IV. Sovereignty Over Pulau Ligitan and Pulau Sipadan (Indonesia V Malaysia), Merits, Judgment of 17 December

2003 ◽  
Vol 52 (3) ◽  
pp. 797-802
Author(s):  
Malcom D Evans ◽  
JG Merrills

On 17 December 2002 the International Court gave its judgment in a dispute over two small islands in the Celebes Sea claimed by both Indonesia and Malaysia. The islands in question, Ligitan and Sipadan, are located off the north-east coast of Borneo and lie approximately 15.5 nautical miles apart. Both are very small and Ligitan is uninhabited; Sipadan, on the other hand, was developed by Malaysia into a tourist resort for scuba diving in the 1980s. In 1998 Indonesia and Malaysia referred the dispute to the Court by means of a Special Agreement, asking for a decision ‘on the basis of the treaties, agreements and any other evidence furnished by the Parties’ on whether sovereignty over the islands belonged to Indonesia or to Malaysia.

1929 ◽  
Vol 6 (2) ◽  
pp. 76-78
Author(s):  
J. Reid Moir

The object of this paper is to describe and to figure accurately a remarkable double-ended rostro-carinate flint implement found by me during this year (1929) upon the north-east coast of Norfolk. The discovery was made upon the foreshore about mid-way between East and West Run ton, where at low water there are exposed considerable areas of the Basement Bed, resting upon the chalk, and referable to either the lowermost division of the Cromer Forest Bed or to the Stone Bed beneath the Norwich Crag. The implement was not found in situ in the Basement Bed, but was lying, with other stones, close to an exposure of this deposit. Apart, also, from this association, the specimen contains, in some of its interstices, portions of the highly ferruginous sand of the Basement Bed, while its colour and condition make it clear to those who are familiar with the stones in this deposit, that the implement at one time—and that recently—formed a part of it. The implement exhibits a typical mottled colouration consisting of areas of black, tawny brown and chocolate brown, while its ridges and outstanding portions show in most cases a rounded and somewhat broken-down appearance, which may be due to attrition by water-rolling, but which I am inclined to regard, as I have stated elsewhere, is to be accounted for by the action of some solvent present in the Basement Bed. The specimen exhibits but few incipient cones of percussion upon its flaked surfaces (which show a well-marked glaze), and cannot, therefore, have been subjected to collisions with other stones set in movement by running water. On the other hand a certain number of striae are to be observed upon the flake-scars of the implement, and these scratches not only, as it appears, cut into the patinated surfaces, but are in a weathered-out condition, thus showing that the flint was first patinated, then striated, and afterwards exposed to atmospheric effects.


Toxins ◽  
2020 ◽  
Vol 12 (8) ◽  
pp. 485 ◽  
Author(s):  
Theo Tasoulis ◽  
Anjana Silva ◽  
Punnam Chander Veerati ◽  
Mark Baker ◽  
Wayne C. Hodgson ◽  
...  

Intra-specific venom variation has the potential to provide important insights into the evolution of snake venom, but remains a relatively neglected aspect of snake venom studies. We investigated the venom from 13 individual coastal taipans Oxyuranus scutellatus from four localities on the north-east coast of Australia, spanning a distance of 2000 km. The intra-specific variation in taipan venom was considerably less than the inter-specific variation between it and the other Australian elapids to which it was compared. The electrophoretic venom profile of O. scutellatus was visually different to six other genera of Australian elapids, but not to its congener inland taipan O. microlepidotus. There was minimal geographical variation in taipan venom, as the intra-population variation exceeded the inter-population variation for enzymatic activity, procoagulant activity, and the abundance of neurotoxins. The pre-synaptic neurotoxin (taipoxin) was more abundant than the post-synaptic neurotoxins (3FTx), with a median of 11.0% (interquartile range (IQR): 9.7% to 18.3%; range: 6.7% to 23.6%) vs. a median of 3.4% (IQR: 0.4% to 6.7%; range: 0% to 8.1%). Three taipan individuals almost completely lacked post-synaptic neurotoxins, which was not associated with geography and occurred within two populations. We found no evidence of sexual dimorphism in taipan venom. Our study provides a basis for evaluating the significance of intra-specific venom variation within a phylogenetic context by comparing it to the inter-specific and inter-generic variation. The considerable intra-population variation we observed supports the use of several unpooled individuals from each population when making inter-specific comparisons.


1964 ◽  
Vol 55 (1) ◽  
pp. 97-124 ◽  
Author(s):  
E. C. C. van Someren ◽  
M. Furlong

Descriptions are given of 24-hour biting catches, made in and around Faza, a village on Pate Island, off the north-east coast of Kenya, East Africa.Aedes pembaensis Theo. was the predominant mosquito in these catches but fair numbers of Aedes mombasaensis Mattingly were also taken; the biting cycles of these two are discussed. Six other species were taken in small numbers.For Ae. pembaensis, biting cycles calculated on catches grouped for site, moon phases, neap tides and spring tides show that both moon and tide and light intensity influence the biting behaviour. Different but recurring patterns occur with various combinations of these factors.For Ae. mombasaensis, the cycles have a very constant biphasic pattern. Catches grouped for moon phases, tides and catch sites, as for Ae. pembaensis, show that more biting females are taken at neap tides than at spring tides. Two patterns of behaviour occur, one associated with spring tides and the other with neap tides. An even level of biting activity occurs during the night with intense and prolonged moonlight; otherwise moon-phase cycles have little effect on biting behaviour.It is felt that 24-hour biting catches can give useful information on behaviour patterns but it is desirable to have a long series of catches to analyse. For the purpose of calculating biting cycles, the results of catches showing similar modifications in behaviour should be treated separately.


