scholarly journals Coping measures not enough to avoid loss and damage from drought in the North Bank Region of The Gambia

2013 ◽  
Vol 5 (4) ◽  
pp. 467 ◽  
Author(s):  
Sidat Yaffa
1977 ◽  
Vol 15 (4) ◽  
pp. 651-656 ◽  
Author(s):  
James Kingsland

The SettingThe rumble of military jeeps throughout the continent has obscured the fact that there are still a few places where lively elections are held from time to time. Before the rash of coups, and even in several countries with a dominant party, there were local opportunities for intensive competition. Where electoral politics still exist today, groups which might not carry much national weight have the chance to win a slice of the political system at the local level. Such a case was the 1975 election of the chief or seyfo for the Lower Saloum District which is part of the McCarthy Island Division on the north bank of the Gambia River. The three largest ethnic groups here are the Olof, the Mandinka, and the Fula.


2005 ◽  
Vol 12 (4) ◽  
pp. 508-512 ◽  
Author(s):  
Bonto Faburay ◽  
Susanne Munstermann ◽  
Dirk Geysen ◽  
Lesley Bell-Sakyi ◽  
Ansumana Ceesay ◽  
...  

ABSTRACT Using the MAP1-B enzyme-linked immunosorbent assay, we tested 1,318 serum samples collected from sheep and goats at 28 sites in the five divisions of The Gambia to determine the Ehrlichia ruminantium seroprevalence rates and to assess the risk for heartwater. About half (51.6%) of 639 sheep were positive, with seroprevalence rates per site varying between 6.9% and 100%. The highest seroprevalence was detected in the western part of the country (88.1% in the Western Division and 62.1% in the Lower River Division). Sheep in the two easterly divisions (Central River and Upper River divisions) showed the lowest seroprevalence of 29.3% and 32.4%, respectively, while those in the North Bank Division showed an intermediate prevalence of 40.6%. In goats, less than one-third (30.3%) of 679 animals tested were positive. The highest seroprevalence was detected in goats in the North Bank Division (59%) and Western Division (44.1%). Goats in the Lower River Division showed an intermediate level of 21.9%, whereas the lowest rates were found in the eastern part of the country (4.8% in the Central River Division and 2.3% in the Upper River Division). At nearly all sites, seroprevalence rates were higher in sheep than in goats. The results show a gradient of increasing heartwater risk for susceptible small ruminants from the east to the west of The Gambia. These findings need to be taken into consideration when future livestock-upgrading programs are implemented.


2012 ◽  
Vol 57 (13) ◽  
pp. 1578-1589 ◽  
Author(s):  
DaiDu Fan ◽  
GuoFu Cai ◽  
Shuai Shang ◽  
YiJing Wu ◽  
YanWei Zhang ◽  
...  

1940 ◽  
Vol 5 (4) ◽  
pp. 334-335
Author(s):  
Vladimar Alfred Vigfusson

In recent years, the attention of some archaeologists has been directed to the Canadian Northwest with the expectation of finding some evidence or indication of the early migrations of man on this continent. That man reached North America by Bering Strait from Asia, is generally accepted, but the theory that the migrations took place in late Pleistocene times and by way of an open corridor between the Keewatin ice and the Rockies, requires confirmation. It is significant that Folsom and Yuma points from Saskatchewan, described by E. B. Howard, were found mainly in areas bordering the ancient glacial Lake Regina.As a further contribution to this problem, it seems desirable to present a brief description of a carved stone relic found in gravel in central Saskatchewan about three years ago.The stone was found about seven miles southeast of the town of D'Arcy in a gravel pit located on Sec. 9, Tp. 28, Rge. 18, W. 3rd Meridian, on the north bank of a ravine running east into Bad Lake.


Africa ◽  
1965 ◽  
Vol 35 (2) ◽  
pp. 125-142 ◽  
Author(s):  
Claude Meillassoux

Opening ParagraphAccording to a partial census taken in 1960, Bamako city has about 130,000 inhabitants. Small by Western standards, it is still by far the largest city in Mali. At the time of the French conquest Bamako had only between 800 and 1,000 inhabitants; it was the capital of a Bambara chiefdom, grouping about thirty villages on the north bank of the Niger river, with a total of about 5,000 people. The ruling dynasty was that of the Niaré, who, according to their traditions, came from the Kingi eleven generations ago (between 1640 and 1700). For defence against the neighbours and armed slave-raiders fortifications were built around the town and a permanent army of so-fa (horsemen) was raised. Soon after its foundation Bamako attracted Moslem Moors from Twat who settled as marabouts and merchants under the protection of the Niaré's warriors. Among them, the Twati (later to be called Touré) and the Dravé became, alongside and sometimes in competition with the Niaré, the leading families.


