912 resultados para Manly Hardy
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A finales de la década de los años veinte el cine mudo estaba llegando a su fin y comenzaron a producirse masivamente películas habladas. Los grandes estudios de Hollywood temen perder público fuera de Estados Unidos y antes de decidirse por el doblaje, ya que este sistema presentaba en aquella época problemas de sincronización, comienzan filmar versiones múltiples de un mismo guion en diferentes idiomas para exportar a los países de habla no inglesa. Dentro de todas las películas en español producidas por Hollywood, esta tesis doctoral está centrada únicamente en las de género fantástico. Es cierto que en las versiones en español encontramos pocas de dicho género, pero dentro de las existentes hay películas muy variadas, desde películas totalmente de género como las dos versiones de Drácula hasta otras que contienen elementos fantásticos lo suficientemente interesantes como para ser incluidas en esta investigación. La mayoría de las versiones en español que se produjeron en la década de los años treinta eran comedias o melodramas, los dos géneros más populares de la época. Pero de las más de cien películas en español que se filmaron en Hollywood durante la década de los años treinta algunas pueden catalogarse dentro del género fantástico. Estas películas son: ¡Pobre infeliz! (Charles Rogers, 1930), versión en español de The Shrimp (Ídem, Charles Rogers ,1930); Noche de duendes (James Parrott, 1930), versión en español de The Laurel-Hardy Murder Case (Ídem, James Parrot, 1930); La voluntad del muerto (George Melford, 1930), versión en español de The Cat Creeps (Rupert Julian, John Willard, 1930); Wu Li Chang (Nick Grinde, 1930), versión en español de Mr. Wu (William Night, 1927); Drácula (George Melford, 1931), versión en español de Drácula (Dracula, Tod Browning, 1931); Cheri-Bibi (Carlos F. Borcosque, 1931), versión en español de The Phantom of Paris (Ídem, John S. Robertson, 1931) y El último varón sobre la tierra (James Tinling, 1933), versión en español de It's Great to Be Alive (Alfred L. Werker, 1933)...
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One octavo-sized leaf containing a one-page handwritten draft of a resolution by a Harvard Corporation Committee appointed to "lay out an High Way thro' Rogers's Farm & determine about the Cost of the Sd way & the making the fences to enclose it." The resolution permits the town of Waltham to lay a highway on the farm's property as long as it is enclosed by a stone wall.
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Trabalho Final do Curso de Mestrado Integrado em Medicina, Faculdade de Medicina, Universidade de Lisboa, 2014
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The aim of this thesis was to evaluate historical change of the landscape of Madeira Island and to assess spatial and temporal vegetation dynamics. In current research diverse “retrospective techniques”, such as landscape repeat photography, dendrochronology, and research of historical records were used. These, combined with vegetation relevés, aimed to gather information about landscape change, disturbance history, and vegetation successional patterns. It was found that landscape change, throughout 125 years, was higher in the last five decades manly driven by farming abandonment, building growth and exotic vegetation coverage increase. Pristine vegetation was greatly destroyed since early settlement and by the end of the nineteenth century native vegetation was highly devastated due to recurrent antropogenic disturbances. These actions also helped to block plant succession and to modify floristical assemblages, affecting as well as species richness. In places with less hemeroby, although significant growth of vegetation of lower seral stages was detected, the vegetation of most mature stages headed towards unbalance between recovery and loss, being also very vulnerable to exotic species encroachment. Recovery by native vegetation also occurred in areas formerly occupied by exotic plants and agriculture but it was almost negligible. Vegetation recovery followed the successional model currently proposed, attesting the model itself. Yet, succession was slower than espected, due to lack of favourable conditions and to recurrent disturbances. Probable tempus of each seral stage was obtained by growth rates of woody taxa estimated through dendrochronology. The exotic trees which were the dominant trees in the past (Castanea sativa and Pinus pinaster) almost vanished. Eucalyptus globulus, the current main tree of the exotic forest is being replaced by other cover types as Acacia mearnsii. The latter, along with Arundo donax, Cytisus scoparius and Pittosporum undulatum are currently the exotic species with higher invasive behaviour. However, many other exotic species have also proved to be highly pervasive and came together with the ones referred above to prevent native vegetation regeneration, to diminish biological diversity, and to block early successional phases delaying native forest recovery.
