East Side, West Side, All Around the Town: APA’s Planned Tours Get You There

2004 ◽  
Vol 39 (4) ◽  
pp. 52-84
Author(s):  
Mark Moran
Keyword(s):  
East Side ◽  
West Side ◽  
The Town

XIV.—The Discovery of Prehistoric Pits at Peterborough and the Development of Neolithic Pottery

Archaeologia ◽  
1910 ◽  
Vol 62 (1) ◽  
pp. 333-352 ◽  
Author(s):  
G. Wyman Abbott ◽  
Reginald A. Smith
Keyword(s):  
Sea Level ◽  
East Side ◽  
The West ◽  
West Side ◽  
North East ◽  
The North ◽  
South West ◽  
Early Settlement ◽  
Human Habitation ◽  
The Town

The series of relics exhibited to the Society come from an early settlement at Peterborough, dating from a time when flint was in general use, perhaps before the introduction of metal, at least among the poorer inhabitants of the country. The site is a promontory rising out of the Fens and lying on the north-east side of the town. The river Nene joined the Fens about half a mile to the south-west of the site, which is only a few feet above sea-level, and was almost surrounded in times of flood. So far as can be determined at present, the extent of the settlement is several acres, but the ground has not yet been moved except on the west side, where unfortunately no observations were taken. There were no surface indications of human habitation, and no burrows noticed on the promontory or in its neighbourhood. The subsoil is gravel, fine and coarse, varying in depth from 8 to 10 feet. The top 18 inches of gravel, underlying the soil, is reddish brown, mixed with a reddish loam, which sometimes occupies natural pockets 3 to 8 feet deep, cutting down through the gravel and at times reaching the cornbrash below.

Churches Under Enemy Occupation Philadelphia, 1777–8

1945 ◽  
Vol 14 (1) ◽  
pp. 33-60
Author(s):  
Nelson Waite Rightmyer
Keyword(s):  
Entire Length ◽  
Western Boundary ◽  
British Army ◽  
East Side ◽  
The West ◽  
West Side ◽  
The Town

When the British Army entered Philadelphia on September 26, 1777, they entered the largest town in the colonies. But Philadelphians of today might be amused by the extent of the great metropolis, Philadelphia proper extended from Vine Street to South Street and westward to Fifth. “There were few houses west of Sixth street and most of these were on Chestnut and Market streets…”1 Fifth Street was really the western boundary of the town as we may see from the number of cemeteries along its entire length, For example, at Cherry Street there were two Lutheran graveyards; (diagonally opposite at the northwest corner of Arch was the Presbyterian yard. At the southeast corner of this same street was the Episcopal yard; farther down, just below Market Street, was the graveyard of the Baptists. On the east side of Fifth below Walnut was the Romanists' cemetery and on the west side was that of the Free Quakers. Phjladelphians at least had the grace to remove their graveyards to the extreme limits of the town. Perhaps this is one of the reasons why colonial Philadelphia missed some of the worst epidemics.

A Bastion of the Town Wall of London, and the Sepulchral Monument of the Procurator Julius Classicianus

1936 ◽  
Vol 16 (1) ◽  
pp. 1-7
Author(s):  
F. Cottrill
Keyword(s):  
Retaining Wall ◽  
Passenger Transport ◽  
East Side ◽  
The North ◽  
Inner Circle ◽  
External Face ◽  
The Town ◽  
Made In

Excavations made in June 1935 for the foundations of a new sub-station of the London Passenger Transport Board at Trinity Place, Trinity Square, E.C., brought to light some remains of the Roman town wall of London. A large portion of the medieval superstructure is still standing on the east side of Trinity Place, and to the north of this the Inner Circle Railway runs in a cutting under the roadway. The construction of this cutting involved the removal of a length of 73 ft. of the wall in 1882 (R.C.H.M. Roman London, 83). The site of the discoveries to be described here was immediately behind the southern retaining wall of the cutting. Both faces of the Roman wall were exposed at this point, and could be examined in detail, and against the external face was a fragment of one of the later Roman bastions (pl. 1). These remains were investigated by the writer on behalf of this Society, and the Passenger Transport Board kindly granted all necessary facilities, and rendered every possible assistance.

scholarly journals SPATIAL COMPOSITION OF BENTHIC SUBSTRATE AROUND BONTOSUA ISLAND

2018 ◽  
Vol 4 (1) ◽  
Author(s):  
Muhammad Banda Selamat ◽  
Mahatma Lanuru ◽  
Amir Hamzah Muhiddin
Keyword(s):  
Reef Flat ◽  
Live Coral ◽  
Percent Cover ◽  
Small Islands ◽  
East Side ◽  
Coral Rubble ◽  
West Side ◽  
Spatial Composition ◽  
Index Ratio ◽  
Benthic Substrate

Coral reefs and seagrass are natural fortress for small islands from waves and ocean currents. The spatial distribution of these benthic substrate should be known and monitored regularly. This study aims were to map existing benthic substrates on the reef flat of Bontosua Island, determine the spatial composition and develop index ratio. Benthic substrates were surveyed using geotagging technique. Their distribution were estimate using Quickbird image that was rectified and classified using ISOcluster method and validate by 240 selected photos. The seagrass were surveyed at 8 stasions to record percent cover and species composition. Depth profiles were track along 10 reef flat line segment. Bontosua Island has an elongated shape from South to Northwest. This study had produced a benthic substrate distribution map with thematic accuracy 76%. Total area able to map were 54.2 hectares. About 43% benthic substrates at Bontosua were mixture of coral rubble, seagrass and algae, 20% was mixture of rubble and algae, 16% dominated by seagrass, 13% mixture of sand and seagrass and 8% substrate were dominated by live coral. There were eight seagrass species found with average percent cover 37.2 ± 12.5 percent. The spatial ratio of live coral, seagrass and mixed substrate for West side reef flat was 2:20:49 and 1:9:9 for East side. This indicate that the distribution of benthic substrates on the West side is much wider than on the East side. This approach potentially applied to study the relationship between benthic substrate composition and the deformation of small islands.

scholarly journals Fabric and Origin of Lateral Moraines, Bethartoli Glacier, Garhwal Himalaya, India

1978 ◽  
Vol 20 (84) ◽  
pp. 547-553 ◽  
Author(s):  
Gerald D. Osborn
Keyword(s):  
Garhwal Himalaya ◽  
Lateral Moraine ◽  
East Side ◽  
The West ◽  
West Side ◽  
Lateral Ridge ◽  
Moraine Ridge

AbstractUnusually strong till fabrics in lateral moraines of Bethartoli Glacier provide information on the genesis and growth of the moraines. On the west side of the valley, down-stream of the present glacier snout, several lateral moraine crests are juxtaposed. Because the crests generally become higher towards the valley axis, they must represent re-advances of the glacier rather than recessional stages. On the east side of the valley only a single lateral ridge is found; presumably the ridge is composed of debris from several glacial advances. On the eroded proximal flank of this ridge a strong fabric is visible; the plane defined by a- and b-axes of stones is parallel to the distal flank of the moraine ridge, indicating that the moraine grew mainly by accretion of debris on to its distal flank. On the eroded proximal flank of the innermost west-side ridge the equivalent fabric is weaker, suggesting that distal flank accretion was less significant and proximal flank accretion more significant than on the east side.

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