IV.—The Upper Trias of Leicestershire

1913 ◽  
Vol 10 (5) ◽  
pp. 205-215 ◽  
Author(s):  
A. R. Horwood
Keyword(s):  
Black Shales ◽  
The South ◽  
The West ◽  
West Side ◽  
North West ◽  
The North ◽  
Eastern Boundary ◽  
East End

Although the Rhætic beds are not exposed continuously along the eastern boundary of the Keuper outcrop, they have been proved at many points from the River Trent in the north on the Nottinghamshire border to Glen Parva in the south. South of this point there is so much drift, and borings within the Liassic outcrop have been so isolated or shallow, that there is a gap in our knowledge of the intervening ground between the last point and the Rugby district. The Countesthorpe boring, carried to a depth of over 600 feet, encountered Upper Keuper beneath the Drift, with no intervening Rhætics. Commencing in the north in the Gotham district the two outliers are capped above the Red Marl and Tea-green Marl with Rhætic beds, and Lower Lias Limestone (Ps. planorbe zone) above. At Ash Spinney at the south end of the southern outlier, and at the east end of Crownend Wood, Black Shales with Avicula contorta crop out; and on the west side septaria are seen. On the north-west side of the northern outlier at Cottager's Hill Protocardium phillipianum has been found in a well-section near the lane. Rhætic shales are seen in the shafts driven for gypsum works about Gotham.

I 10, 8 and 9

1997 ◽  
Author(s):  
Roger Ling ◽  
Paul Arthur ◽  
Georgia Clarke ◽  
Estelle Lazer ◽  
Lesley A. Ling ◽  
...  
Keyword(s):  
Late Stage ◽  
The South ◽  
The West ◽  
West Side ◽  
South Side ◽  
North West ◽  
The North ◽  
Eastern Boundary ◽  
The One ◽  
Northeast Corner

This complex consists of an atrium-house from which a front room has been separated at a late stage to form an independent shop or workshop. Together they occupy the north-west corner of the insula, the house opening northwards and the shop westwards. Before the shop was separated from it, the house had a relatively broad facade (approx. 14 m.), but the oblique alignment of the insula boundary to the west resulted in a considerable contraction towards the rear. At the southern end of the roofed part of the house, coinciding with the south walls of rooms 10 and 12, the property is only 10 m. wide; and the garden beyond this, thanks primarily to a shift in the line of the eastern boundary becomes even narrower, contracting to less than 8.50 m. As in the Casa del Fabbro, the atrium (1) is set against one of the property boundaries, this time the west rather than the east; but, owing to the greater width of the house, it is broader (from 7.20 to 8.20 m.) and still allows space for a deep room on the east. The impluvium is centrally positioned in relation to the short (south) side. The fauces, however, enters the atrium somewhat off-centre, 3.80 m. from the northeast corner and 2.70 m. from the north-west, presumably in order to obtain three more or less equally sized rooms on the north facade. As the plot contracts toward the rear, this tripartite division becomes more difficult; the outlying rooms, on the west side particularly are uncomfortably narrow and cramped. Of the three rooms on the north front, the westernmost is the one which in the final period had become a shop with an independent entrance (I 10, 9); it had formerly been a corner room opening from the atrium via a doorway immediately adjacent to the fauces, but this doorway was blocked and a new entrance, 2.30 m. wide, quoined in opus listatum, was opened in the west wall (Pl 90). The lava threshold (Fig. 61) points to fittings typical of a shop: a separate pivoted door and vertical planks set overlapping in a groove.

