History of the Pacific Railway Co.'s 1st mortgage 30 year 6 per cent paramount lien bonds /

Cover title.

Service report on technical education, with special reference to the Baltimore & Ohio railroad service. Dr. W.T. Barnard October 1st, 1886.

Mode of access: Internet.

Shall the extension or recreating of the Camden & Amboy Railroad monopoly be permitted by the people of New Jersey, and made perpetual?

Cover title.

Central Vermont R.R. reorganization : House bill no. 70. Hearing before the Railroad committees of the Senate and House of Representatives, sitting jointly. Argument in behalf of the bill, November 10, 1898 /

Mode of access: Internet.

Judah P. Benjamin collection, undated, 1838-1942.

The collection consists of 25 letters written by Benjamin between 1838 and 1881 on a variety of subjects, four Confederate notes and two bonds bearing his picture, miscellaneous items about Benjamin (1893-1942), nine issues of the Congressional globe with speeches by Benjamin, as well as separate copies of his printed speeches, and a photostatic copy of the "Diary of Events" (400 pp.) kept by Benjamin, the original of which is in the Library of Congress (1862-1864).

Seismic structure above and below the core-mantle boundary

Seismic structure above and below the core-mantle boundary (CMB) has been studied through use of travel time and waveform analyses of several different seismic wave groups. Anomalous systematic trends in observables document mantle heterogeneity on both large and small scales. Analog and digital data has been utilized, and in many cases the analog data has been optically scanned and digitized prior to analysis.

Differential travel times of S - SKS are shown to be an excellent diagnostic of anomalous lower mantle shear velocity (V s) structure. Wavepath geometries beneath the central Pacific exhibit large S- SKS travel time residuals (up to 10 sec), and are consistent with a large scale 0(1000 km) slower than average V_s region (≥3%). S - SKS times for paths traversing this region exhibit smaller scale patterns and trends 0(100 km) indicating V_s perturbations on many scale lengths. These times are compared to predictions of three tomographically derived aspherical models: MDLSH of Tanimoto [1990], model SH12_WM13 of Suet al. [1992], and model SH.10c.17 of Masters et al. [1992]. Qualitative agreement between the tomographic model predictions and observations is encouraging, varying from fair to good. However, inconsistencies are present and suggest anomalies in the lower mantle of scale length smaller than the present 2000+ km scale resolution of tomographic models. 2-D wave propagation experiments show the importance of inhomogeneous raypaths when considering lateral heterogeneities in the lowermost mantle.

A dataset of waveforms and differential travel times of S, ScS, and the arrival from the D" layer, Scd, provides evidence for a laterally varying V_s velocity discontinuity at the base of the mantle. Two different localized D" regions beneath the central Pacific have been investigated. Predictions from a model having a V_s discontinuity 180 km above the CMB agree well with observations for an eastern mid-Pacific CMB region. This thickness differs from V_s discontinuity thicknesses found in other regions, such as a localized region beneath the western Pacific, which average near 280 km. The "sharpness" of the V_s jump at the top of D", i.e., the depth range over which the V_s increase occurs, is not resolved by our data, and our data can in fact may be modeled equally well by a lower mantle with the increase in V_s at the top of D" occurring over a 100 krn depth range. It is difficult at present to correlate D" thicknesses from this study to overall lower mantle heterogeneity, due to uncertainties in the 3-D models, as well as poor coverage in maps of D" discontinuity thicknesses.

P-wave velocity structure (V_p) at the base of the mantle is explored using the seismic phases SKS and SPdKS. SPdKS is formed when SKS waves at distances around 107° are incident upon the CMB with a slowness that allows for coupling with diffracted P-waves at the base of the mantle. The P-wave diffraction occurs at both the SKS entrance and exit locations of the outer core. SP_dKS arrives slightly later in time than SKS, having a wave path through the mantle and core very close to SKS. The difference time between SKS and SP_dKS strongly depends on V_p at the base of the mantle near SK Score entrance and exit points. Observations from deep focus Fiji-Tonga events recorded by North American stations, and South American events recorded by European and Eurasian stations exhibit anomalously large SP_dKS - SKS difference times. SKS and the later arriving SP_dKS phase are separated by several seconds more than predictions made by 1-D reference models, such as the global average PREM [Dziewonski and Anderson, 1981] model. Models having a pronounced low-velocity zone (5%) in V_p in the bottom 50-100 km of the mantle predict the size of the observed SP_dK S-SKS anomalies. Raypath perturbations from lower mantle V_s structure may also be contributing to the observed anomalies.

