DESCRIPTION OF A NEW ENGLAND DISTRICT SCHOOL AS IT APPEARED IN 1804

PEDIATRICS ◽  
1974 ◽  
Vol 54 (1) ◽  
pp. 14-14
Author(s):  
T. E. C.
Keyword(s):  
New England ◽  
New Hampshire ◽  
Outer Side ◽  
The Road ◽  
The North ◽  
North Side ◽  
The People ◽  
Human Dwelling ◽  
East End ◽  
Very High

The Reverend Warren Burton (1800-1866) of Wilton, New Hampshire described the District School he attended between 1804 and 1817 in these words: The Old School-house, in District No. 5, stood on the top of a very high hill, on the north side of what was called the County road. The house of Capt. Clark, about ten rods off, was the only human dwelling within a quarter of a mile. The reason why this seminary of letters was perched so high in the air, and so far from the homes of those who resorted to it, was this: Here was the center of the district, as near as surveyor's chain could designate. The people east would not permit the building to be carried one rod further west, and those of the opposite quarter were as obstinate on their side. The edifice was set half in Capt. Clay's field, and half in the road. The wood-pile lay in the corner made by the east end and the stone wall.... The doorstep was a broad unhewn rock, brought from the neighboring pasture. It had not a flat and even surface, but was considerably sloping from the door to the road; so that, in icy times, the scholars, in passing out, used to snatch from the scant declivity the transitory pleasure of a slide.... The outer side of the structure was never painted by man; but the clouds of many years had stained it with their own dark hue....

scholarly journals Analisis Kelayakan Perubahan fungsi Terminal Penumpang menjadi Fasilitas Parkir Angkutan Barang (Studi Kasus Terminal Terboyo Semarang)

2017 ◽  
Vol 23 (1) ◽  
pp. 14
Author(s):  
Kami Hari Basuki ◽  
Wahyudi Kushardjoko ◽  
Andreana J. G. S. Pratama
Keyword(s):  
Local Area ◽  
Freight Transport ◽  
Heavy Vehicles ◽  
Coverage Area ◽  
Transport Modelling ◽  
The Road ◽  
The North ◽  
North Side ◽  
Study Results ◽  
Regional Basis

Semarang City has public transport terminal at Terboyo. It is unperformance terminal has caused by land subsidden and flood. The aims of this study is determined fisibility of Terboyo freight-transport terminal park at Semarang City. Methodology analysis at this study is improved transport modelling to determine freight-transport demand. Traffic counting survey with Manual Kapasitas Jalan Indonesia (MKJI) 1997 method are used to know the road and intersection performances that closest to Terminal Terboyo. The study results have showed most trucks parked in Kaligawe road and Yos Sudarso road was continuous journey, while trucks parked in Ronggowarsito road was a truck with the origin or destination of Semarang. Potential park fasilities at Terboyo is indicated by the length of the vehicle configuration plan of 8 meters and parking 45° obtained as much as 73 PSU (Parkign Space Unit), while the north side of the field with a length of 18 meters and plan vehicle parking configuration 30° obtained 76 PSU. It has powerfull to accommodate parking of heavy vehicles. This studi has not identified the potential of regional freight-transport. Occutionally, the pattern of movement of freight transport does not occur in the local area only. So, that further studies need to be conducted with respect to the coverage area of study on a regional basis.

IV.—Stratigraphical Note

1907 ◽  
Vol 4 (12) ◽  
pp. 537-538
Author(s):  
T. C. Cantrill
Keyword(s):  
Geological Survey ◽  
The West ◽  
The Road ◽  
The North ◽  
North Side ◽  
The Town

The fossils which Mr. V. M. Turnbull has collected from supposed Slade Beds on the “roadside near St. Martin's Cemetery, Haverfordwest,” were obtained along the north side of a road leading westward from St. Martin'ls Cemetery to Portfield House, on the west aide of the town. About half-way between the Cemetery and Port-field House the road is crossed by a by-road known as Jury Lane; one of the fossiliferous localities lies 110 yards east of Jury Lane crossing, another is 100 to 150 yards west of it. The area in question is contained in the Old Series one-inch Geological Survey map, Sheet 40, the New Series one-inch map, Sheet 228, and in the six-inch map, Pembrokeshire, Sheet 27 N.E.

