See also:ELGINSHIRE, or See also:MORAY (Gaelic " among the See also:sea-See also:board men ")
, a See also:northern See also:county of See also:Scotland, bounded N. by the See also:Moray See also:Firth, E. and S.E. by See also:Banffshire, S. and S.W. by See also:Inverness and W. by See also:Nairnshire
.
It comprises only the eastern portion of the See also:ancient See also:province of Moray, which extended from the See also:Spey to the See also:Beauly and from the See also:Grampians to the See also:sea, embracing an See also:area of about 3900 sq. m
.
The area of the county is 305,119 acres, or 477 sq. m
.
See also:Elginshire is naturally divided into two sections, the level and fertile See also:coast and its See also:hinterland—" the Laigh o' Moray," a See also:tract 30 M. See also:long by from 5 to 12 M. broad—and the hilly See also:country in the See also:south
.
There are, however, no high mountains
.
Carn Ruigh (1784 ft.), Larig See also:- HILL
- HILL (0. Eng. hyll; cf. Low Ger. hull, Mid. Dutch hul, allied to Lat. celsus, high, collis, hill, &c.)
- HILL, A
- HILL, AARON (1685-175o)
- HILL, AMBROSE POWELL
- HILL, DANIEL HARVEY (1821-1889)
- HILL, DAVID BENNETT (1843–1910)
- HILL, GEORGE BIRKBECK NORMAN (1835-1903)
- HILL, JAMES J
- HILL, JOHN (c. 1716-1775)
- HILL, MATTHEW DAVENPORT (1792-1872)
- HILL, OCTAVIA (1838– )
- HILL, ROWLAND (1744–1833)
- HILL, SIR ROWLAND (1795-1879)
Hill (1783) and Carn Kitty (1711) are the See also:chief eminences in the south-central See also:district until the See also:ridge of the Cromdale Hills is reached on the Banffshire border, where the highest point is 2329 ft. above the sea
.
The two most important See also:rivers, the Spey (q.v.) and the Findhorn, both have their See also:sources in Inverness-See also:shire
.
About 5o m. of the course of the Spey are in Elginshire, to which it may be roughly said to serve as the boundary See also:line on the south-See also:east and east
.
The Findhorn rises in the Monadliadh Mountains which See also:form the See also:watershed for several See also:miles between it and the Spey
.
Of its See also:total course of nearly 70 M. only the last 12 are in the county, where it separates the See also:woods of Altyre from the See also:Forest of Darnaway, before entering the Moray Firth in a See also:bay on the See also:north-eastern See also:shore to which it has given its name
.
During the first 7 M. of its flow in Elginshire the stream passes through some of the finest scenery in Scotland
.
It is liable to sudden risings, and in the memorable Moray floods of See also:August 1829 wrought the greatest havoc
.
Of other rivers the Lossie rises in the small lakes on the flanks of Carn Kitty and pursues a very winding course of 34 M. till it reaches the Moray Firth; Ballintomb See also:Burn, See also:Rothes Burn and Tulchan Burn are See also:left-See also:hand affluents of the Spey; the Dorbock and Divie, uniting their forces near Dunphail See also:House, join the Find-See also:horn at Relugas; and Muckle See also:Water, a left-hand tributary of the Findhorn, comes from Nairnshire
.
The Spey and Findhorn are famous for See also:salmon, but some of the smaller streams, too, afford See also:good See also:sport
.
The lochs are few and unimportant, among them being See also:Loch Spynie, 22 M
.
N., and Loch-na-Bo, 4 M
.
S.E. of See also:Elgin; Loch of Blairs, 22 m
.
S. of See also:Forres; Loch Romach, 3 M
.
S. of Rafford; Loch See also:Dallas, about 4 m
.
S.W. of Dallas, and Lochindorb in the S.W., 6 m
.
N.N.W. of See also:Grantown
.
