Los indios de Riobamba y la revolución de Quito, 1757-1814 (Debates)

Este estudio analiza las diversas posiciones asumidas por los indígenas frente a la Revolución de Quito de 1809. Siguiendo a dos personajes clave del Corregimiento de Riobamba, un cacique y un indio, busca las causas de la adhesión o del rechazo. Con ese propósito se estudian varias coyunturas que empiezan a mediados del siglo XVIII, desde las peticiones caciquiles y el posterior reacomodo de las autoridades indígenas efectuadas por los reformistas borbónicos, las continuas imposiciones tributarias y el terremoto de 1797, que desembocan en el levantamiento indígena de 1803. El artículo muestra una ruptura radical entre los indios del común y el pensamiento criollo fundador de la nación.

El legado de Cádiz: ciudadanía y cultura política en la Gobernación de Cuenca, 1812-1814 (Estudios)

Este trabajo analiza el legado de las Cortes de Cádiz y de la Constitución de 1812 en Cuenca entre 1812 y 1814. Estudia los principales cambios políticos relacionados con los derechos de diversos actores sociales, así como el rompimiento de antiguas formas de relación social. Los cambios políticos se relacionaron con la introducción de nuevos conceptos y prácticas como ciudadanía, soberanía, elección y representación, tanto en el mundo criollomestizo como en el indígena (población cañari) de la provincia. Se analiza la abolición del tributo indígena, el servicio personal y la mita, además se estudian algunos cambios administrativopolíticos como la creación de los ayuntamientos constitucionales, las diputaciones provinciales y nacionales.

Las Guyanas holandesas en América Latina (1600-1814) [Estudios]

This article starts by considering the fact that the Guyanas can be understood as an atypical region in the Latin-American context. The lapse of analysis of this study is from 1600 to 1814, period of development of Dutch Guyanas, which was the base of the Surinam Republic and the Co-operative Republic of Guyana. These are highlighted for being the unique Latin-American entities that were not colonized by the Catholics Monarchies, for the absence of missionary activities until 1735, and also for the absence of private action. These colonies offer an interesting study field about comparative development with other South American regions.

Sailing through stone. Carved ships and the rockface at Revheim, southwest Norway

The relationship between rock art and the material qualities of the rock surface on which it is executed is investigated. The case study of Revheim, Rogaland, Southwest Norway, is the starting-point for a discussion on the way in which the contours of the rock, quartz outcrops and the flow of water across the rock surface affect the placement of images on the rock. It is argued that a fuller examination of the interrelationship between rock and rock art provides a more coherent interpretation of rock art images.

Mapping the spatial distribution of geomorphological processes in the Okstindan area of northern Norway, using Geomorphic Process Units as derived from remote sensing and ground survey

The delineation of Geomorphic Process Units (GPUs) aims to quantify past, current and future geomorphological processes and the sediment flux associated with them. Five GPUs have been identified for the Okstindan area of northern Norway and these were derived from the combination of Landsat satellite imagery (TM and ETM+) with stereo aerial photographs (used to construct a Digital Elevation Model) and ground survey. The Okstindan study area is sub-arctic and mountainous and is dominated by glacial and periglacial processes. The GPUs exclude the glacial system (some 37% of the study area) and hence they are focussed upon periglacial and colluvial processes. The identified GPUs are: 1. solifluction and rill erosion; 2. talus creep, slope wash and rill erosion; 3. accumulation of debris by rock and boulder fall; 4. rockwalls; and 5. stable ground with dissolved transport. The GPUs have been applied to a ‘test site’ within the study area in order to illustrate their potential for mapping the spatial distribution of geomorphological processes. The test site within the study area is a catchment which is representative of the range of geomorphological processes identified.

Seasonal trends in the stable isotopic composition of snow and meltwater runoff in a subarctic catchment at Okstindan, Norway

Seasonal variations in the stable isotopic composition of snow and meltwater were investigated in a sub-arctic, mountainous, but non-glacial, catchment at Okstindan in northern Norway based on analyses of delta(18)O and deltaD. Samples were collected during four field periods (August 1998; April 1999; June 1999 and August 1999) at three sites lying on an altitudinal transect (740-970 m a.s.l.). Snowpack data display an increase in the mean values of delta(18)O (increasing from a mean value of - 13.51 to - 11.49% between April and August), as well as a decrease in variability through the melt period. Comparison with a regional meteoric water line indicates that the slope of the delta(18)O - deltaD line for the snowpacks decreases over the same period, dropping from 7.49 to approximately 6.2. This change points to the role of evaporation in snowpack ablation and is confirmed by the vertical profile of deuterium excess. Snowpack seepage data, although limited, also suggest reduced values of deltaD, as might be associated with local evaporation during meltwater generation. In general, meltwaters were depleted in delta(18)O relative to the source snowpack at the peak of the melt (June), but later in the year (August) the difference between the two was not statistically significant. The diurnal pattern of isotopic composition indicates that the most depleted meltwaters coincide with the peak in temperature and, hence, meltwater production.

Sediment magnetic properties of glacial till deposited since the Little Ice Age maximum for selected glaciers at Svartisen and Okstindan, northern Norway

Samples of glacial till deposited since the Little Ice Age (LIA) maximum by two glaciers, North Bogbre at Svartisen and Corneliussen-breen at Okstindan, northern Norway, were obtained from transects running from the current glacier snout to the LIA (c. AD 1750) limit. The samples were analysed to determine their sediment magnetic properties, which display considerable variability. Significant trends in some magnetic parameters are evident with distance from the glacier margin and hence length of subaerial exposure. Magnetic susceptibility (X) decreases away from the contemporary snout, perhaps due to the weathering of ferrimagnetic minerals into antiferromagnetic forms, although this trend is generally not statistically significant. Trends in the ratios of soft IRM/hard IRM which are statistically significant support this hypothesis, suggesting that antiferromagnetic minerals are increasing relative to ferrimagnetic minerals towards the LIA maximum. Backfield ratios (IRM -100 mT/SIRM) also display a significant and strong trend towards magnetically harder behaviour with proximity to the LIA maximum. Thus, by employing a chronosequence approach, it may be possible to use sediment magnetics data as a tool for reconstructing glacier retreat in areas where more traditional techniques, such as lichenometry, are not applicable.