Gerga in Caria

1969 ◽  
Vol 19 ◽  
pp. 179-182
Author(s):  
G. E. Bean
Keyword(s):  
Good Deal ◽  
The South ◽  
The West ◽  
North Eastern ◽  
In The Wild ◽  
South Slope ◽  
Mountain Country ◽  
Natural Way

The interesting village-site of Gerga was first described by G. Cousin in BCH XXIV (1900), 28–31. He was followed in 1933 by A. Laumonier, who published two articles in BCH LVIII (1934), 304–7 and LX (1936), 286–97; cf. Les Cultes Indigènes en Carie 446–51. The ruins, now known as Gâvurdamları or Gâvurpazarı, lie in the wild mountain country some 6 km. east-south-east of Eski Çine, above the valley of the Marsyas river. The nearest city is Alabanda 12 or 13 km. to the northwest. Both of the French scholars approached the site in what was then the natural way, from the west and north; but the fine new tarmac road from Çine to Yatağan has now made the approach from the south much easier, and on 6th October, 1968, I visited Gerga from this direction, crossing the Marsyas near the fine old Turkish bridge at Incekemer. The site proves to be a good deal more extensive than had previously been realised. It extends over two hills, which I call the eastern and western, though north-eastern and south-western would perhaps be more accurate. The principal centre, with the very handsome “funerary temple”, the strange statue, the curious pyramidal stelae and other features, is on the south slope of the higher eastern hill, and neither Cousin nor Laumonier seems to have penetrated much, if at all, beyond this.

Note on Testing the Water from the Asklepion Area, Athens

1993 ◽  
Author(s):  
Dora P. Crouch
Keyword(s):  
Drinking Water ◽  
Water Resources ◽  
Detailed Analysis ◽  
Water Samples ◽  
Assistant Professor ◽  
The South ◽  
The West ◽  
South Slope ◽  
Technical University

These tests were performed at the Technical University of Athens, Department of Water Resources, by Assistant Professor Alexandra Katsiri during November-December 1988. The problem she was asked to investigate was in what ways these waters differed from ordinary drinking water in Athens. (I am extremely grateful to her for this gracious assistance.) The waters were gathered from three separate sites in and near the Asklepieion on the south slope of the Acropolis, Athens (Fig. 18.5). Specifically, they are: A. Sacred Spring in Asklepion B. Archaic shaft immediately west of Asklepion C. Byzantine cistern immediately adjacent to B, to the west Table 19.1 gives a detailed analysis of the water samples. The fact that the figures from the three sources differ significantly indicates that the three places derive their water from different channels within the Acropolis. Thus the belief of the workmen on the site that these are different waters has been verified.

The Newton-St.-Loe Pavement

1936 ◽  
Vol 26 (1) ◽  
pp. 43-46
Author(s):  
G. R. Stanton
Keyword(s):  
The South ◽  
The West ◽  
Railway Station ◽  
Late Professor ◽  
Main Road ◽  
Roman Villa ◽  
South Slope ◽  
Viii And Ix ◽  
Great Western Railway

The mosaic pavement illustrated on plates VII VIII and IX was found in a Roman villa at Newton-St.-Loe, near Bath, in 1837–38. It was taken up and relaid at Keynsham Railway Station; in 1851 it was taken up again for the Bristol Museum, but when the Bristol Institution moved into a new museum in 1871 the pavement remained stored away, and was never shown again. Several removals and neglect reduced it to a mere pile of fragments, so that the late Professor F. J. Haverfield, writing about 1906, said that it had perished. In 1930–32 it was, however, brought to light. Plates VIII and IX show pieces assembled on a floor awaiting restoration. The site of the villa, which is of an ordinary corridor type (fig. 4), is just outside, and to the west of, Bath, within a few yards to the east of the bridge carrying the main road to Bristol across the Great Western Railway. Most of it was cut away by the railway, but the site of the outbuilding is said to be marked by the broken surface of the south slope of the railway cutting. There are as yet no modern structures at the place. The pavement has frequently been wrongly called after Keynsham or Saltford.