Outer core structure is investigated using the family of SmKS (m=2,3,4) seismic waves. SmKS are waves that travel as S-waves in the mantle, P-waves in the core, and reflect (m-1) times on the underside of the CMB, and are well-suited for constraining outermost core V_p structure. This is due to closeness of the mantle paths and also the shallow depth range these waves travel in the outermost core. S3KS - S2KS and S4KS - S3KS differential travel times were measured using the cross-correlation method and compared to those from reflectivity synthetics created from core models of past studies. High quality recordings from a deep focus Java Sea event which sample the outer core beneath the northern Pacific, the Arctic, and northwestern North America (spanning 1/8th of the core's surface area), have SmKS wavepaths that traverse regions where lower mantle heterogeneity is pre- dieted small, and are well-modeled by the PREM core model, with possibly a small V_p decrease (1.5%) in the outermost 50 km of the core. Such a reduction implies chemical stratification in this 50 km zone, though this model feature is not uniquely resolved. Data having wave paths through areas of known D" heterogeneity (±2% and greater), such as the source-side of SmKS lower mantle paths from Fiji-Tonga to Eurasia and Africa, exhibit systematic SmKS differential time anomalies of up to several seconds. 2-D wave propagation experiments demonstrate how large scale lower mantle velocity perturbations can explain long wavelength behavior of such anomalous SmKS times. When improperly accounted for, lower mantle heterogeneity maps directly into core structure. Raypaths departing from homogeneity play an important role in producing SmKS anomalies. The existence of outermost core heterogeneity is difficult to resolve at present due to uncertainties in global lower mantle structure. Resolving a one-dimensional chemically stratified outermost core also remains difficult due to the same uncertainties. Restricting study to higher multiples of SmKS (m=2,3,4) can help reduce the affect of mantle heterogeneity due to the closeness of the mantle legs of the wavepaths. SmKS waves are ideal in providing additional information on the details of lower mantle heterogeneity.

Interannual variability in the PFEG coastal upwelling indices

Numerous studies examine decadal-scale variability in basin-scale parameters in the Northern Pacific. Characterizing such interannual-to-interdecadal variability is essential to identifying long-term climate changes. The Pacific Fisheries Environmental Group (PFEG) coastal upwelling indices display variability on these time scales and may help explain the mechanisms responsible for such climate variability. ... In this study, examination of 49-year time series of monthly mean upwelling indices at the 15 PFEG-standard positions along the west coast of North America revealed variability on large spatial scales as well as temporal scales.

Interannual to decadal time-scale variations in glacier mass balance [abstract]

EXTRACT (SEE PDF FOR FULL ABSTRACT): The mass balance of glaciers depends on the seasonal variation in precipitation, temperature, and insolation. For glaciers in western North America, these meteorological variables are influenced by the large-scale atmospheric circulation over the northern Pacific Ocean. The purpose of this study is to gain a better understanding of the relationship between mass balance at glaciers in western North America and the large-scale atmospheric effects at interannual and decadal time scales.

Erie & Niagara Railway Collection, 1864-1884

William Alexander Thomson (1816-1878) was a promoter and developer of railway systems in western Ontario. He incorporated the Fort Erie Railroad Company in 1857, purchased the Erie and Ontario Railroad in 1863, and incorporated the Erie and Niagara Extension Railway Company in 1868 (later renamed the Canada Southern Railway). Thomson was also elected to the House of Commons for Welland in 1872, and re-elected in 1874. He was known for his support of public management of the currency and is seen as a pioneer advocate of government monetary policy. He was also an advocate of radical agrarian economic doctrine, believing that Canadian laws favoured mercantile interests over those of the producers of goods, and that this hindered national development.

Proceso de internacionalización de los grupos económicos: el caso colombiano

En un mundo globalizado, las estructuras organizacionales han complejizado en mayor medida su operación. Si bien la Teoría de la organización, menciona el comportamiento de una empresa como un sistema, la mundialización permite que el entorno de dicho sistema se vuelva mucho más ininteligible de manera que la dependencia entre organizaciones, ya sean globales o locales, sea más fuerte entre sí. Este trabajo fue elaborado con el fin de hacer un análisis sobre la existencia y constitución de los Grupos Económicos de Colombia.

