To regulate the production and ginning of cotton : hearings before the Committee on Agriculture and Forestry, United States Senate, Seventy-third Congress, second session, on S. 1974, a bill to place the cotton industry on a sound basis, and to prevent unfair competition and practices in putting cotton into the channels of interstate and foreign commerce. January 15, 16, 17, and 20, 1934.

Ellison D. Smith, chairman; John H. Bankhead, presiding, Jan. 16, 1934.

Post office appropriation bill, 1917. Railway mail pay Hearings before the Committee on post offices and post roads, United States Senate, Sixty-fourth Congress, first session, on H. R. 10484, an act making appropriations for the service of the Post office department for the fiscal year ending June 30, 1917, and for other purposes. April 14, 15, 17, 18, & 19, 1916 ...

John H. Bankhead, chairman.

Historical romances of William Harrison Ainsworth.

"Printed for subscribers only."

The Loma Prieta, California, earthquake of October 17, 1989--main-shock characteristics /

Mode of access: Internet.

Guilford, Maine, 1816-1916; proceedings of the centennial celebration June 17-18, 1916,

Vital records: p. 162-190.

Transactions at the Conference on Environmental Management and Economic Growth in the Smaller Caribbean Islands, September 17-21, 1979 /

Mode of access: Internet.

TRANSFORMAÇÃO SOCIAL SERVIDA À MESA Interpretação cultural e sociorreligiosa do lava-pés em Jo 13,1-17

O lava-pés em Jo 13,1-17 é objeto dessa tese que tem por objetivo apresentar sua significação cultural e sociorreligiosa. Em meio à complexidade do caráter polissêmico do relato joanino o foco da análise volta-se para o contexto das características do costume cultural implicados no lava-pés em ambiente de refeição no mundo mediterrâneo do primeiro século da EC. Com base na análise da história da redação o relato joanino é apresentado como fruto de um processo de recuperação da memória tradicional para ressignificar o valor e dignidade do lava-pés e dos sujeitos aos quais essa tarefa era atribuída: mulheres, escravos e crianças. No contexto da comunidade joanina o lava-pés transforma-se em proposta não apenas de renúncia ou inversão de status, mas de reciprocidade de papéis assumida por todos como gesto concreto e, ao mesmo tempo, simbólico, de abolição de qualquer discriminação ou desigualdade que possa existir entre as pessoas. O lava-pés, nos dois estratos que descrevem as primeiras interpretações predominantes na comunidade (Jo 13, 12-17 e Jo 13,6-10), não é, pois, ritual religioso de purificação de pecado, nem apenas o testemunho de um serviço humilde de quem renuncia provisoriamente ao seu status, mas sim a expressão da identidade de um discipulado que pretende viver um igualitarismo radical no cotidiano do exercício de poder e da divisão de suas tarefas.

Annotated record of the detailed examination of Mn deposits recovered from dredges and cores from VEMA 17 Expedition stations

The cores and dredges described in this report were taken during the Vema 17 Expedition from December 1960 until October 1961 by the Lamont Geological Observatory, Columbia University from the R/V Vema. An approximate total of 210 cores, dredges and camera stations were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.

(Tables, page 17-18), Chemical composition of ferromanganese concretions of the lakes of Northern Savolax in Eastern Finland

This paper discusses the occurrence of manganese-rich concretions in the lakes of Northern Savolax in Eastern Finland. The samples were collected in the summer of 1905 and left to dry for 2 months at room temperature. The quantity of H2O mentionned in the analysis was obtained by dessication at 155°C. The amount of Mn is calulated as MnO2 although other valences might be present in the samples. The contents in CO2 and organic substances was not determined. J. Aschan determined that as a general rule, in Finland the manganese rich lake deposits are rather associated with soft bottom sediments while the iron rich deposits are more assocaited with hard or sandy bottoms.