Les glissements rocheux du versant sud du Layens (Vallee d'Aspe, Pyrenees occidentales)

2000 ◽  
Vol 171 (4) ◽  
pp. 407-418 ◽  
Author(s):  
Richard Fabre ◽  
Christian Desreumaux ◽  
Thomas Lebourg
Keyword(s):  
Lower Cretaceous ◽  
Geodynamic Setting ◽  
Field Observations ◽  
Mechanical Instability ◽  
The South ◽  
Structural Context ◽  
Geological Surveys ◽  
North Eastern ◽  
South Slope ◽  
Two Stages

Abstract Detailed geological surveys carried out recently on the Layens have permitted to redefine the lithostratigraphy and to establish the structure of its south slope where several rockslides have been precisely located. This south slope is composed of a carbonaceous Mesozoic series ranging from the Triassic up to the Lower Cretaceous which is located on the reverse flank of a large overfolded north north-eastern syncline. The lithological and structural heritage, together with its special geodynamic setting, generate many brittle zones which favour the mechanical instability of the slope. On this basis the morphostructural position of the rockslides has been established, some of which are unstable while others are stable. Two stages in the evolution of the rockslides have been deduced from the geomorphology and mapping. These field observations have enabled us to distinguish three different rockslides (A, B, C) which are either deep or superficial. The analysis of the causes of their instability have been considered by taking into account the orientation of the major mechanical discontinuities, inherited from the structural context, as well as the sensitivity to the slipping of Triassic clay formations. The natural causes of the destabilization of the south slope of the Layens have been established for the most active rockslide : the geological surveys permit an evaluation of the volume and the total displacements.

The Flint Gravel Deposit of Orleigh Court, Buckland Brewer, North Devon

1937 ◽  
Vol 74 (7) ◽  
pp. 309-316 ◽  
Author(s):  
Inkermann Rogers ◽  
Brian Simpson
Keyword(s):  
Average Distance ◽  
Good Deal ◽  
Left Bank ◽  
The South ◽  
North East ◽  
The North ◽  
South West ◽  
North Eastern ◽  
Low Levels ◽  
Gravel Deposit

The deposit to be described is situated at Orleigh Court, in the parish of Buckland Brewer, some four miles west of south from Bideford, where it rests unconformably on the steeply dipping Upper Culm sandstones. Its greatest extent is from Orleigh Mill to Yeo Bridge, a distance of about three-quarters of a mile in a northwest to south-east direction, and from this line it extends to the south-west for an average distance of about one-third of a mile, only exceeding that amount to the south of the Higher Lodge. The only extensive section was seen in the Rookery, where 25 feet of material rest on a yellow clay. The highest point reached by the deposit, to the south-west of the Higher Lodge, is about 400 feet above O.D. From this point it slopes to the north-east, extending down to about the 100 ft. contour on the left bank of the River Yeo. It is possible that the north-eastern boundary does not reach such low levels as those indicated on the map, Text-fig. 1, for it is difficult to distinguish the original gravel from relatively recent hill wash; and, without a good deal of trenching or augering, it would not be possible to determine the boundary more closely than has been done in the present work.

Craton-Mobile Belt relations with particular reference to the Mosetse-Matsitama area, north-eastern Botswana

1970 ◽  
Vol 107 (2) ◽  
pp. 113-123 ◽  
Author(s):  
John D. Bennett
Keyword(s):  
Metamorphic Grade ◽  
Granitic Rocks ◽  
Mobile Belt ◽  
Schist Belt ◽  
The South ◽  
The West ◽  
South West ◽  
Metavolcanic Rocks ◽  
North Eastern ◽  
Area North

