A Late Minoan III ‘kitchen’ at Makritikhos (Knossos) (Knossos Survey 90)

1959 ◽  
Vol 53 ◽  
pp. 182-193 ◽  
Author(s):  
Sinclair Hood ◽  
Piet de Jong
Keyword(s):  
Ground Level ◽  
Western Boundary ◽  
The South ◽  
Deep Trench ◽  
The North ◽  
Natural Rock ◽  
High Bank ◽  
Small Room ◽  
North End

In the summer of 1951 N. Dadoudis, while digging a deep trench to bury stones from a plot of land belonging to him on the east edge of Makritikhos village, about 250 metres north of the Palace of Minos, found a complete Minoan amphora (Plan, Fig. 5, no. 3). He reported this discovery to the Ephor of Antiquities for Crete, Dr. N. Platon, who invited Piet de Jong, then the School's Curator at Knossos, to examine the area. Excavation revealed a small room, against the east wall of which the amphora had evidently once stood. The room was cleared by Piet de Jong assisted later by Sinclair Hood. To judge from the character of the vases found in it, the room might have been used as a kitchen.The ground on the edge of Makritikhos village here slopes steeply down through a series of terraces to the bed of the Kairatos stream about 40 metres to the east. The ‘Kitchen’ lay just below a high bank, forming the western boundary of the plot of ground, with the natural rock exposed at the north end and Minoan house walls showing in it to the south. There seems to have been a marked slope down towards the north as well as to the east here in Minoan times. The wall a–a (Fig. 2) at the north end of the original trench dug by Dadoudis, of squared limestone blocks measuring up to about half a metre in length and 0–35 thick, lay at a lower level than the Kitchen, although it appeared to be of the same period with it. A roughly constructed wall b–b south of a–a may have supported a terrace marking this change in ground level. The corner d–d of another, presumably contemporary, house built of squared limestone blocks was exposed in the south part of the original trench.

scholarly journals The influence of the Brazil and Malvinas Currents on the Southwestern Atlantic Shelf circulation

Ocean Science ◽  
2010 ◽  
Vol 6 (4) ◽  
pp. 983-995 ◽  
Author(s):  
R. P. Matano ◽  
E. D. Palma ◽  
A. R. Piola
Keyword(s):  
World Ocean ◽  
Deep Ocean ◽  
Western Boundary ◽  
Oceanic Circulation ◽  
Southwestern Atlantic ◽  
The South ◽  
Wind Speeds ◽  
The North ◽  
Brazil Current ◽  
South Brazil

Abstract. The oceanic circulation over the southwestern Atlantic shelf is influenced by large tidal amplitudes, substantial freshwater discharges, high wind speeds and – most importantly – by its proximity to two of the largest western boundary currents of the world ocean: the Brazil and Malvinas currents. This review article aims to discriminate the dynamical processes controlling the interaction between this extensive shelf region and the deep-ocean. The discussion is focused on two broad regions: the South Brazil Bight to the north, and Patagonia to the south. The exchanges between the Brazil Current and the South Brazil Bight are characterized by the intermittent development of eddies and meanders of the Brazil Current at the shelfbreak. However, it is argued that this is not the only – nor the most important – influence of the Brazil Current on the shelf. Numerical simulations show that the thermohaline structure of the South Brazil Bight can be entirely ascribed to steady state, bottom boundary layer interactions between the shelf and the Brazil Current. The Malvinas Current does not show the development of eddies and meanders, but its influence on the Patagonian shelf is not less important. Models and observations indicate that the Malvinas Current not only controls the shelfbreak dynamics and cross-shelf exchanges but also influences the circulation in the shelf's interior.

