scholarly journals XXXIX.—On the Great Drift Beds with Shells in the South of Arran

1864 ◽  
Vol 23 (3) ◽  
pp. 523-546 ◽  
Author(s):  
Robert Boog Watson
Keyword(s):  
The South ◽  
The North ◽  
Stratified Rock ◽  
The Hill ◽  
Tilled Land ◽  
As If

The whole southern part of Arran forms a field by itself, and whatever may be the deeper connections of the agencies that have fashioned the north and the south of the island, the result is a trappean area to the south, as distinct as if it lay in another hemisphere from the north, with its granitic nucleus, and encompassing rings of stratified rock.This district is little visited, and is almost, if not quite, undescribed; it presents, however, much beautiful scenery, and for the geologist, problems of extreme difficulty and interest, which deserve more attention than they have got.It may be divided into two belts of tilled land and moorland, above which are the hill tops. This division corresponds roughly to three regions, the lowest chiefly of sandstone, the middle where felstone prevails over the sandstone, and the highest of greenstone.

Art. VII.—Notes on Persian Belúchistán. From the Persian of Mirza Mehdy Khán. Published Teheran, July, 1875

1876 ◽  
Vol 9 (1) ◽  
pp. 147-154
Author(s):  
A. H. Schindler
Keyword(s):  
Indian Ocean ◽  
Temperate Climate ◽  
The South ◽  
The West ◽  
The North ◽  
The People ◽  
The Indian Ocean ◽  
The Hill ◽  
Cool Climate

The part of Belúchistán now under Persian rule is bounded upon the north by Seistán, upon the east by Panjgúr and Kej, upon the south by the Indian Ocean, and upon the west by Núrámshír, Rúdbár, and the Báshákerd mountains.This country enjoys a variety of climates; almost unbearable heat exists on the Mekrán coast, we find a temperate climate on the hill slopes and on the slightly raised plains as at Duzek and Bampúr, and a cool climate in the mountainous districts Serhad and Bazmán. The heat at Jálq is said to be so intense in summer that the gazelles lie down exhausted in the plains, and let themselves be taken by the people without any trouble.

scholarly journals II.—Topography: Bardoúnia and North-Eastern Maina

1910 ◽  
Vol 16 ◽  
pp. 62-71
Author(s):  
H. A. O.
Keyword(s):  
The South ◽  
Hill Country ◽  
The Road ◽  
Eastern Side ◽  
The North ◽  
North Eastern ◽  
The Hill

The following paper, which completes the series of papers on the classical topography of Laconia, is an account of the hill-country on the eastern side of Taÿgetos, bounded on the north by the road from Sparta to Anavryté, on the south by Gytheion and Pánitsa. (Fig.1.)

An Iron Age Hill-Fort at Grimthorpe, Yorkshire, England

1969 ◽  
Vol 34 ◽  
pp. 148-190 ◽  
Author(s):  
I. M. Stead ◽  
M. Jarman ◽  
Angela Fagg ◽  
E. S. Higgs ◽  
C. B. Denston
Keyword(s):  
Iron Age ◽  
The South ◽  
The West ◽  
Circular Area ◽  
North West ◽  
The North ◽  
South West ◽  
White Horse ◽  
The Hill ◽  
Grave Goods

The Iron Age hill-fort at Grimthorpe (Grid reference SE.816535) in the parish of Millington, East Riding of Yorkshire, is on the western edge of the Yorkshire Wolds, with a commanding position over the Vale of York. There is an uninterrupted view to the White Horse on the Hambleton Hills, 25 miles to the north-west; beyond York, 13 miles to the west, to the Pennines; and to the south 25 miles to the chimneys of Keadby and Scunthorpe. To the west and south the land slopes away to the Vale of York, and to the north and east there is a sharper fall to Given Dale and Whitekeld Dale. The hill-fort defences follow the 520 feet contour, and enclose an approximately circular area of eight acres (fig. 1).A traditional reference may be preserved in the field-name—Bruffs—perhaps a variation of ‘Brough’, which ‘refers in all cases to ancient camps, usually Roman ones’. But all surface indications have now been obliterated by ploughing, and even a century ago there was little more to be seen. John Phillips in 1853 noticed ‘unmistakable traces of ancient but unascertainable occupation’, and in 1871 an excavation by J. R. Mortimer located ‘the filled up inner ditch of a supposed camp’. But Mortimer was not concerned with the settlement; his interest had been aroused by the discovery, in 1868, of a burial with rich grave-goods, including metalwork with La Tène ornament, in a chalk-pit within the south-west sector of the hill-fort.