SummaryThe Pre-Cambrian rocks of north-eastern Botswana comprise two major geotectonic domains: the south-western extremity of the Rhodesian craton, and the surrounding mobile belts– namely the Limpopo Mobile Belt to the south and the Shashi Mobile Belt to the west-southwest. The Mosetse-Matsitama area bears affinity to both these environments and this contribution attempts to assess the relationships of the area within the context of the regional geological framework. The area is underlain by a supracrustal schist belt which is interfolded with an infracrustal basement of gneisses and granitic rocks. The schist belt includes metasedimentary and probably metavolcanic rocks of low metamorphic grade and, therefore, contrasts sharply with the rocks of higher metamorphic grade which comprise the basement. Only in the south-west of the belt does a transitional relationship between the two major units occur. Geographical and geological criteria characteristic of both the major geotectonic environments are described, and it is concluded that the area shows a transition from a cratonic to a mobile belt environment. Involvement in a developing mobile belt would initially affect the infracrustal basement, allowing the supracrustal rocks to retain their cratonic characteristics to a more advanced stage.

V.—The Upper Trias of Leicestershire

1913 ◽  
Vol 10 (2) ◽  
pp. 73-86 ◽  
Author(s):  
A. R. Horwood
Keyword(s):  
Good Deal ◽  
The South ◽  
The West ◽  
North West ◽  
The North ◽  
South West ◽  
Good Feature ◽  
Boulder Clay ◽  
Lower Keuper ◽  
Coal Measures

This district is bounded on the north by the Coalville and Ashby line, on the west and south by the county boundaries, on the east by the Shackerstone and Market Bosworth lines. In the north are exposures of Coal-measures, Permian breccias, and Bunter, which the Trias in turn rests upon unconformably. The Lower Keuper forms a long tract on the west not more than two miles in breadth, forming a good feature, the sandstones giving rise to scarps, whilst the Red Mail occupies the rest of the district to the east. On the south-west beds of sandstone form marked features, which also give rise to bold escarpments, whilst the Red Marl itself constitutes a uniform plateau with little or no variation in heights. There are few exposures in the marls, which on the extreme east are covered by a mantle of Boulder-clay and sands. The River Sence and the Sence Brook, however, cut down to the lower parts of the Red Marl, and a good deal of alluvium fills the valleys to the south. The altitude over most of this ground rises uniformly above 300 feet, and in some parts to over 400, rarely sinking below 250. A ridge of hills is formed by the Orton Sandstone striking north-west and south-east, and another ridge meets it at right angles from Market Bosworth.

Belarusian

2020 ◽  
pp. 1-18
Author(s):  
Sonya Bird ◽  
Natallia Litvin
Keyword(s):  
Eastern Europe ◽  
The Other ◽  
Slavic Language ◽  
The South ◽  
The West ◽  
The North ◽  
North Eastern ◽  
The Republic

Belarusian (ISO 639-3 BEL) is an Eastern Slavic language spoken by roughly seven million people in the Republic of Belarus (Zaprudski 2007, Census of the Republic of Belarus 2009), a land-locked country in Eastern Europe, bordered by Russia to the north and east, Ukraine to the south, Poland to the west and Lithuania and Latvia to the northwest (Figure 1). Within the Belarusian language, the two main dialects are North Eastern and South Western (Avanesaǔ et al. 1963, Lapkoǔskaya 2008, Smolskaya 2011). Two additional regional forms of Belarusian can be distinguished: the Middle Belarusian dialectal group, incorporating some features of North Eastern and South Western dialects together with certain characteristics of its own, and the West-Polesian (or Brest-Pinsk) dialectal group. The latter group is more distinct linguistically from the other Belarusian dialects and is in many respects close to the Ukrainian language (Lapkoǔskaya 2008, Smolskaya 2011). The focus of this illustration is Standard Belarusian, which is based on Middle Belarusian speech varieties. For details on the phonetic differences across dialects, the reader is referred to Avanesaǔ et al. (1963) and Lapkoǔskaya (2008).

scholarly journals Daya Tarik Wisata Rohani Gua Kerep Ambarawa

Media Wisata ◽  
2021 ◽  
Vol 14 (2) ◽  
Author(s):  
T. Prasetyo Hadi Atmoko
Keyword(s):  
Tourist Attraction ◽  
The South ◽  
The West ◽  
Tourist Destinations ◽  
Spiritual Tourism ◽  
Religious Tourism ◽  
The World ◽  
Parking Lot ◽  
South Slope ◽  
The City