Excavations on Pilsdon Pen, Dorset, 1964–71

1977 ◽  
Vol 43 ◽  
pp. 263-286 ◽  
Author(s):  
Peter S. Gelling
Keyword(s):  
Natural History ◽  
Iron Age ◽  
The South ◽  
The West ◽  
North West ◽  
The North ◽  
Nearest Point ◽  
Daunting Task ◽  
East End ◽  
The Hill

Pilsdon Pen is in west Dorset, very close to the Devon border, some 6 miles north-west of Bridport, and about 5½ miles from the nearest point of the coast (ST 413013). It is a long flat-topped hill, the highest in Dorset, reaching 908 ft above OD, and dominating Marshwood Vale from the north. The hill-fort occupies the south-east end of the Pen, at the north-west end of which there is a small embanked enclosure, much levelled by ploughing, which could be of Iron Age date also. The two nearest hill-forts are Lambert's Castle and Coneys Castle, about 3 and 3½ miles away respectively, which overlook Marshwood Vale from the west (fig. 1).Excavation began in 1964, and continued annually until 1971, all but one of the seasons lasting four weeks. The work was initiated, and largely supported, by the owner of the site, Mr Michael Pinney, of Bettiscombe Manor, to whom archaeology owes a great debt. Mrs Betty Pinney was one of our most skilful excavators, and all those who took part will remember her hospitality. Financial help was also given by the Dorset Natural History and Archaeological Society and by Birmingham University. Among many helpers, to all of whom I am most grateful, I should like to mention in particular my wife, who shouldered the daunting task of keeping the camp supplied, and Mr Jack Wells, of Tanyard Farm, Marshwood, without whose regular assistance the excavation would have taken much longer, and cost a great deal more.

Casa del Fabbro (I 10,7)

2007 ◽  
Author(s):  
Penelope M. Allison
Keyword(s):  
Small Ring ◽  
East Side ◽  
The South ◽  
The West ◽  
Partition Wall ◽  
West Side ◽  
North West ◽  
West Wall ◽  
The North ◽  
North Wall

The doorposts and the walls of the entranceway to this house were coarsely plastered and the pavement was of lavapesta. The walls have been much restored since excavation, prohibiting the identification of any breaches that might provide evidence for disturbance. Outside the entrance, on the west side, is a low, plastered, masonry bench (1.57 m × 0.38 m × 0.42 m), which Elia identified as a seat for waiting clients. Within the entranceway, a few centimetres above the pavement, a number of finds were made. These were all of iron—a large lock, two hooks, a handle, two keys, at least one door latch and numerous studs and nails—and no doubt mainly the fittings for the house door. One of the keys was large and probably a door key. Its discovery here suggests that the occupants were still in residence, or at least had not had the time or inclination to lock up their house, before fleeing from the eruption. A small ring was also found in this entranceway, and was probably a lost finger-ring. This room is closed to the street but almost completely open along its east side onto the entranceway. The walls had a high, pink-plastered socle, to 1.6 m above the pavement, with white plaster above, and the pavement was of tiles and mortar. There are breaches in the west and south walls, possibly the result of post-eruption disturbance. A stairway ran along the north wall, rising from east to west. Underneath was a low partition wall jutting out at right angles from the west wall, to partition off a latrine in the north-west corner. This partition wall post-dates the plaster on the west wall. A line of roof tiles, set into the floor and running from this partition wall to the south jamb on the east wall, is assumed to have been for flushing the latrine. A truncated amphora, with visible organic contents, was set into the pavement in the south-east corner. Other finds from this room, but with no precise provenances, include: two relatively small bronze strap hinges, possibly from furniture; a bronze casseruola; two ceramic jugs; a hoe, probably for gardening; an axehead, probably a woodman’s; and a bronze brooch.

