Uncover detailed information about So Ends Our Night (1941). Explore interactive visualizations about the cast, ratings, awards, photos, plot, and more. Overview of So Ends Our Night, 1941, directed by John Cromwell, with Fredric March, Margaret Sullavan, Frances Dee, at Turner Classic Movies. Amazon CAPTCHAIntroduce los caracteres que se muestran a continuaci. Para obtener el mejor resultado, aseg. So Ends Our Night,' a Tragic Story of Refugees, at the Music Hall - - 'Come Live With Me,' at Capitol. Only one of the many horrible features of the tragedy which the Nazis began has been the plight of the German political refugee, cast out or escaped from his native land without passport or identity papers and forced to roam in an alien world like a hunted beast. He has probably been the most pathetic and helpless of the dispossessed. And it is the story of several of these persons—of three in particular—which is told with great poignance and sympathy in the new Loew- Lewin film. For the story which Talbot Jennings has derived from Erich Maria Remarque's novel, . And although John Cromwell has drawn much pathos and affecting tenderness from individual scenes, his direction of the picture as a whole has been too slow, too solemn and much too tedious. The older man hopes only to return to his wife again, the young couple seek security and a future. Their various disheartening vicissitudes are revealed as they roam over Europe —from Vienna, to Prague, to Zurich, to Geneva and on to Paris—sometimes together, sometimes apart. And finally the man goes back to his wife and to death, the young people on to America. A large and uniformly excellent cast plays the picture as well as could be wished. Fredric March is properly defiant and ruggedly idealistic as the older man, Margaret Sullavan is fragile and confused as the Jewish girl, and Glenn Ford, a most promising newcomer, draws more substance ands appealing simplicity from his role of the boy than any one else in the cast. ![]() Several prominent players appear briefly in very minor roles. But all—even the principal characters—are made little more than shadows on the screen, pitiful outcasts of fortune, but never fully realized persons. For the picture merely states a tragic condition, never gets beneath the obvious facts. It gives a heart- rending illustration of the sad words of Christ: . Loew and Albert Lewin and released through United Artists. At the Radio City Music Hall. Fredric March. Ruth Holland . Margaret Sullavan. ![]()
Marie Steiner . Frances Dee. Ludwig Kern . Erich von Stroheim. Watch the latest So Ends Our Night trailer on Video Detective. Amazon.es - Compra So Ends Our Night a un gran precio, con posibilidad de env. Ver opiniones y detalles sobre la gran selecci So Ends Our Night Genres: War, Drama The Nazis are clearly the villains in So Ends Our Night, but since the film was made before America's entry into World War II. ![]() Marrill . Allan Brett. Potzloch . Joseph Cawthorn. The Chicken . Leonid Kinskey. The Pole . Alexander Granach. Mr. Roman Bohnen. Ammers . Sig Rumann. Professor Meyer . William Stack. Barnekrogg . Ernst Deutsch. Swiss Policeman . Spencer Charters.
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![]() Life is filled with little mysteries: thankfully, science is able to answer some of them. Strange-but-true facts and analysis of unexplained mysteries. Sea - Wikipedia. Seas are important for human development and trade, as at Singapore, the world's busiest entrep. The sea moderates Earth's climate and has important roles in the water cycle, carbon cycle, and nitrogen cycle. Although the sea has been travelled and explored since prehistory, the modern scientific study of the sea. About 8. 5% of the solids in the open sea are sodium chloride. Deep- sea currents are produced by differences in salinity and temperature. ![]() ![]() Surface currents are formed by the friction of waves produced by the wind and by tides, the changes in local sea level produced by the gravity of the Moon and Sun. The direction of all of these is governed by surface and submarine land masses and by the rotation of the Earth (the Coriolis effect). Former changes in sea levels have left continental shelves, shallow areas in the sea close to land. These nutrient- rich waters teem with life, which provide humans with substantial supplies of food. The most diverse areas surround great tropical coral reefs. On the Greenland Ice Sheet — The midnight sun still gleamed at 1 a.m. Brandon Overstreet, a. Of our cryosphere Archive of daily polar