Central Jawa Province obviously one of the tourist destinations in Indonesia either nature or historical and cultural attractions. The existence of Mary Cave Kerep Ambarawa also contributes to tourism in Central Jawa as the attraction of spiritual tourism. The objectives of this research are to acknowledge how to access the location of Mary Cave Kerep Ambarawa as well as to recognize how are the facilities that support Mary Cave Kerep Ambarawa. The methods of research being used are observation, interview and book study. Mary Cave Kerep Ambarawa resides in Jl. Tentara Pelajar, Dusun Kerep, Panjang Sub-district, Ambarawa District, Semarang Regency, Central Jawa Province. Geographically Mary Cave Kerep Ambarawa is located on the south slope hill of Ungaran mountain. The attraction of Mary Cave Kerep Ambarawa appeals from its Mary Cave views. It is the highest Mother Mary statue in the world and its inscriptions. Mary Cave Kerep Ambarawa is shaped in an artificial cave with a stacked stone bonded with cement, sand and lime. The cave overlooks to the east and is shaded by tall trees and lush. From one of the caves, there is a statue of Mother Mary Lourdes style without a crown. Viewed from the access, to object of religious tourism in Mary Cave Keep with an area around 5 hectares or more is not stiff. When leaving the city of Semarang the visitor can be able to grab a Yogyakarta line bus. Vice versa, when leaving from Yogyakarta select bus to Semarang, down to Ambarawa terminal. Similarly, when using personal vehicle travel to Semarang- Yogyakarta route, arrive at Ambarawa terminal bus, there is a signpost for the entrance to the tourist attraction, which is the entrance to the west and down to the ramp about 1KM. The facilities are provided in Mary Cave Keep Ambarawa specifically: hall, transit building, and prayer room, parking lot, shops object spiritual, church, food stalls around the area of the Cave, and accommodation, such as hotels and homestay.

scholarly journals The North or the South? Early medieval ceramics decorated with a zoned ornament – the result of local changes or interregional contacts?

2021 ◽  
Vol 73 (3) ◽  
pp. 423-454
Author(s):  
Justyna Kolenda ◽  
Kinga Zamelska-Monczak
Keyword(s):  
Middle Ages ◽  
The South ◽  
The West ◽  
Native Communities ◽  
The North ◽  
North Eastern ◽  
Close Relationship ◽  
North Eastern Part ◽  
Lower Silesia ◽  
South Bohemia

The article underlines the need to re-discuss the prevailing views in archaeological literature on the provenance and transformation stages of completely wheel-turned ceramics decorated with zoned ornament. This class of ceramics was used in the Early Middle Ages (for about 100 years) by communities living in the area of southern Greater Poland and the north-eastern part of Lower Silesia. The previous ideas suggesting a close relationship between zoned ceramics and vessels produced in northern Bohemia are reconsidered, with the internal diversity of zoned ceramics being pointed out. We argue that inspiration in ceramics manufacturing came not only from the south (Bohemia), but also from the north (Pomerania) and the west (the middle Elbe region), and that there were also changes that appeared independently of these impulses in the ceramics production of small, native communities.

US and Russian policies and strategies in the Middle East: Iraq and Syria as a model

2019 ◽  
pp. 220
Author(s):  
Esraa Aladdin Noori ◽  
Nasser Zain AlAbidine Ahmed
Keyword(s):  
Middle East ◽  
East Asia ◽  
Balance Of Power ◽  
Western World ◽  
International Conflicts ◽  
The South ◽  
The West ◽  
The North ◽  
East Region ◽  
Middle East Region

The Russian-American relations have undergone many stages of conflict and competition over cooperation that have left their mark on the international balance of power in the Middle East. The Iraqi and Syrian crises are a detailed development in the Middle East region. The Middle East region has allowed some regional and international conflicts to intensify, with the expansion of the geopolitical circle, which, if applied strategically to the Middle East region, covers the area between Afghanistan and East Asia, From the north to the Maghreb to the west and to the Sudan and the Greater Sahara to the south, its strategic importance will seem clear. It is the main lifeline of the Western world.

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