X.—Geology of the Outer Hebrides. Part III.—North Uist and Benbecula

1926 ◽  
Vol 54 (2) ◽  
pp. 467-489 ◽  
Author(s):  
T.J. Jehu ◽  
R.M. Craig
Keyword(s):  
Narrow Channel ◽  
Central Position ◽  
The South ◽  
North West ◽  
North East ◽  
The North ◽  
Outer Hebrides ◽  
The Hill ◽  
North And South ◽  
Southern Extremity

Benbecula signifies “the hill of the fords,” and the island was so designated owing to the fact that there is on it only one hill of any prominence, and that it is connected with the larger islands to the north and south by fords passable only at low water. The origin of the name “Uist” is referred to in a previous communication.These islands occupy a central position in the Outer Hebrides, lying between South Uist and Harris. They are bounded on the west and north-west by the Atlantic Ocean; on the north-east by the Sound of Harris; on the east by the Little Minch, which at its narrowest part is about 16 miles broad; and on the south by a narrow channel separating Benbecula from South Uist. The area embraced in this communication extends from the Isle of Shillay in the north to the Isle of Wiay at the south-east corner of Benbecula, and includes not only the main islands of North Uist and Benbecula but also a number of smaller isles adjoining the main ones. Including the intervening channels, the total length from Shillay in the north to the southern extremity of Benbecula is about 28 miles.

Excavations at Castlelaw, Midlothian, and the Small Forts of North Britain

1933 ◽  
Vol 13 (1) ◽  
pp. 1-12 ◽  
Author(s):  
V. Gordon Childe
Keyword(s):  
Sea Level ◽  
The South ◽  
Detailed Report ◽  
Main Mass ◽  
South Eastern ◽  
The North ◽  
Outer Bank ◽  
The Hill

The fort at Castlelaw is one of a group of four, strung out along a front of five miles on the south-eastern slopes of the Pentlands. Like the rest, it does not occupy the summit of the hill (which is just under 1,600 ft. in height) but is built some 990 ft. above sea-level on an elevated spur projecting from the main mass which rises steeply above the fort, just out of bowshot. The spur ends in a slight knoll the oval summit of which is 93 yds. long by 40 yds. wide. This area is enclosed within a very low Inner Bank, while a more conspicuous rampart, Middle Bank, supplemented on the north only by an Outer Bank, impeded progress up the slope. Two rock-cut fosses, superficially invisible, were revealed between the ramparts by excavations carried out during 1931 and 1932. A detailed report of these operations will be published elsewhere, but the results which concern Britain on both sides of the Border may be summarized here.

scholarly journals I. A Letter from John Gage, Esq. F.R.S., Director, to Hudson Gurney, Esq. F.R.S. V.P. &c. containing an account of further discoveries of Roman sepulchral relics at the Bartlow Hills

Archaeologia ◽  
1839 ◽  
Vol 28 (1) ◽  
pp. 1-6 ◽  
Author(s):  
John Gage
Keyword(s):  
The Other ◽  
The South ◽  
The North ◽  
North Side ◽  
The Hill

Lord Maynard having directed a further excavation to be made at the Bartlow hills, a gallery was commenced early in April last on the north side of the south barrow. This hill, according to the plan, is about thirty-five feet high, the diameter having been computed at ninety feet, but it exceeds a hundred. The gallery was constructed in the same manner as that opened in 1835 in the largest barrow, and had reached the centre of the hill on the 16th April, upon which day I inspected it in company with Lord Braybrooke and the Honourable Captain Percy. It extended fifty-two feet, and we observed that the tumulus was formed, like the largest barrow, of earth and chalk, in horizontal strata. Our arrival took place shortly after the workmen had broken in upon a hollow, where we gladly anticipated the finding a sepulchral deposit, appearances heing much the same as those observed on first opening the cavity in the centre of the other barrow.

Excavations at Rams Hill, Uffington, Berks.

1940 ◽  
Vol 20 (4) ◽  
pp. 465-480 ◽  
Author(s):  
Stuart Piggott ◽  
C. M. Piggott
Keyword(s):  
The South ◽  
The West ◽  
The North ◽  
White Horse ◽  
North Edge ◽  
The Hill

Rams Hill is an inconspicuous knoll of the Berkshire Downs (Berks. O.S. 6 in. XIX, NW. and NE.) on the ridge overlooking the Vale of the White Horse. It lies within the 700-ft. contour, with the ground sloping gently to the south and falling steeply to 400 ft. on the northern escarpment. To the west, a mile away, the land rises to White Horse Hill, a bluff over 800 ft. high, crowned by the hill-fort of Uffington Castle and with the eponymous turf-cut Horse on the westward slope slightly below.The Ridgeway runs along the crest of the downs, south of Uffington Castle but on the north edge of Rams Hill, while along the bottom of the escarpment the Ickneild Way winds in and out of the coombes between the 400- and 500-ft. contours.

