scholarly journals Phases of Ptolemaic Roman 273-30BC: مراحل العلاقات البطلمية الرومانية 273 ق.م – 30 ق.م

2020 ◽  
Vol 4 (6) ◽  
Author(s):  
Hassan Togun Abdullah, Marwa Habib Hassan
Keyword(s):  
Mediterranean Sea ◽  
Red Sea ◽  
Analytical Method ◽  
Diplomatic Relations ◽  
Gulf Of Suez ◽  
Historical Evidence ◽  
Historical Events ◽  
The West ◽  
The North ◽  
Over Time

This research dealt with the development of Egypt's Ptolemaic relations with Rome and took the appearance of its development and the increasing interest of the Romans in the affairs of Egypt. The Ptolemaic state and its fall in the hands of the Romans year 30 BC, represented by the State of Egypt on the continent of Africa and its borders extending from the Mediterranean Sea in the north to the Gulf of Suez and the Red Sea in the east and the deserts of Libya in the west and Nubia in the south and using the historical and analytical method based on linking historical events and facts with each other and analysis starting from a historical prelude is a presentation of the by collecting historical evidence and linking them together and presenting them correctly in their connotations which enabled the Romans to reach the goal of times the kingdoms of the East, including Egypt, so that they could conquer them by building Diplomatic relations during the early Ptolemaic era under the Treaty of Friendship between Rome and Egypt Over time, it turned into a policy of protection and then a policy of appointing and isolating the Ptolemaic kings, taking advantage of the conflict in the Ptolemaic House. The study recommends the need to study the urban side during that period as well as the cultural aspect.

scholarly journals The Development of Labial Clusters in the Aśokan Rock Edicts

2021 ◽  
Vol 9 (1) ◽  
pp. 160-172
Author(s):  
Yasuko Suzuki
Keyword(s):  
Consonant Clusters ◽  
The West ◽  
North West ◽  
The North ◽  
Over Time

The original range of consonant clusters in Indo-Aryan reduced significantly over time, developing into geminates, homorganic nasal-stop clusters, and sonorant-h clusters in Middle Indo-Aryan. Early Middle Indo-Aryan, as represented in the Aśokan inscriptions, however, still maintained the original clusters, or what appear to be transitional stages of the extensive changes. Salient among those cluster changes that are observed in the Aśokan inscriptions are the changes tm, tv> tp and dv > db in Girnār in the west; sm, sv > sp in Shāhbāzgaṛhī and Mānsehrā in the north-west; and mh > mbh in Kālsī in the north and in Dhaulī and Jaugaḍa in the east. The idiosyncratic nature of these changes lies in the development of a stop from m or v, where the more usual changes would be loss or assimilation of m after a stop and of v after a stop or a sibilant, while sm and hm would normally change to mh. This paper examines the manner assimilation of the “labial” clusters (that is, the clusters with m or v that normally do not incur assimilation of the adjacent consonant) in the Aśokan Rock Edicts. It discusses the conditions, the motivation, the course of the change of m/v to a labial stop, and the dialectal differences associated with this change.

Some Eighteenth Century Ferryhouses in Appin, Lorn, Argyll: the Development of the Single-Storeyed Mortared Stone Cottage in the West Highlands

1997 ◽  
Vol 77 ◽  
pp. 243-289 ◽  
Author(s):  
Euan W. MacKie
Keyword(s):  
Eighteenth Century ◽  
Architectural History ◽  
Historical Evidence ◽  
The West ◽  
The North ◽  
North Side ◽  
Piped Water ◽  
History Of ◽  
The One ◽  
Made In

The evolution of the single-storeyed mortared stone cottage in the western highlands of Scotland seems to mirror that of the upper strata of late seventeenth and eighteenth century clan society in the region, and in particular to reflect a little of the disintegration of that society after the two failed Stuart uprisings and its consequent gradual integration with the lowland economy. An analysis of the architectural history of the Ferry House (let to the ferryman as a combined inn and home for his family) at Port Appin provides a foundation for the survey. The earliest part of the building, probably thatched, may well date from the 1740s but already it had lintelled hearths with flues in each gable wall - a lowland urban feature. A major extension with a slate roof was built in about 1770 and the earlier part was probably also slated at this time and subdivided inside to provide rooms for wealthier guests. Thereafter only relatively minor internal improvements were made, in the newer half, until the early 1950s when piped water was introduced and a separate bathroom and kitchen built. The cottages were sold to incomers not long after.A study of other ferries in the area confirms that mortared cottages almost identical to those in Port Appin, and in identical situations, are still to be found at two of these. The one on the south side of the abandoned Rugarve ferry over Loch Creran can also be dated to between about 1750 and 1770 from historical evidence. Also at Rugarve, on the north side, are the remains of a more primitive thatched drystone cottage, probably an early ferry house, which is smaller than the others and lacks hearths with chimneys.

