scholarly journals A Romano-British House near Bedmore Barn, Ham Hill, Somerset

1913 ◽  
Vol 3 ◽  
pp. 127-133
Author(s):  
I. Hamilton Beattie ◽  
W. J. Phythian-Adams

Ham Hill forms the north-western and highest part of an irregular upland overlooking the lowlands of Somerset, some five miles west of Yeovil. The hill is famous for its earthworks, and for many antiquities of the Stone, Bronze, Late Celtic, and Roman periods which have been found upon it. Most of these seem to belong to its western portion, but the south-east corner near Bedmore, or Batemoor, Barn in the parish of Montacute has yielded interesting finds.

1862 ◽  
Vol 152 ◽  
pp. 1019-1038 ◽  

The little town or village of Bovey Tracey, in Devonshire, nestles at the foot of Dartmoor, very near its north-eastern extremity; it is situated on the left bank of the river Bovey, about two miles and a half above the point at which it falls into the Teign, and is about eleven miles from each of the towns Exeter, Torquay, and Totnes*,—bearing south-westerly from the first, north-westerly from the second, and northerly from the last. A considerable plain stretches away from it in a south-easterly direction, having a length of six miles from a point about a mile west of Bovey to another nearly as far east of Newton; its greatest breadth, from Chudleigh Bridge on the north-east to Blackpool on the south-west, is four miles. It forms a lake-like expansion of the valleys of the Teign and Bovey rivers, especially the latter, whose course it may be said to follow in the higher part, where it is most fully developed; whilst the Teign constitutes its axis below the junction of the two streams. Its upper, or north-western portion, immediately adjacent to the village, is known as “Bovey Heathfield,” and measures about 700 acres.


1921 ◽  
Vol 58 (5) ◽  
pp. 215-225 ◽  
Author(s):  
J. S. Flett ◽  
H. H. Read

CAPPING many of the hill-tops of the Buchan district of Aberdeenshire there are extensive spreads of gravel containing pebbles of white quartzite and of flint. Their north-western limit is on the Delgaty estate, near Turrifi, where, at an elevation of 350–400 feet, there is a small patch of quartzite gravel a mile and a half to the north-east of the town. Nearly eight miles to the south, on Windyhills, two miles north-east of Fyvie, a more extensive outlier occurs. These two patches are shown in Fig. 1. The Windyhills spread is nearly a square mile in area, and it occupies the summit of a low flat-topped ridgo at an elevation of 370–400 feet. Like the Delgaty gravels, it is evidently the remains of a deposit formerly much more extensive and reduced greatly in area by denudation. It consists mainly of white quartzite pebbles, flint pebbles, and white clayey sand, and its resemblance to the Delgaty gravels is so close that no doubt has been entertained that they belong to the same period and formation.


1876 ◽  
Vol 9 (1) ◽  
pp. 147-154
Author(s):  
A. H. Schindler

The part of Belúchistán now under Persian rule is bounded upon the north by Seistán, upon the east by Panjgúr and Kej, upon the south by the Indian Ocean, and upon the west by Núrámshír, Rúdbár, and the Báshákerd mountains.This country enjoys a variety of climates; almost unbearable heat exists on the Mekrán coast, we find a temperate climate on the hill slopes and on the slightly raised plains as at Duzek and Bampúr, and a cool climate in the mountainous districts Serhad and Bazmán. The heat at Jálq is said to be so intense in summer that the gazelles lie down exhausted in the plains, and let themselves be taken by the people without any trouble.


1950 ◽  
Vol 82 (3-4) ◽  
pp. 127-148
Author(s):  
Shih-Yü Yü Li

Tibetans inhabit three major regions, Tibet proper, Khams, and A-mdo. Tibet is the region so marked on the maps; Khams is the province marked as Sikang; A-mdo does not exist as a political entity, but is divided into a number of Hsien (counties) in the north-western part of Szechwan, the south-western part of Kansu, and the area inhabited by Tibetans in Ts'inghai or Kokonor. My four years' field experience of Tibetan culture was in A-mdo on the Kansu-Ts'inghai border. My study of Tibetan folk-law, therefore, is based on conditions in A-mdo. The appended translation of “Rules of Punishment for Tibetans” (promulgated by the Manchu Imperial Court in 1733) applies mainly to Tibetans in A-mdo and secondarily to those in Tibet and Khams.


2019 ◽  
Vol 23 (1) ◽  
pp. 83-86
Author(s):  
Soroush Akbarzadeh

The article presents an analysis of the place-names with the formants -(v)īγ/-(w)yq/ and - vīǰ, attested in the South Caspian and the north-western provinces of Iran.