Loch Spynie was once a See also:lake extending from the Firth to within 22 M. of Elgin and covering an area of over 2000 acres
.
Its shores were the haunt of a See also:great variety of birds, and its See also:waters were full of salmon, sea-See also:trout and See also:pike
.
But See also:early in the 19th See also:century it was resolved to reclaim the See also:land, and the drainage See also:works then undertaken reduced the beautiful loch to a swamp of some 120 acres
.
Lochindorb is now the largest lake, being 2 M. in length and fully a m. wide
.
In the upper end, on an See also:island believed to be artificial, stand the ruins of Lochindorb See also:Castle, in the 14th century the stronghold of the See also:Wolf of See also:Badenoch, and afterwards successively the See also:property of the See also:earl of Moray, the Campbells of See also:Cawdor and the earl of See also:Seafield
.
See also:Sir Thcmas See also:Dick See also:Lauder saw at Cawdor Castle a massive See also:iron See also:gate which, according to tradition, Sir Donald See also:- CAMPBELL, ALEXANDER (1788–1866)
- CAMPBELL, BEATRICE STELLA (Mrs PATRICK CAMPBELL) (1865– )
- CAMPBELL, GEORGE (1719–1796)
- CAMPBELL, JOHN
- CAMPBELL, JOHN (1708-1775)
- CAMPBELL, JOHN CAMPBELL, BARON (1779-1861)
- CAMPBELL, JOHN FRANCIS
- CAMPBELL, LEWIS (1830-1908)
- CAMPBELL, REGINALD JOHN (1867— )
- CAMPBELL, THOMAS (1777—1844)
Campbell of Cawdor carried on his back from Lochindorb to Cawdor, a distance of 13 M
.
In the See also:southern See also:half of the county, amongst the hills, are several glens, among them the Glen of Rothes, Glen Lossie, Glen Gheallaidh, Glen Tulchan and Glen Beag
.
Strathspey, though more of a valley than a glen, is remarkable for its extent and beauty
.
See also:Geology.—This county may be divided geologically into two areas, the hilly region to the south being composed of the crystalline See also:schists of the Central See also:Highlands and the fertile See also:plain of Moray being made up of Old Red See also:Sandstone and Triassic strata
.
In the Cromdale Hills in the south-east of the county the metamorphic See also:series comprises schistose See also:quartzite, See also:quartz-schists, micaceous flagstones and See also:mica-schists, which are granulitic and holocrystalline, the dark laminae in some cases containing heavy residues such as See also:ilmenite and See also:zircon
.
The greater portion of the metamorphic area See also:west of the Spey consists of granulitic quartz-See also:biotite-granulites and bands of See also:muscovite-biotite-schist belonging to the Moine series of the See also:Geological Survey (see SCOTLAND: Geology)
.
In certain areas theseare permeated by granitic material in the form of thin strings, knots and See also:veins
.
Excellent sections of these rocks are exposed in the Findhorn, the Divie and the tributaries of the Spey
.
Near Gran-See also:town there is a See also:group locally See also:developed, comprising crystalline See also:limestone with See also:tremolite, kyanite See also:gneiss, muscovite-hiotite-schist and quartzite, the See also:age and relations of which are still uncertain
.
The See also:general strike of the crystalline schists, See also:save where there are See also:local deflections, is north-east and south-west, and the general See also:dip is to the south-east
.
Between Lochindorb and Grantown there is a See also:mass of See also:granite belonging to the later intrusions of the Highlands represented by the See also:Cairngorm granite
.
Within the county there are representatives of the See also:middle and upper divisions of the Old Red Sandstone resting unconformably on the crystalline schists
.
The strata of the middle or Orcadian series consist of conglomerates, sandstones, shales and See also:clays, with limestone nodules containing See also:fish remains
.
This sequence is well displayed in the See also:banks of the Spey north of See also:Boat of See also:Bridge and in the Tynet Burn east of See also:Fochabers, the latter being one of the well-known localities for ichthyolites in the middle or Orcadian See also:division
.
