Cone Cultures in the Wensum Valley

1916 ◽  
Vol 2 (2) ◽  
pp. 194-209
Author(s):  
W. G. Clarke ◽  
H. H. Halls ◽  
J. E. Sainty

Early this year we discovered a station, apparently with a homogeneous culture, on an arable field in the parish of Hellesdon, about half-a-mile above Norwich. The field, which has an area of about 12 acres, is on the north side of the river Wensum, from which it is about 74 yards distant at the south-east corner of the field, and 150 yards distant at the south-west corner. Between the field and the river is alluvium 12 ft. above O.D., and the field is 2—3 ft. higher. Flint implements, flakes and potboilers are very abundant on the lower part of the field, thin out rapidly on the higher part, and occur sporadically on the more elevated ground in the immediate vicinity.Several thousand cones, flakes and chips were examined on the spot, but the number of implements retained was 482. The flint of which they are made is easily divisible into three groups.

Archaeologia ◽  
1887 ◽  
Vol 50 (2) ◽  
pp. 251-262
Author(s):  
Thomas F. Kirby

The Priory of St. Andrew, at Hamble, near Southampton, was a cell to the Benedictine abbey of Tyrone (Tirun or Turun), in La Beauce, a district southwest of Chartres, included in the old province of Orléannois. In the Monasticon and Tanner's Notitia it is called a Cistercian abbey, but this is a mistake, and so is the statement in the Notitia that the priory was annexed to New College, Oxford. The priory stood on a “rise” or point of land.—“Hamele-en-le-rys” or “Hamblerice” is its old name—at the confluence of the Hamble river with southampton Water, opposite Calshot castle. Hamble gets its name from Hamele, a thane of the Saxon Meonwaris. Leland calls the place “Hamel Hooke.” The priory church of St. Andrew is now the parish church. It was rebuilt by winchester college in the early part of the fifteenth century, and consists of channel and nave, to which a south aisle was added five or six years ago, and a tower with three bells. There are scarcely any traces above ground of the priory buildings. Like those of the Benedictine convent of St. Swithun, at Winchester, they stood on the south and south-west of the church, so that the graveyard, as at Winchester, is on the north side of the church.


Author(s):  
Donovan Kelley

0-group bass were sampled from the shallow creeks of the Tamar and Camel estuaries at regular intervals from May to September in 1981 to 2000 to measure relative year-class abundance. From 1989 onwards classes were generally strong, especially those of 1989, 1992 (Tamar only), 1995 and 1998. Sampling at age-4, before departure from the nursery at the onset of adolescent movements, gave broadly similar relativities. Numbers were greater, and growth faster, in the Tamar than in the smaller and cooler Camel. Temperature was an important factor in both abundance and growth. Occasional major differences in abundance between the two estuaries were reported. Factors which might bias the age-4 result are considered. Other estuaries on the south side of the south-west peninsula, sampled less frequently, reflected Tamar abundances; others on the north side reflected Camel abundances. Limited analysis of stomach contents of older juvenile bass often present in the same habitats revealed no evidence of cannibalism on 0-groups. The shallow creeks of the Tamar and Camel were deserted in winter but a deeper creek on the Taw, frequented throughout winter, was sampled monthly in the 1982–1996 winters to measure losses, if any, in cold periods. In the mainly mild winters, losses were infrequent and small except in the five-week cold spell of early 1986, when the 1985 class suffered an estimated 58% loss in the Taw and possible total loss in the Camel and the Tamar. Sudden heavy flooding of the estuaries caused no apparent losses when they occurred in late summer and autumn but might be damaging if they occur soon after post-larvae arrive.