Charles Edward Inglis, 1875 - 1952

1953 ◽  
Vol 8 (22) ◽  
pp. 444-457
Keyword(s):  
The South ◽  
Art Gallery ◽  
The West ◽  
West Side ◽  
The North ◽  
The Right

Charles Edward Inglis was the second surviving son of Dr Alexander Inglis, M.D., M.R.C.S.E., of Auchindinny and Redhall, and of his first wife, Florence, the second daughter of John Frederick Feeney, proprietor of the Birmingham Daily Post, whose family founded the Feeney Art Gallery in that city. The Inglis family of Auchindinny appear first as tenants and afterwards owners of the farm of Langbyres, which adjoins the west side of Murdostoun in the parish of Shotts, Lanarkshire. The first mention of them in connexion with the place is found in the Lord High Treasurer’s accounts for 1543 when John Inglis in Langbyres and James Kneland in Swyntre had to pay £13 6s. 8d. to redeem their movable goods, which had been escheated as a penalty for their absence from the army, mustered by James V to invade England, which was routed at Solway Moss. The estate of Auchindinny, about 730 acres, was purchased in 1702 by one John Inglis, a Writer to the Signet, who had succeeded to Langbyres in 1685. Auchindinny lies about eight miles south of Edinburgh, on the right bank of the North Esk and at the south end of the parish of Lasswade. The house, completed in 1707, is a severe substantial sandstone building. John Inglis had eleven children. One of his grand-daughters, Barbara, co-heiress of Archibald, Laird of Auchindinny, married in 1777 her cousin, Captain, afterwards Admiral, John Inglis, R.N., of Redhall, whose father had left Scotland and settled in Philadelphia as a merchant about 1736. Captain Inglis commanded H.M.S. Belliqueux at the battle of Camperdown. The ship took a conspicuous share in the fighting, there being a hundred and three casualties out of a complement of four hundred and ninety-one, and quite redeemed the character which she had lost in the Mutiny at the Nore a few months earlier. It is said that the Captain was puzzled in the battle by his Admiral’s frequent signals and at last threw his signal book on deck exclaiming, ‘Damn the signals; up wi’ the hellem and gang into the middle o’ it’. He thus anticipated Nelson’s celebrated memorandum that ‘when a captain should be at a loss he cannot do very wrong if he lay his ship alongside of the enemy’.

The armies of the Ṣaffārids

1968 ◽  
Vol 31 (3) ◽  
pp. 534-554 ◽  
Author(s):  
C. E. Bosworth
Keyword(s):  
Ninth Century ◽  
The South ◽  
The West ◽  
Islamic World ◽  
North West ◽  
The Third ◽  
The Core ◽  
The North ◽  
Frontier Region ◽  
Short Time

It is not too much to describe the Ṣaffārids of S‚stān as an archetypal military dynasty. In the later years of the third/ninth century, their empire covered the greater part of the non-Arab eastern Islamic world. In the west, Ya'qūb. al-Laith's army was only halted at Dair al-'Āqūl, 50 miles from Baghdad; in the north, Ya'qūb and his brother 'Arm campaigned in the Caspian coastlands against the local 'Alids, and 'Amr made serious attempts to extend his power into Khwārazm and Transoxania; in the east, the two brothers pushed forward the frontiers of the Dār al-Islām into the pagan borderlands of what are now eastern Afghanistan and the North-West Frontier region of West Pakistan; and in the south, Ṣaffārid authority was acknowledged even across the persion Gulf in ‘Umān. This impressive achievement was the work of two soldiers of genius, Ya'qūub and 'Amr, and lasted for little more than a quarter of a century. It began to crumble when in 287/900 the Sāmānid Amīr Ismā'īl b. Aḥmad defeated arid captured ‘Amr b. al-Laith, and 11 years later, the core of the empire, Sīstān itself, was in Sāmānid hands. Yet such was the effect in Sīstān of the Ṣaffārid brothers’ achievement, and the stimulus to local pride and feeling which resulted from it, that the Ṣaffārids returned to power there in a very short time. For several more centuries they endured and survived successive waves of invaders of Sīstān—the Ghaznavids, the Seljūqs, the Mongols—and persisted down to the establishment of the Ṣafavid state in Persia.