In the Tynet and Gollachie Burn sections, the fish See also:bed is overlaid by conglomerates and red pebbly sandstones, passing upwards into a thin See also:zone of See also:andesite lavas, indicating contemporaneous volcanic See also:action
.
West of the Tynet Burn and Spey sections there is no trace of the members of the Orcadian division till we reach the Muckle Burn and Lethen See also:Bar in Nairnshire, save the coarse See also:conglomerate filling the ancient hollow of the valley of Rothes which may belong to the middle series
.
In that direction they are overlapped by the Upper Old Red Sandstone, which in the See also:river Lossie, in the Lochty Burn and the Findhorn See also:rest directly on the metamorphic rocks
.
Even to the south of the See also:main boundary of the upper division there are small outliers of that series resting on the crystalline schists
.
Hence there must be a discordance between the Middle and Upper Old Red Sandstone in this county
.
The strata of the upper division consist of red, See also:grey and yellow false-bedded sandstones with conglomeratic bands, which are well seen in the Findhorn between Sluie and Cothall, where they are associated with a bed of cornstone, all dipping to the N.N.W. at See also:gentle angles
.
South of Elgin they are exposed in the Lossie and at Scaat See also:Craig, while to the north of that town they extend along the ridge from Bishopmill to Alves
.
By means of the fish remains, which occur at Scaat Craig, in the Bishopmill quarries, at Alves, in the Findhorn cliffs and in the Whitemyre See also:quarry on the Muckle Burn, the Upper Old Red Sandstone in this county is arranged in two See also:groups, the Alves and Rosebrae
.
In the area lying to the north of the Upper Old Red Sandstone ridge at Bishopmill and Quarry-See also:wood, the strata of Triassic age occur, where they consist of See also:pale grey and yellow sandstones and a See also:peculiar cherty and calcareous See also:band, known as the cherty See also:rock of Stotfield
.
The,sandstones are visible in quarries on the north slope of Quarry Wood, at Findrassie, at Spynie and along the ridge and sea-shore between Burghead and See also:Lossiemouth
.
They are invested with See also:special See also:interest on See also:account of the remarkabfe series of reptilian remains obtained from them, 'comprising Stagonolepis, a See also:crocodile allied to the See also:modern caiman in form; Telerpeton and Hyperedapedon, See also:species of lizards; Dicynodonts (Gordonia and Geikia) and a horned reptile, Elginia mirabilis (see SCOTLAND: Geology)
.
The palaeontological See also:evidence points to the conclusion that these reptiliferous sandstones must belong in See also:part to the Trias, indeed it is possible that the See also:lower portion may be of See also:Permian age
.
In the Cutties Hillock quarry west of Elgin these reptiliferous beds rest directly on the sandstones containing Holoptychius of Upper Old Red Sandstone age, so that the apparent conformability must be entirely deceptive
.
Within the area occupied by the Trias west of Stotfield, flagstones appear, charged with fish scales of Upper Old Red age, where they form a See also:low ridge protruding through the younger strata
.
Both the Upper Old Red and Triassic sandstones have been largely quarried for See also:building purposes
.
On the shore at Lossiemouth there is a patch of greenish See also:- WHITE
- WHITE, ANDREW DICKSON (1832– )
- WHITE, GILBERT (1720–1793)
- WHITE, HENRY KIRKE (1785-1806)
- WHITE, HUGH LAWSON (1773-1840)
- WHITE, JOSEPH BLANCO (1775-1841)
- WHITE, RICHARD GRANT (1822-1885)
- WHITE, ROBERT (1645-1704)
- WHITE, SIR GEORGE STUART (1835– )
- WHITE, SIR THOMAS (1492-1567)
- WHITE, SIR WILLIAM ARTHUR (1824--1891)
- WHITE, SIR WILLIAM HENRY (1845– )
- WHITE, THOMAS (1628-1698)
- WHITE, THOMAS (c. 1550-1624)
white sandstones yielding fossils characteristic of the Lower Oolite
.