sea ice cap concentrations (1979 - present) Dowload the historical sea ice dataset here Questions and/or comments about polar. Find out more about the history of Sherman’s March, including videos, interesting articles, pictures, historical features and more. Get all the facts on. A comprehensive and regularly updated interactive map of the world's major submarine cable systems and landing stations. Get the latest international news and events from Asia, Europe, the Middle East, and more. See world news photos and videos at ABCNews. Each December on National Wreaths Across America Day, our mission is carried out in part by coordinating wreath-laying ceremonies at Arlington National Cemetery, as. Whaling in the deep sea was once common but whales' dwindling numbers prompted international conservation efforts and finally a moratorium on most commercial hunting. Oceanography has established that not all life is restricted to the sunlit surface waters: even under enormous depths and pressures, nutrients streaming from hydrothermal vents support their own unique ecosystem. Life may have started there and aquatic microbial mats are generally credited with the oxygenation of Earth's atmosphere; both plants and animals first evolved in the sea. The sea is an essential aspect of human trade, travel, mineral extraction, and power generation. This has also made it essential to warfare and left major cities exposed to earthquakes and volcanoes from nearby faults; powerful tsunami waves; and hurricanes, typhoons, and cyclones produced in the tropics. This importance and duality has affected human culture, from early sea gods to the epic poetry of Homer to the changes induced by the Columbian Exchange, from burial at sea to Basho's haikus to hyperrealist marine art, and inspiring music ranging from the shanties in The Complaynt of Scotland to Rimsky- Korsakov's . It is the scene of leisure activities including swimming, diving, surfing, and sailing. However, population growth, industrialization, and intensive farming have all contributed to present- day marine pollution. Atmospheric carbon dioxide is being absorbed in increasing amounts, lowering its p. H in a process known as ocean acidification. The shared nature of the sea has made overfishing an increasing problem. Definition. The remainder (about 0. Clarke once noted that . The more recent study of the sea in particular is oceanography. This began as the study of the shape of the ocean's currents. Both are informed by chemical oceanography, which studies the behavior of elements and molecules within the oceans: particularly, at the moment, the ocean's role in the carbon cycle and carbon dioxide's role in the increasing acidification of seawater. Marine and maritime geography charts the shape and shaping of the sea, while marine geology (geological oceanography) has provided evidence of continental drift and the composition and structure of the Earth, clarified the process of sedimentation, and assisted the study of volcanism and earthquakes. The salinity varies from 3. The surface salinity of waters in the Northern Hemisphere are generally closer to the 3. Other solutes include metal ions such as magnesium (Mg) and calcium (Ca) and negative ions such as sulfate (SO. In the absence of other pollution, seawater would not be harmful to drink except that it is much too saline. For scientific and technical purposes, a standardized form of artificial seawater is often used. Variations in salinity are caused by many factors: currents flowing between the seas; incoming freshwater from rivers and glaciers; precipitation; the formation and melting of sea ice; and evaporation, which is in turn affected by temperature, winds, and waves. For example, the upper level of the Baltic Sea has a very low salinity (1. Its salinity averages 4. In the tropics where sunlight falls more directly, the temperature of the surface layers can rise to over 3. Its salinity makes this lower than freshwater's, usually about . These temperature differences contribute to the continuous circulation of water through the sea. Warm surface currents cool as they move away from the tropics; as the water becomes denser, it sinks. The cold water in the deep sea moves back towards the equator before welling up again to the surface. Deep seawater has a temperature between . These break into small pieces and coalesce into flat discs that form a thick suspension known as frazil. In calm conditions, frazil will freeze into a thin, flat sheet called nilas, which thickens as new ice forms in