A note on deformed igneous sheets in the Durness Limestone of the Strath district of Skye

1970 ◽  
Vol 107 (3) ◽  
pp. 229-233 ◽  
Author(s):  
Robin Nicholson
Keyword(s):  
The Other ◽  
The South ◽  
South Side ◽  
North West ◽  
The North

SummaryClearly boudined and folded igneous sheets occur in Durness Limestone on the south side of the Tertiary Ben an Dubhaich granite. Obvious Tertiary dykes in nearby Mesozoic rocks are not deformed at all, nor has such deformation been described previously from the Caledonian activity in the Cambro-Ordovician of the north-west Highlands. Its appearance here does fit Clough's description (in Peach et al. 1907) of an unusually strong Caledonian penetrative deformation in the Strath Limestone, while the fact that all but one of the sheets are dolerites, a rock not elsewhere known from the Cambro-Ordovician but typical rather of the Tertiary activity for which Skye is famous, and that the other is a two feldspar porphyry very like the Ben an Dubhaich granite, point to the possibility of Tertiary deformation.

Casa del Menandro (I 10,4)

2007 ◽  
Author(s):  
Penelope M. Allison
Keyword(s):  
The Other ◽  
Small Hole ◽  
Public Facility ◽  
The South ◽  
South Side ◽  
North West ◽  
The North ◽  
Volcanic Deposit ◽  
Bone Fragments ◽  
Wall Decoration

To either side of this main entranceway, on the street front, are fixed masonry seats. Such seats have been assumed to have been for waiting clients. However, in Pompeii these seats are not always in front of the largest and most elaborate houses, that is those whose occupants were likely to have had clients. They were therefore likely to have served as a public facility available to anyone, including the house occupants. No loose finds were reported from this entranceway. The only visible sign of possible post-eruption disturbance to the volcanic deposit is a small hole towards the south end of the east wall of this ‘atrium’. However, the hole seems too small to have been the breach made by a post-eruption intruder. Maiuri noted, that the wall decoration of this ‘atrium’ was of a fresh and well-preserved Fourth Style executed after the last transformation of the house. The pavement was in lavapesta. Fixtures here included a central catchment pool (impluvium), revetted in white marble that was damaged either before or during the eruption, and a lararium aedicula in the north-west corner. According to Maiuri, the aedicula was constructed after the last well-preserved wall decoration, but Ling believes they are contemporary. At least forty-five small bronze studs were found in the north-west corner of this area. These had decorated the wooden lattice of the aedicula, now reconstructed in plaster. All the other recorded moveable finds were from the south side of this space. These included: a household storage jar; two clay lamps; bronze and iron fittings, possibly from the closing system for room 8, the so-called ‘tablinum’; and bone fragments probably from a piece of furniture. In the south-west corner were found a large bronze basin and a bronze patera, both of which were conceivably associated with bathing. Contrary to what might be expected, no statuettes of Lares or other representations were found in the lararium aedicula. Maiuri therefore concluded that these must have been made of wood. If this were so, then the excavators, who were able to make a cast of the wooden latticing, would surely also have observed any statuettes inside the aedicula, objects which would seem to have been more important than the latticing.

scholarly journals I.—Microscopic Structure of Irish Granites. No. 2. Granite of Aillemore, Co. Mayo

1874 ◽  
Vol 1 (1) ◽  
pp. 1-2
Author(s):  
Edward Hull
Keyword(s):  
The Other ◽  
Microscopic Structure ◽  
South Side ◽  
North West ◽  
Fine Grained ◽  
Lower Silurian ◽  
The North ◽  
Geological Map ◽  
Vertical Walls ◽  
Dark Green

This granite forms an isolated mass, rising into two eminences a few miles south of Louisburg, called Corvock Brack (1287 feet) and Knockaskeheen (1288 feet). It is a greyish granite—generally fine—grained—consisting of quartz, two felspars,—one orthoclase, the other triclinic, probably oligoclase—and dark green mica. In some places there are patches in which the felspar assumes the appearance of “graphic granite.” Numerous boulders of this granite are strewn over the district to the north-west, and on the south side of Knockaskeheen; the rock is traversed by regular joints ranging N. 10 W., along which it splits off into nearly vertical walls. The position of the granite is shown on Griffith's Geological Map of Ireland, and it is surrounded by schistose beds, generally metamorphosed, and probably of Lower Silurian age. The granite itself is of older date than the Upper Llandovery beds, which lie to the southward.

scholarly journals Observations upon the marine barometer, made during the examina­tion of the coasts of New Holland and New Wales, in the Years 1801, 1802, and 1803. By Matthew Flinders, Esq. Com­mander of His Majesty’s Ship Investigator . In a letter to the Right Hon. Sir Joseph Banks, K. B. P. R. S. &c. &c. &c

