Chapter 24

2020 ◽  
pp. 327-342
Author(s):  
Mark Glancy
Keyword(s):  
San Francisco ◽  
State Building ◽  
Feature Location ◽  
The South ◽  
Historical Drama ◽  
Crucial Element ◽  
Love Story ◽  
Empire State Building ◽  
Modern Era ◽  
Made In

In later years, Cary Grant would claim that he did retire in the early 1950s. In fact, he had only an 18 month hiatus between films, and during that time he knew that he would return to the screen in Alfred Hitchcock’s To Catch A Thief (1955). Hitchcock not only revived Grant’s career but also brought it into the modern era. All of his future films would be made in Technicolor and in a widescreen format, and all would feature location shooting in a spectacular setting. With To Catch A Thief, he found his favourite leading lady, Grace Kelly, and enjoyed a summer of filming with friends Alfred and Alma Hitchcock on location in the south of France. The Pride and the Passion (1956) was an epic historical drama filmed on location in Spain, where Grant fell deeply in love with his co-star Sophia Loren. The bittersweet love story An Affair to Remember (1957), co-starring Deborah Kerr, was filmed on location in Manhattan. Remarkably, the film’s producers tried to convince Grant that the setting should be changed to San Francisco, but he insisted on filming in Manhattan, citing the scene atop the Empire State Building as a crucial element of the film. He was correct. The scene is now considered iconic, and the film has become a perennially popular classic.

Virtual Embodiment as/and the Threshold of Love

2013 ◽  
Vol 3 (2) ◽  
pp. 97-109 ◽  
Author(s):  
Anne Harris
Keyword(s):  
Urban Space ◽  
State Building ◽  
Modern Life ◽  
Space And Time ◽  
Empire State Building ◽  
Arcades Project ◽  
Performance Texts ◽  
And Performance ◽  
The Stranger

This essay draws upon the author’s performance script Fall and Walter Benjamin’s The Arcades Project as a provocation for considering the ways performance texts provide a threshold for somatic inquiry, and for recognizing the limits of scholarly analysis that does not take up performance-as-inquiry. Set at the Empire State Building, this essay embodies the connections and missed possibilities between strangers and intimates in the context of urban modern life. Fall’s protagonist is positioned within a landscape of capitalist exchange, but defies this matrix to offer instead a gift at the threshold of life/death, virtual/real, and love/loss. Through somatic inquiry and witnessing as threshold experiences, the protagonist (as Benjamin’s flaneur) moves through urban space and time, proving that both scholarship and performance remain irrevocably embodied, and as such invariably tethered to the visceral, the stranger, risk, and death.

El viaje botánico de Pierre Edmond Boissier por el sur de España (1837). The botanical trip of Pierre Edmond Boissier by the South of Spain

2010 ◽  
Vol 35 ◽  
pp. 5-21 ◽  
Author(s):  
Antonio González Bueno
Keyword(s):  
The South ◽  
200Th Anniversary ◽  
Made In

Español.  Coincidiendo con el 200 aniversario del nacimiento de Pierre-Edmond Boissier (1810-1885), presentamos un análisis de su primer viaje por el Sur de España, realizado en 1837: estudiamos los motivos que le impulsaron a llevarlo a cabo, la información que tuvo disponible, el viaje en sí y la publicación de sus resultados en la más señera de sus obras, el Voyage botanique dans le midi de l’Espagne… (París, 1839-1845).English. In the 200th anniversary of the birth of Pierre-Edmond Boissier (1810-1885) we analized his first trip to the south of Spain, made in 1837, the reasons that prompted him to carry out, the information available, the trip itself and the publication of their results in the most outstanding of his works, the Voyage botanique dans le midi de l’Espagne ... (Paris, 1839-1845).

scholarly journals Revisiting the construction of the Empire State Building: Have we forgotten something?

2018 ◽  
Vol 61 (1) ◽  
pp. 47-57
Author(s):  
Mattias Jacobsson ◽  
Timothy L. Wilson
Keyword(s):  
State Building ◽  
Empire State Building

A Study of the Chemical and Physical Characteristics of the Soils from the South of Piauí for Soil-Cement Brick Production

2016 ◽  
Vol 869 ◽  
pp. 112-115 ◽  
Author(s):  
Francisca Pereira de Araújo ◽  
Edson Cavalcanti Silva Filho ◽  
João Sammy Nery de Souza ◽  
Josy Anteveli Osajima ◽  
Marcelo Barbosa Furtini
Keyword(s):  
Organic Matter ◽  
Particle Density ◽  
Environmentally Friendly ◽  
Physical Characteristics ◽  
Chemical Characteristics ◽  
The South ◽  
Physical Chemical ◽  
Soil Cement ◽  
Made In

Soil-cement bricks are good examples of environmentally friendly products. This brick is the combination of soil with compacted cement with no combustion in its production. In this work the physical chemical characteristics of the soil from Piaui for producing this material were investigated. Samples of the soil were collected in three potteries from the county of Bom Jesus and pH analysis were carried out, as well as the rate of organic matter, texture, particle density, limits of liquidity and plasticity rates. The results have shown that the soils have acid tones (pH 5,49 a 6,11), which can be neutralized by adding cement, and organic matter percentages up to 1%. The samples have shown predominantly clay-rich textures with adequate plasticity limits, however, values of liquidity limits and particle density above recommended. Altogether, these soils tend to present viability concerning soil-cement brick production, provided that corrections with additives are made in order to minimize this effect.

