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.

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.

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.

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.

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.

Excavations in Ithaca, III

1935 ◽  
Vol 35 ◽  
pp. 45-73 ◽  
Author(s):  
Sylvia Benton
Keyword(s):  
The Other ◽  
The South ◽  
West Side ◽  
North West ◽  
Preceding Article ◽  
Lime Kiln ◽  
The North ◽  
General Plan ◽  
Steep Hill

The site lies on the north-west side of the Bay of Pólis (Fig. 1), in a gash on the hillside where rock has fallen away, leaving a sheer face on the south of the site and the débris of undercliff on the north. The sea lies to the east and the entrance to the site on the north is blocked by fallen rocks (Fig. 3). Its position with regard to the other excavations round Stavrós in North Ithaca can be seen on the general plan of the area (Fig. 2 of the preceding article); our Fig. 2 shews the steep hill-side round the site.The cave was accidentally discovered by the proprietor Louisos when digging a pit for a lime-kiln. Schliemann found the excavation in progress in 1864, but did not realize its importance.

scholarly journals XXIV. Observations on the eclipse of the sun, April 1, 1764: In a letter to the Right Honourable James Earl of Morton, Pres. R. S. from the Rev. Nathanael Bliss, M. A. Savilian Professor of Mathematics at Oxford, and Astronomer Royal

1764 ◽  
Vol 54 ◽  
pp. 141-144
Keyword(s):  
The Sun ◽  
The South ◽  
North West ◽  
The North ◽  
South West ◽  
Royal Observatory ◽  
The Right

My Lord, As I had reason to believe, from a calculation made from the best lunar tables, that the north-west limit of the annular appearance, in the late great eclipse of the Sun, would pass but a few miles to the South-west of the Royal Observatory at Greenwich, I thought myself indispensably obliged, to leave Oxford, where my employment then called me;

Depositional Environment Drive as Overpressure Generation: Study Case in “Gap” Field, North West Java Basin

2020 ◽  
Author(s):  
A., C. Prasetyo
Keyword(s):  
Clay Mineral ◽  
Depositional Environment ◽  
Mineral Content ◽  
Hydrocarbon Generation ◽  
Well Test ◽  
Burial History ◽  
The South ◽  
North West ◽  
The North ◽  
Geological Processes

Overpressure existence represents a geological hazard; therefore, an accurate pore pressure prediction is critical for well planning and drilling procedures, etc. Overpressure is a geological phenomenon usually generated by two mechanisms, loading (disequilibrium compaction) and unloading mechanisms (diagenesis and hydrocarbon generation) and they are all geological processes. This research was conducted based on analytical and descriptive methods integrated with well data including wireline log, laboratory test and well test data. This research was conducted based on quantitative estimate of pore pressures using the Eaton Method. The stages are determining shale intervals with GR logs, calculating vertical stress/overburden stress values, determining normal compaction trends, making cross plots of sonic logs against density logs, calculating geothermal gradients, analyzing hydrocarbon maturity, and calculating sedimentation rates with burial history. The research conducted an analysis method on the distribution of clay mineral composition to determine depositional environment and its relationship to overpressure. The wells include GAP-01, GAP-02, GAP-03, and GAP-04 which has an overpressure zone range at depth 8501-10988 ft. The pressure value within the 4 wells has a range between 4358-7451 Psi. Overpressure mechanism in the GAP field is caused by non-loading mechanism (clay mineral diagenesis and hydrocarbon maturation). Overpressure distribution is controlled by its stratigraphy. Therefore, it is possible overpressure is spread quite broadly, especially in the low morphology of the “GAP” Field. This relates to the delta depositional environment with thick shale. Based on clay minerals distribution, the northern part (GAP 02 & 03) has more clay mineral content compared to the south and this can be interpreted increasingly towards sea (low energy regime) and facies turned into pro-delta. Overpressure might be found shallower in the north than the south due to higher clay mineral content present to the north.

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.

A gold diadem from Aegina

1987 ◽  
Vol 107 ◽  
pp. 182-182
Author(s):  
Reynold Higgins
Keyword(s):  
Bronze Age ◽  
British Museum ◽  
The South ◽  
North West ◽  
The North ◽  
The Dead ◽  
Middle Helladic ◽  
Dead Man ◽  
The Bronze Age ◽  
Grave Goods

A recent discovery on the island of Aegina by Professor H. Walter (University of Salzburg) throws a new light on the origins of the so-called Aegina Treasure in the British Museum.In 1982 the Austrians were excavating the Bronze Age settlement on Cape Kolonna, to the north-west of Aegina town. Immediately to the east of the ruined Temple of Apollo, and close to the South Gate of the prehistoric Lower Town, they found an unrobbed shaft grave containing the burial of a warrior. The gravegoods (now exhibited in the splendid new Museum on the Kolonna site) included a bronze sword with a gold and ivory hilt, three bronze daggers, one with gold fittings, a bronze spear-head, arrowheads of obsidian, boar's tusks from a helmet, and fragments of a gold diadem (plate Va). The grave also contained Middle Minoan, Middle Cycladic, and Middle Helladic (Mattpainted) pottery. The pottery and the location of the grave in association with the ‘Ninth City’ combine to give a date for the burial of about 1700 BC; and the richness of the grave-goods would suggest that the dead man was a king.

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