Matrilineal Kinship among the Kunda

Africa ◽  
1958 ◽  
Vol 28 (3) ◽  
pp. 207-224 ◽  
Author(s):  
J. P. Van S. Bruwer
Keyword(s):  
Western Boundary ◽  
The South ◽  
Administrative District ◽  
Eastern Province ◽  
The North ◽  
Eastern Boundary ◽  
Game Reserve ◽  
Opening Paragraph

Opening ParagraphThe Kunda, a matrilineal Bantu people numbering about 20,000, occupy part of the Luangwa valley in the Eastern Province of Northern Rhodesia. Their country, located within the administrative district of Fort Jameson, stretches along the east bank of the Luangwa between the Lusangazi in the south and the Lukuzi in the north. Its western boundary is the Luangwa river proper; across the river a game reserve, stretching up from the Muchinga range, forms an uninhabited barrier between them and the tribes beyond the mountains. The eastern boundary is less clearly demarcated, but marches with the territory of the adjacent Cewa. To the south and north live the Nsenga and Bisa respectively. All these adjacent tribes are matrilineal.

Transporting Urban Inequality through Public Transit Designs & Systems

2017 ◽  
Vol 16 (4) ◽  
pp. 364-368 ◽  
Author(s):  
Gwendolyn Y. Purifoye
Keyword(s):  
The South ◽  
Large White ◽  
Train Station ◽  
Urban Inequality ◽  
Bus Stop ◽  
Far North ◽  
The North ◽  
Predominantly Minority ◽  
Bus Stops ◽  
North End

Four large, and often overflowing, dumpsters are situated at one of the more than dozen bus stops at the Chicago Transit Authority's (CTA) Red Line 95th Street/Dan Ryan train station. This station is on the city's far south side and the ridership on the buses that board and disembark there and the train is predominantly minority. On a warm or hot day, the smell of bus engines and dumpster contents fill the waiting areas. One 28–year–old Black male passenger (BMP) noted, as he stood at one of the nearly one dozen (no seating available) bus stops at the station, “In the summer it's really horrible because of the smells, flies, and bees.” He also added that as far as he could remember “they've [the bus stop dumpsters] been here my whole life” (June 2012). His experience at the south end of this train line, which also has a majority minority ridership, is starkly different from the waiting experiences on the far north end of the same line, Howard Street, where the ridership is diverse (with a large white ridership). The north end station is surrounded by shops and restaurants, more open waiting spaces, and places to sit to wait for buses that travel through the adjoining bus depot. There are no bus stop benches at the south end station, even though there are over a dozen buses that use that station's depot.

scholarly journals The Rainbow Site, An Unusual Syrup Mill in Gregg County, Texas

2005 ◽  
Author(s):  
S. Alan Skinner
Keyword(s):  
Sugar Cane ◽  
Ground Level ◽  
Archaeological Site ◽  
Cultural Resources ◽  
The North ◽  
North End

The Rainbow site is a historic archaeological site that was recorded during a cultural resources survey of a proposed Wal-Mart SuperCenter site in Longview, Texas. It was first interpreted as the location of an illegal whiskey still, but testing revealed that the furnace had been part of a sugar cane syrup mill. The early 1900s furnace is unusual when compared to other reported furnaces in that the firebox had been constructed below the original ground level and the flue/pan area had walls that were barely 1.5 ft. above the surrounding ground, whereas most furnaces were constructed on level ground and had waist-high walls where workers could stand upright when processing syrup. In addition, a brick vault had been constructed over the north end of the firebox and no other examples of such a feature have been reported from syrup mill furnaces.

Structure du plateau continental armoricain

1975 ◽  
Vol 279 (1288) ◽  
pp. 109-121 ◽  
Keyword(s):  
Ground Level ◽  
Magnetic Anomalies ◽  
Magnetic Survey ◽  
Positive Anomaly ◽  
The South ◽  
The North ◽  
Basement Rocks ◽  
Average Accuracy ◽  
Magnetic Field Model ◽  
History Of

