VII.—“Analysis of Stilbite of an unusual form, from Faröe”

Author(s):  
Heddle
Keyword(s):  

At the foot of the terminal and almost inaccessible cliff of the hill—name unknown—which towers immediately to the south west of the harbour of Waii or Hoiwig, in Bordöe, Faröe, the writer obtained the specimen—a single one—of which the following is an analysis:The island of Bordöe, like the most of Faröe, is built up of strata of bedded trap with mural cliffs, which alternate with terraces of grass clad debris. At this part of the island, the terraced trap consists of a wackenitic “claystone,” which is very friable, light in colour, easily disintegrated, and in places tufaceous in aspect. Its amygdaloidal druses are very few and far between.

1898 ◽  
Vol 30 (12) ◽  
pp. 298-300
Author(s):  
F. H. Wolley Dod
Keyword(s):  
The Past ◽  
To Come ◽  
The Hill ◽  

Chionobas.—To hear of the occurence of Chionobas Macounii in the hill-prairie district south of Calgary will doubtless be as much of a surprise to most entomologists as the discovery of it here has been to myself. That a man who, like myself, is ever on the outlook for anything fresh in the way of butterflies, should have lived for five years in Macounii locality without knowing it surpasses my comprehension. whilst overhauling, relaxing, and setting last winter from the captures of the past two seasons, I came across, amongst some papered specimens that had been handed to me by a Mr. Hudson, an ardent collector here, a papered butterfly labelled “Chionobas Chryxus, ♀, July 4th 1896,” taken amongst the spruce about twelve miles west of here; that is to say, about 26 miles to the south-west of Calgary. Now, though I have never yet seen Chryxus here, I have always been expecting to come across it amongst the spruce, and was not much surprised. However, after relaxing and setting me specimen, lo and behold! it was not Chryxus, but agreed rather closely with some C. californica♂ ♂ that I have from Ft. Klamoth, Oregon.


1969 ◽  
Vol 34 ◽  
pp. 148-190 ◽  
Author(s):  
I. M. Stead ◽  
M. Jarman ◽  
Angela Fagg ◽  
E. S. Higgs ◽  
C. B. Denston

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.


1928 ◽  
Vol 65 (1) ◽  
pp. 12-25 ◽  
Author(s):  
F. Smithson

From the southern shores of Dublin Bay there stretches to the south-west a broad granite intrusion with rocks of supposed Ordovician age on both sides of it. These rocks are metamorphosed near the granite, and the belt of metamorphism is wider on the south-east than on the north-west side, indicating, no doubt, that the plane of junction dips more steeply on the latter side. Near Dublin the Lower Carboniferous rocks rest unaltered upon the granite. On the south-east side, in the northern part of the county of Wicklow, the belt of Ordovician rocks is only some 2 miles wide, and a large area of supposed Cambrian rocks lies between it and the sea. Around the hill of Carrickgollogan a. patch of similar rocks appears incongruously in the middle of the Ordovician belt. After a study of the region to the south of Dublin one seems to be naturally drawn towards this small area around Carrickgollogan, for it presents a problem, the key to which may explain the geological structure of a much wider area.


1945 ◽  
Vol 41 ◽  
pp. 72-74 ◽  
Author(s):  
John L. Myres

The North Range of Cyprus is a long, narrow, rugged ridge of hard steeply-inclined limestones, flanked southwards by coarse grits and sandstones, also steeply-inclined. On both sides of the range the lower slopes consist of later and softer limestones and marls, which overlie the rocks of the range unconformably, and have not been much disturbed since they were formed. The contrast is very marked between (1) the rugged peaks and spurs of the mountains, which run up, barren or sparsely forested, to more than 3000 feet, with passes as low as 1000 feet; (2) the dry brown barren ‘hummocks’ of the grits and sands, and (3) the light soil and great local fertility of the recent lowlands. This fertility depends, however, directly on the water supply; and as the greater part of the rainfall of Cyprus seems to come up from the south-west, and is liable to be intercepted by the hills, the north coast depends mainly on the discharge of the hill rainfall in springs, which break out at intervals along the upper margin of the later limestones, particularly if they are marly, and cut steep-sided torrent beds which widen seawards, and have formed alluvial coast deposits here and there.


Author(s):  
Dennis Harding

For much of the past two hundred years, a basic assumption has been that hillforts had a primarily defensive function. That they served also as settlements or for community gatherings, perhaps even for ritual or ceremonial activities such as seasonal festivals or inaugurations of kings, has been variously inferred, but it was not until relatively recently that the purpose of community defence within the framework of a hierarchical society was so fundamentally challenged. The reasons, however, were often based upon individual site circumstances, from which generalization hardly seems justified. At the Chesters, Drem in East Lothian (Figure 5.2a), for example, it was argued (Bowden and McOmish 1987) that the hillfort's defensive capability was compromised by being overlooked from the south by higher ground, from which missiles might have been projected into the enclosure. Tactically this seems odd, since the fort's multiple lines of enclosure, especially at its northwest- and east-facing entrances, makes it on plan one of the more complex multivallate hillforts in Britain. Whether these had realistic defensive capability or were intended primarily for display and status remains open to debate. Whilst it is certainly true in individual cases that hillforts were not sited topographically with tactical advantage as a paramount consideration, or that a regional class like the hill-slope forts of the south-west were apparently at a disadvantage from higher ground, or that the area enclosed by some hillforts was so great as to make their defence logistically impractical, equally we could cite hillforts where the enclosing earthworks by any standard would have been a very formidable barrier to assault. Every generation reads its archaeology in the conceptual context of its own time, and it is hardly surprising that a generation brought up with two world wars should have interpreted hillforts in terms of ‘invasions’. Wheeler's (1953: 12) description of Bindon Hill, Dorset, as a ‘beach-head’ could hardly have been conceived by anyone other than the brigadier who had fought through North Africa and the Salerno landing in Italy. Nevertheless it is hard to avoid the conclusion that the current challenge to the defensive role of hillforts stems not so much from individually anomalous sites as from a more general objection to the concept of conflict in prehistory, and is one facet of what has been noted earlier as the ‘pacification of the past’ (Keeley 1996: 23).