The glacial deposits distributed over the fertile plain of Moray and in the upland valleys are of interest
.
The low grounds were crossed by the See also:ice descending the Moray Firth in an easterly and south-easterly direction, which carried boulders of granite from Strath See also:Nairn and augen gneiss from See also:Easter See also:Ross
.
In the Elgin district, boulders belonging to the horizons of the Lower and Middle See also:Lias, the See also:- OXFORD
- OXFORD, EARLS OF
- OXFORD, EDWARD DE VERE, 17TH EARL
- OXFORD, JOHN DE VERE, 13TH EARL OF (1443-1513)
- OXFORD, PROVISIONS OF
- OXFORD, ROBERT DE VERE, 9TH EARL OF (1362-1392)
- OXFORD, ROBERT HARLEY, 1ST
Oxford See also:Clay and the Upper See also:Chalk are found both in the glacial deposits and on the See also:surface of the ground
.
The largest trans-ported mass occurs at Linksfield, where a See also:succession of limestones and shales rests on See also:boulder clay and is covered by it, which from the fossils may be of See also:Rhaetic or Lower Lias age
.
See also:Climate and See also:Agriculture.—The climate of the coast is equable and mild, even See also:exotic fruits ripening readily in the open
.
The uplands are colder and See also:damp: The See also:average temperature in See also:January is 38° F. and in See also:July 58.5°, while for the See also:year the mean is 47° F
.
The rainfall for the year averages 26 in
.
Considering its See also:latitude and the extent of its arable land the See also:standard of farming in Elginshire is high
.
The See also:rich See also:soil of the lowlands is well adapted for See also:wheat, See also:barley and oats The acreage confined
to the glens and straths under barley approximates that under oats
.
In the uplands, oats is the See also:principal cereal
.
The breeding of live-stock is profitable, and some of the finest specimens of shorthorned and polled See also:cattle and of crosses between the two are bred
.
On the larger farms in the Laigh See also:Leicester See also:sheep are kept all the year See also:round, but in the uplands the Blackfaced take their See also:place
.
Large See also:numbers of horses and pigs are also raised
.
Other See also:Industries.—See also:Whisky is the chief product, and the numerous distilleries are usually busy
.
There are woollen See also:mills at Elgin and elsewhere and chemical works at Forres and See also:Burg-See also:head
.
Owing to the See also:absence of See also:coal what little See also:mineral See also:wealth there is (iron and See also:lead) cannot be remuneratively worked
.
The sandstone quarries, yielding a building-See also:- STONE
- STONE (0. Eng. shin; the word is common to Teutonic languages, cf. Ger. Stein, Du. steen, Dan. and Swed. sten; the root is also seen in Gr. aria, pebble)
- STONE, CHARLES POMEROY (1824-1887)
- STONE, EDWARD JAMES (1831-1897)
- STONE, FRANK (1800-1859)
- STONE, GEORGE (1708—1764)
- STONE, LUCY [BLACKWELL] (1818-1893)
- STONE, MARCUS (184o— )
- STONE, NICHOLAS (1586-1647)
stone of See also:superior quality, are practically inexhaustible
.
The plantations mainly consist of See also:larch and See also:fir and, to a smaller extent, of See also:oak
.
Much See also:timber was once floated down the Spey and other rivers, but, since the increased facilities of See also:carriage afforded by the See also:railways, trees have been felled on a wider See also:scale
.
Boat-building is carried on at Burghead, Lossiemouth and See also:Kingston—so-called from the fact that a See also:firm from Kingston-on-See also:Hull laid down a yard there in 1784—while at Garmouth the fishing See also:fleet lies up during the See also:winter and is also repaired there
.
The Firth See also:fisheries are of considerable value
.