scholarly journals The Cowie Line

2006 ◽  
Vol 135 ◽  
pp. 119-161
Author(s):  
Gordon J Barclay
Keyword(s):  
Second World War ◽  
World War ◽  
The West ◽  
North East ◽  
The North ◽  
Complete Survey ◽  
Large Groups ◽  
The Town ◽  
Second World ◽  
Over Time

The Cowie stop line, running west from the town of Stonehaven, the county town of the historical county of Kincardineshire, some 19km south of Aberdeen, has been recognized for some time as a well-preserved example of a Second World War anti-tank obstacle, but has not hitherto been described in detail. Its purpose was to stop any German force landing in the north-east penetrating into Angus and further south. To work effectively the line was extended to the west, by defences at the Bridge of Dye (on the Strachan–Fettercairn road) and the Devil’s Elbow (on the Braemar–Blairgowrie road) and planned demolitions on the Inverness–Perth road and railway. It originally comprised a dozen pillboxes, over 5km of anti-tank barrier, eight small and one large groups of anti-tank cubes and other defensive features. This paper outlines the strategic background, how the Cowie Line fitted into it, how the Line was constructed, and how its intended function changed over time. The results of the first complete survey of the surviving remains are also presented.

Studies in the Dialect of Basilicata

PMLA ◽  
1915 ◽  
Vol 30 (4) ◽  
pp. 788-820
Author(s):  
Alfonso de Salvio
Keyword(s):  
Mediterranean Sea ◽  
Southern Italy ◽  
The West ◽  
The North ◽  
The Mediterranean ◽  
Territorial Division

Basilicata is the name of that territorial division of Southern Italy which is now known as the province of Potenza and which formed a part of the ancient Lucania. It is bounded on the north by the province of Foggia, on the northeast by the provinces of Bari and Lecce, on the east by the province of Cosenza, and on the west by the Mediterranean sea and the provinces of Salerno and Avellino. It has a population of about 512,000 inhabitants and comprises the circondari of Lagonegro, Matera, Melfi, and Potenza. The region is mountainous and the population is given largely to agriculture and sheep-raising. Although centrally located, the province possesses no mercantile towns of any great importance. Many objects of antiquity were discovered in this region: inscriptions, vases, fragments of statues, medallions, and two bronze tables, known as the Heraclean Tables, now in the Naples Museum.

General Geology

1995 ◽  
Author(s):  
K. O. Emery ◽  
David Neev
Keyword(s):  
Red Sea ◽  
Dead Sea ◽  
Strike Slip ◽  
The South ◽  
The West ◽  
The North ◽  
Central Segment ◽  
Crystalline Crust ◽  
Major Fault ◽  
The Dead

The Dead Sea occupies a linear down-dropped region between two roughly parallel faults along the central segment of the major northsouth- trending crustal rift that extends about 1,100 km from the Red Sea through the Gulf of Elath to Turkey. This rift or geosuture separates the Arabian crustal sub-plate on the east from the Sinai one on the west. An origin as early as Precambrian is possible (Bender, 1974; Zilberfarb, 1978). Crystalline crust along the north-south trough of the Sinai sub-plate is about 40 km thick in contrast with a thickness of half as much above ridges along both flanks (Ginsburg and Gvirtzman, 1979). Toward the north the ridges appear to converge (Neev, Greenfield, and Hall, 1985). Since the Miocene period the Arabian plate has moved north about 105 km relative to the Sinai plate. This sort of crustal movement along either side of a rift is termed strike-slip faulting. One result of it was the opening of the Red Sea relative to the Gulf of Suez. The Dead Sea graben, a down-dropped block between two roughly parallel faults, occupies the central segment of the long crustal rift. The boundary between these is rather sharp along the east shore of the sea (Frieslander and Ben-Avraham, 1989). Actual post-Miocene movement was along not just a single major fault but was distributed among numerous sub-parallel faults that form a 100-km-wide belt in which movements were transferred from one fault to another (Eyal et al., 1981; Gilat and Honigstein, 1981). Recent movements have occurred along the south segment of the north-south-trending Arava fault south of the Amazyahu transverse fault (Zak and Freund, 1966). These strike-slip movements probably did not continue after Miocene along the main East fault of the Dead Sea, which is the north extension of the Arava wrench fault. In contrast, recent movements have been present along the north-northeast- trending Jordan or Dead Sea fault (Ben-Menahem et al., 1977, fig. 1). The movements extend south from east of Jericho in the north along the base of the west submarine slope of the sea and the elongate salt diapir of Mount Sedom as far as the Amazyahu fault in the south.

