SLOPE STABILITY ANALYSIS OF MOUNT MEAGER, SOUTH-WESTERN BRITISH COLUMBIA, CANADA

The Mount Meager Volcanic Complex (MMVC) in south-western British Columbia is a potentially active, hydrothermally altered massif comprising a series of steep, glaciated peaks. Climatic conditions and glacial retreat has led to the further weathering, exposure and de-buttressing of steep slopes composed of weak, unconsolidated material. This has resulted in an increased frequency of landslide events over the past few decades, many of which have dammed the rivers bordering the Complex. The breach of these debris dams presents a risk of flooding to the downstream communities. Preliminary mapping showed there are numerous sites around the Complex where future failure could occur. Some of these areas are currently undergoing progressive slope movement and display features to support this such as anti-scarps and tension cracks. The effect of water infiltration on stability was modelled using the Rocscience program Slide 6.0. The main site of focus was Mount Meager in the south- east of the Complex where the most recent landslide took place. Two profiles through Mount Meager were analysed along with one other location in the northern section of the MMVC, where instability had been detected. The lowest Factor of Safety (FOS) for each profile was displayed and an estimate of the volume which could be generated was deduced. A hazard map showing the inundation zones for various volumes of debris flows was created from simulations using LAHARZ. Results showed the massif is unstable, even before infiltration. Varying the amount of infiltration appears to have no significant impact on the FOS annually implying that small changes of any kind could also trigger failure. Further modelling could be done to assess the impact of infiltration over shorter time scales. The Slide models show the volume of material that could be delivered to the Lillooet River Valley to be of the order of 109 m3 which, based on the LAHARZ simulations, would completely inundate the valley and communities downstream. A major hazard of this is that the removal of such a large amount of material has the potential to trigger an explosive eruption of the geothermal system and renew volcanic activity. Although events of this size are infrequent, there is a significant risk to the communities downstream of the complex.

Bilan des pratiques professionnelles de nouvelles enseignantes et de nouveaux enseignants du collégial suite à l'autoévaluation de leur enseignement

La présente recherche, à caractère descriptif, avait comme objectif général de dresser un bilan des pratiques professionnelles de nouvelles enseignantes et de nouveaux enseignants du collégial à partir d'une autoévaluation de leur enseignement. Le contexte particulier dans lequel s'inscrit l'enseignement collégial suscite bien des réflexions quant à l'insertion professionnelle du nouveau personnel enseignant. La diversité des profils des enseignantes et des enseignants qui entrent au collégial avec ou sans formation initiale en pédagogie, la complexité de la tâche et le renouvellement massif du corps professoral accentuent le rôle important des institutions dans le soutien à offrir, et ce, tout au long du développement professionnel et plus particulièrement dans la période d'insertion professionnelle. Les fondements de la recherche s'appuient sur les concepts de développement professionnel, d'insertion professionnelle et d'identité professionnelle et sur la politique de gestion des ressources humaines des collèges. Cette politique s'applique à travers les programmes qui y sont rattachés, notamment le programme d'insertion professionnelle et celui d'évaluation des enseignants. La grille d'analyse a été élaborée à partir du profil de compétences du Conseil supérieur de l'éducation. Le fait que les enseignantes et les enseignants participent à un programme d'évaluation dans une optique de développement professionnel a orienté les choix méthodologiques de la recherche et a permis d'atteindre les objectifs spécifiques. Ceux-ci étaient de recueillir les perceptions qu'ont les enseignantes et les enseignants novices de leurs pratiques professionnelles lors de l'autoévaluation de leur enseignement, d'effectuer un bilan de ces pratiques professionnelles et de cibler les éléments qui semblent les plus difficiles, cela pouvant servir à dégager des pistes d'accompagnement pour le nouveau personnel enseignant. Une approche méthodologique interprétative a été adoptée. Les données provenaient d'un organisme externe, le Centre d'Intervention et de Recherche en Évaluation du Personnel Enseignant, avec le consentement éclairé des individus constituant l'échantillon. Celui-ci compte 30 enseignantes et enseignants du secteur régulier de quatre collèges publics francophones, qui avaient deux ans et moins d'expérience en enseignement collégial. Une analyse combinée des deux types de données — les données issues des réponses fermées des questionnaires d'autoévaluation et celles issues des variables contextuelles et des commentaires — a fait ressortir les forces et les difficultés que le nouveau personnel éprouve dans ses pratiques, auxquelles on puisse apporter une valorisation ou un soutien, selon les besoins. En ce sens, il apparaît d'une part, que les modes d'apprentissage de la profession enseignante sont fort diversifiés. D'autre part, la majorité des nouvelles enseignantes et des nouveaux enseignants qui entrent dans la profession rencontrent des difficultés liées aux dimensions pédagogiques et didactiques du métier. Cela a permis de dégager des pistes qui ont trait, par exemple, à la gestion de classe, à l'évaluation des apprentissages ou encore à l'utilisation de la langue d'enseignement. Ces pistes pourraient éventuellement assurer le soutien de ce nouveau personnel et maintenir chez lui l'enthousiasme et la passion qui le motivent.