Eficiência em serviço de IT terceirizados : o caso CPR/IBM

Alegando razões de eficiência, muitas firmas vêm crescentemente adotando a terceirização de TI como um meio de conseguir economia de custos, maior foco em suas operações e alinhamento estratégico. Não obstante as razões verbalmente alegadas pelas empresas para terceirizar serviços de TI todas elas buscam a prestação de serviço em TI como uma forma de transferir a eficiência da prestadora de serviços para a empresa cliente. Com a competitividade cada vez maior entre as prestadoras de serviço e por mais que as empresas prestadoras de serviço tentem diferenciar-se entre si, o fato é que não existem muitas diferenças que possam saltar a vista entre os grandes prestadores de serviço de terceirização de TI atuais, pois fornecem de forma quase que indiferente custo, qualidade, expertise técnica, métodos e processos, experiência comprovada, boa saúde financeira, presença global. Mas porque alguns provedores de serviço de TI conseguem ser mais eficiente que seus clientes? Porque os departamentos de TI, das empresas clientes, têm dificuldade de copiar o modelo destes fornecedores e operar com os mesmos patamares de eficiência? Quais as dificuldades e barreiras que existem? Quais as melhores práticas adotadas pela provedora de serviço e pelo cliente para realizar uma terceirização de serviços de TI com sucesso? Este trabalho analisa em caráter exploratório, através de um estudo de caso, a terceirização de TI feita pela CPR (Canadian Pacific Railroad) em 2003 junto à IBM Canadá, aonde seu custo contratual teve uma redução de cerca de 20% do custo original de operação da CPR , buscando identificar porque que algumas empresas prestadoras de serviço de TI conseguem ser mais eficiente que seus clientes, porque não se optou em realizar a transformação internamente e quais as melhores práticas adotadas pela provedora de serviço para realizar uma terceirização de serviços de TI com sucesso. Para isto, o trabalho parte da literatura para indicar possíveis fatores motivadores para a terceirização assim como as melhores práticas de gestão utilizadas atualmente pelas prestadoras de serviço e empresas clientes para uma terceirização de serviços de TI. Posteriormente segue para uma etapa de campo, em busca de elementos que permitam a análise de sua relevância. Os fundamentos teóricos para a terceirização se basearam na: Teoria de Custos de Transação (TCT -Transaction Cost Theory) e na Teoria Baseada em Recursos (RBT-Resource Base Theory). Na etapa de campo explorou-se um projeto de terceirização de infra-estrutura de TI entre a IBM e CPR (Canadian Pacific Railroad), aonde foram feitas entrevistas estruturadas com os gestores do cliente CPR, gestores da prestadora de serviços IBM, assim como analisados materiais produzidos pelo projeto, com o objetivo de identificar porque algumas empresas prestadoras de serviço de TI conseguem ser mais eficiente que seus clientes. Os resultados encontrados apontam que a CPR possuía uma menor eficiência do que a IBM por razões: de foco, de processo e de escala. Tais características são em si não facilmente imitáveis pela empresa cliente tornando a parceria estratégica a melhor solução para o aumento de eficiência operacional na empresa cliente.

Deformational evolution of a Cretaceous subduction complex: Elephant Island, South Shetland Islands, Antarctica

New structural data from Elephant Island and adjacent islands are presented with the objective to improve the understanding of subduction kinematics in the area northeast of the Antarctic Peninsula. on the island, a first deformation phase, D-1, produced a strong SL fabric with steep stretching and mineral lineations, partly defined by relatively high pressure minerals, such as crossite and glaucophane. D-1 is interpreted to record southward subduction along an E-W trench with respect to the present position of the island. A second phase, D-2, led to intense folding with steep E-W-trending axial surfaces. The local presence of sinistral C'-type sheer bands related to this phase and the oblique inclination of the L-2 stretching lineations are the main arguments to interpret this phase as representing oblique sinistral transpressive shear along steep, approximately E-W-trending shear zones, with the northern (Pacific) block going down with respect to the southern (Antarctic Peninsula) block. The sinistral strike-slip component may represent a trench-linked strike-slip movement as a consequence of oblique subduction. Lithostatic pressure decreased and temperature increased to peak values during D-2, interpreted to represent the collision of thickened oceanic crust with the active continental margin. The last deformation phase, D-3, is characterised by post-metamorphic kink bands, partially forming conjugate sets consistent with E-W shortening and N-S extension. The rock units that underlie the island probably rotated during D-3, in Cenozoic times, together with the trench, from an NE-SW to the present ENE-WSW position, during the progressive opening of the Scotia Sea. The similarity between the strain orientation of D-3 and that of the sinistral NE-SW Shackleton Fracture Zone is consistent with this interpretation. (C) 2000 Elsevier B.V. B.V. All rights reserved.

Para além do Rio Grande: Os impactos da economia paulista sobre O Triângulo Mineiro

In this work our intention was to investigate the impact of Sao Paulo's coffee economy on the Minas Gerais Triangle Region, during its penetration into the area because of the extension of the Mogiana Railroad Company in 1889. We attempt to understand the impact caused along this coffee railroad in a region where this product almost did not exist, and the changes that occurred to the economic panorama of the region. Furthermore we have taken as an example, the city of Uberaba, the most important, in this region at that time.