The boats go out from Findhorn, Burghead, Hopeman and Lossiemouth, which are all furnished with safe harbours
.
Findhorn has been twice vsited by calamities
.
The first See also:village was overwhelmed by the drifting sands of Culbin, and the second was buried beneath the waves in 1701
.
Kingston See also:harbour is tidal, exposed, and liable to interruption from a shifting bar
.
The deep sea fisheries comprise See also:haddock, See also:cod, See also:ling and See also:herring, and the Spey, Findhorn and Lossie yield large quantities of salmon
.
The Great North of Scotland railway enters the shire in the S.E. from Craigellachie, whence a See also:branch runs up the Spey to Boat of Garten in Inverness-shire, and in the N.E. from See also:Port See also:Gordon, See also:running in both cases to Elgin, from which a branch line extends to Lossiemouth
.
The Highland railway traverses the western limits of the shire running almost due north to Forres, whence it turns westward to Nairn and eastward to Elgin
.
From the county town it runs to See also:Aberdeen via Orbliston and See also:Keith, with a branch to Fochabers from Orbliston
.
See also:Population and See also:Government.—The population was 43,471 in 1891 and 44,800 in 1901, when 1865 persons spoke both Gaelic and See also:English, and 2 spoke Gaelic only
.
The chief towns are Elgin (pop. in 19oi, 8460), Forres (4313) and Lossiemouth (3904), to which may be added Rothes (1621), Grantown (1568) and Burghead (1531)
.
In See also:conjunction with Nairnshire the county returns one member to See also:parliament
.
Elgin and Forres are royal burghs; the municipal and See also:police burghs include Burghead, Elgin, Forres, Grantown, Lossiemouth, and Rothes
.
Elginshire is included in one sheriffdom with Inverness and Nairn, and there is a See also:resident See also:sheriff-substitute at Elgin
.
The county is under school-See also:board See also:jurisdiction, several of the See also:schools earning grants for higher See also:education
.
There are See also:academies at Elgin and Fochabers and See also:science and See also:art and technical schools at Elgin and Grantown
.
The bulk of the " See also:residue " See also:- GRANT (from A.-Fr. graunter, O. Fr. greanter for creanter, popular Lat. creantare, for credentare, to entrust, Lat. credere, to believe, trust)
- GRANT, ANNE (1755-1838)
- GRANT, CHARLES (1746-1823)
- GRANT, GEORGE MONRO (1835–1902)
- GRANT, JAMES (1822–1887)
- GRANT, JAMES AUGUSTUS (1827–1892)
- GRANT, ROBERT (1814-1892)
- GRANT, SIR ALEXANDER
- GRANT, SIR FRANCIS (1803-1878)
- GRANT, SIR JAMES HOPE (1808–1895)
- GRANT, SIR PATRICK (1804-1895)
- GRANT, U
- GRANT, ULYSSES SIMPSON (1822-1885)
grant is spent in subsidizing the agricultural See also:department of Aberdeen University and the science schools and art and technical classes in the county
.
See also:History.—Moray, in the wider sense, was first peopled by Picts of the Gaelic branch of Celts, of whom See also:relics are found in the stone circle at Viewfield and at many places in Nairnshire
.