Bilan des pratiques professionnelles de nouvelles enseignantes et de nouveaux enseignants du collégial suite à l'autoévaluation de leur enseignement.

La présente recherche, à caractère descriptif, avait comme objectif général de dresser un bilan des pratiques professionnelles de nouvelles enseignantes et de nouveaux enseignants du collégial à partir d'une autoévaluation de leur enseignement. Le contexte particulier dans lequel s'inscrit l'enseignement collégial suscite bien des réflexions quant à l'insertion professionnelle du nouveau personnel enseignant. La diversité des profils des enseignantes et des enseignants qui entrent au collégial avec ou sans formation initiale en pédagogie, la complexité de la tâche et le renouvellement massif du corps professoral accentuent le rôle important des institutions dans le soutien à offrir, et ce, tout au long du développement professionnel et plus particulièrement dans la période d'insertion professionnelle. Les fondements de la recherche s'appuient sur les concepts de développement professionnel, d'insertion professionnelle et d'identité professionnelle et sur la politique de gestion des ressources humaines des collèges. Cette politique s'applique à travers les programmes qui y sont rattachés, notamment le programme d'insertion professionnelle et celui d'évaluation des enseignants. La grille d'analyse a été élaborée à partir du profil de compétences du Conseil supérieur de l'éducation. Le fait que les enseignantes et les enseignants participent à un programme d'évaluation dans une optique de développement professionnel a orienté les choix méthodologiques de la recherche et a permis d'atteindre les objectifs spécifiques. Ceux-ci étaient de recueillir les perceptions qu'ont les enseignantes et les enseignants novices de leurs pratiques professionnelles lors de l'autoévaluation de leur enseignement, d'effectuer un bilan de ces pratiques professionnelles et de cibler les éléments qui semblent les plus difficiles, cela pouvant servir à dégager des pistes d'accompagnement pour le nouveau personnel enseignant. Une approche méthodologique interprétative a été adoptée. Les données provenaient d'un organisme externe, le Centre d'Intervention et de Recherche en Évaluation du Personnel Enseignant, avec le consentement éclairé des individus constituant l'échantillon. Celui-ci compte 30 enseignantes et enseignants du secteur régulier de quatre collèges publics francophones, qui avaient deux ans et moins d'expérience en enseignement collégial. Une analyse combinée des deux types de données - les données issues des réponses fermées des questionnaires d'autoévaluation et celles issues des variables contextuelles et des commentaires - a fait ressortir les forces et les difficultés que le nouveau personnel éprouve dans ses pratiques, auxquelles on puisse apporter une valorisation ou un soutien, selon les besoins. En ce sens, il apparaît d'une part, que les modes d'apprentissage de la profession enseignante sont fort diversifiés. D'autre part, la majorité des nouvelles enseignantes et des nouveaux enseignants qui entrent dans la profession rencontrent des difficultés liées aux dimensions pédagogiques et didactiques du métier. Cela a permis de dégager des pistes qui ont trait, par exemple, à la gestion de classe, à l'évaluation des apprentissages ou encore à l'utilisation de la langue d'enseignement. Ces pistes pourraient éventuellement assurer le soutien de ce nouveau personnel et maintenir chez lui l'enthousiasme et la passion qui le motivent.

NEW DATA ON THE CHRONOLOGY OF THE VALE DO FORNO SEDIMENTARY SEQUENCE (LOWER TAGUS RIVER TERRACE STAIRCASE) AND ITS RELEVANCE AS FLUVIAL ARCHIVE OF THE MIDDLE PLEISTOCENE IN WESTERN IBERIA

