scholarly journals Short Report: A déjeté Levallois tool from Khyber Pakhtunkhwa (Pakistan) and the role it plays in the chronology of the Pleistocene terraces of the Bannu Basin

2020 ◽  
Vol 7 (1) ◽  
pp. 1-10
Author(s):  
Paolo Biagi ◽  
Renato Nisbet ◽  
Romana Haider
Keyword(s):  
Short Report ◽  
Middle Palaeolithic ◽  
The South ◽  
Khyber Pakhtunkhwa ◽  
South Eastern ◽  
Neolithic Site ◽  
South West ◽  
Pleistocene Period ◽  
Definition Of

This paper discusses the importance of the discovery of one déjeté Levallois tool from the surface of a dark grey and black patinated gravel terrace located ca. 500 m south-west of the Neolithic site of Sheri Khan Tarakai in the Bannu Basin (Khyber Pakhtunkhwa, Pakistan), and provides a detailed geomorphological description of the area where it was found. The Neolithic site rests on a large gravelly fan, at present terraced and dismembered by small seasonal streams. Scatters of black varnished pebbles, at the top of a thick ochre silt of possible alluvial origin, cover its surface. Amongst the numerous siliceous gravels forming the deposit, some are of a good quality chert, whose source can be found in the Tertiary Sulaiman Formation. The typological characteristics of the tool, the chert employed for its manufacture, its location and the presence of black patina on its cortex are all important elements that contribute to the definition of the Pleistocene period during which pebble terraces formed. The tool comes from a region where Middle Palaeolithic artefacts had never been found before, though the re-analysis of old collections would suggest their presence as far as the course of the Indus in Lower Sindh. Moreover, its discovery contributes to the study of the south-eastern spread of the Middle Palaeolithic Levallois technique, an important topic that still needs to be fully understood.

scholarly journals Anuran fauna of the Lesotho Highlands in the Khatse Dam catchment area and Jorodane River region

Koedoe ◽  
1996 ◽  
Vol 39 (2) ◽  
Author(s):  
D.E. Van Dijk
Keyword(s):  
Catchment Area ◽  
Wide Spread ◽  
The South ◽  
South Eastern ◽  
South West ◽  
River Region ◽  
Probable Impact ◽  
Phase 1B ◽  
The One ◽  
Reproductive Cycles

Surveys were made of the anuran fauna of the Khatse Dam catchment area in the Lesotho Highlands, and of the region between the Central Mountains and the Thaba Putsoa Range which would be affected by Phase 1B of the Lesotho Highlands Water Scheme, if implemented. The Khatse Dam is at present filling. Seven species of anurans were encountered in the Khatse Dam catchment, and five of them also in the valley to the south-west. Four taxa occur all around central Lesotho, but one, the Gariep toad, has its south-eastern limit on the Drakensberg Escarpment, and another. Gray's frog, shows indications in Lesotho, as elsewhere, of being distinct from the typical taxon. Two taxa are endemic to the mountains of the Lesotho region, the one being more rheophilic and more wide-spread. The remaining anuran, previously unknown in Lesotho, is now recorded from the highly characteristic, strongly rheophilic tadpoles, as Heleophryne. The various available habitats and the associated anurans are reviewed. Features of the reproductive cycles, are noted. Dispersal and isolation are outlined. Reference is made to the most probable additions to the anuran fauna which further collecting might reveal. The probable impact of the Khatse Dam is discussed.

scholarly journals An account of some operations executed at Cape Frio, by the officers and crew of His Majesty's ship algerine, for the purpose of raising a part of the stores, &c. lost in His Majesty's ship thetis

1837 ◽  
Vol 3 ◽  
pp. 266-267
Keyword(s):  
Atlantic Ocean ◽  
Rio De Janeiro ◽  
South Atlantic ◽  
The South ◽  
South Eastern ◽  
South West