scholarly journals XVII. Description of the mineral bason in the counties of Monmouth, Glamorgan, Brecon, Carmarthen, and Pembroke. By Mr. Edward Martin

1806 ◽  
Vol 96 ◽  
pp. 342-347 ◽  
Keyword(s):  
Iron Ore ◽  
The South ◽  
South Side ◽  
The North ◽  
North Side ◽  
South Wales ◽  
East And West ◽  
East End

1. The irregular oval line, delineated on the annexed map (Plate XIV.) shows nearly the inner edge of a limestone bason, in which all the strata of coal and iron ore (commonly called Iron Stone) in South Wales are deposited; the length of this bason is upwards of 100 miles, and the average breadth in the counties of Monmouth, Glamorgan, Carmarthen, and part of Brecon, is from 18 to 20 miles, and in Pembrokeshire only from 3 to 5 miles. 2. On the north side of a line, that may be drawn in an east and west direction, ranging nearly through the middle of this bason, all the strata rise gradually northward; and on the south side of this line they rise southward, till they come to the surface, except at the east end, which is in the vicinity of Pontipool, where they rise eastward.

IX.—An Exposure of Middle and Newer Pleistocene Boulder Clay in Derby

1889 ◽  
Vol 6 (5) ◽  
pp. 224-226 ◽  
Author(s):  
R. M. Deeley
Keyword(s):  
Main Mass ◽  
The Road ◽  
The North ◽  
North Side ◽  
Boulder Clay

Some very interesting deposits of Pleistocene age have lately been exposed on the Burton Road, Derby. The road rises on the north side of Mill Hill, and near the top, at the height of 260 feet, cuts into a mass of Boulder-clay, which is, or was, well shown in the cuttings for the new roads leading into Byron Street. Another outlier of the same clay is exposed in Littleover Lane to the southwest. The main mass of the deposit cut into on the Burton Road is a red morainic clay with boulders; apparently a subaerial moraine subsequently modified by the passage over it of land ice. Unlike the tough, silty, red and blue aqueous Boulder Clays so plentifully spread over the Midland counties, it shows little or no signs of aqueous action. Sometimes it has a banded or streaked appearance, but this seems to be due rather to a crushing or pressing-out action than to original conditions of deposition.

Prehistoric Human Remains at Little Cornard, Suffolk

1913 ◽  
Vol 1 (3) ◽  
pp. 297-300
Author(s):  
H. Dixon Hewitt
Keyword(s):  
Human Remains ◽  
The Road ◽  
The North ◽  
North Side ◽  
Gravel Pit ◽  
The Subject ◽  
Break Up ◽  
Scientific Value

The discovery which is the subject of these notes was unfortunately rendered incomplete by the fact that the initial exhumation of the bones was not witnessed by me, as I came on the scene after the greater part of the skeleton had been shovelled away by those ignorant of its scientific value.The gravel-pit in which I found the remains appears to be cut into a Plateau gravel, probably of an age corresponding to the break-up of one of the great glaciations. It is situated near, but not on, the summit of an eminence called Kedington Hill, about 2 miles South-by-East of Sudbury Station. The site was once included under the name of Kedington Common, and is on the North side of the road called Kedington Lane.