1876 ◽  
Vol 3 (8) ◽  
pp. 360-361
Author(s):  
T. Mellard Reade

As a contribution to our knowledge of the formation of these very interesting “natural embankments of the sea,” I may point to a little bay in Anglesea, immediately westward of the Bryn Ddu Limestone quarries on the north-east coast of Anglesea, about two miles and a half westward of Puffin Island. This little bay is not more than about a furlong across, and may be roughly described as semicircular in form, lying nearly due west to east from point to point. From being in miniature as it were, the ridge can be readily studied, and it is very striking to see how, commencing in the westward as a beach, it gradually rises into a ridge having very steep sides. No less remarkable is the way in which the stones increase in size as the ridge does in height. At the west end it may be described as composed of Limestone pebbles, with here and there a boulder, while at the east end it is built up almost entirely of large limestone boulders and blocks, many containing from one to two cubic feet and some more. Intermixed there are boulders from the size of the closed hand and upwards. The larger blocks are sub-angular and rounded, and no doubt get gradually worn down smaller and rounder, until they become “boulders.” by being moved about, by the sea; but some on the other hand, being thrown over on to the back of the bank, cannot be further affected by the waves. In this ridge, as I have pointed out is the case with the Chesil Bank, the stones follow the law of the bank itself, the largest being collected to form the highest part of the bank, which in both occurs where the wave-action is most intense.


Twejer ◽  
2021 ◽  
Vol 4 (1) ◽  
pp. 589-628
Author(s):  
Dilshad Aziz Marif ◽  

This paper deals with the ancient settlements in the plain where the city of Sulaimani found in 1874 A.D. In his book (Babylonian Problems) Lane (1923) proposes that modern Sulaimani built on the long-lost city of Celonae that was mentioned by the Roman historian Quintus Curtius Rufus (1st century A.D.) in his book "Histories of Alexander the Great.” Also, the Kurdish historian Amin Zeki in his book (The History of Sulaimani)1951, agrees with Lane, and he suggests that the name of modern Sulaimani’s name perhaps derived from the same name of Celonae. Many other historians and archaeologists repeat the same identification. In this paper, we investigated this identification, and we found that the city of Celonae was mentioned only once by the Roman historian Quintus Curtius Rufus (1st century A.D.) in his book "Histories of Alexander the Great,” he refers to the journey of Alexander the Great from Susa to Ekbatana, according to Rufus, on his way, Alexander camped in Celonae. We suggest a new identification for the Celonae Town in the northern edges of Garmian district at the foot or on the top of one of the mountains of the modern Qaradagh ranges, because, Alexander took the road from Susa to the north then east crossing the city of Sittake on the Tigris near Celucia/al-Madain, then moving to other cities along the road to the direction of the north-east, camped in Celonae, then moved to the east and reached Bagastana (Behistun) and after wards to Ecbatana, the capital of the Median Empire in (modern Hamadan). We found also, that the Assyrian royal inscriptions refer to a mountain called Siluna, the Assyrian king Adad-Narari III (811-783 B.C.) in his campaign on Namri and Media, after crossing the Lower Zab toward the east, first he mentions the mountain Siluna, where the sun rises, then he occupied Namri and crossed the other lands in the east to reach Media, and since Namri was the land of the Kassites (in the post-Kassite period) located in the area of Sangaw-Garmian-Qaradagh-Bamo ranges, we can conclude that the mountain Siluna and the city Celonae were located in the same place somewhere in Qaradagh ranges. In the base of the above-mentioned evidence, we can reject the previous identification of Celonai with modern Sulaimani. On the other hand, in this paper we discussed other identifications of modern Sulaimani with ancient cities and towns mentioned in the cuneiform records, for instance, Radner (2017), suggests that the Zamuan capital city of Arrakdi of the Lullubu people located under modern Sulaimani, but this is not a proper identification, because the city of Arrakdi was mentioned in the cuneiform records three times, and in all records they refer to the point that the city located beyond a roughed mountain, the Annals of Ashurnasirpal II refers that the city located at the foot of the roughed mountain Lara, and this mountain should be modern Lare mountain in the east of Shabazher district far east from modern Sulaimani. Also, the cuneiform tablet that was discovered in Sitak in Sharbazher district and that tablet also refers to Arrakdi. Also, we found that Spiser linked the village of Uluba (Ulubulagh) now it is a district in the southern east of Sulaimani, with the Lullubian City of Lagalaga, this identification only based on the similarities between the two toponyms. On the other hand, Abdulraqeeb Yusuf, suggests that the old village of Daragha, which is now a district in the eastern part of Sulaimani derived from the Zamuan city Dagara of the Lullubies, this identification also not appropriate one, because the village and district named after the name of a nobleman called Mr. Dara Agha, and there is no archaeological ruin in this district as well. The city of Sulaimani was built on an area where a huge archaeological Gird/Tell existed, the Babanian princes built their palace on this artificial hill and the administrative buildings to the east of it, when they dug for the foundations, they discovered coins, a stone with unknown script, and many jars, some of them big jars contained human skulls. In 2005, when the modern building Kaso Mall constructed on the northwest of the hill, we found two seals date back to Jamdet-Naser = Nineveh V period, and Ubaid potsherds, and some bull skulls, their horns cut with a sharp instrument. This evidence indicate that the city was built on a settlement date back to the 5th-4th millennium B.C. Other archaeological discoveries in Girdi Kunara and Girdi De Kon in the western part of the city at the bank of Qiliasan and Tanjero rivers, in Kunara many cuneiform tablets discovered there, we can link these sites also with the Lullubies in the third & second millennium B.C.