the sea beneath it. In turbulent waters, frazil instead join together into larger flat discs known as . These slide over and under one another to form floes. During these processes, salt water and air are trapped amid the ice. Nilas forms with a salinity around 1. Of the light that reaches the surface of the sea, much of it is reflected at the surface and its redwavelengths are absorbed in the top few meters. Yellow and green reach greater depths, and the longer blue and violet wavelengths may penetrate as deep as 1,0. The amount of oxygen present in seawater depends primarily upon its temperature and the photosyntheticorganisms living in it, particularly algae, phytoplankton, and plants such as seagrass. During the day, their photosynthetic activity produces oxygen, which dissolves into the seawater and is used by marine animals. The water's oxygen saturation is lower during the night and much lower in the deep sea. Below a depth of about 2. Below this, anaerobic bacteria break down falling organic material, producing hydrogen sulfide (H. Note the large swells in the southern oceans. Ocean surface waves are oscillations caused by the friction from air moving across the surface of the water. This friction transfers energy and forms surface waves in the water perpendicular to the direction of the wind. The top of a wave is known as its crest and its foot as its trough; the distance between two crests is the wavelength. These waves are mechanical: as they approach, the water molecules at a given point rise up and, as they pass, the water molecules go down, tracing a roughly circular path. The energy is passed across the surface and does not represent a horizontal motion of the water itself. The sea state of the ocean is determined by the size of these waves, which. The smallest waves are called ripples. As strong and prolonged winds push against ripples' raised crests, larger and more irregular waves form, which known as seas. These waves reach their maximum height when the rate at which they are traveling nearly matches the speed of the wind and, over time, they naturally separate. These swells are particularly common in the Roaring Forties of the Southern Hemisphere where the wind blows continuously. If approaching at an angle, waves may bend or wrap rocks and headlands. When the wave reaches a point where its deepest oscillating molecules contact the seabed, friction begins to slow the wave down. This pulls the crests closer together and increases the waves' height. When the ratio of a wave's height to its wavelength exceeds 1: 7, it . These events can temporarily lift or lower the surface of the sea in the affected area, usually by a few feet. The potential energy of the displaced seawater is turned into kinetic energy, creating a shallow wave radiating outwards at a velocity proportional to the square root of the depth of the water. Tsunamis, therefore, travel much faster in the open ocean than on a continental shelf. The energy of the wave is dissipated only gradually but is spread out over the wave front. As the wave radiates away from the source, the front gets longer and the average energy reduces, so distant shores will generally be hit by weaker waves. However, as the speed of the wave is controlled by the water depth, it does not travel at the same speed in all directions and this affects the direction of the wave front. This effect, known as refraction, can focus the strength of an advancing tsunami on some areas while weakening it in others, according to the undersea topography along its path. Much of the disaster's destruction can be produced by these flood waters, which drain back into the sea while pulling people and debris along. Several tsunamis can be caused by a single geological event. In such cases, it is common for the later waves to arrive between eight minutes and two hours after the first, which may not be the biggest or most destructive. At any given place, the water rises over the course of the tidal cycle to a maximum height known as . As the water recedes, it uncovers more and more of the foreshore or intertidal zone. The difference in height between the high tide and low tide is known as the tidal range or tidal amplitude. At Hangzhou in China, the bore can reach 9 meters (3. Most places experience two high tides each day, occurring at intervals of about 1. Earth to make a complete revolution and return the Moon to its previous position relative to an observer. The Moon's mass is some 2. Sun, but it is 4. Earth. On the opposite side of the Earth, the lunar force is at its weakest and this causes another bulge to form. These bulges rotate around the Earth as the moon does. The Sun's effect is less powerful but, when the Sun, Moon and Earth are all aligned at the full and new moons, the combined effect results in the high . In contrast, when the Sun is at 9. In places like the Gulf of Mexico where land constrains the movement of the bulges, only one set of tides may occur each day. Inshore from an island, there may be a complex daily cycle with four high tides. Isabelle Adjani, som Oscarnominerades f. ![]()