See also:Christianity, introduced under the auspices of See also:Columba (from whose See also:- TIME (0. Eng. Lima, cf. Icel. timi, Swed. timme, hour, Dan. time; from the root also seen in " tide," properly the time of between the flow and ebb of the sea, cf. O. Eng. getidan, to happen, " even-tide," &c.; it is not directly related to Lat. tempus)
- TIME, MEASUREMENT OF
- TIME, STANDARD
time the site of Burghead See also:- CHURCH
- CHURCH (according to most authorities derived from the Gr. Kvpcaxov [&wµa], " the Lord's [house]," and common to many Teutonic, Slavonic and other languages under various forms—Scottish kirk, Ger. Kirche, Swed. kirka, Dan. kirke, Russ. tserkov, Buig. cerk
- CHURCH, FREDERICK EDWIN (1826-1900)
- CHURCH, GEORGE EARL (1835–1910)
- CHURCH, RICHARD WILLIAM (1815–189o)
- CHURCH, SIR RICHARD (1784–1873)
church has probably been so occupied), flourished for a See also:period until the See also:Columban church was expelled in 717 by See also:- KING
- KING (O. Eng. cyning, abbreviated into cyng, cing; cf. O. H. G. chun- kuning, chun- kunig, M.H.G. kiinic, kiinec, kiinc, Mod. Ger. Konig, O. Norse konungr, kongr, Swed. konung, kung)
- KING [OF OCKHAM], PETER KING, 1ST BARON (1669-1734)
- KING, CHARLES WILLIAM (1818-1888)
- KING, CLARENCE (1842–1901)
- KING, EDWARD (1612–1637)
- KING, EDWARD (1829–1910)
- KING, HENRY (1591-1669)
- KING, RUFUS (1755–1827)
- KING, THOMAS (1730–1805)
- KING, WILLIAM (1650-1729)
- KING, WILLIAM (1663–1712)
King Nectan
.
Thereafter the district was given over to internecine strife between the northern and southern Picts, which was ended by the crushing victory of See also:Kenneth See also:MacAlpine in 831, as one result of which the See also:kingdom of Pictavia was superseded by the principality of See also:Moravia
.
Still, settled See also:- ORDER
- ORDER (through Fr. ordre, for earlier ordene, from Lat. ordo, ordinis, rank, service, arrangement; the ultimate source is generally taken to be the root seen in Lat. oriri, rise, arise, begin; cf. " origin ")
- ORDER, HOLY
order had not yet been secured, for the Norsemen raided the country first under Thorstein and then under two Sigurds
.
It was in the time of the second See also:Sigurd that the Firthwas fixed as the northern boundary of Moray
.
In spite of such interruptions as the See also:battle of Torfness (Burghead) on the 14th of August 1040, in which Thorfinn, earl of See also:Orkney and See also:Shetland, overthrew a strong force of Scots under King See also:Duncan, the consolidation of the kingdom was being gradually accomplished
.
After See also:Macbeth ascended the See also:throne the Scandinavians held their hands
.
Though Macbeth and his faineant successor, " daft " Lulach, were the only See also:kings whom Moray gave to See also:Scot-land, the province never lacked for able, if headstrong, men, and it continued to enjoy See also:home See also:rule under its own marmaer, or great steward (the See also:equivalent of earl, the See also:title that replaced it), until the See also:dawn of the 12th century, when as an entity it ceased to exist
.
With a view to breaking up the See also:power of the marmaers See also:David I. and his successors colonized the seaboard with settlers from other parts of the kingdom
.
Nevertheless, from time to time the clansmen and their chiefs descended from their fastnesses and plundered the Laigh, keeping the See also:people for generations in a See also:state of panic
.
Meanwhile, the Church had become a civilizing force
.
In 1107 See also:Alexander had founded the see of Moray and the churches of Birnie, Kinneddar and Spynie were in turn the See also:cathedral of the early bishops, until in 1224 under the episcopate of See also:Andrew of Moray (de Moravia), the church of the See also:Holy Trinity in Elgin was chosen for the cathedral
.
Another See also:factor that See also:drew men together was the struggle for See also:independence
.
In his effort to See also:stamp out Scottish See also:nationality See also:Edward I. came as far north as Elgin, where he stayed for four days in July 1296, and whence he issued his See also:writ for the parliament at See also:Berwick
.