1962 ◽  
Vol 3 (1) ◽  
pp. 255-256

ExcerptFossil collections have been obtained from a large number of localities in the Girvan area. Most of them have been referred to in the text, but those described below are localities from which figured material and types have been obtained.(a) AUCHENSOUL LIMESTONE AND CONFINIS FLAGS(1) Red mudstones and limestone breccias exposed on the south bank of the River Stinchar, 100 yards east of the bridge leading to Auchensoul Farm, 1i88 miles out of Barr on the Pinmore road (Auchensoul Limestone and Mudstones, Auchensoul Bridge).(2) Brown- and yellow-weathering calcareous confinis siltstones exposed on the hillside, 100 yards west of Struit Well, 300 yards west-north-west of Kirkdominae ruins on the north side of the Stinchar Valley, 1i89 miles west of Barr (confinis Flags, Kirkdominae Hill).(3) Brown-weathering calcareous confinis siltstones exposed in the bank of the pathway leading from the old limekiln to the quarry excavated in Stinchar Limestone, 450 yards west-south-west of Minuntion Farm on the north side of the River Stinchar and about 1i89 miles north-east of Pinmore bridge (confinis Flags, Minuntion).(4) Yellow-weathering, pebbly siltstones and impure nodular limestones transitional from confinis Flags to Stinchar Limestone, exposed on the eastern side of the water-filled quarry 300 yards south-west of Bougang Farm, 3 miles east of Ballantrae on the ColmoneU road (top of the confinis Flags, Bougang).(b) STINCHAR LIMESTONES AND SUPERSTES MUDSTONES (1) Mudstones with nodular limestones exposed on the north bank of the Water of Gregg, half a mile east of its junction with the


1980 ◽  
Vol 99 ◽  
pp. 43-49
Author(s):  
J.R Ineson

In south-western Peary Land a thick carbonate dominated sequence of Early to Late Cambrian Age conformably overlies the Early Cambrian Buen Formation, and is overlain, unconformably, by the Wandel Valley Formation of Early-Middle Ordovician age (Peel, 1979; Palmer & Peel, 1979). This sequence is subdivided into the Brønlund Fjord Group and the overlying Tavsens Iskappe Group (Peel, 1979; Ineson & Peel, this report). The Brønlund Fjord Group characteristically forms resistant bluffs along the north side of Wansel Dal from J. P. Koch Fjord in the west to Independence Fjord (fig. 20) in the east. The Tavsens Iskappe Group is confined to western areas by the south-easterly overstep of the Wandel Valley Formation.


1932 ◽  
Vol 69 (5) ◽  
pp. 209-233 ◽  
Author(s):  
G. D. Osborne

THE Carlingford-Barnave district falls within the boundaries of Sheet 71 of the Ordnance Survey of Ireland, and forms part of a broad promontory lying between Carlingford Lough on the north-east and Dundalk Bay on the south-west. The greater part of this promontory is made up of an igneous complex of Tertiary age which has invaded the Silurian slates and quartzites and the Carboniferous Limestone Series. This complex has not yet been investigated in detail, but for the purposes of the present paper certain references to it are necessary, and these are made below. The prevalence of hybrid-relations and contamination-effects between the basic and acid igneous rocks of the region is a very marked feature, and because of this it has been difficult at times to decide which types have been responsible for the various stages of the metamorphism.


1907 ◽  
Vol 7 (1) ◽  
pp. 22-31 ◽  
Author(s):  
R. Tanner Hewlett ◽  
George S. Barton

In view of the importance of a pure milk supply, we considered that it might be of interest to examine chemically, microscopically, and bacteriologically, a number of specimens of milk coming into the Metropolis for which purpose we decided to select samples from the various counties, the milk of which is consigned to London. We found that milk so consigned comes from about twenty-six counties extending from Derby in the North, to Hampshire and Devonshire in the South and South-West, and from Hereford in the West, to Norfolk in the East.


1954 ◽  
Vol 49 ◽  
pp. 267-291
Author(s):  
Elizabeth B. Wace

The Cyclopean Terrace Building lies to the north-west of the Lion Gate on the northern end of the Panagia Ridge and faces almost due west across the valley of the Kephissos and modern main road from Corinth to Argos. It lies just below the 200 m. contour line, and one terrace below the houses excavated in 1950–51 by Dr. Papadimitriou and Mr. Petsas to the east at the same end of the ridge. The area contains a complex of buildings, both successive and contemporary, and in view of the discovery of structures both to the south-west and, by the Greek Archaeological Service, to the north-east it is likely that this whole slope was covered by a portion of the outer town of Mycenae. This report will deal only with the structure to which the name Cyclopean Terrace Building was originally given, the so-called ‘North Megaron’, supported by the heavy main terrace wall.The excavation of this structure was begun in 1923. The main terrace wall was cleared and two L.H. IIIC burials discovered in the top of the fill in the south room. In 1950 it was decided to attempt to clear this building entirely in an endeavour to find out its date and purpose. The clearing was not, however, substantially completed until the close of the 1953 excavation season, and this report presents the available evidence for the date as determined by the pottery found beneath the building; the purpose is still a matter for study, though various tentative conclusions can be put forward.


