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.

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’.

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.

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).

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.

scholarly journals From Riot to Revolt: Asbury Park in July 1970

2016 ◽  
Vol 2 (2) ◽  
pp. 80
Author(s):  
Daniel Weeks
Keyword(s):  
New York ◽  
New Jersey ◽  
New York Times ◽  
The West ◽  
West Side ◽  
Civil Unrest ◽  
The Media ◽  
The City ◽  
General Conditions ◽  
Violent Events

This paper investigates the civil unrest that rocked the New Jersey resort city of Asbury Park for four days in July 1970. It focuses particularly on how various participants and the media represented the violent events in the West Side of the city. These representations, which were publicized in the <em>Asbury Park Press</em>, the <em>New York Times</em>, and elsewhere, demonstrate two interrelated dynamics. First, that in attempting to characterize the events in Asbury Park—either as a criminal riot or justifiable revolt—participants on all sides resorted to well-worn stereotypes, and second, that these stereotypes, once publicized in the media, began to shape events in the city in consequential ways. This study also demonstrates that the civil unrest moved through several phases—from a teenage “rock and bottle festival” to a true revolt against discrimination, segregation, and the general conditions of the ghetto.

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.

scholarly journals The Sam D. Carpenter Garden Plot Site (41CP496), Camp County, Texas

2013 ◽  
Author(s):  
Timothy K. Perttula
Keyword(s):  
Material Culture ◽  
The South ◽  
The West ◽  
West Side ◽  
Unknown Number ◽  
The North ◽  
Garden Plot

Robert L. Turner, Jr. obtained a surface collection of ancestral Caddo material culture remains from the Sam D. Carpenter Garden Plot site (41CP496) some unknown number of years ago. With records provided by Turner, Bo Nelson has recently recorded the site, and provided the artifacts from the surface collection for analysis. The site is located in the uplands (330ft. amsl) on the west side of the Big Cypress Creek valley, about 2 km west of the modem channel of Big Cypress Creek. The Sam D. Carpenter Bottom site (41CP495), another Caddo site, is about l km to the east. Prairie Creek lies several kilometers to the south. while Dry Creek is a comparable distance to the north of the site.

XLII. A letter from Thomas Lawrence, M.D. to William Heberden, M.D. and F. R. S. concerning the effects of lightning, in Essex-street, on the 18th of June, 1764

1764 ◽  
Vol 54 ◽  
pp. 235-238
Keyword(s):  
The South ◽  
The West ◽  
West Side ◽  
North East ◽  
The North

Sir, I send you, as you desired, an account of the effects the lightning on Monday se'nnight had in my neighbourhood. The storm, which came from the south-east, broke first on the two houses at the bottom of Essex-street (which look from their south windows upon the river) and beat down several feet of the east-flue of the chimney on the west side, and separated the remainder down to the roof of the house from the western flue by a wide crack. From hence the lightning went higher up the street, and at the distance of about eighteen yards from the chimney just mentioned, went thro' the eves of a house, in a direction from the north-east to the southwest, as appeared by the breach, and forced the cieling of the garret inward by a kind of pointed bulge, without breaking the laths.

scholarly journals NOTE ON STATEN ISLAND NOCTUIDÆ

1886 ◽  
Vol 18 (5) ◽  
pp. 95-96
Author(s):  
A. R. Grote
Keyword(s):  
New York ◽  
New Jersey ◽  
The United States ◽  
Seasonal Migration ◽  
Red Squirrel ◽  
The South ◽  
Staten Island ◽  
Southern Boundary ◽  
The North ◽  
Southern Species

My earliest collecting field was the south side of Staten Island, where I found many rare insects, especially among the Coleoptera. This south beach of the Island is visited by the warm spring coming from the south very early in the year, and is a good collecting field. Staten Island is a continuation of the Jersey coast, and one finds on it southern species of butterflies such as Argynnis Idalia, which are less frequent on Long Island, the next extension of the coast to the north. So far as the fauna is concerned, I am inclined to class Staten Island with New Jersey, rather than with New York. It forms the beautiful southern boundary of New York Harbor. At the same time Mr. Davis informs us that the Red Squirrel, not uncommon on the mainland of New Jersey, is not found on Staten Island, and thus has not crossed the narrow Kills. But I have abundant faith it will yet turn up on the Island, where all good things naturally live. I have collected on Staten Island a good many of those kinds of moths which come up our coast with the warmer weather and the Gulf Stream. I have in various papers called attention to the seasonal migration, from south to north, of many species of moths, which adds so much to the fauna of the United States.

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