1971 ◽  
Vol 51 (2) ◽  
pp. 177-239 ◽  
Author(s):  
G. J. Wainwright ◽  
J. G. Evans ◽  
I. H. Longworth

SummaryExcavations in 1969 within a 35-acre enclosure at Marden on the north bank of the River Avon in the Vale of Pewsey confirmed its association with the Grooved Ware ceramic style and its superficial resemblances to the Durrington Walls enclosure ten miles downstream. A survey of the enclosure produced an unusual plan bounded by a bank with an internal ditch and on the south side by the River Avon itself, whilst the position of the Hatfield Barrow was established by geophysical means. Within the north-entrance causeway a small circular timber structure was recorded in a comparable position to the much larger building at Durrington Walls.


2021 ◽  
pp. 63-71
Author(s):  
Dominic Perring

The archaeology of the first permanent settlement of London is described. New roads were laid out c. AD 48 leading to a site that may have served as a supply-base on the north bank of the Thames. This was set out following a grid-plan around a central area where the forum was later established. Various features illustrate the importance of the managed traffic of military supplies. The topographic, ritual, and political importance of the Thames crossing at London Bridge is stressed, and the evidence of foundation burials and deposits associated with the early layout of the settlement summarized.


Author(s):  
Peter Thomson

The Barguzin River flows out of the Barguzin Mountains, through the town of Barguzin and then the coastal community of Ust-Barguzin before it finally loses itself in a broad cove of Baikal known as Barguzin Bay. The only way across the river for miles upstream from the lake is a ramshackle little wooden ferry with a tiny, corrugated steel shed with a wood stove in it and room on its deck for about half a dozen cars. The ferry slips noiselessly away from the end of the road on the south bank, and looking west toward the lake, two ghostly, rusting timber loading cranes loom on the horizon while the river spills over into a grassy marsh on its north bank. Turning back to the east, there’s a small motorboat laboring to get upstream—laboring because it’s attached to a tow rope, which is attached to the ferry. The ferry, it turns out, is just a hapless little barge, at the mercy of the river without the guidance of the motorboat pilot on the other end of the towline. Our crossing takes less than five minutes, and connected to it by nothing but that single strand, the pilot directs the barge into place perfectly on the far side. But the deckhand fails to secure it, the ferry swings wide in the current, spins ninety degrees, and slams butt-end into the dock. The pilot scowls as he turns the motorboat around and uses its blunt bow, covered in a tractor tire, to push the barge back into place, where the deckhand finally lashes it to the dock. The Barguzin is Baikal’s third largest tributary, after the Selenga to the south of here and the Upper Angara to the north. It carries about six percent of the water flowing into the lake, along with migratory fish like omul and sturgeon, born in the shallow gravel beds upriver before wandering downstream to spend most of their lives in the lake. And even though it flows through only two towns between its headwaters and the lake, the Barguzin carries a significant pollution load into Baikal, as well, especially organic chemicals from timber operations.


1902 ◽  
Vol 9 (1) ◽  
pp. 8-16 ◽  
Author(s):  
Canon T. G. Bonney

It has often occurred to me during my Alpine wanderings that masses of earthy material containing boulders are too readily identified as moraines. That the latter exist, both here and in other mountain regions, no one would for a moment dispute, but deposits, sometimes very closely resembling till, may be produced in other ways. One is by a bergfall. The result of this in some cases, as at Goldau, Plurs, near San Vito (Ampezzo road), or the Col de Cheville, can be easily recognized; but when the fallen material consists largely of shale and friable rock, when there is a certain admixture of boulders from a distance (formerly perched blocks), its origin is not so readily determined. The enormous mass of débris on the north bank of the Rheinthal, between Chur and Ilanz—a mass which extends from Digg, through Flims, to rather beyond Laax, consisting of earthy stuff, probably mainly smashed shale or slate, and of boulders, apparently limestone—is regarded as bergfall by the Swiss geologists, and yet any section in it might readily be taken for moraine. Even more moraine-like in general aspect are the singular mounds of débris in the valley of the Rhone near Sierre.


1955 ◽  
Vol 87 (6) ◽  
pp. 241-245 ◽  
Author(s):  
W. W. Judd

On February 13, 1954 a heavy infestation of small galls was noted on a growth of willow shrubs (Salix sp.) in London Township about a mile north of London, Ontario. The exact location was on the north bank of the North Branch of the Thames River about 100 yards west of the bridge by which Adelaide Street crosses the river. The bushes were crowded along the bank and several of them had their lower branches under water and their roots extending well out into the mud of the river. The galls were one-eighth to three-eighths of an inch long (Fig. 1) and were roughly spherical to oval in shape. The bark of a gall was scarred by shallow furrows running along its length. At its upper end each gall bore the scales of a withered bud or an oval scar from which the scales had fallen. Flanking the scar were two rounded swellings of incipient buds. Many of the galls were separatelv developed along the twigs, being well apart from one another, hut in some cases they were crowded against one another so that three or four galls occupied one inch of the length of the twig, and in several instances a number of adjacent galls had coalesced to form an irregular swelling one or two inches long, along the length of a twig. In the key to insect galls of willow in Felt (1940) the galls were identified as scarred willow galls caused by the gall fly Phytophaga tumidosae (Felt).


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