1927 ◽  
Vol 55 (2) ◽  
pp. 303-315 ◽  
Author(s):  
George Slater

Lønstrup is a small fishing village and summer resort, situated on the west coast of North Jutland, a few miles west of Hjørring in the district known as Vendsyssel. The country generally is low and treeless, but is noted for its comprehensive schemes of land reclamation, and the scientific development of its agriculture.In the neighbourhood of Lønstrup the monotony of the country is relieved by two low hills, the one, a little inland, is known as Vennebjerg, the other, known as Rubjerg Knude, lies some 2 miles to the south-west and is dissected by the coast-line, the apex of the hill being marked by a lighthouse. These two adjacent hills formed islands in the Yoldia Sea.The coast-line has a uniform north-east, south-west trend, and cliffs occur from Lønstrup to Lokken in the south-west, a distance of between 7 or 8 miles, the cliff-scenery being generally similar to that of the Norfolk coast near Cromer.


1895 ◽  
Vol 2 (10) ◽  
pp. 452-458 ◽  
Author(s):  
S. F. Peckham

Near the crest of the ascent to the lake the road divides: one branch passing to the left and south ascends over the rim of the basin of the lake, and skirting the lake for about a quarter of its circumference passes over the hill to the south-west, as described by Mr. Manross. The right-hand branch follows the flow of the pitch and enters upon the lake simply by a change of grade from a sharp ascent to a very slight inclination upwards towards the centre of the lake. I was particularly impressed with this fact, and took pains to verify my first impression upon a second visit, as it proved conclusively that, notwithstanding the vast quantities of pitch that had been removed from the lake, there is still a movement out of the lake, glacier-like, down the slope to the sea.


2018 ◽  
Vol 1 (126) ◽  
pp. 135-148
Author(s):  
Ahmed Kamil Mohammed ◽  
Shaymaa Abdel zahra Habeeb

Tel Abu Antiq is located in an area that has borders with three governorates, which are Bebel from Altaleea Side, Alnajaf Alashraf nearby Alhurriya sub district and Alqadisiya Al mhannawiya sub district. It is around 50 km away to the south of the historic city of Babel. It is located western to the archeological city of Mard 15km away nearly. . The location is famous of agriculture like the date palms and rice in particular. The hill is penetrated by drainage 20m wide known as Al haffar or the Eastern Drainage. The Drainage located to the west of it is called Alqawsi. It was dug to dry up the marshes waters in 1994.   The highest point in the hill reaches 20m above sea level. The lands surrounding the hill were plain, fertile and suitable for agriculture. Many decades ago the lands were immersed by waters of Ibn Najim Marsh; one of Alshamiya and Almishkhab marshes. This immersion led to disapearance of its features. It was forgotten by the Archeological inspectors who surveyed the agricultural lands within the farms especially those were subject to settlement of the land rights in the thirties of the last century.   The state organization for archeology and heritage marked in their records and maps at that time two archeological hills connected by an old irrigation canal, they are at close distance from Abu Antiq hill. The 1st is known as (Zghaitan), it is to the south west of Abu Antiq. The second is known as (Jeghaiman) to the North West. Total area of both hills with Abu Antiq is 9 square kilometers. They all make mostly a settlement. The surface areas of Zghaitan hill indicates that it belongs to the aancient babylonic era.


1980 ◽  
Vol 11 ◽  
pp. 45-52 ◽  
Author(s):  
Olwen Brogan

In the Gebel Garian, about 20 kilometres south of Asabaa, the map-makers of 1964 indicated an ancient wall (Fig. 1) called Hadd Hajar (i.e. wall of stone) running south-west for six kilometres from Ras al Tays al Abyad (858 m; the Hill of the White Goat) on which stood a watch tower, to Ras al Said (764 m). The country crossed by Hadd Hajar is about 690-730 m above sea-level with a gently-undulating surface constituting a fairly open and level valley. The hills are covered with esparto-grass. On the west the Wadi Wamis winds among closely-set hills while, in the north-east, the wall is carried for a further three quarters of a kilometre across a narrow valley from Ras al Tays al Abyad to another hill Ras al Saqifah. An old track comes southwards down this valley flanked on the east side by a barrier of hills over 800 m high. Where the track crosses the wall there is a Roman building (Gasr al Saqifah) with traces of an archway for people and flocks to pass through. Two kilometres to the south is an old cistern (Majin Saqifah) presumably Roman. Beyond, the track continues about 25 kilometres to a large well, Bir al Shaqaykah (Sceghega), after which it is another 28 kilometres south-eastwards to Mizdah on the Wadi Sofeggin.


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