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In the Río Valdez mouth, located in the southeastern coast of Fagnano lake, Tierra del Fuego, an outcrop of m thick lacustrine sediments was identified. Taking into account geomorphological and sedimentological surveys, such outcrop was interpreted as a rhythmic glacio-lacustrine deposit, formed in a frontal morainic complex during the Pleistocene. Ground magnetic and resistivity surveys were carried out, trying to determine the thickness and areal extension of these lacustrine sediments. A maximum E-W extension of ~ 220 m and a minimum NNW-SSE one of ~ 180 m were determined. A minimum thickness of ~ 20 m was estimated. Taking into account this thickness and an assumed average sedimentation rate, the natural dam that promoted the paleolake and their related lacustrine sediments could have existed previously to MIS 2, when the Last Glacial Maximum took place in the region. The applied geophysical methods proved to be a powerful tool for the investigation of palaeo-lake deposits.

A late Pleistocene glaciolacustrine record was studied at Fagnano Lake (54°35´S, 67°20´W), central Isla Grande de Tierra del Fuego, southernmost South America. Two profiles from the Río Valdéz outcrop were collected for isotopic, geochemical, sedimentological, and geophysical analyses. The sedimentological characteristics, such as rhythmites, presence of dropstones, absence of fossil record, and scarce presence of organic matter, suggest deposition in an ice-contact lake, possibly dammed by the Fagnano paleoglacier. Organic matter of C3 plant origin suggests certain cold and wet conditions. A chronology of the late Pleistocene outcrop was obtained from five 14C ages resulting in an age-depth model. The time span covered 49.01 cal ka BP to 32.14 cal ka BP. Based on the thickness of the deposit and the calculated average sedimentation rate, the glacial environment could have been present in the study area prior to the last glacial maximum, in agreement with the Inútil-San Sebastián paleoglacier. Both glaciers flowed from the same mountain ice sheet in the Darwin Cordillera, which makes it possible to infer a different behavior of this ice cap from those of the Patagonian Andes, perhaps forced by different atmospheric dynamics and proximity to the wet and cold subantarctic air masses.

This study aimed at analyzing how the critical success factors in the optics of its stakeholders, impact the effectiveness of the deployment project of the Air Force Sports Centre (CDAer). The main actors involved in the process were identified and subjected to an investigation through a questionnaire. The instrument was based on the critical success factors proposed by Pinto and Slevin (1987). The questions were adapted to the reality of the proposal in order to allow analysis of the degree of importance of each critical and strategic effectiveness and project tactics. The results showed that most of the stakeholders understand that the project follows the right track and has a high strategic rather than tactical effectiveness, but some need to receive more attention so that their expectations are met. The methodology enabled even to point out potential errors that may occur in the implementation of the CDAer and that they should be better managed. In conclusion, we suggest that a clear diagnosis of their problems is to be carried out, especially those related to customers, personnel, financial resources and the organizational structure, respecting the balance between the strategic and tactical effectiveness of the proposal in order to cater to all interested parties.

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This study was carried out on sediment cores collected with a gravity corer from Laguna Cháltel, an almost circular crater lake located in Patagonia, Argentina (49.9°S, 71°W). The main magnetic carrier was Ti-magnetite in the pseudo–single domain range. A model using magnetic grain size and concentration, previously applied to Laguna Potrok Aike to infer lake-level changes, was used for Laguna Cháltel. The main requirement to apply the model is uniform magnetic mineralogy, which is the case for Laguna Cháltel. After magnetic data were compared with previously studied lake levels, it was found that the magnetic proxies that best follow hydrologic changes are ARM/SIRM (anhysteretic remanent magnetisation/saturation of isothermal remanent magnetisation) and ARM. The concentration proxy (ARM measured with a 100 mT alternating field and 0.05 mT direct field) was also used as wind indicator. High wind strength was found at around 3650 cal yr BP, and low wind strength for the last century. ARM/SIRM and ARM were used to infer the strength of fluvial runoff into the lake for a core collected close to the shore and near a tributary. The results show that the magnetic model is promising for inferring lake-level variations, particularly in Patagonian lakes.