Submarine gravity measurements in the Atlantic Ocean, Indian Ocean, Red Sea and Mediterranean Sea

1957 ◽  
Vol 239 (1217) ◽  
pp. 202-213 ◽  
Keyword(s):  
Indian Ocean ◽  
Atlantic Ocean ◽  
Mediterranean Sea ◽  
Red Sea ◽  
North Atlantic ◽  
Isle Of Wight ◽  
The North ◽  
Gravity Measurements ◽  
The Indian Ocean ◽  
The North Atlantic

The results are given of fifty-eight gravity measurements made at sea in H. M. Submarine Acheron between April and October 1955. Of these, six lie in the North Atlantic, eight in the South Atlantic and thirty-seven in the Indian Ocean. The remainder are in the Red Sea (four), the Mediterranean Sea (two) and off the Isle of Wight (one).

Chronological list of expeditions and historical events in northern Canada. VI. 1821–45

Polar Record ◽  
1972 ◽  
Vol 16 (100) ◽  
pp. 41-61 ◽  
Author(s):  
Alan Cooke ◽  
Clive Holland
Keyword(s):  
Rocky Mountains ◽  
Fur Trade ◽  
River Delta ◽  
Rich Country ◽  
Historical Events ◽  
The West ◽  
Northern Canada ◽  
North West ◽  
The North ◽  
Yukon River

In this instalment of our list, we see that the Hudson's Bay Company, under the shrewd direction of its overseas governor, George Simpson, quickly recovered from its exhausting struggle with the North West Company and, strengthened by amalgamation with its rival in 1821, began vigorously to push into unknown country both west and east. In the east, the Ungava venture was an attempt, mainly unsuccessful, to develop a fur trade in the interior of the Quebec-Labrador peninsula. And in the west, the exertions of a few hardy men opened the fur-rich country of the Liard River and its tributaries, the Peel River and the region of the Mackenzie River delta, and crossed the Rocky Mountains to the upper drainage of the Yukon River.

scholarly journals Seasonal dynamics of phytoplankton and bacterioplankton at the ultra-oligotrophic southeastern Mediterranean Sea

2021 ◽  
Author(s):  
Tom Reich ◽  
Tal Ben-Ezra ◽  
Natalya Belkin ◽  
Anat Tsemel ◽  
Dikla Aharonovich ◽  
...  
Keyword(s):  
Mediterranean Sea ◽  
Red Sea ◽  
Seasonal Dynamics ◽  
Eastern Mediterranean ◽  
Western Mediterranean ◽  
Bacterial Productivity ◽  
The North ◽  
Chemical Conditions ◽  
South Pacific Gyre ◽  
Physical And Chemical

The Eastern Mediterranean Sea (EMS) is an ultra-oligotrophic, enclosed basin strongly impacted by regional and global anthropogenic stressors. Here, we describe the annual (2018-19) dynamics of phyto- and bacterioplankton (abundances, pigments and productivity) in relation to the physical and chemical conditions in the photic water column at the offshore EMS water (Station THEMO-2, ~1,500m depth, 50km offshore). Annual patterns in phytoplankton biomass (as chlorophyll a), primary and bacterial productivity differed between the mixed winter (January-April) and the thermally stratified (May-December) periods. Prochlorococcus and Synechococcus numerically dominated the picophytoplankton populations, with each clade revealing different temporal and depth patterns, while pico-eukaryotes (primarily haptophytes) were less abundant, yet likely contributed significant biomass. Integrated primary productivity (~32 gC m-2 y-1) was lower compared with other well-studied oligotrophic locations, including the north Atlantic and Pacific (HOT and BATS observatories), the western Mediterranean (DYFAMED observatory) and the Red Sea, and was on-par with the ultra-oligotrophic South Pacific Gyre. In contrast, integrated bacterial production (~11 gC m-2 y-1) was similar to other oligotrophic locations. Phytoplankton seasonal dynamics were reminiscent of those at BATS and the Red Sea, suggesting an observable effect of winter mixing in this ultra-oligotrophic location. These results highlight the ultra-oligotrophic conditions in the EMS and provide, for the first time in this region, a full-year baseline and context to ocean observatories in the region.

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