Author(s):  
Germaine A. Joplin

The writer has recently described a small collection of glaucophane- schists from the Diahot valley and the north-east coast of New Caledonia (Jensen, 1936), and four of these contain lawsonite.Lacroix (1897) has recorded lawsonite from New Caledonia, but the occurrence seems worthy of further mention as in two cases the lawsonite is found to be pseudomorphing plagioclase in doleritic rocks which show a relict ophitic fabric. So far as the writer is aware, such an occurrence of lawsonite pseudomorpbing felspar has not been recorded, though Lacroix figures a glaucophane-schist from Corsica which suggests this structure. The other two lawsonitebearing rocks from New Caledonia seem to have been coarse-grained plutonic rocks and probably never had an ophitic fabric.


1973 ◽  
Vol 39 ◽  
pp. 354-382 ◽  
Author(s):  
Claire O'Kelly

The art in question is found on the structural slabs of a group of megalithic tombs in the valley of the Boyne in Ireland. The tombs are all passage-graves and are characteristically situated on the highest local ground and grouped in a ‘cemetery’. The Boyne cemetery is about 15 km from the east coast and about 50 km by road north of Dublin. In an area approximately 4 × 4 km are situated the three large tumuli of Newgrange, Knowth and Dowth, as well as over 40 other monuments, more than half of which are passage-graves (fig. 1).The three large mounds are only a few kilometres apart; in fact, from any one of them the other two can be seen since all are in commanding situations. They are similar as regards size and appearance, that is to say, each consists of a mound of stones, or stones, earth, etc., circular in plan and flat-topped, about 85 m in diameter at the base and 12 to 15 m in height. The base of each is surrounded by a continuous kerb of large slabs, 97 at Newgrange, an estimated 110 at Dowth, and an estimated 120 at Knowth. Newgrange is the central tumulus, Dowth is to the north-east, and Knowth to the north-west.


2009 ◽  
Vol os16 (2) ◽  
pp. 75-78 ◽  
Author(s):  
Robert G Jagger ◽  
Chand A Shah ◽  
Indika D Weerapperuma ◽  
Daryll C Jagger

Aim To assess the prevalence of orofacial complications associated with SCUBA (self-contained underwater breathing apparatus) diving. Main outcome measures were prevalence of orofacial pain and odontocrexis. Method Two hundred divers at four dive centres on the north-east coast of Australia were asked to complete a questionnaire that requested information regarding diving experience and facial pain and dental symptoms experienced during diving. Results One hundred and twenty-five completed questionnaires were returned (63% response rate). The prevalence of reported orofacial pain was 44%. Twenty-one per cent reported toothache, 27% sinus pain, 16% jaw pain, and 12% other pain. The prevalence of odontocrexis was less than 1%. Less than 1% had lost a filling when diving. No divers reported a crown or bridge being dislodged during diving. Conclusion Among those who returned questionnaires, orofacial pain in divers was common and odontocrexis was rare.


1902 ◽  
Vol 34 (4) ◽  
pp. 733-784
Author(s):  
G. Le Strange

Khurāsān in the middle ages was far more extensive than is the province of this name in modern Persia. Mediæval Khurāsān extended on the north-east to the Oxus, and included all the districts round Herat which now belong to Afghanistān. On the other hand, the small province of Kūmis, on the northern boundary of the Great Desert, which at the present day is included within the limits of Persian Khurāsān, was of old a separate district, and formed in the time of Mustawfi a province apart.


1954 ◽  
Vol 1954 ◽  
pp. 17-25 ◽  
Author(s):  
J. L. Corbett

There is little doubt that the lowest costs of beef or milk production are achieved when the animals are grazed on pastures from which they obtain most or all of their sustenance. On the other hand the most expensive phase of cattle production is the winter period when stock are usually housed and must be hand-fed. The results from numerous investigations firmly support these assertions. In the large mixed farming area of the North-East of Scotland virtually no grazing is normally available from the middle or end of October until the beginning of May when normal grass growth has resumed.


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