(Tables, page 17-18), Chemical composition of ferromanganese concretions in lake Storsjøen

This paper discusses the occurrence of manganese-rich concretions (Seeerz or see-erz, in german) in Storsjöen (46 km**2, 130 m above sea level) in southern Norway, (in the basement area, 70 km. Northeast of Oslo, then named Kristiania) and thereby contains a general discussion about the relationship between manganese and iron in the concretions as well as on the different precipitation of Mn-poor iron-manganese oxide concretions in the bottom of lakes from that manganese oxide rich concretions which are relatively Fe-poor.

Annotated record of the detailed examination of Mn deposits from DSDP Site 34, Leg 5 (Core 5-34-17)

Site 34 had been located by the JOIDES Pacific Advisory Panel to be over a negative magnetic anomaly (31 million years B.P.) immediately to the east of Anomaly 10 (Site 33). The primary objective was to obtain samples of basement and basal sediment to provide comparison between adjacent positive and negative magnetic anomalies. A second objective was to obtain samples which would permit an analysis of the variability in sediment over relatively short distances (about 10 miles). Although basement had not been reached at Site 33 because of the unexpected chert, the use of a massive diamond bit at Site 34 permitted coring through the chert to basement at 383 meters below the sea floor. Even though the near basement sections of the paired sites (33 and 34) could not be compared, comparison would be possible above the chert layer.

Annotated record of Mn deposits from R/V Anton Bruun, Cruise 17 Expedition stations

Station 678E (29°22'S. latitude, 80WW. longitude) is roughly midway between San Felix and Juan Fernandez Islands, and approximately 700 km west of the coast of Chile. The sample at Station 678E was collected in a Riedl Dredge with a finer net sewn into the cod end of the 500 JJ mesh bag. The change in depth during the dredging operation indicated a rather rapid shelving. The bottom was a red clay with some volcanic ash. Manganese nodules were present (rock dredge sample).

Percentiles de la prueba de carrera de ida y vuelta 4x10 m en escolares de 9 a 17 años de Bogotá, Colombia: Estudio FUPRECOL

Objetivo: Este estudio describe los percentiles de la prueba de carrera de ida y vuelta 4 x 10 m en escolares de 9 a 17 años, de Bogotá, Colombia, pertenecientes al estudio Asociación de la fuerza prensil con manifestaciones tempranas de riesgo cardiovascular en niños colombianos. “FUPRECOL” Métodos: Estudio descriptivo transversal, en 2502 varones (42.7%) y 3349 mujeres (57,2%), de edades entre 9 y 17 años, pertenecientes a 24 instituciones educativas del sector oficial, en Bogotá, Colombia. La velocidad/agilidad se evaluó con la prueba de carrera de ida y vuelta 4 x 10 m (componente motor de la batería Fuprecol). Se calcularon los percentiles (P3, P10, P25, P50, P75, P90 y P97) y curvas centiles por el método LMS, según el sexo y la edad; y se realizó una comparación entre los valores de la velocidad-agilidad observados con estudios internacionales. Resultados: La edad promedio de los participantes fue 12,7 (DE 2,4) años. Al comparar por sexos, los varones presentan un mejor rendimiento en la prueba de carrera 4 x 10 m que las mujeres. En varones, el P50 osciló entre 11,9 segundos y 13,1 segundos, mientras que en mujeres el P50 osciló entre 14,3 segundos y 15,0 segundos. Al comparar los resultados de este estudio por grupos de edades y sexos, con trabajos internacionales, el P50 fue mayor al reportado en los trabajos de España, Portugal y el estudio HELENA realizado en 9 países europeos. Esta misma tendencia fue observada al comparar la media y la desviación estándar con escolares de Argentina, Francia y el mismo estudio HELENA. Conclusiones: Se registran percentiles de la prueba de carrera de ida y vuelta 4 x 10 m en función de las edades y el sexo. Estos valores pueden ser utilizados tanto para evaluar los niveles de aptitud de los estudiantes como para detectar a estudiantes cuyos niveles de condición física están por debajo de un mínimo saludable.