908 resultados para Grimsby Beach
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Summary of bacteria monitoring of Iowa's beaches.
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Este trabajo busca investigar el fenómeno de lo generacional en el cine a través de su relación con la música. Para ello, utiliza como punto de partida la filmografía de los Rolling Stones y aplica elconcepto de aura de Walter Benjamin. Así, explora las tensiones generacionales entre jóvenes y adultos, que se reflejan en los ámbitos del creador, la audiencia y la industria como tensiones entre invención y comercialización, entre libertad y represión o entre rebeldía y conservadurismo. De ese modo, procura identificar en la puesta en escena la capacidad contracultural del cine que apela a lo juvenil y oponerla a los simulacros oportunistas que utiliza el sistema de la industria cultural.
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The diversity of algal banks composed of species out the genera Gracilaria Greville and Hypnea J.V. Lamouroux have been impacted by commercial exploitation and coastal eutrophication. The present study sought to construct dynamic models based on algal physiology to simulate seasonal variations in the biomasses of Gracilaria and Hypnea an intertidal reef at Piedade Beach in Jaboatão dos Guararapes, Pernambuco State, Brazil. Five 20 × 20 cm plots in a reef pool on a midlittoral reef platform were randomly sampled during April, June, August, October, and December/2009 and in January and March/2010. Water temperature, pH, irradiance, oxygen and salinity levels as well as the concentrations of ammonia, nitrate and phosphate were measured at the sampling site. Forcing functions were employed in the model to represent abiotic factors, and algal decay was simulated with a dispersal function. Algal growth was modeled using a logistic function and was found to be sensitive to temperature and salinity. Maximum absorption rates of ammonia and phosphate were higher in Hypnea than in Gracilaria, indicating that the former takes up nutrients more efficiently at higher concentrations. Gracilaria biomass peaked at approximately 120 g (dry weight m-2) in March/2010 and was significantly lower in August/2009; Hypnea biomasses, on the other hand, did not show any significant variations among the different months, indicating that resource competition may influence the productivity of these algae.
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Since the first offshore Lake Erie well was drilled in 1941, the Grimsby and Thorold formations of the Cataract Group have been economically important to the oil and gas industry of Ontario. The Cataract Group provides a significant amount of Ontario's gas production primarily from wells located on Lake Erie. The Grimsby - Thorold formations are the result of nearshore estuarine processes influenced by tides on a prograding shelf and are composed of subtidal channel complexes, discrete tidal channels, mud flats and non-marine deposits. Deposition was related to a regressive - transgressive cycle associated with eustatic sea level changes caused by the melting and resurgence of continental glaciation centred in Africa in the Late Ordovician/Early Silurian. Grimsby deposition began during a regression with the deposition of subtidal channel complexes incised into the marine deposits of the Cabot Head Formation. The presence of mud drapes and mud couplets suggest that these deposits were influenced by tides. These deposits dominate the lower half of the Grimsby. Deposition continued with a change from these subtidal channel complexes to laterally migrating, discrete, shallow tidal channels and mud flats. These were in turn overlain by the non-marine deposits of the Thorold Formation. Grimsby - Thorold deposition ended with a major transgression replacing siliciclastic deposition with primarily carbonate deposition. Sediment was sourced from the east and southeast and associated with a continuation of the Taconic Orogeny into the Early Silurian. The fluvial head of the estuary prograded from a shoreline that was located in western New York and western Pennsylvania running NNE-SSW and then turning NW-SE and paralleling the present day Lake Erie shoreline. iii The facies attributed to the Grimsby - Thorold formations can be ascribed to the three zones within the tripartite zonation suggested by Dalrymple et ale (1992) for estuaries, that is, a marine-dominated facies, a mixed energy facies, and a facies that is dominated by fluvial processes. Also, sediments within the Grimsby - Thorold are commonly fining upwards sequences which are common in estuarine settings whereas deltaic deposits are normally composed of coarsening upwards sequences in a vertical wedge shape with coarser material near the head. The only coarsening observed was in the Thorold Formation and attributed to non-marine deposition by palynological evidence. The presence of a lag deposit at the base of the sediments of the Grimsby Thorold formations suggests that they were incised into the Cabot Head Formation. Further, the thickness of Early Silurian sediments located between the top of the Queenston Formation, where Early Silurian sedimentation began, to the top of the Reynales - Irondequoit formation are constant whether the Grimsby - Thorold formations are present or not. Also, cross-sections using a sand body located in the Cabot Head Formation for correlation further imply that the Grimsby Formation has been incised into the previous deposits of the Cabot Head.
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Joyce Chapman at Uncle Charlie's birthday party, an all-day event at C. C. Chapman's home, 4th Street, Long Beach, California, 1933.
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Cover title: Illustrated guide to Niagara Falls and vicinity.
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Josephine and Albert Sloman are pictured in this undated black and white photograph. The beach location is unknown. This photo was among the Sloman - Bell family memorabilia in the possession of Rick Bell, grandson of Josephine and Albert. The family is descended from Black slaves who escaped from the United States and settled in southern Ontario.
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A vignette of the Mansion House in Grimsby, Andrew Randall, Proprietor.
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Contains information about the campground, the hotel, church services and includes advertisements.
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Board with six postcards of Crystal Beach. First postcard, Steamer "Americana" leaving foot of Main St. Second postcard, Divers at Crystal Beach, Canada. Third postcard, Cyclone Coaster, Crystal Beach, Ontario. Fourth postcard, Scenic Railway, Crystal Beach, Ont. Fifth postcard, Scene in the Park, Crystal Beach, Ont. Sixth postcard, Scene on the Midway, Crystal Beach, Canada.
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An account with W.M. Forbes dated April 1st, 1875 and amounting to $21.38. There is a line at the bottom of the receipt that reads "I don't care about any money but my creditors seem hard up".