Fish, the People, and Theodore Lyman The Moderate Approach

2001 ◽  
Author(s):  
John T. Cumbler
Keyword(s):  
New England ◽  
New Hampshire ◽  
Republican Party ◽  
Boards Of Directors ◽  
Public Servant ◽  
The People ◽  
Long Time ◽  
River Fishery ◽  
River Valleys ◽  
Lake Winnipesaukee

On November 3, 1865, Theodore Lyman III handed his report for the River Fishery Commission to Massachusetts governor John Andrew. Then he headed north from Boston to Lawrence, where he met with newly elected New Hampshire governor Frederick Smyth and the fishery commissioners from other New England states. At that meeting, Governor Smyth, in Lyman’s words, “undertook the high horse and said they would shut down the water from Lake Winnepiseogee [the nineteenth century name for Lake Winnipesaukee] if we did not give the fishways.” Smyth was no one to take lightly. As the son of a New Hampshire farmer, he knew the importance offish to the rural diet, and as a founding member of the Republican Party, he was a politician of some significance. Smyth was also under pressure from rural farmers in the Connecticut and Merrimack River Valleys who had depended upon spring fish runs and now faced depleted rivers. Regarding the New Hampshire governor, Lyman wrote in his diary: “The threats of New Hampshire were some of my business as commissioner.” These threats were Lyman’s business in more than just his role as fish commissioner. The waters of Lake Winnipesaukee fed into the Winnipesaukee River, one of the main sources of the Merrimack River, which provided the power for the mills at Lowell and Lawrence. Without that water, those mills could not function. Lyman enjoyed healthy returns on his holdings in those mills. He not only held stock in these companies and in mills in Holyoke, he was also on several of their boards of directors. As he stated when he later ran for Congress, “I have been connected, and my father before me with the manufacturing interest.” As a major stockholder, Lyman had reason to be concerned about the waterpower of the mills along the Merrimack. Yet when he met with the governor and fish commissioners, he thought of himself not as the representative of the manufacturing interests but as a scientist and public servant. It was a role for which he had been preparing for a long time.

The Defences of the Iron Age Hill-Fort at Winklebury, Basingstoke, Hampshire

1977 ◽  
Vol 43 ◽  
pp. 131-154 ◽  
Author(s):  
Reay Robertson-Mackay
Keyword(s):  
Iron Age ◽  
Anglo Saxon ◽  
13Th Century ◽  
The North ◽  
North Side ◽  
The People ◽  
Ancient Monuments ◽  
The Hill ◽  
River Test

This report should be read in conjunction with the report on the excavations in the interior of the fort (previous paper in these Proceedings).The site of the hill-fort lies on the north side of the North Downs Trackway (National Grid Reference SU/614528). It is also on the southern edge of the Lower Thames valley. In this area there is a gap through the Hampshire Downs which connects the Thames valley with that of the River Test.The derivation of the place name Winklebury is not entirely clear. Medieval spellings, e.g. Wiltenischebury, c. 1290; Wyltenysshbury, 1407; Wynnyshbery and Wynlysbery, 1443, suggest that the name may be of Anglo-Saxon derivation and mean the ‘fort or stronghold of the people of Wilton’, i.e. the fort owned, occupied or built by the Wiltshiremen. However, Wiltonish occurs as a surname in Romsey in the 1289 Assize Rolls, in Walter le Wyltenysshe, and thus the site name may have evolved in the 13th century through associations with this family.Building development threatened the north side of the hill-fort in 1959. Excavations were accordingly carried out by the Ancient Monuments Inspectorate of the then Ministry of Works (now the Department of the Environment), under the direction of the writer in July and August of that year.

A Re-examination of the Therfield Heath Long Barrow, Royston, Hertfordshire

1935 ◽  
Vol 1 ◽  
pp. 101-107 ◽  
Author(s):  
C. W. Phillips
Keyword(s):  
Sea Level ◽  
The West ◽  
West Side ◽  
East Anglia ◽  
Ordnance Survey ◽  
The North ◽  
North Side ◽  
Nearest Neighbours ◽  
East End