1832 ◽  
Vol 1 ◽  
pp. 230-232
Keyword(s):  
The State ◽  
The Other ◽  
South Coast ◽  
The South ◽  
South Side ◽  
The North ◽  
North Side ◽  
Northern Half ◽  
Southern Half ◽  
The Right

The chief circumstance that induced Capt. Flinders to think his observations Upon the marine barometer were worthy of attention, was the coincidence that took place between the rising and falling of the mercury, and the setting in of winds that blew from the sea and from off the land, to which there seemed to be at least as much reference as to the strength of the wind or the state of the atmosphere. Our author’s examination of the coasts of New Holland and the other parts of the Terra Australis, began at Cape Leuwen, and con­tinued eastward along the south coast. His observations, which, on account of their length, we must pass over, show, that a change of wind from the northern half of the compass to any point in the southern half, caused the mercury to rise; and that a contrary change caused it to fall. Also, that the mercury stood considerably higher When the wind came from the south side of east and west, than when, in similar weather, it came from the north side.

scholarly journals Lovenula (Neolovenula) alluaudi (Guerne and Richard, 1890) in the Canary Islands (Copepoda: Calanoida: Paradiaptominae)

1989 ◽  
Vol 59 (4) ◽  
pp. 239-241 ◽  
Author(s):  
Thomas E. Bowman
Keyword(s):  
Canary Islands ◽  
The Other ◽  
Small Island ◽  
African Continent ◽  
The South ◽  
South Side ◽  
North West ◽  
West Part ◽  
Extreme North

Lovenula (Neolovenula) alluaudi is widespread on Lanzarote, where it occurred at 22 of the 105 stations. On Fuerteventura it was found at only 2 of the 53 stations, both in the extreme north-west part of the island. It was also found in a reservoir on the south side of the small island of Alegranza. Samples collected at several hundred stations in the other Canary Islands failed to yield a single calanoid, supporting the belief that the eastern islands are fragments of the African continent that drifted to deeper waters.

scholarly journals Kos Astypalaia

1898 ◽  
Vol 4 ◽  
pp. 95-100
Author(s):  
Duncan Mackenzie
Keyword(s):  
The Other ◽  
Mountain Region ◽  
The South ◽  
North West ◽  
North East ◽  
The North ◽  
South West ◽  
The Village

From the modern town of Kos, on the site of the ancient capital at the north-east extremity of the island, to the village of Kephalos at the southwest end is a ride of eight hours.The village stands on a chalky plateau which beyond the isthmus marks the beginning of the mountain district of south-west Kos. This in turn is a repetition on a smaller scale of the mountain region, at the other end of the island, which forms the lofty termination to the long central tableland. The highest points of the mountain district are towards the south-east where the fall to the sea is very rapid. The highest neighbouring peak, Mount Ziní, is about an hour distant from the village in a south-easterly direction, while all that lies to the north-west of the main range is high pastoral country with many torrent beds.

scholarly journals An account of two rainbows, seen at the same time, at Alverstoke, Hants, July 9, 1792

1793 ◽  
Vol 83 ◽  
pp. 1-2
Keyword(s):  
The Other ◽  
The Sun ◽  
Considerable Time ◽  
The South ◽  
North West ◽  
The North ◽  
Sea Coast

On the evening of the 9th of July, 1792, between seven and eight o'clock, at Alverstoke, near Gosport, on the sea coast of Hampshire, there came up, in the south-east, a cloud with a thunder-shower; while the sun shone bright, low in the hori­zon to the north-west. In this shower two primary rainbows appeared, AB and AC, (Tab. I.) not concentric, but touching each other at A, in the south part of the horizon; with a secondary bow to each, DE and DF (the last very faint, but discernible), which touched likewise, at D. Both the primary were very vivid for a considerable time, and at different times nearly equally so; but the bow AB was most permanent, was a larger segment of a circle, and at last, after the other had vanished, became almost a semicircle; the sun being near setting. It was a perfect calm, and the sea was as smooth as glass.

The Position of Kajkavian in the South Slavic Dialect Continuum in Light of Old Accentual Isoglosses

2017 ◽  
Vol 62 (1) ◽  
Author(s):  
Mate Kapović
Keyword(s):  
The Other ◽  
The South ◽  
North West ◽  
Slavic Languages ◽  
The North ◽  
Other Hand

SummaryAll South Slavic languages, from Bulgaria in the South-East to Slovenia in the North-West, are part of a dialect continuum. This paper outlines the position of what is traditionally called Kajkavian in that continuum in light of old accentual isoglosses. Kajkavian shares several old prosodic-phonological isoglosses with Slovene (such as the rise of the neocircumflex), while on the other hand it is connected with Western Štokavian and Čakavian through some morphological-categorial accentual isoglosses (like the innovative accent of the infinitive and

