Giegling's Market on south end of the Northern Hotel

verso: Louie Larsen said this was Nick Waal's Market for as long as he can remember. After the market quit Aug Redman had a cigar factory in the building. Later he added a pool room to the cigar factory. Harold (Capt.) Edwardsen tore it down about in the 1930's and built a summer cottage up north from the material. The market was adjacent [to] the Northern Hotel on the south.

Bijou Inn - a camping spot at the south end of Lake Tahoe," page 5

2 scans made - 1of1 includes caption pasted below, 2of2 = image only

Map of Jackson City opposite the city of Washington at the south end of the Potomac Free Bridge.

Shows proposed town of Jackson City in Alexandria County D.C.

Pieces of the Past, March 9, 2011

In 1938, the Iowa State Library consisted of four departments: the general library, the library of sociology and economics, the law library, and the medical library. The south end of the law library was being used for the library of sociology and economics.

Crustal structure and reflectivity of the Swiss Alps from 3-Dimensional seismic modeling. 2. Penninic Nappes

Surface geological mapping, laboratory measurements of rock properties, and seismic reflection data are integrated through three-dimensional seismic modeling to determine the likely cause of upper crustal reflections and to elucidate the deep structure of the Penninic Alps in eastern Switzerland. Results indicate that the principal upper crustal reflections recorded on the south end of Swiss seismic line NFP20-EAST can be explained by the subsurface geometry of stacked basement nappes. In addition, modeling results provide improvements to structural maps based solely on surface trends and suggest the presence of previously unrecognized rock units in the subsurface. Construction of the initial model is based upon extrapolation of plunging surface. structures; velocities and densities are established by laboratory measurements of corresponding rock units. Iterative modification produces a best fit model that refines the definition of the subsurface geometry of major structures. We conclude that most reflections from the upper 20 km can be ascribed to the presence of sedimentary cover rocks (especially carbonates) and ophiolites juxtaposed against crystalline basement nappes. Thus, in this area, reflections appear to be principally due to first-order lithologic contrasts. This study also demonstrates not only the importance of three-dimensional effects (sideswipe) in interpreting seismic data, but also that these effects can be considered quantitatively through three-dimensional modeling.

1008-003 White Oak Watershed Final Report

Whit Oak Lake was listed on the 2008 Section 303(d) List if impaired waters in four categories. The first phase of the project has already helped to affect approximately 60% of the watershed. There has been an estimated sediment reduction of 609 tons per year with phase one. The structure being planned for the South end of the lake, (phase two) will affect nearly all of the remaining 40%. If we can accomplish similar results, we can expect a sediment reduction of approximately 273 tons additional per year. We have been working with the Mahaska County NRCS office, Snyder & Associates (engineers) and private landowners in the watershed to make this project a reality.

Huoltopolitiikka naisten ja perheen arjessa

Kirjallisuusarvostelu

La revolución como metáfora política: para una comprensión de la revolución fascista de Benito Mussolini

Asumiendo que existe una tendencia de la opinión pública y académica por relacionar la idea de revolución con procesos netamente de izquierda, se propone comprender el término como concepto y como metáfora con el fin de alejarlo de la polarización ideológica. En esta investigación se abordan los conceptos políticos y su relación con las metáforas a partir de unos principios teóricos básicos: la idea de Koselleck de que los conceptos tienen historia, y la idea de Blumenberg de que muchos conceptos fundamentales son potentes porque en el fondo son metáforas. Posteriormente se observa cómo las diferentes posturas políticas han adoptado o rechazado la idea de revolución como parte de sus proyectos políticos. Finalmente, el caso del fascismo se presenta como un escenario clave para comprobar la trascendencia del concepto y las implicaciones de su uso en términos discursivos y prácticos

Inversión extranjera de España en Cuba a partir de 1991. Perspectivas de una transición económica.