Laconia

1950 ◽  
Vol 45 ◽  
pp. 261-298 ◽  
Author(s):  
J. M. Cook ◽  
R. V. Nicholls
Keyword(s):  
Sea Level ◽  
The Other ◽  
The South ◽  
The West ◽  
Urban Settlement ◽  
West Side ◽  
The North ◽  
The Village

The village of Kalývia Sokhás lies against the base of one of the massive foothills in which Taygetus falls to the plain three or four miles to the south of Sparta (Plate 26, 1). It is bounded by two rivers which flow down in deep clefts from the mountain shelf. The hillside above rises steeply to a summit which is girt with cliffs on all but the west side and cannot be much less than four thousand feet above sea level; this von Prott believed to be the peak of Taleton. Its summit is crowned by the ruins of a mediaeval castle which was undoubtedly built as a stronghold to overlook the Spartan plain; the only dateable object found there, a sherd of elaborate incised ware, indicates occupation at the time when the Byzantines were in possession of Mystra. The location of the other sites mentioned by Pausanias in this region remains obscure, but fortunately that of the Spartan Eleusinion has not been in doubt since von Prott discovered a cache of inscriptions at the ruined church of H. Sophia in the village of Kalývia Sokhás. In 1910 Dawkins dug trenches at the foot of the slope immediately above the village and recovered a fragment of a stele relating to the cult of the goddesses and pieces of inscribed tiles from the sanctuary. The abundance of water in the southern ravine led von Prott to conclude that the old town of Bryseai with its cult of Dionysus also lay at Kalývia Sokhás; but no traces of urban settlement have come to light at the village, and the name rather suggests copious springs such as issue from the mountain foot at Kefalári a mile to the north where ancient blocks are to be seen in the fields.

scholarly journals An ultrabasic pipe in the eastern Sukkertoppen region, southern West Greenland

1980 ◽  
Vol 100 ◽  
pp. 69-73
Author(s):  
R.P Hall
Keyword(s):  
Granulite Facies ◽  
The South ◽  
The West ◽  
West Side ◽  
West Greenland ◽  
North East ◽  
The North ◽  
South West ◽  
Unusual Occurrence ◽  
Anorthosite Complex

An unusual occurrence of ultrabasic material was located in the eastern Sukkertoppen region during the reconnaissance mapping programme of 1977, the findings of which were described by Allaart et al. (1978). It occurs on a small exposure on the west side of a north-pointing peninsula in the middle of the large nunatak Majorqap alangua (65°53'N, 50°40'W), to the north-east of the Majorqaq valley (Hall, 1978, fig. 21). The area is composed predominantly of a suite of granulite facies granitic gneisses which contain numerous enclaves of pyroxene-bearing amphibolites, and locally anorthositic and gabbroic rocks similar to those seen in the Fiskenæsset anorthosite complex (Myers, 1975). The gneisses in the centre af the nunatak are highly irregular in orient at ion, occupying the complex interseclion af closures af at least two major fold phases. A belt af amphibolitcs forms the cliff at the south-west tip af Majorqap alangua. Related rocks occur in arnphibolite facies in the acea around the lakc Qardlit taserssuat immediately to the soulh (Hall, 1978).

GEOLOGICAL FRAMEWORK OF THE GREAT AUSTRALIAN BIGHT

1969 ◽  
Vol 9 (1) ◽  
pp. 60
Author(s):  
R. Smith ◽  
P. Kamerling
Keyword(s):  
Middle Eocene ◽  
Early Stage ◽  
Upper Jurassic ◽  
The South ◽  
The West ◽  
Offshore Area ◽  
North West ◽  
Carbonate Sedimentation ◽  
The North ◽  
Great Australian Bight