The Vassal-Treaties of Esarhaddon

Iraq ◽  
1958 ◽  
Vol 20 (1) ◽  
pp. 1-99 ◽  
Author(s):  
D. J. Wiseman
Keyword(s):  
The Other ◽  
The South ◽  
North West ◽  
South Eastern ◽  
The North ◽  
British School ◽  
The Temple ◽  
Made In

The sixth (1955) season of excavation by the British School of Archaeology in Iraq at Nimrud (ancient Kalḫu, Biblical Calah) was mainly devoted to clearing buildings in the south-eastern corner of the akropolis. One building to the north of Ezida, the temple of Nabu, contained a long Throne-room (SEB2) where lay a varied collection of ivories and bronzes from Assyrian furniture broken when the building was destroyed by fire. Amid this debris more than three hundred and fifty fragments of baked clay tablets were found scattered in the north-west corner of the room between the dais which once supported the royal throne and the door leading to a small ante-chamber (NTS3). Some fragments were also found in the southern doorway of the Throne-room and in the adjacent courtyard (Fig. 1). It will probably never be known with certainty, whether the documents had once been housed in this room or thrown there when the building was sacked by the Medes about 612 B.C. A special room (NT12) in the neighbouring Nabu Sanctuary seems to have been set aside for the use of scribes and for the storage of tablets and this may have been their original location.These fragments proved to be parts of a few large tablets of which one was reconstituted in the field. Miss Barbara Parker, who was present at the time of discovery, soon identified the text as a treaty made in 672 B.C. by Esarhaddon, king of Assyria (681–669 B.C.), with a chieftain of the Medes named Ramataia of Urukazaba(r)na. The remaining texts were duplicates except that they named different city-govenors, or chieftains, as the other party to the agreement. The dated fragments bear the same Eponym year-date of 672 B.C. With commendable speed Miss Parker published a brief report based on her preliminary reading of about three hundred lines of the Ramataia text and some of the fragments.

I 10, 8 and 9

1997 ◽  
Author(s):  
Roger Ling ◽  
Paul Arthur ◽  
Georgia Clarke ◽  
Estelle Lazer ◽  
Lesley A. Ling ◽  
...  
Keyword(s):  
Late Stage ◽  
The South ◽  
The West ◽  
West Side ◽  
South Side ◽  
North West ◽  
The North ◽  
Eastern Boundary ◽  
The One ◽  
Northeast Corner

This complex consists of an atrium-house from which a front room has been separated at a late stage to form an independent shop or workshop. Together they occupy the north-west corner of the insula, the house opening northwards and the shop westwards. Before the shop was separated from it, the house had a relatively broad facade (approx. 14 m.), but the oblique alignment of the insula boundary to the west resulted in a considerable contraction towards the rear. At the southern end of the roofed part of the house, coinciding with the south walls of rooms 10 and 12, the property is only 10 m. wide; and the garden beyond this, thanks primarily to a shift in the line of the eastern boundary becomes even narrower, contracting to less than 8.50 m. As in the Casa del Fabbro, the atrium (1) is set against one of the property boundaries, this time the west rather than the east; but, owing to the greater width of the house, it is broader (from 7.20 to 8.20 m.) and still allows space for a deep room on the east. The impluvium is centrally positioned in relation to the short (south) side. The fauces, however, enters the atrium somewhat off-centre, 3.80 m. from the northeast corner and 2.70 m. from the north-west, presumably in order to obtain three more or less equally sized rooms on the north facade. As the plot contracts toward the rear, this tripartite division becomes more difficult; the outlying rooms, on the west side particularly are uncomfortably narrow and cramped. Of the three rooms on the north front, the westernmost is the one which in the final period had become a shop with an independent entrance (I 10, 9); it had formerly been a corner room opening from the atrium via a doorway immediately adjacent to the fauces, but this doorway was blocked and a new entrance, 2.30 m. wide, quoined in opus listatum, was opened in the west wall (Pl 90). The lava threshold (Fig. 61) points to fittings typical of a shop: a separate pivoted door and vertical planks set overlapping in a groove.

scholarly journals A Cave of the Nymphs on Mount Ossa

1909 ◽  
Vol 15 ◽  
pp. 243-247
Author(s):  
A.J.B. Wace ◽  
M.S. Thompson
Keyword(s):  
The South ◽  
West Side ◽  
South Side ◽  
North West ◽  
The North ◽  
Central Cone ◽  
The Village

On the north-west side of the great central cone of Mount Ossa a wide fissure runs right across the mountain from Mega Keserlì to Tságezi. On the south side of this fissure and at the base of the central cone lies the village of Spiliá, which is to be distinguished from another village of the same name near Laspochori at the eastern entrance to Tempe. To the north of the fissure rises a peak known as Pláka, which is the part of Ossa that directly overhangs Tempe. A little below the bare rocky summit of this peak, which rises to a height of at least 3,500 feet, and on its south side about an hour's walk from Spiliá, is a cave, which, though long known to the inhabitants of the district, has never before been visited by archaeologists.

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