Between 1965 and 1970 there has been conducted, in collaboration with the hydrographic service of the French navy, a magnetic survey of the Armorican continental plateau. The zone, covered with 48000 km of profiles, stretches between the parallels of 46° 10' N and 49° 30' N and between the meridians 4° W and 7° 15' W. Position fixing was carried out by means of Toran, with an average accuracy of 50 m. Maps of the total field intensity, reduced to epoch 1967.5, and the magnetic anomalies have been drawn to the scale 1:250000. The magnetic anomalies have been calculated by means of a magnetic field model defined by Jensen and Cain. Two major zones of anomaly can be identified: a northern one, bounded to the south by the 48° N parallel, with strong relief, where the magnetic anomalies are numerous and include major ones at the entrance to the Channel; a southern zone, with considerably less relief, but where the anomalies present several major directions. Several of these anomalies have been interpreted by three different methods with the intention of determining the depth of the sources of disturbance and of specifying possible relationships between these sources and the structural geology of the Armorican plateau. From the south to the north of the region studied, the floor of the continental plateau appears to be divided into compartments by large SW-NE horst and graben structures of Hercynian age. In each compartment the depth to basement increases from east to west by step-faulting with a NW-SE orientation, such faulting has played a role throughout the geological history of the continental plateau. Finally, it emerges from this study that the magnetic anomalies are, for the most part, related to the major structural and tectonic lines of the metamorphic basement visible at ground level. Several areas of high positive anomaly may be associated with basic intrusions emplaced along the lines of major faults in the basement rocks of the Armorican platform.

The Plans of a New Asylum for East Sussex

1900 ◽  
Vol 46 (195) ◽  
pp. 673-688
Author(s):  
H. Hayes Newington
Keyword(s):  
Water Supply ◽  
County Council ◽  
Western Boundary ◽  
The South ◽  
Railway Station ◽  
Efficient System ◽  
Isle Of Wight ◽  
The North ◽  
General Contour ◽  
Suitable Site

When East Sussex determined a year or two back to build an asylum for its sole use, a Visiting Committee, appointed for the purpose, was fortunate enough to find in the centre of the county a suitable estate which the County Council purchased. It is situated at Hellingly, a village about nine miles north of Eastbourne. The area is four hundred acres, compact, as you will see on the plan, having within 400 yards of its western boundary a railway station which we propose to connect with the main asylum by a full gauge tramway. It slopes gently upwards from the south towards the north, where it attains its highest level of about 130 feet above the sea. The subsoil is most favourable, being, with the exception of two patches of clay, of a sandy or gravelly nature. The water supply is adequate, and the general contour lends itself readily to an efficient system of drainage, which will be bacterial. The views are excellent, extending to the sea and the south downs. It would be difficult to find a more suitable site for an asylum. A sub-committee was authorised to travel about the country to inspect other asylums, I being appointed its chairman. We visited the Hartwood, Lenzie, Gartloch, Hawkhead, Cheddleton, Burntwood, Glamorgan, Dorchester, Isle of Wight, and Chichester Asylums.

Sur la stratigraphie et la tectonique du groupe du Jebel Musa (Rif septentrional, Maroc)

1963 ◽  
Vol S7-V (1) ◽  
pp. 70-79 ◽  
Author(s):  
Michel Durand Delga ◽  
Michel Villiaumey
Keyword(s):  
Upper Cretaceous ◽  
Upper Triassic ◽  
The South ◽  
The North ◽  
Jurassic Limestone ◽  
North End

Abstract The allochthonous Musa group of upper Triassic shale, Jurassic limestone, dolomite, marl, and radiolarite, and Cretaceous to Paleogene clastics lies upon Senonian (upper Cretaceous) autochthonous marl and shale of the Tangier massif at the north end of the Rif mountains in Morocco. The group more closely resembles the formations of the Gibraltar area than nearby formations to the south in Morocco. The significance of the Beliounis flysch, believed to be of Cretaceous to Oligocene age, is unexplained. It may be a remnant of the cover of the Musa group although presence of other facies of the same age in the area contradicts this possibility.

scholarly journals On the anomalous magnetic action of hot iron between the white and blood-red heat

1833 ◽  
Vol 2 ◽  
pp. 164-164
Keyword(s):  
Cast Iron ◽  
The South ◽  
Iron And Steel ◽  
The North ◽  
Magnetic Attraction ◽  
Hard Steel ◽  
Malleable Iron ◽  
Magnetic Action ◽  
Cold Iron ◽  
North End