The author, who had the command of His Majesty’s ship Algerine, was instructed to take charge of the enterprise commenced by the officers and crew of His Majesty’s ship Lightning, having for its object the recovery of the treasure and stores from the wreck of the Thetis, which, in the month of December 1830, had sunk in a cove to the south-east of Cape Frio. He reached this spot on the 6th of March, 1832, having with him eleven officers and eighty-five men. A certain number of men were appointed to remain on board the ship, which was moored in a harbour two miles off a party of artificers and others were employed at the huts which they inhabited near the Cape; and the rest, nearly thirty-five in number, were stationed at the wreck. The author gives a description of Cape Frio, and of the island of which it forms the south-eastern extremity, and which is an immense promontory of insulated granite jutting into the Atlantic Ocean, sixty miles east of Rio de Janeiro. The cove, in the middle of which the wreck of the Thetis lay, is a square indenture in the cliffs, six hundred feet deep by as many wide. It is surrounded by nearly perpendicular masses of granite, from one hundred to two hundred feet high, and is exposed to the whole swell of the South Atlantic, which sets in with remarkable force in that direction. The weather is singularly variable; and transitions frequently take place in the course of few hours, from perfect stillness to the most tremendous swell. The author states that he has witnessed few scenes in nature more sublime than that presented by the Thetis Cove during a gale of wind from the south-west.

scholarly journals VIII.—On the Relations between the Skiddaw Slates and the Green Slates and Porphyries of the Lake-district

1869 ◽  
Vol 6 (58) ◽  
pp. 167-173
Author(s):  
Henry Alleyne Nicholson
Keyword(s):  
Short Distance ◽  
Lake District ◽  
The South ◽  
Main Area ◽  
South Eastern ◽  
The North ◽  
South West ◽  
Eastern Boundary ◽  
North Western ◽  
Great Mass

In the former portion of this paper, the Tipper or south-eastern boundary of the Skiddaw Slates, in their main area, had been traced from Troutbeck, on the N.E., as far as the head of Buttermere, onthe S.W. From this point (i.e. the north-western end of Honister Crag), the Skiddaw Slates can be traced for a very short distance across Warnscales Bottom. They are still overlaid by the felspathic trap and succeeding band of slates and breccias, which together compose Fleetwith Pike and the S.E. end of Honister Crag, and the relations between the two formations are the same as in the Gatescarth Valley. When however the pass of Scarf Gap on the south-west of Warnscales is reached, the Skiddaw Slates have disappeared and the base of the Green Slate Series now rests upon a great mass ofiatrusive felstone-porphyry (here almost a true syenite) which forms High Crag and High Stile. Though the Skiddaw Slates are absent here, it is interesting to observe that the stratification of the Green Slate Series can be particularly well made out in this region. The rugged hills to the S.E. of Scarf Gap are occupied by a prolongation of the great slaty band of Honister, but the beds have now to a great extent lost their former character, and have assumed very much the mineral aspect of trap, from which however they are easily distinguished by the fact that the bedding, in spite of a rough but well marked cleavage, is unusually distinct. The strata displayed in a number of magnificently moutonné'd crags and bosses, in which they are seen to undulate repeatedly, forming a series of small but well-preserved anticlinals and synclinals, the dips of which are N.N.W. and S.S.E. at angles of from 25° to 35°. The inclination therefore of these beds is only about half as high as that of the Skiddaw Slates in the Gatescarth Valley.

scholarly journals http://habibiaislamicus.com/index.php/hirj/article/view/220

2021 ◽  
Vol 5 (3) ◽  
pp. 57-68
Author(s):  
Sami ur Rahman ◽  
Keyword(s):  
Research Paper ◽  
The State ◽  
The South ◽  
Khyber Pakhtunkhwa ◽  
The Past ◽  
South West ◽  
The Status ◽  
Princely State

The word Dir is derived from Sanskrit language, which means a place of worship or a monastery. The Greek would call Dir as "Goraaye". At some point in the past the word "yaghestᾱn" was used as the name for Dir, Bajaur and Gilgit areas. Dir is comprised of beautiful valleys in the high peaked Hamalyas mountains in the province of Khyber pakhtunkhwa. It was a princely state. It is bounded by Chitral to the northe west, swat to the east, Malakand to the south, Bajaur and Afghanistan to its south west. At the time of independence of Pakistan, the state of Dir was ruled by Nawab shah jehan. Dir was acceded to Pakistan in 1969. It was given the status of district in 1970 and in 1996 it was devided into two districts ,i.e lower and upper Dir. Dir has produced many renowned personalities in the politcs as well as in the religious field. This article belonges to the religious scholars ('ulamᾱ) of District Dir and their remarkable contributions in the field of Fiqa, specially in the Urdu language. Some of these scholars are; Maulana Abdul Ghani, Qazi wali Ur Rahman,Qazi Adusalam, Maulana Hzrat Said, Dr Izaz Ali, Shaikh Abdul haleem,Qazi Hazrat Mahmood,Mulana Abdullah and Mulana Zia Ul Haq. In this research paper introduction of the Ulamᾱ-e-Dir and their services of Fiqa in Urdu language have been mentioned which will help inculcate the readers their outlook and will be an advantageous adition to the research endeavors.