Observations of the Coyote Lake, California earthquake sequence of August 6, 1979

1980 ◽  
Vol 70 (2) ◽  
pp. 559-570 ◽  
Author(s):  
R. A. Uhrhammer
Keyword(s):  
San Francisco ◽  
Fault Zone ◽  
Strong Earthquake ◽  
Main Shock ◽  
B Value ◽  
Aftershock Sequence ◽  
The South ◽  
The North ◽  
Temporal And Spatial Characteristics ◽  
Largest Aftershock

abstract At 1705 UTC on August 6, 1979, a strong earthquake (ML = 5.9) occurred along the Calaveras fault zone south of Coyote Lake about 110 km southeast of San Francisco. This strong earthquake had an aftershock sequence of 31 events (2.4 ≦ ML ≦ 4.4) during August 1979. No foreshocks (ML ≧ 1.5) were observed in the 3 months prior to the main shock. The local magnitude (ML = 5.9) and the seismic moment (Mo = 6 × 1024 dyne-cm from the SH pulse) for the main shock were determined from the 100 × torsion and 3-component ultra-long period seismographs located at Berkeley. Local magnitudes are determined for the aftershocks from the maximum trace amplitudes on the Wood-Anderson torsion seismograms recorded at Berkeley (Δ ≊ 110 km). Temporal and spatial characteristics of the aftershock sequence are presented and discussed. Some key observations are: (1) the first six aftershocks (ML ≧ 2.4) proceed along the fault zone progressively to the south of the main shock; (2) all of the aftershocks (ML ≧ 2.4) to the south of the largest aftershock (ML = 4.4) have a different focal mechanism than the aftershocks to the north; (3) no aftershocks (ML ≧ 2.4) were observed significantly to the north of the main shock for the first 5 days of the sequence; and (4) the b-value (0.70 ± 0.17) for the aftershock sequence is not significantly different from the average b-value (0.88 ± 0.08) calculated for the Calaveras fault zone from 16 yr of data.

V.—The Brookwood Deep-Well Section

1886 ◽  
Vol 3 (8) ◽  
pp. 353-357
Author(s):  
A. Irving
Keyword(s):  
Loamy Sand ◽  
Free Access ◽  
The South ◽  
Pebble Bed ◽  
Deep Well ◽  
Western Side ◽  
High Road ◽  
Made In ◽  
Geological Magazine

This section, which was completed last year, appears of such value and interest to students of the Tertiary strata of the London Basin, that I have thought it worth while to offer a description of it to the readers of the Geological Magazine. Through the courtesy of Dr. Barton, the Governor of the Asylum, I have had free access to the specimens preserved of the various strata passed through, and very careful use of them has been made in the preparation of the tabulated statement which follows; much of the information having been kindly furnished from the engineers who were employed. The Asylum is situated at Knap Hill, about a mile and a quarter from Brookwood Station on the South-Western Eailway, and is on the Upper Bagshot Sands. The mouth of the well is in the valley just below, about 140 feet above O. D., and about the same level as that at which the Middle Bagshot Beds occur in the famous Goldsworthy section, which furnished Prof. Prestwich, some forty years ago, with the clue to the succession of the beds of the Bagshot Formation. It is about a mile and a half distant therefrom. The evidence as to the horizon in the Bagshot Series, at which the well commences, is very clear to those who are familiar with the stratigraphy. The widely-extended pebble-bed at the base of the Upper Bagshot Sands occurs here very near the top of the well, and I saw it exposed again at about the same level in an excavation made by the side of the high road which runs along the western side of the Asylum Estate. The same greenish loamy sand was intermingled with the pebbles in both cases. In the ploughed field a stiff yellow loam, such as so commonly occurs above this pebble-bed in the Bagshot area, crops out in the valley where the well is situated. The ‘brown sandy bed’ which occurs at the top of the section is probably a portion of this, re-constructed by later drift action, and mingled with more sandy materials washed down from the sandy strata situated at higher levels on the slopes of the valley.

In a Flying Boat Across the Greenland Ice Cap to U.S.A.

1932 ◽  
Vol 36 (263) ◽  
pp. 917-944
Author(s):  
Wolfgang von Gronau
Keyword(s):  
The South ◽  
Ice Cap ◽  
Made In

My flight from List, Germany, to Chicago, via Greenland and Labrador, was made in July and August of 1931. I had previously made a similar flight to America in 1930 when I chose the south point of Greenland and became very much impressed by this magnificently interesting country. Ever since that flight I had a strong desire to explore this country more closely. My desire for a second flight became acute when we, in Germany, received the first reports of the British Arctic Air-Route Expedition, under the leadership of Mr. Watkins.Their weather reports for our prospective flight were very favourable and I immediately set to work to organise my second venture.

On the Chloride Waters of Great Britain

1945 ◽  
Vol 82 (6) ◽  
pp. 267-273 ◽  
Author(s):  
W. Anderson
Keyword(s):  
Great Britain ◽  
The South ◽  
Very Old ◽  
North East ◽  
The North ◽  
Exact Position ◽  
The Many ◽  
The Village ◽  
Made In

Formerly there were several surface brine springs in the North-East Coalfield; to-day there are none. From the many accounts of their occurrence nothing has been learned of their exact position, and very little of the composition of their waters. The earliest record, made in 1684, described the Butterby spring (Todd, 1684), and then at various times during the next two centuries brine springs at Framwellgate, Lumley, Birtley, Walker, Wallsend, Hebburn, and Jarrow were noted. In particular the Birtley salt spring is often mentioned, and on the 6-in. Ordnance map, Durham No. 13, 1862 edition, it is sited to the south-east of the village. Although no record has been found there must have been either a brine spring or well at Gateshead, for the name of the present-day suburb, Saltwell, is very old, and brine springs are still active in the coal workings of that area.

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