Finding the attractive power of soft malleable iron and steel for a magnet greater than that of cast-iron and hard steel, the author was desirous of ascertaining the effect of heating these bodies in a furnace, so as to render them perfectly soft, upon their magnetic power. With this view the bars were rendered white-hot, and being placed in the direction of the dip, their powers were found nearly equal. It was however found that there was a point between the white heat, at which all magnetic action was lost, and the blood -red heat, at which it was strongest, at which the iron attracted the needle the contrary way to which it did when cold; viz. if the bar and compass were so placed that the north end of the needle was drawn to it when cold, the south end was attracted during the interval above mentioned. The author then proceeds to detail some further experiments in illustration of this anomalous magnetic action, from which it appears that the quantity of magnetic attraction at a red heat is influenced by the height or depth of the centre of the bar from the compass; and as the natural effect of the cold iron was changed by placing the compass below the centre of the bar, it became a question how far the negative attraction was also changed. To decide, the compass was lowered to within six inches of the bottom of the bar, when the cold iron produced a deviation of 21°, by attracting the south end of the needle. At a white heat its power ceased ; but as this subsided to bright red the negative attraction amounted to 101/2°, the north end of the needle being attracted to the iron; it then gradually returned to due north, and ultimately to 70° 30' on the opposite side.

FARMING IN HAWKES BAY

1955 ◽  
pp. 18-36
Author(s):  
R.H. Scott
Keyword(s):  
Daily Basis ◽  
Western Boundary ◽  
Limited Extent ◽  
The South ◽  
The West ◽  
The North ◽  
Westerly Winds

You are in sunny Hawkes Bay, the word "sunny" having become synonymous with the name Hawkes Bay, and there is justification for this when one examines the sunshine records for the district. This city of Napier enjoys an average of 2,420 hours of sunshine per annum which, if you look at it on a daily basis, is equivalent to just over 6% hours of sunshine per day for every day of the year. Lying to the south-east of the North Island as it does, and protected from the prevailing westerly winds by the Ruahine Ranges on its western boundary, and to a more limited extent from the southerly winds by the hills to the 'south, it escapes much of the cloud that districts to the west of the ranges experience.

scholarly journals The influence of the Brazil and Malvinas Currents on the southwestern Atlantic shelf circulation

2010 ◽  
Vol 7 (2) ◽  
pp. 837-871 ◽  
Author(s):  
R. P. Matano ◽  
E. D. Palma ◽  
A. R. Piola
Keyword(s):  
World Ocean ◽  
Deep Ocean ◽  
Western Boundary ◽  
Oceanic Circulation ◽  
Southwestern Atlantic ◽  
The South ◽  
Wind Speeds ◽  
The North ◽  
Brazil Current ◽  
South Brazil

Abstract. The oceanic circulation over the southwestern Atlantic shelf is influenced by large tidal amplitudes, substantial freshwater discharges, high wind speeds and – most importantly – by its proximity to two of the largest western boundary currents of the world ocean: the Brazil and Malvinas currents. This review article aims to describe the dynamical processes controlling the interaction between the shelf and the deep-ocean. The discussion is focused on two broad regions: the South Brazil Bight to the north, and Patagonia to the south. The exchanges between the Brazil Current and the South Brazil Bight are characterized by the intermittent development of eddies and meanders of the Brazil Current at the shelfbreak. However, it is argued that this is not the only – nor the most important – influence of the Brazil Current on the shelf. Numerical simulations show that the thermohaline structure of the South Brazil Bight can be entirely ascribed to steady state, bottom boundary layer interactions between the shelf and the Brazil Current. The Malvinas Current does not show the development of eddies and meanders, but its influence on the Patagonian shelf is no less important. Models and observations indicate that the Malvinas Current not only controls the shelfbreak dynamics and cross-shelf exchanges but also the circulation in the shelf's interior.

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