NEW DATA ON THE CHRONOLOGY OF THE VALE DO FORNO SEDIMENTARY SEQUENCE (LOWER TAGUS RIVER TERRACE STAIRCASE) AND ITS RELEVANCE AS FLUVIAL ARCHIVE OF THE MIDDLE PLEISTOCENE IN WESTERN IBERIA Pedro P. Cunha 1, António A. Martins 2, Jan-Pieter Buylaert 3,4, Andrew S. Murray 4, Luis Raposo 5, Paolo Mozzi 6, Martin Stokes 7 1 MARE - Marine and Environmental Sciences Centre, Department of Earth Sciences, University of Coimbra, Portugal: pcunha@dct.uc.pt 2 MARE - Marine and Environmental Sciences Centre, Dep. Geociências, University of Évora, Portugal; aam@uevora.pt 3 Centre for Nuclear Technologies, Technical University of Denmark, Risø Campus, Denmark; jabu@dtu.dk 4 Nordic Laboratory for Luminescence Dating, Aarhus University, Risø DTU, Denmark; anmu@dtu.dk 5 Museu Nacional de Arqueologia, Lisboa, Portugal; 3raposos@sapo.pt 6 Department of Geosciences, University of Padova, Italy; paolo.mozzi@unipd.it 7 School of Geography, Earth and Environmental Sciences, University of Plymouth, UK; m.stokes@plymouth.ac.uk The stratigraphic units that record the evolution of the Tagus River in Portugal (study area between Vila Velha de Ródão and Porto Alto villages; Fig. 1) have different sedimentary characteristics and lithic industries (Cunha et al., 2012): - a culminant sedimentary unit (the ancestral Tagus, before the drainage network entrenchment) – SLD13 (+142 to 262 m above river bed – a.r.b.; with probable age ca. 3,6 to 1,8 Ma), without artefacts; - T1 terrace (+84 to 180 m; ca. 1000? to 900 ka), without artefacts; - T2 terrace (+57 to 150 m; top deposits with a probable age ca. 600 ka), without artefacts; - T3 terrace (+43 to 113 m; ca. 460 to 360? ka), without artefacts; - T4 terrace (+26 to 55 m; ca. 335 a 155 ka), Lower Paleolithic (Acheulian) at basal and middle levels but early Middle Paleolithic at top levels; - T5 terrace (+5 to 34 m; 135 to 73 ka), Middle Paleolithic (Mousterian; Levallois technique); - T6 terrace (+3 to 14 m; 62 to 32 ka), late Middle Paleolithic (late Mousterian); - Carregueira Sands (aeolian sands) and colluvium (+3 a ca. 100 m; 32 to 12 ka), Upper Paleolithic to Epipaleolithic; - alluvial plain (+0 to 8 m; ca. 12 ka to present), Mesolithic and more recent industries. The differences in elevation (a.r.b.) of the several terrace staircases results from differential uplift due to active faults. Longitudinal correlation with the terrace levels indicates that a graded profile ca. 200 km long was achieved during terrace formation periods and a strong control by sea base level was determinant for terrace formation. The Neogene sedimentary units constituted the main source of sediments for the fluvial terraces (Fig. 2). Geomorphological mapping, coupled with lithostratigraphy, sedimentology and luminescence dating (quartz-OSL and K-feldspar post-IRIR290) were used in this study focused on the T4 terrace, which comprises a Lower Gravels (LG) unit and an Upper Sand (US) unit. The thick, coarse and dominantly massive gravels of the LG unit indicate deposition by a coarse bed-load braided river, with strong sediment supply, high gradient and fluvial competence, during conditions of rapidly rising sea level. Luminescence dating only provided minimum ages but it is probable that the LG unit corresponds to the earlier part of the MIS9 (ca. 335 to 325 ka), immediately postdating the incision promoted by the very low sea level (reaching ca. -140 m) during MIS10 (362 to 337 ka), a period of relatively cold climate conditions with weak vegetation cover on slopes and low sea level. Fig. 1. Main Portuguese reaches in which the Tagus River can be divided (Lower Tagus Basin): I – from the Spanish border to Arneiro (a general E–W trend, mainly consisting of polygonal segments); II – from Arneiro to Gavião (NE–SW); III – from Gavião to Arripiado (E–W); IV – from Arripiado to Vila Franca de Xira (NNE-SSW); V – from Vila Franca de Xira to the Atlantic shoreline. The faults considered to be the limit of the referred fluvial sectors are: F1 – Ponsul-Arneiro fault (WSW-ENE); F2 – Gavião fault (NW-SE); F3 – Ortiga fault (NW-SE); F4 – Vila Nova da Barquinha fault (W-E); F5 – Arripiado-Chamusca fault (NNE-SSW). 1 – estuary; 2 – terraces; 3 – faults; 4 – Tagus main channel. The main Iberian drainage basins are also represented (inset). The lower and middle parts of the US unit, comprising an alternation of clayish silts with paleosols and minor sands to the east (flood-plain deposits) and sand deposits to the west (channel belt), have a probable age of ca. 325 to 200 ka. This points to formation during MIS9 to MIS7, under conditions of high to medium sea levels and warm to mild conditions. The upper part of the US unit, dominated by sand facies and with OSL ages of ca. 200 to 154 ka, correlates with the early part of the MIS6. During this period, progradation resulted from climate deterioration and relative depletion of vegetation that promoted enhanced sediment production in the catchment, coupled with initiation of sea-level lowering that increased the longitudinal slope. The Vale do Forno and Vale da Atela archaeological sites (Alpiarça, central Portugal) document the earliest human occupation in the Lower Tagus River, well established in geomorphological and environmental terms, within the Middle Pleistocene. The Lower Palaeolithic sites were found on the T4 terrace (+26 m, a.r.b.). The oldest artefacts previously found in the LG unit, display crude bifacial forms that can be attributed to the Acheulian, with a probable age of ca. 335 to 325 ka. The T4 US unit has archaeological sites stratigraphically documenting successive phases of an evolved Acheulian, that probably date ca. 325 to 300 ka. Notably, these Lower Palaeolithic artisans were able to produce tools with different sophistication levels, simply by applying different strategies: more elaborated reduction sequences in case of bifaces and simple reduction sequences to obtain cleavers. Fig. 2. . Simplified geologic map of the Lower Tagus Cenozoic basin, adapted from the Carta Geológica de Portugal, 1/500000, 1992). The study area (comprising the Vale do Forno and Vale de Atela sites) is located on the more upstream sector of the Lower Tagus River reach IV, between Arripiado and Chamusca villages. 1 – alluvium (Holocene); 2 – terraces (Pleistocene); 3 – sands, silts and gravels (Paleogene to Pliocene); 4 – Sintra Massif (Cretaceous); 5 – limestones, marls, silts and sandstones (Mesozoic); 6 – quartzites (Ordovician); 7 – basement (Proterozoic to Palaeozoic); 8 – main fault. The main Portuguese reaches of the Tagus River are identified (I to V). The VF3 site (Milharós), containing a Final Acheulian industry, with fine and elaborated bifaces) found in a stratigraphic level located between the T4 terrace deposits and a colluvium associated with Late Pleistocene aeolian sands (32 to 12 ka), has an age younger than ca. 154 ka but much older than 32 ka. In the study area, the sedimentary units of the T4 terrace seem to record the river response to sea-level changes and climatically-driven fluctuations in sediment supply. REFERENCES Cunha P. P., Almeida N. A. C., Aubry T., Martins A. A., Murray A. S., Buylaert J.-P., Sohbati R., Raposo L., Rocha L., 2012, Records of human occupation from Pleistocene river terrace and aeolian sediments in the Arneiro depression (Lower Tejo River, central eastern Portugal). Geomorphology, vol. 165-166, pp. 78-90.