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Owing to limited knowledge of the habitat use and diet of juvenile Arctic charr from the High Arctic, particularly young-of-the-year (YOY), we assembled data obtained from samples taken in and around Lake Hazen, Nunavut, Canada, to assess juvenile habitat use and feeding. Juvenile charr demonstrated a preference for stream environments, particularly those fed by warm upstream ponds. Charr occupying both stream and nearshore lake habitats were found to feed similarly, with chironomids occurring most frequently in diets. Some older stream-dwelling charr preyed on smaller, younger Arctic charr. Preferred stream occupancy is likely mediated by physical barriers created mainly by water velocity, and by distance from the lake, lake-ice dynamics, low water depth, and turbidity. Water velocities resulted in stream habitat segregation by size, with YOY mainly found in low-velocity pools and back eddies adjacent to stream banks, but not in water velocities >0.1 m/s. Greatest charr densities in streams were found in small, shallow, slow-flowing side channels, which are highly susceptible to drought. Under predicted climate change scenarios, streams fed by small ponds will be susceptible to intermittent flow conditions, which could result in increased competition among juvenile charr for the remaining stream habitats. In addition, glacier-fed streams are likely to experience increased flow conditions that will exacerbate physical barriers created by water velocity and further reduce the availability of preferred stream habitat.
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This chapter provides a review of proxy data from a variety of natural archives sampled in the Wollaston Forland region, central Northeast Greenland. The data are used to describe long-term environmental and climatic changes. The focus is on reconstructing the Holocene conditions particularly in the Zackenberg area. In addition, this chapter provides an overview of the archaeological evidence for prehistoric occupation of the region. The Zackenberg area has been covered by the Greenland Ice Sheet several times during the Quaternary. At the Last Glacial Maximum (LGM, about 22,000 years BP), temperatures were much lower than at present, and only very hardy organisms may have survived in the region, even if ice-free areas existed. Marked warming at around 11,700 years BP led to ice recession, and the Zackenberg area was deglaciated in the early Holocene, prior to 10,100 years BP. Rapid early Holocene land emergence was replaced by a slight transgression in the late Holocene. During the Holocene, summer solar insolation decreased in the north. Following deglaciation of the region, summer temperatures probably peaked in the early to mid-Holocene, as indicated by the occurrence of a southern beetle species. However, the timing for the onset of the Holocene thermal maximum is rather poorly constrained because of delayed immigration of key plant species. During the thermal maximum, the mean July temperature was at least 2-3°C higher than at present. Evidence for declining summer temperatures is seen at around 5500, 4500 and 3500 years BP. The cooling culminated during the Little Ice Age that peaked about 100-200 years ago. The first plants that immigrated to the region were herbs and mosses. The first dwarf shrubs arrived in Northeast Greenland prior to 10,400 years BP, and dwarf birch arrived around 8800 years BP. The first people arrived about 4500 years BP, but the region was depopulated several times before the last people disappeared some time after 1823 AD, perhaps as a consequence of poor hunting conditions during the peak of the Little Ice Age.
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Edition limited to 800 numbered sets.
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Back Row: Student Manager Adam Rosen, Groundskeeper Erich Keil, Tony Agosta, Billy Hardy, Kevin Crociata, Ryan Van0everen, Jason Mahoney, Dan Weeks, Matt Humbles, Scott Niemiec, Todd Fracassi, Jasen Livingston, Rodney Goble, Trainer Rex Thompson.
Middle Row: Grad Assistant Ed Turek, Assistant Coach Dan O'Brien, Bubba Wyngarden, Aaron Toth, Heath Murray, Nate Holdren, Matt Idoni, Chad Chapman, Ron Hollis, Matt Copp, Chris Newton, Volunteer Coach Ernie Savas, Assistant Coach Ace Adams.
Front Row: (from left): Bryan Santo, Eric Heintschel, Chris Michalek, Terry Woods, Toby Brzoznowski, Todd Marion, Head Coach Bill Freehan, Steve Buerkel, Eric Persinger, Pat Maloney, Scott Winterlee, Scott Timmerman, Dennis Konuszewski.
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Back Row: asst. coach Bill Frieder, coach John Orr, Mark Lozier, David Baxter, Rickey Green, David Stavale, Thomas Staton, William Lelich, asst. coach Jim Boyce, asst. coach Dan Fife
Front Row: mngr. Mitchell Kaufman, Len Lillard, Alan Hardy, Phil Hubbard, co-captain Steve Grote, co-captain John Robinson, Jake Whitten, Joel Thompson, Robert Jones. mngr. John Anderson
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Mode of access: Internet.
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Mode of access: Internet.
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"Second printing, April, 1928."