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Sin olvidar los calificados trabajos hist. Colnago Valdovinos, Pedro Antonio Alvarenga Caballero, Rafael Eladio Vel. Antonia Ortellado de Fossati. En 1. 4 cap. Paraguayos en su gran mayor. Sus aportes a la historia nacional no necesitan ya de la decantaci. Con el valioso apoyo del Prof. Carreras Saguier, Villa Montes. Fue designado Comandante interino el RA 1 . Obtuvo las palmas de General de Brigada en 1. En 1. 95. 6, y en virtud de la Ley 3. Comenzaba una era de realizaciones sin precedentes en nuestra historia, que abarcan todo el . Son esas realizaciones las que justifican y respaldan la inclusi. Stroessner, Saltos del Guair. Franco, Ayolas; son apenas nombres de los m. Con su infraestructura para el desarrollo con m. Esta, con escasas calles pavimentadas o empedradas, sin los servicios que caracterizan al progreso y la comodidad de las ciudades modernas: agua corriente, sistema cloacal, desag. La potencia instalada de su usina el. La red vial pavimentada, cuyas gestiones in. El servicio educativo ten. Acaray primero, Itaip. Y como un aura bienhechora, la paz social que ambienta la arm. Hoy los ciudadanos convocados por el servicio militar ya no tienen la opresiva sombra de las guerras civiles, que por obra de los ambiciosos sembraron de cruces los . Y los conscriptos convertidos en ciudadanos optimistas, instruidos en provechosas profesiones, regresan a sus lares convertidos en ciudadanos progresistas, amantes de la paz y el trabajo, . Por obra de sus Tenientes surgieron y se afirmaron hacia el interior, las primeras poblaciones, con la capitalidad de Asunci. Cada uno de los 4 Adelantados y sus Tenientes, aport. Muchos son los nombres, especialmente de los hoy casi olvidados capitanes: Nufrio de Chaves, fundador de Nueva Asunci. El nombre de Marciel de Lorenzana est. Otros nombres de gran significaci. De otros se habla por separado. CAPITULO 1. FUNDADORES Y CIVILIZADORESJUAN DE SALAZAR DE ESPINOSA. La Provincia del Paraguay, todav. Fue especialmente elocuente la decisi. Producida la independencia nacional, mediante el consenso y decisi. Desde los combatientes de Paraguar. PROCERES DE LA INDEPENDENCIAJOS. Antes, en el extendido per. Francia hubiera tenido plena vigencia las palabras de Lu. No es que Don Carlos, y tampoco el Mariscal, haya sido mucho menos absorbente; pero con su gobierno, el Estado paraguayo se perfil. Los hitos relevantes de la magna obra son: la Declaraci. Y otras decisiones que evidenciaban el firme prop. Y una medida de denso contenido humanitario y trascendente proyecci. Por razones comprensibles; la carencia de un cuerpo de juristas calificados, sigui. ADMINISTRACION DE LOS L. Y apenas comenzaba 1. Venancio Flores inicia en el Uruguay su revoluci. Se estaban dando los primeros pasos conducentes a la integraci. El emperador Pedro II, y los Presidentes Mitre y Flores, fueron los art. Aunque de apariencia y con fama de infranqueable, durante la guerra qued. Sus proyectiles chatos rebotaban por el blindaje de los acorazados. En general, el armamento del Ej. Con elementos proporcionados por la . LOS GENERALES DE LA GRAN EPOPEYAFRANCISCO SOLANO, L. En enero de 1. 54. Obispo Barrios hizo . De las cuestiones fundamentales estudiadas en el primero de ellos, fueron las referidas a la evangelizaci. Y a partir del Obispado de fray Bernardino de C. Y hubo memorables enfrentamientos como el del Dr. Adrian Cornejo, Gobernador Eclesi. Y el caso de un Obispo de Buenos Aires, fray. Juan de Arregui , quien llegado a la Asunci. GOBIERNO DE LA DIOCESIS ASUNCENAPEDRO GARC. Brasil desalentaba cualquier posibilidad de poseer frontera com. JB Gill para lograr que las pretensiones argentinas bajaran al Pilcomayo. Firmado el tratado Sosa- Tejedor, en 1. Paz y L. Para la intelectualidad paraguaya signific. El Laudo Hayes basado en una aplastante documentaci. En el siglo pasado cobraron relevancia los trabajos de investigaci. INTELECTUALES Y ESTADISTAS EN DEFENSA DEL CHACOJOS. MANUEL SOSA ESCALADA, (1. XI - 1. 