Scale Differences: Akragas and Morgantina

1993 ◽  
Author(s):  
Dora P. Crouch
Keyword(s):  
Sea Level ◽  
Water System ◽  
South Coast ◽  
The South ◽  
The North ◽  
Geological Situation ◽  
The Hill ◽  
The Impact ◽  
The City ◽  
North And South

Can we discern differences in the way water was managed at larger and smaller Greek cities? Let us take two Greek cities in Sicily as case studies, examining them in some detail as to area, population, date, geological situation, and the water system elements known at each. The aim of this exercise is to begin to understand the impact of scale differences on the clusters of water system elements in ancient cities. Useful examples are Akragas—modern Agrigento—and Morgantina (Figs. 15.1, 15.2). Akragas is located on the south coast of Sicily, approximately in the center, and occupies a dramatic site on a hill between two rivers. The earliest settlement—and later the medieval town—were located on the highest peak of the 280-meter hill (Storia della Sicilia, 1979, map 1), but during classical and Hellenistic times the city spread down the hill to the wide and gentle valley to the south, which then rises again to form a ridge that separates that valley from the plain leading to the sea. In the sixth and fifth centuries B.C. a line of temples was built along the lower ridge, forming today the single largest, best preserved, and most impressive group of Greek temples anywhere. These architectural glories were possible because of the size and wealth of the city, the same factors that necessitated and made possible the extensive water system of the city. In contrast, Morgantina was built inland, on a ridge at the juncture of the Catania plain with the plateaus of the center of Sicily. This ridge stands 578 to 656 meters above sea level, higher by 300 to 350 meters than the valleys to the north and south, but lower than the site of the nearest modern town, Aidone (885 meters), about 3 kilometers away. Morgantina began as a prehistoric settlement of migrant tribes from Italy whose king, Merges, gave his name to the city. The earliest Sikel settlement was on Cittadella, the easternmost wedge of the ridge, during the archaic period, no later than the sixth century.

Northern teachers in northern schools: the Greenland experience

Polar Record ◽  
1978 ◽  
Vol 19 (120) ◽  
pp. 209-216 ◽  
Author(s):  
Jack Cram
Keyword(s):  
School Administrators ◽  
Quality Of Education ◽  
School Buildings ◽  
The South ◽  
Northern Canada ◽  
The North ◽  
Native Teachers ◽  
Total Lack ◽  
As If

It often appears as if circumpolar school administrators believe that the quality of education varies with the number of photocopiers purchased, the variety of textbooks available or the shape and novelty of their school buildings. The idea that a teacher might be the single most important factor in a child's education often escapes mention. Yet the failure of schools in northern Canada and Alaska to produce enough graduates to meet even the limited local demand for workers can be traced, almost certainly, to the absence of trained native teachers and to the total lack of continuity provided by southern teachers, who stay for only two or three years in the north, keeping their locus of existence firmly rooted in the south.

Excavations on Pilsdon Pen, Dorset, 1964–71

1977 ◽  
Vol 43 ◽  
pp. 263-286 ◽  
Author(s):  
Peter S. Gelling
Keyword(s):  
Natural History ◽  
Iron Age ◽  
The South ◽  
The West ◽  
North West ◽  
The North ◽  
Nearest Point ◽  
Daunting Task ◽  
East End ◽  
The Hill

Pilsdon Pen is in west Dorset, very close to the Devon border, some 6 miles north-west of Bridport, and about 5½ miles from the nearest point of the coast (ST 413013). It is a long flat-topped hill, the highest in Dorset, reaching 908 ft above OD, and dominating Marshwood Vale from the north. The hill-fort occupies the south-east end of the Pen, at the north-west end of which there is a small embanked enclosure, much levelled by ploughing, which could be of Iron Age date also. The two nearest hill-forts are Lambert's Castle and Coneys Castle, about 3 and 3½ miles away respectively, which overlook Marshwood Vale from the west (fig. 1).Excavation began in 1964, and continued annually until 1971, all but one of the seasons lasting four weeks. The work was initiated, and largely supported, by the owner of the site, Mr Michael Pinney, of Bettiscombe Manor, to whom archaeology owes a great debt. Mrs Betty Pinney was one of our most skilful excavators, and all those who took part will remember her hospitality. Financial help was also given by the Dorset Natural History and Archaeological Society and by Birmingham University. Among many helpers, to all of whom I am most grateful, I should like to mention in particular my wife, who shouldered the daunting task of keeping the camp supplied, and Mr Jack Wells, of Tanyard Farm, Marshwood, without whose regular assistance the excavation would have taken much longer, and cost a great deal more.

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