El interés que presenta esta investigación es analizar la manera en que la inversión española influye en la economía cubana para generar en la isla perspectivas de transición económica desde 1991. Se explica la situación de expectativa en relación con la posible transición económica cubana por las reformas legislativas, los lazos económicos generados con nuevos socios y la reentrada en escena de la propiedad privada en el entorno cubano. No obstante, el embargo económico estadounidense, la persistencia del régimen castrista, su aparente falta de voluntad hacia el cambio y la no ejecución de algunas decisiones de la Asamblea Nacional actúan como obstáculos para dicho proceso de transición. La metodología de investigación es de tipo descriptivo-analítico, en donde se emplean conceptos de relaciones internacionales para alcanzar un mayor grado de comprensión.

Preguntas a la desigualdad. Ensayos sobre análisis de clase, socialismo y marxismo

Este texto comienza con un ensayo autobiográfico que explora los retos y beneficios de lo que implica ser un académico marxista en este tiempo. A este ensayo le sigue una discusión sobre varios temas del análisis de clase, con particular énfasis en dos temas: las clases y la desigualdad, y la relación entre clase y poder. La segunda sección aborda el tema del socialismo como posible futuro del capitalismo. Su autor procura clarificar el estatus conceptual del socialismo y discute las razones por las que ciertas reformas, tales como los subsidios básicos universales, en últimas no podrían realizarse por completo sin la introducción de alguna forma de socialismo. Preguntas a la desigualdad concluye con un examen del problema general del marxismo, en tanto que tradición radical de la teoría social. Allí se discuten tres temas en particular: los principios fundamentales del marxismo analítico como estrategia para reconstruir el marxismo como teoría social científica; la relación entre el marxismo y el feminismo como teorías sociales emancipadoras y las perspectivas del marxismo tras el colapso de los regímenes comunistas.

Neoplecostomus doceensis: a new loricariid species (Teleostei, Siluriformes) from the rio Doce basin and comments about its putative origin

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Estudo da inflexão da Serra do Garrote e sua influência na zona de falha de Vazante (MG)

The Vazante Fault Zone (VFZ), located northwestward of Minas Gerais, host the largest zinc deposit known in the Brazilian territory. This structure is hosted in Vazante’s Group rocks, a metassedimentary sequence of marine environment. Near Vazante is situated the south end of the VFZ. To the west, occur the Serra do Garrote inflexion, characterized by a curvature in the contact of Formations Serra do Garrote and Serra do Poço Verde. This structure is through the analysis of aerial imagery of the region and represented in the published geological maps. The objective of this work is to understand what causes this inflexion and determine whether it affects the VZF, causing a shift in the same, and possibly, in the mineralization as well. To this end, it was done a mapping work in the region covering the Serra do Garrote inflexion and the south end of the VFZ, in 1:25.000 scale, supplemented by petrographic description of thin section and geologic sections, with cooperated to the understanding of the structural evolution of the region. Data analysis allowed the identification of six deformation phases. The D1 an D2 phases generated the main foliation. The D3 phase generate kink bands folds, with NS axis and vertical axial plane. The fourth phase is responsible for generating the Vazante Fault Zone. The fifth phase produces low angle folds and shear zones, subparallel to S1//S2. The last phase generates folds with NW axis and vertical axial plane, with causes the inflection of lithologic contactas. Field observations also make possible the conclusion that the Vazante Fault Zone presents a south continuation, which is affected by deformation associated to D6 phase attributing to the trace of the VFZ a curved geometry, similar to that exhibited by lithologic contacts between units of the map

Annotated record and spectrochemical analyses of Mn nodules from Georgia Strait, British Columbia obtained during CNAV Laymore in 1970