An elephant (Loxodonta africana) survey using dung counts in the forests of the Central African Republic

1991 ◽  
Vol 7 (1) ◽  
pp. 25-36 ◽  
Author(s):  
J. Michael Fay
Keyword(s):  
Central African Republic ◽  
Loxodonta Africana ◽  
The South ◽  
Low Level ◽  
South Eastern ◽  
South West ◽  
Forested Areas ◽  
Line Transects

ABSTRACTIn May and June of 1989 data on elephant (Loxodonta africana) dung density were collected in the main forested areas of the Central African Republic. A total of 147.0 km of line transects (N = 14 transects, = 10.50 km, SD = 3.79) was completed. Dung was recorded in 37.4% of the 294 sectors of 0.5 km each. The overall dung density was estimated to be 266 piles km-2 (= 382, SD = 383.7). The highest dung density was found in the proposed Dzanga-Sangha Reserve in the extreme south-west with 1166 piles km-2 (N = 12 sectors of 0.5 km). The south-eastern forests were found to have an intermediate dung density of 336 piles km-2 (N = 215 sectors of 0.5 km, = 419, SD = 308). In the eastern section of the south-western forests no dung was recorded along survey transects (N = 67 sectors of 0.5 km). These data indicate that elephant populations are still relatively high in the forests of south-western and south-eastern Central African Republic, while the population in the eastern section of the south-western forests has diminished to a very low level.

Geopotential Topographies and Associated Circulation in the South-Eastern Indian Ocean

1962 ◽  
Vol 13 (1) ◽  
pp. 1 ◽  
Author(s):  
K Wyrtki
Keyword(s):  
Indian Ocean ◽  
Internal Waves ◽  
Eastern Indian Ocean ◽  
Surface Currents ◽  
The South ◽  
The West ◽  
South Eastern ◽  
South West ◽  
Surface Circulation ◽  
Current Systems

Geopotential topographies of the surface and several subsurface depths are drawn from the observations on three cruises of H.M.A.S. Diamantina in the waters to the west and south of Australia in 1959 and 1960. The associated circulation is discussed. Surface circulation is found to be in general agreement with the observed surface currents. The subsurface flow between 300 and 1200 m depth indicates an entry of water from the south across 32� S. which turns to the west south of 20� S. Transports in certain current systems and eddies are calculated. The importance of internal waves in the south-west of the region, having amplitudes of more than 100 m, is discussed.

scholarly journals Structure of the bazhenov reservoir and forecast of oil content of the Yu0 productive level of the Bazhenov Formation in the south-eastern regions of Western Siberia

2020 ◽  
Vol 15 (4) ◽  
Author(s):  
S.V. Ryzhkova ◽  
◽  
E.V. Ponomareva ◽  
A.G. Zamiraylova ◽  
◽  
...  
Keyword(s):  
Oil Content ◽  
Western Siberia ◽  
Oil And Gas ◽  
Comprehensive Analysis ◽  
The South ◽  
The West ◽  
Bazhenov Formation ◽  
South Eastern ◽  
The North ◽  
South West

For the South-Eastern regions of the West Siberian oil and gas province, a model of the structure of the Bazhenov reservoir and criteria for selecting areas that are promising for detecting oil accumulations in the productive level of the South-West Bazhenov Formation are proposed. According to the our criteria, the following characteristics of the object of research are given: the thickness of rocks of the Bazhenov Formation, the thickness of rocks with a Corg content > 7%, catagenesis degree of organic matter, the thickness of the underlying and overlying fluid barriers, current reservoir temperatures of rocks and reservoir pressures in the Bazhenov Formation. Based on a comprehensive analysis of the materials that characterize the above criteria, promising zones of two categories are identified. The Central-Nyurol zone is assigned to the 1st category (the most promising), and the North-Nyurol, East-Nyurol, South-Nyurol, West-Parabel, and Ust-Tym zones are assigned to the 2nd category.

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