An analysis of Venezuela's foreign policy during the period of the Betancourt doctrine and Caldera's ideological pluralism

This thesis examines the foreign policy of Venezuela during the period of the Betancourt Doctrine (1945-1948 and 1959-1963), and Caldera's Ideological Pluralism (1969-1973). The study seeks to determine whether, and to what extent the pursuit of political and economic interests and ideology determined Venezuela's foreign policy. Based on primary and secondary sources, this study examines political economy and ideology and how these affected the outcome of Venezuela's foreign policy. The major finding of this thesis is that Venezuelan foreign policy was a pragmatic one but it was rationalized within an ideological framework. In fact, Venezuela was most concerned in pursuing its domestic economic and political interests but these were hidden behind an ideological facade.

A model of the hydrothermal system at Casa Diablo in Long Valley, California, based on resistivity profiles and soil mercury analyses

A description and model of the near-surface hydrothermal system at Casa Diablo, with its implications for the larger-scale hydrothermal system of Long Valley, California, is presented. The data include resistivity profiles with penetrations to three different depth ranges, and analyses of inorganic mercury concentrations in 144 soil samples taken over a 1.3 by 1.7 km area. Analyses of the data together with the mapping of active surface hydrothermal features (fumaroles, mudpots, etc.), has revealed that the relationship between the hydrothermal system, surface hydrothermal activity, and mercury anomalies is strongly controlled by faults and topography. There are, however, more subtle factors responsible for the location of many active and anomalous zones such as fractures, zones of high permeability, and interactions between hydrothermal and cooler groundwater. In addition, the near-surface location of the upwelling from the deep hydrothermal reservoir, which supplies the geothermal power plants at Casa Diablo and the numerous hot pools in the caldera with hydrothermal water, has been detected. The data indicate that after upwelling the hydrothermal water flows eastward at shallow depth for at least 2 km and probably continues another 10 km to the east, all the way to Lake Crowley.