1889 ◽  
Vol 6 (9) ◽  
pp. 425-427
Author(s):  
Alexander Somervail

On De La Beche's Geological Survey Map of Cornwall are three colours representing the associated rocks at, and on each side of the Manacle Point. The Point itself and for a considerable distance south of it is represented as a greenstone. Partially encased in the greenstone and to the south of it is gabbro, which forms the main mass of this rock in the Lizard district. On the north side of the greenstone which forms the extreme south wall of Porthonstock Cove is hornblende-schist, which with some serpentine and other rocks terminates against the killas, or slates near Porthalla.Several observers with seeming good reason have drawn attention to the fact that the greenstone as represented on the map is made to cover much too large an area to the south, and that any one walking from this direction, or the reverse, finds gabbro where the former rock was expected to occur.


Starinar ◽  
2013 ◽  
pp. 269-286
Author(s):  
Perica Spehar ◽  
Natasa Miladinovic-Radmilovic ◽  
Sonja Stamenkovic

In 2012, in the village Davidovac situated in south Serbia, 9.5 km south-west from Vranje, archaeological investigations were conducted on the site Crkviste. The remains of the smaller bronze-age settlement were discovered, above which a late antique horizon was later formed. Apart from modest remains of a bronze-age house and pits, a late antique necropolis was also excavated, of which two vaulted tombs and nine graves were inspected during this campaign. During the excavation of the northern sector of the site Davidovac-Crkviste the north-eastern periphery of the necropolis is detected. Graves 1-3, 5 and 6 are situated on the north?eastern borderline of necropolis, while the position of the tombs and the remaining four graves (4, 7-9) in their vicinity point that the necropolis was further spreading to the west and to the south?west, occupying the mount on which the church of St. George and modern graveyard are situated nowadays. All graves are oriented in the direction SW-NE, with the deviance between 3? and 17?, in four cases toward the south and in seven cases toward the north, while the largest part of those deviations is between 3? and 8?. Few small finds from the layer above the graves can in some way enable the determination of their dating. Those are two roman coins, one from the reign of emperor Valens (364-378), as well as the fibula of the type Viminacium-Novae which is chronologically tied to a longer period from the middle of the 5th to the middle of the 6th century, although there are some geographically close analogies dated to the end of the 4th or the beginning of the 5th century. Analogies for the tombs from Davidovac can be found on numerous sites, like in Sirmium as well as in Macvanska Mitrovica, where they are dated to the 4th-5th century. Similar situation was detected in Viminacium, former capital of the roman province of Upper Moesia. In ancient Naissus, on the site of Jagodin Mala, simple rectangular tombs were distributed in rows, while the complex painted tombs with Christian motifs were also found and dated by the coins to the period from the 4th to the 6th century. Also, in Kolovrat near Prijepolje simple vaulted tombs with walled dromos were excavated. During the excavations on the nearby site Davidovac-Gradiste, 39 graves of type Mala Kopasnica-Sase dated to the 2nd-3rd century were found, as well as 67 cist graves, which were dated by the coins of Constantius II, jewellery and buckles to the second half of the 4th or the first half of the 5th century. Based on all above mentioned it can be concluded that during the period from the 2nd to the 6th century in this area existed a roman and late antique settlement and several necropolises, formed along an important ancient road Via militaris, traced at the length of over 130 m in the direction NE-SW. Data gained with the anthropological analyses of 10 skeletons from the site Davidovac-Crkviste don't give enough information for a conclusion about the paleo-demographical structure of the population that lived here during late antiquity. Important results about the paleo-pathological changes, which do not occur often on archaeological sites, as well as the clearer picture about this population in total, will be acquired after the osteological material from the site Davidovac-Gradiste is statistically analysed.


1981 ◽  
Vol 106 ◽  
pp. 69-75
Author(s):  
I Parsons

A series of smal! volcanic centres cut Ordovician turbidites of Formation A in the southem part of Johannes V. Jensen Land between Midtkap and Frigg Fjord (Map 2). Their general location and main rock types were described by Soper et al. (1980) and their nomenclature is adopted here for fig. 22 with the addition of the small pipe B2. A further small intrusion, south-west of Frigg Fjord, was described by Pedersen (1980). The centres lie 5-10 km south of, and parallel to, the important Harder Fjord fault zone (fig. 22) which traverses the southern part of the North Greenland fold belt and shows substantial downthrow to the south (Higgins et al., this report).


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