Geophysical exploration carried out in the Great Australian Bight since 1966, combined with geological fieldwork in the adjacent land areas, has made it possible to outline the broad geological framework of the area.The "basement" consists of two major units, an offshore extension of the locally metamorphic Cambrian Kanmantoo Group in the south-east and the extension of the West Australian Archaean shield in the north-west. The boundary is thought to follow a trend extending westerly from the Cygnet-Snelling fault zone on Kangaroo Island.In two areas the basement has been downfaulted, thus creating depositional areas for thick sequences of sediments, namely the Elliston trough to the west of Eyre Peninsula and the Duntroon basin, south of Eyre Peninsula and west of Kangaroo Island.The geological setting of the Duntroon basin appears to be comparable with the Otway basin and a Jurassic- Cretaceous age is assumed for the folded sequence of sediments overlying the basement and underlying the Tertiary with angular unconformity. The basin was possibly partially and temporarily closed to the south and open to marine influences from the west.In the Elliston trough the lower part of the section which has low to medium velocity seismic character, is probably Mesozoic, as is evidenced by the Upper Jurassic encountered in its onshore extension. Proterozoic-Cambrian sediments may overlie the basement in the eastern part of the trough. Deformation of the Mesozoic is limited to the mouth of the trough where there is indication of a base- Tertiary unconformity. This trough was probably also open to marine influences to the west.Along the continental margin between the basins and also south of the Eucla basin a thin Mesozoic section, conformably underlying the Tertiary, is probably present, gradually thickening towards the continental slope.In the onshore area Tertiary sedimentation started with local deposition of clastics during the Middle Eocene, which also may have been the case off the Eucla basin, in the Elliston trough and in the Duntroon basin. Carbonate sedimentation took place from the Middle-Upper Eocene onwards, to reach its widest areal extent during the Lower Miocene. A hiatus during the Oligocene may have occurred in the western part of the Bight as is the case in the Eucla basin.Only weak deformation of the Tertiary in the offshore area has been observed. This generally occurs over Mesozoic structures in the Duntroon basin and as draping over topographic basement highs at the mouth of the Elliston trough.No significant hydrocarbon indications are known from the surrounding land areas, but the well-documented bitumen strandings along the coast point to offshore seepages indicating generation of hydrocarbons in the general area.At this stage prospects must be regarded as speculative.although a folded probable Mesozoic sequence forms an objective in the Duntroon basin while prospective Mesozoic-Tertiary section appears to be present in the Elliston trough, where structural evaluation is still at a relatively early stage.

The Bullae of Gobekly-depe

2007 ◽  
Author(s):  
VASIF GAIBOV
Keyword(s):  
Small Group ◽  
The South ◽  
The West ◽  
North West ◽  
The North

This chapter describes the bullae or collection of imprints of seals on clay found at the Gobekly-depe in the Merv Oasis. The majority of bullae from Gobekly were found in the north and west corridors and in the north-west room of the Parthian building, and a few bullae were also recorded in the south courtyard, adjacent to the west corridor, which came in various shapes and sizes. The chapter also describes a small group of bullae found on the floor of the courtyard that showed a scene with figures standing either side of a fire altar, representing a scene of the investiture of a king by a female deity.

Hoboken Ho

2021 ◽  
pp. 65-88
Author(s):  
Ann L. Buttenwieser
Keyword(s):  
New York ◽  
New Jersey ◽  
Feasibility Study ◽  
Hudson River ◽  
The South ◽  
The West ◽  
Professional Help ◽  
West Side ◽  
The North ◽  
Community Trust

This chapter recounts how the author became an evangelist for floating pools by the end of the 1990s. It mentions plans for twenty-five major projects by 1986 that went before the New Jersey Waterfront Commission for approval, from Fort Lee on the north of Hoboken to Bayonne eighteen miles to the south. It also talks about proposals that included parks, marinas, and a continuous waterfront walkway along the west side of the Hudson River. The chapter details how the author won a $25,000 grant from the New York Community Trust to do a feasibility study for the floating project, which in turn brought her to architect Jonathan Kirschenfeld's office to seek his professional help. It describes Kirschenfeld as an earnest man and the very picture of a serious idealist.

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