Therfield heath, the expanse of chalk downland on the west side of Royston, has long enjoyed a local fame for the number of barrows and other antiquities which diversify its surface. On the north side it is bounded by the Icknield Way and so is well placed on the corridor between Wessex and East Anglia.By far the most important monument on the Heath is a small long barrow notable as the only example known in East Anglia, its nearest neighbours being the destroyed Dunstable barrow 25 miles to the west, and, further still, the Churn barrow west of the Thames near the Goring Gap.The outward form of the barrow is well-preserved (fig. 1, plan 1), exhibiting the typical club-shaped plan, the broader and higher end to the east. It is 110 feet long, 56 feet wide and 6 feet high at the east end, and 25 feet wide and 2 feet wide at the west. The Ordnance Survey references are Herts 6 inch 4 NE and 25 inch 4, 8. The latitude is 52°2′35″ and the longitude 0° 2′ 40″ w. The height above sea level is 385 feet.It is unfortunate that the late E. B. Nunn of Royston, who opened most of the barrows on the Heath, completely gutted the interior of this long barrow. By the courtesy of Dr W. M. Palmer, M.A., M.D., F.S.A. I am able to publish the following extract from Nunn's manuscript describing his operations here eighty years ago. Fig. 2 is a reproduction of the sketch which illustrates his account.

THE CONTRIBUTION OF E. M. MELETINSKY TO THE CAUCASIAN EPOS STUDIES. ON THE 100TH ANNIVERSARY OF THE BIRTH OF THE SCHOLAR

2020 ◽  
Vol 3 (4) ◽  
pp. 76-89
Author(s):  
Zurab D. Dzhapua ◽  
Keyword(s):  
Early Stage ◽  
100Th Anniversary ◽  
North Caucasus ◽  
The North ◽  
The People ◽  
History Of ◽  
High Level ◽  
Very High ◽  
Cultural Hero

The article analyses the contribution of Meletinsky to Caucasian epic studies. The role of Caucasian epic traditions in the study of the problem of the origins and the early forms of the epos is considered. A significant number of the comparative-typological studies of Meletinsky are based on the materials of mythoepic cultures of Caucasus mountain people. The scholar singled out the Caucasian epics, along with some other traditions, as the special early stage in the history of the epic. Meletinsky was one of the pioneers in the fundamental studies of the Caucasian Nart epics. Based on the analysis of materials available to him at that time, Meletinsky comes to the fundamental conclusions on the genre nature, national versions, images, subjects and motifs of the Nart epic. The scholar considered Sataney and Sasrykua to be the earliest characters in the epic, whose images clearly reflected the features of a cultural hero, especially in the close Abkhaz and Adyg versions. Furthermore, according to Meletinsky, the Transcaucasian legends about the chained heroes – Abkhaz Abryskil, Armenian Mger and Georgian Amiran – represent a kind of interweaving of mythological epic and heroic tales, in which the motives of cultural exploits are largely supplanted by episodes of the heroic struggle with Giants. In the studies of Meletinsky, the epic traditions of the people of the North Caucasus and Transcaucasia are subjected to the deepest analysis at a very high level of comparative studies.

Chastleton Camp, Oxfordshire, a hill-fort of the Early Iron Age

1931 ◽  
Vol 11 (4) ◽  
pp. 382-398 ◽  
Author(s):  
E. Thurlow Leeds
Keyword(s):  
Iron Age ◽  
Short Distance ◽  
The Other ◽  
Early Iron Age ◽  
Original Condition ◽  
North West ◽  
The Road ◽  
The North ◽  
East End ◽  
The One

Chastleton Camp, or Chastleton Barrow (pl. LIV, 1 and 2), as it is sometimes called, is situated at the south-east end of the parish, which projects like some huge spur from the north-west edge of the county and from the line of the road which on either side of the base of the spur for a short distance divides Oxfordshire from Gloucestershire on the one hand and from Warwickshire on the other. This road is an age-long trackway running diagonally across England by way of the Jurassic Belt from the Cotswolds to Northamptonshire, and is fringed by many remains of prehistoric man, in addition to the Rollright Stones and the dolmen known as the Whispering Knights. Along it must have moved the invaders of the early Iron Age to their conquest of the Midlands, establishing a line of strongholds of which Chastleton must in its original condition have been a formidable example.

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