C (39 °F); for July 15°C (59 °F). The major part of the land is either waste or poor pasture.

Population and Government
The population was 39,985 in 1891 and 39,383 in 1901, when 98 persons spoke both Gaelic and English. The use of has never been enquired of in a census. The chief towns are (population in 1901, 3018),  (3469),  (2386),  (5796) with Creetown, and  (1013). The county forms part of the sheriffdom of Dumfries and Galloway.

In 1930 Maxwelltown was transferred to Dumfriesshire, so it is debatable whether it should be regarded as part of the geographical county of Kirkcudbrightshire.

History
The country west of the Nith was originally peopled by a tribe of called Novantae, or Atecott, who long retained their independence. After 's invasion in the country nominally formed part of the  province of, but the evidence is against there ever having been a prolonged effective Roman occupation. The view that there were in Galloway in historical times is now rejected.

After the retreat of the Romans the Novantae remained for a time under their own chiefs, but in the 7th century accepted the overlordship of. The, soon engaged in struggles with the , had no leisure to look after their tributaries, and early in the 9th century the Atecotts made common cause with the Vikings. There may also have been significant immigration in Galloway around that time. Henceforward they were styled, probably in contempt, Gallgaidhel, or "stranger Gaels" (i.e. Gaels who fraternised with the foreigners), the Welsh equivalent for which, Galiwyddel, gave rise to the name of "Galloway" (of which is a variant), which was applied to their territory and still denotes the Stewartry of Kirkcudbright and the shire of.

When Scotland consolidated under (crowned at  in 844), Galloway did not form part of the kingdom; but in return for the services rendered to him at this crisis Kenneth gave his daughter in marriage to the Galloway chief,, and also conferred upon the men of Galloway the privilege of marching in the van of the Scottish armies, a right exercised and recognized for several centuries.

During the next two hundred years the country had no rest from Danish and Saxon incursions and the continual lawlessness of the Scandinavian rovers. When defeated and slew  in  he married the dead king's relative Ingibiorg, a Pictish princess, an event which marked the beginning of the decay of Norse influence. The Galloway chiefs hesitated for a time whether to throw in their lot with the Northumbrians or with Malcolm; but language, race and the situation of their country at length induced them to become lieges of the Scottish king.

By the close of the 11th century the boundary between England and Scotland was roughly delimited on what became permanent lines. The system ultimately destroyed the power of the Galloway chiefs, who resisted the innovation to the last. Several of the lords or "kings" of Galloway, a line said to have been founded by, the greatest of them all, asserted in vain their independence of the Scottish crown; and in the line became extinct in the male branch on the death of Fergus's great-grandson.

One of Alan's daughters,, had married , he and Dervorguilla being parents of King ( - ), and the people, out of affection for Alan's daughter, were lukewarm in support of. In the district was cleared of the English and brought under allegiance to the king, when the lordship of Galloway was given to. Later in the 14th century Galloway espoused the cause of Edward Baliol, who surrendered several counties, including Kirkcudbright, to.

In, a natural son of , became Lord of Galloway and received in perpetual fee the Crown lands between the Nith and the Cree. He appointed a steward to collect his revenues and administer justice, and there thus arose the designation of the "Stewartry of Kirkcudbright".

The high-handed rule of the Douglases created general discontent, and when their treason became apparent their territory was overrun by the king's men in ; Douglas was attainted, and his honours and estates were forfeited. In that year the great stronghold of the, the most important fortress in Galloway, which Archibald the Grim had built on the Dee immediately to the west of the modern town of , was reduced and converted into a royal keep. (It was dismantled in by order of the  in consequence of the hostility of its keeper, Lord Nithsdale, to the .) The famous cannon, now in , is said, apparently on limited evidence, to have been constructed in order to aid in this siege.

As the Douglases went down the Maxwells rose, and the debatable land on the south-east of Dumfriesshire was for generations the scene of strife and raid, not only between the two nations but also among the leading families, of whom the Maxwells, Johnstones and Armstrongs were always conspicuous. After the  the shires of Kirkcudbright and Dumfries fell under English rule for a short period. The treaty of  established a truce between the nations for ten years; and in, the  consenting, the debatable land ceased to be matter for debate, the parish of Canonbie being annexed to Dumfriesshire, that of Kirkandrews to.

Though at the the Stewartry became fervent in its ism, it was to Galloway, through the influence of the great landowners and the attachment of the people to them, that  owed her warmest adherents, and it was from the coast of Kirkcudbright that she made her luckless voyage to England.

Even when the crowns of Scotland and England were united in turbulence continued; for trouble arose over the attempt to establish, and nowhere were the s more cruelly persecuted than in Galloway.

After the  things mended slowly but surely, curious evidence of growing commercial prosperity being the enormous extent to which smuggling was carried on. No coast could serve the "free traders" better than the shores of Kirkcudbright, and the contraband trade flourished till the 19th century. The  of  and  elicited small sympathy from the inhabitants of the shire.

Kirkcudbrightshire became part of the Region in 1975, as the District of  (which retained a district council until ). It maintains a strong regional identity and is a.

Stewartry Parishes
The Stewartry is composed of the following 29 civil