86. 0/V - 1. ALEJANDRO AUDIBERT. Iniciada las hostilidades se hizo notorio que el Comandante de las fuerzas en operaciones en el Chaco - Estigarribia - actuaba sin atenerse a los criterios operativos del Comandante en Jefe, lo que hizo que esta jerarqu. Todos, incluido el mismo Estigarribia, se hab. Y casi todos Estigarribia, Delgado, Ayala, Irraz. Antes, Estigarribia e Irraz. No pocos jefes eran del sector del Ej. Estigarribia, secundado por los Comandantes de Cuerpos de Ej. LOS CONDUCTORES VICTORIOSOSJOS. En la post guerra del 6. Barbero. Creada la Universidad, se incorporaron al pa. Todos ellos trascendieron m. VII - 1. 90. 4/- )JULIO MANUEL MORALES. NETTO, (1. 7 - V - 1. MAESTROSDurante casi 3 siglos de vida colonial, el quehacer acad. El extendido mestizaje se aferraba al guaran. Contra esos tremendos obst. Las escasas instituciones acad. Los docentes eran egresados con grados acad. En un lapso de medio siglo a partir de la independencia, hay apenas una media docena de nombres de connacionales vinculados con la docencia como dedicaci. Y el argentino Juan Pedro Escalada, a quien hay que sumar el espa. Ello sin olvidar al Colegio Nacional y las Facultades de Derecho y Medicina, especialmente, en cuyas c. CA Levi Ruffinelli; aqu. Maestros de esta tesitura fueron entre otros Delf. MAESTROSJUAN PEDRO ESCALADA. CHAYES, (7 - VI - 1. RICARDO ODR. Historia integral, en su mayor. Blas Garay, El Comunismo en las Misiones.- Pedro Lozano, espa. Y a un paraguayo, Mariano Antonio Molas, pr. HISTORIADORESBLAS MANUEL GARAY. Hasta entonces, la ciencia jur. Fue asesor del Gobierno en Asunci. Producido el movimiento revolucionario, el Dr. Fue sin duda el autor de los m. Francia, fue el autor de los textos de las resoluciones fundamentales de todos los Congresos; el Estatuto Provisorio de Justicia, 1. Constituci. Algunas de esas revistas - la del . Tres de aquellas revistas, una tras la desaparici. Muy pronto el alcohol y especialmente la morfina arruinaron el valioso grupo y casi todos sus componentes murieron tempranamente. Entre los del grupo de Cr. ESCRITORES Y POETASVICTORINO ABENTE DE LAGO. Y toda su existencia se reduce a lo que hab. A medio siglo de la independencia nada hab. Ya casi al promediar el mandato de Don Carlos, llegaron los hermanos Alejandro y Cayetano Ravizza, quienes con el ingl. Los realizadores de los trabajos escult. Durante la guerra se revelaron los primeros artistas paraguayos, de entre quienes, Aurelio Garc. En la post guerra se produjeron importantes incorporaciones: Serafin Marsal; lleg. Sin embargo, sus trabajos m. Francisco Almeida; decano de los escultores paraguayos; naci. Francia, de Don Carlos, del mariscal L. Vicente Pollarolo; asunceno, de descendencia italiana, naci. Sucesor de Almeida, realiz. CULTORES DEL ARTE; PL. De todo lo enunciado no qued. Lynch - mazurcas, minuets y valses. De entonces son algunas danzas y melod. Y una interesante figura; Cantalicio Guerrero, paraguayo, calificado ejecutante y compositor, disc. Prisionero en Yatay, sobrevivi. Entre ellos, Luis Cavedagni, maestro de larga y destacada actuaci. Nicolino Pellegrini, Director de la Banda de Polic. Cardozo Ocampo, por ej. Y otros, solistas de gran influencia; el guitarrista Gustavo Sosa Escalada, los violinistas Carlos Aschermann y Alfredo Kamprad, los pianistas Isabel Anisitz y Miguel Morosoli, y otros como Vicente Maccarone, Erwin Brinicky, Jaime Segal. Toribio Pacheco, en junio de 1. En setiembre del mismo a. Rojas Garrido, por expresas instrucciones del Presidente de la Rep. A poco de consumarse el holocausto de Cerro Cor. Los primeros fueron el peruano Manuel del Castillo, para quien . Lira, invocando al Mariscal proclam. SOLIDARIOS CON NUESTRO VALOR Y SACRIFICIOMART. ACADEMIA PARAGUAYA DE LA HISTORIA - HISTORIA PARAGUAYA, ANUARIOS.*. ALMADA ROCHE, ARMANDO - JOS. ALSINA, ARTURO - PARAGUAYOS DE OTROS TIEMPOS.*. BELMONT PARKER, WILLIAM - PAR. BOETTNER, JUAN MAX - M. BRAY, ARTURO - HOMBRES Y . CARDOZO OCAMPO, MAURICIO - MEMORIAS DE UN PYCH. COMANDO EN JEFE DE LAS FF. ENCINA RAMOS, PEDRO / C. FACULTAD DE MEDICINA - ANALES.*. FURLONG, GUILLERMO, SJ. NATALICIO - PROCESO Y FORMACI. DE - EL MARISCAL DE AM. KALLSEN, OSVALDO - HISTORIA DEL PARAGUAY CONTEMPOR. KOSTIANOVSKY, OLINDA M. DE - EL VICE PRESIDENTE S. MOSQUEIRA, SILVANO - SEMBLANZAS PARAGUAYAS.*. MOSQUEIRA, SILVANO - NUEVAS SEMBLANZAS.*. O'LEARY, JUAN EMILIANO - EL LIBRO DE LOS H. O'LEARY, JUAN EMILIANO - NUESTRA EPOPEYA,*. O'LEARY, JUAN EMILIANO - LOS LEGIONARIOS,*. |
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