Zootaxa ◽  
2009 ◽  
Vol 2009 (1) ◽  
pp. 1-26 ◽  
Author(s):  
JOACHIM SCHMIDT ◽  
MATTHIAS HARTMANN

The genus Pristosia Motschulsky, 1865 was so far only known to be highly diverse in the North-Western Himalaya and present in the Eastern Himalaya. Only a single female specimen has been documented in the literature from the Nepal Himalaya and was described as P. dahud Morvan, 1994. During a study of comprehensive carabid beetle material collected throughout Nepal, which has been deposited at several museums and private collections, a large number of Pristosia specimens from six species have been identified. The only fully winged species P. crenata (Putzeys, 1873), which is widely distributed in South East Asia, was found near Dailekh and is herewith reported for the Nepalese fauna for the first time. The Eastern Himalayan species P. amaroides (Putzeys, 1877) is reported for the first time in Nepal as well and occurs in Eastern Nepal at several localities east of the Arun river. At least four species occur in the Western and Far Western Nepal Himalaya, of which three are described as new to science: P. glabella sp. n. and P. nepalensis sp. n. from the Api Himal, and P. similata sp. n. from the Saipal Himal. An presumably additional new species is known from the north-western slope of the Dhaulagiri Himal, but is represented by a single immature female specimen only, which does not allow for a sufficient species diagnosis. The male external and genital characters of P. dahud Morvan, 1994 are now described for the first time. This species is considered to be polytypic and the geographic subspecies P. dahud polita ssp. n. is described from the south slope of the Kanjiroba Himal. The species P. atrema (Andrewes, 1926) and P. championi (Andrewes, 1934), which occur in the Kumaon Himalaya close to the Nepalese border, are redescribed based on the examination of the type material. Diagnostic features, especially for the male genitalia of all taxa mentioned above, are figured and a key to the species from Nepal is presented. Instead of a phylogenetic analysis, which is needed for Pristosia but not achievable at present, preliminary species groups for species dealt with are proposed: The Eastern Himalayan P. amaroides species group (monotypic), the P. atrema species group with six species from the Kumaon and Western Nepal Himalaya, the P. championi species group with two species from the Kumaon and Western Nepal Himalaya, and the South East Asian P. crenata species group (monotypic). Based on the distributional and ecological data presented in this study, species of the genus Pristosia with reduced hind wings seem to be absent from the entire Central Nepal Himalaya, and the only Eastern Nepalese species, P. amaroides, prefers largely different habitat conditions compared to the species from Western Nepal. Based on biogeographical hypotheses of other Himalayan carabid beetle genera presented in previous studies by the senior author, the observed species groups of Pristosia are considered to be further examples for Tertiary Tibetan faunal components of the Himalaya. Following a diversification of the genus within the Tertiary of Southern Tibet, speciation occurred and these species groups originated from founder populations that moved into the Nepal Himalaya. The colonization of the geologically younger High Himalaya has taken place independently for each of the terminal groups via different dispersal routes and during different periods of mountain uplift.


2011 ◽  
Vol 17 (1) ◽  
pp. 135-156 ◽  
Author(s):  
Vakhtang Licheli

Abstract The settlement and necropolis of Grakliani Hill are located in Central Transcaucasia, Georgia. Excavations of the settlement on the eastern slope and the necropolis on the south-western part of the hill demonstrated that the site had been occupied between the Chalcolithic and the Late Hellenistic periods. The most interesting remains of buildings belong to 2nd and 1st millennium BC. Several sanctuaries of this period were excavated. A monumental altar was discovered in the eastern part of the settlement. The altar was located in the north-western corner of a building. On its eastern side there was an ash pit with a platform along the northern wall. The platform was used for placing offerings, including a South Mesopotamian seal. An architectural complex of the following period (450-350 B.C) was discovered in the western part of the lower terrace. It consisted of three main rooms and three store-rooms. Burials of various periods were discovered in the western part of the hill’s southern slope. The earliest one is a pit-burial dating to the Early Bronze Age, the latest one belongs to the 2nd century BC. After analyses of the finds several directions of cultural and commercial links were identified: Colchis, Persia, Phoenicia, Mesopotamia, Egypt, Asia Minor.


1953 ◽  
Vol 90 (6) ◽  
pp. 377-387 ◽  
Author(s):  
Gilbert Wilson ◽  
Janet Watson ◽  
John Sutton

AbstractThis note records a number of observations of orientation of current-bedding in the Moine Series of Inverness-shire, Wester Ross and Sutherland, in the North-Western Highlands of Scotland. The foreset beds have been found to have a dominant dip towards the north, thus suggesting that the Currents responsible for the transport of the material forming these beds flowed from the south.


1912 ◽  
Vol 44 (3) ◽  
pp. 699-701
Author(s):  
J. F. Fleet

Harappa is a village, having a station on the North-Western Railway, in the Montgomery District, Panjāb: it is situated in lat. 30° 38′, long. 72° 52′, on the south bank of the Ravi, some fifteen miles towards the west-by-south from Montgomery. The place is now of no importance: but extensive ruins and mounds, one of which rises to the height of sixty feet, indicate that the case was otherwise in ancient times; and it has yielded thousands of coins of the “Indo-Scythians” and their successors. Amongst other objects of interest from this place, there are the three seals, full-size facsimiles of which are given in the accompanying Plate. The original seals are now in the British Museum, in the Department of British and Mediæval Antiquities in charge of Mr. Read. In all three cases, the substance of these seals seems to be a claystone, hardened by heat or some other means. In the originals, the devices and characters are sunk: the illustrations represent impressions from the originals, with the devices and characters reversed, as compared with the way in which they lie in the originals, and standing out in relief. The animal on A has been held to be a bull, but not an Indian bull, because it has no hump: another opinion, however, is that it may be a male deer of some kind. The animal on C has a tail of such a nature as to suggest that this creature cannot be a deer. On A the hind legs were not fully formed; and it is possible that a similar tail has been omitted there.


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