See also:Wallace, however, had no doughtier supporter than Sir Andrew Moray of See also:Bothwell, and See also:Bruce recognized the assistance he had received from the men of the north by erecting Moray into an earldom on the morrow of See also:Bannockburn and bestowing it upon See also:- THOMAS
- THOMAS (c. 1654-1720)
- THOMAS (d. 110o)
- THOMAS, ARTHUR GORING (1850-1892)
- THOMAS, CHARLES LOUIS AMBROISE (1811-1896)
- THOMAS, GEORGE (c. 1756-1802)
- THOMAS, GEORGE HENRY (1816-187o)
- THOMAS, ISAIAH (1749-1831)
- THOMAS, PIERRE (1634-1698)
- THOMAS, SIDNEY GILCHRIST (1850-1885)
- THOMAS, ST
- THOMAS, THEODORE (1835-1905)
- THOMAS, WILLIAM (d. 1554)
Thomas See also:Randolph (see MORAY, THOMAS RANDOLPH, EARL OF)
.
Henceforward the history of the county resolved itself in the main into matters affecting the power -of the Church and the ambit ions of theMoray dynasties
.
The Church accepted the See also:Reformation peacefully if not with gratitude
.
But there was strife between See also:Covenanters and the adherents of See also:Episcopacy until, prelacy itself being abolished in 1689, the bishopric of Moray came to an end after an existence of 581 years
.
(For the subsequent history of the earldom, which was successively held by the Randolphs, the Dunbars, the Douglases, the royal Stewarts and an illegitimate branch of the Stewarts, see See also:- MURRAY
- MURRAY (or MORAY), EARLS OF
- MURRAY (or MORAY), JAMES STUART, EARL OF (c. 1531-1570)
- MURRAY (or MORAY), SIR ROBERT (c. 1600-1673)
- MURRAY, ALEXANDER STUART (1841-1904)
- MURRAY, DAVID (1849– )
- MURRAY, EUSTACE CLARE GRENVILLE (1824–1881)
- MURRAY, JAMES (c. 1719-1794)
- MURRAY, JOHN
- MURRAY, JOHN (1778–1820)
- MURRAY, LINDLEY (1745–1826)
- MURRAY, LORD GEORGE (1694–1760)
- MURRAY, SIR JAMES AUGUSTUS HENRY (1837– )
- MURRAY, SIR JOHN (1841– )
MURRAY or MORAY, EARLS or.) Other celebrated Moray families who played a more or less. strenuous part in local politics were the Gordons, the Grants and the Duffs
.
Still, See also:national affairs occasionally evoked interest in Moray
.
In the See also:civil See also:war See also:Montrose ravaged the villages which stood for the Covenanters, but most of the great lairds shifted in their See also:allegiance, and the mass of the people were quite indifferent to the declining fortunes of the Stewarts
.
See also:Charles II. landed at Garmouth on the 3rd of July 165o on his return from his first See also:- EXILE (Lat. exsilium or exilium, from exsul or exul, which is derived from ex, out of, and the root sal, to go, seen in salire, to leap, consul, &c.; the connexion with solum, soil, country is now generally considered wrong)
exile in See also:- HOLLAND
- HOLLAND, CHARLES (1733–1769)
- HOLLAND, COUNTY AND PROVINCE OF
- HOLLAND, HENRY FOX, 1ST BARON (1705–1774)
- HOLLAND, HENRY RICH, 1ST EARL OF (1S9o-,649)
- HOLLAND, HENRY RICHARD VASSALL FOX, 3RD
- HOLLAND, JOSIAH GILBERT (1819-1881)
- HOLLAND, PHILEMON (1552-1637)
- HOLLAND, RICHARD, or RICHARD DE HOLANDE (fl. 1450)
- HOLLAND, SIR HENRY, BART
Holland, but hurried southwards to try the yoke of See also:Presbytery
.
The fight at Cromdale (May See also:day, 1690) shattered the Jacobite cause, for the efforts in 1715 and 1745 were too spasmodic and half-hearted to affect the See also:loyalty of the district to Hanoverian rule
.
A few See also:weeks before See also:Culloden See also:Prince Charles Edward