A study of the distribution, dispersal and composition of surficial sediments in the Strait of Georgia, B.C., has resulted in the understanding of basic sedimentologic conditions within this area. The Strait of Georgia is: a long, narrow, semi-enclosed basin with a restricted circulation and a single, main, sediment source. The Fraser. River supplies practically all the sediment now being deposited in the Strait of Georgia, the bulk of it during the spring and summer freshet. This river is building a delta into the Strait from the east side near the south end. Ridges of Pleistocene deposits within the Strait and Pleistocene material around the margins, like bedrock exposures, provide local sources of sediment of only minor importance. Rivers and streams other than the Fraser contribute insignificant quantities of sediment to the Strait. Sandy sediments are concentrated in the vicinity of the delta, and in the area to the south and southeast. Mean grain size decreases from the delta toward the northwest along the axis of the Strait, and basinwards from the margins. Silts and clays are deposited in deep water west and north of the delta front, and in deep basins northwest of the delta. Poorly sorted sediments containing a gravel component are located near tidal passes, on the Vancouver Island shelf area, on ridge tops within the Strait, and with sandy sediments at the southeastern end of the study area. The Pleistocene ridges are areas of non-deposition, having at most a thin veneer of modern mud on their crests and upper flanks. The southeastern end of the study area contains a thick wedge of shandy sediment which appears to be part of an earlier delta of the Fraser River. Evidence suggests that it is now a site of active submarine erosion. Sediments throughout the Strait are compositionally extremely similar, with-Pleistocene deposits of the Fraser River drainage basin providing the principal, heterogeneous source. Gravels and coarse sands are composed primarily of lithic fragments, dominantly of dioritic to granodloritlc composition. Sand fractions exhibit increasing simplicity of mineralogy with decreasing grain-size. Quartz, felspar, amphibole and fine-grained lithic fragments are the dominant constituents of the finer sand grades. Coarse and medium silt fractions have compositions similar to the fine sands. Fine silts show an increase in abundance of phyllosilicate material, a feature even more evident in the clay-size fractions on Montmorillonite, illite, chlorite, quartz and feldspar are the main minerals in the coarse clay fraction, with minor mixed-layer clays and kaolinite. The fine clay fraction is dominated by montmorillonite, with lesser amounts of illite and chlorite. The sediments have high base-exchange capacities, related to a considerable content of montmorillonite. Magnesium is present in exchange positions in greater quantity in Georgia Strait sediments than in sediments from the Fraser River, indicating a preferential uptake of this element in the marine environment. Manganese nodules collected from two localities in the Strait imply slow sediment accumulation rates at these sites. Sedimentation rates on and close to the delta, and in the deep basins to the northwest, are high.

Dois tempos, uma medida: o cotidiano de Engenheiro Marsilac

A representação da cidade como um território densamente construído, estruturado pela intensidade da velocidade, da tecnologia, de modos de vida embasados na brevidade dos contatos, entre pessoas e entre pessoas e o espaço, não dá conta de explicar as diferenças encontradas ao se percorrer os vários espaços da cidade. Nos limites do território urbano, mais especificamente no extremo sul da cidade de São Paulo, deparamos com Engenheiro Marsilac, um bairro situado dentro de uma área de proteção ambiental, onde os modos de vida mesclam elementos de um passado tradicional com a modernidade proveniente da circularidade de pessoas, da comunicação e das mercadorias. Ademais, acrescenta-se aos mesmos, o convívio direto com áreas naturais, onde a preservação vai além do discurso, sendo incorporada no conjunto de práticas cotidianas. Neste contexto, o objetivo dessa pesquisa foi o de compreender essas relações sociais e as articulações espaciais presentes no dia a dia desse bairro. Para tanto, realizou-se uma pesquisa etnográfica que muitas vezes se estendeu para além da circunscrição do bairro, ao seguir os trajetos dos moradores pelos espaços da cidade.

Back Bay, Boston, Massachusetts, 1861 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Plan of lands on the Back Bay : belonging to the Boston Water Power Co., the Commonwealth, and other parties, showing the system of streets & grades as laid out and recommended by the Back Bay Commissioners, compiled and surveyed under the direction of the Commissioners by James Slade ; H.M. Wightman, surveyor ; E.R. Brown, de. It was printed by A. Meisel, lith., Dec. 31st, 1861. Covers Back Bay and South End, Boston, Massachusetts, and portions of Roxbury and Brookline. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Massachusetts State Plane Coordinate System, Mainland Zone (in Feet) (Fipszone 2001). All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, or other information associated with the principal map. This map shows features such as roads, railroads, drainage, property owners, selected public buildings, parks, radial distances from City Hall, and more. This layer is part of a selection of digitally scanned and georeferenced historic maps of Massachusetts from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of regions, originators, ground condition dates (1755-1922), scales, and purposes. The digitized selection includes maps of: the state, Massachusetts counties, town surveys, coastal features, real property, parks, cemeteries, railroads, roads, public works projects, etc.