From the Humpata Plateau to Namibe Desert, SW Angola

After the Congress, a six-day field trip, will be held through three southwestern provinces of Angola (Huíla, Namibe and Cunene), every day starting and ending in the city of Lubango, for overnight stay in Lubango, with the purpose to observe some of the main sites of geological interest in this zone of Angola. The itinerary of this field trip presents the geologic history of Southwestern Angola and its evolution in the scope of the Congo Craton, through a trip that begins in the first excursion days by the oldest geologic formations and phenomena until the recent geologic formations and phenomena on the last excursion days. On the first and second excursion days, September 5th and September 6th, the field trip will go along the Kunene Anorthosite Complex of Angola (KAC), to observe some petrographic features of the KAC that are important to understand the emplacement of this huge igneous massif of the early Kibarean age. These days of the field trip allow the observation of Earthen Construction, because this region of Cunene is privileged to appreciate a kind of Eco-construction, made of raw earth and in wattle and daub, built with ancient techniques, which constitute a real GeoHeritage. On September 7th, in the morning, the destination will be Tundavala, to visit Tundavala Gap, a huge escarpment of more than 1,000 m high cutted in Neo-Archean and Paleo-Proterozoic igneous rocks, the Ruins of Tundavala (quartzite blocks with sedimentary structures) and Tundavala Waterfalls on a quartzitic scarp. After lunch, the field trip continues towards Humpata plateau to observe the panoramic view over Lubango city from the Statue of Cristo Rei, then the outcrops of dolomitic limestones with stromatolites and dolerites and finally the Leba passage, a huge escarpment and one of the most spectacular parts of the Serra da Chela, traversed by a mountain road built in the early 70s of the last century, that can be observed from the belvedere of the Serra da Chela. On September 8th, the destination is the carbonatite complexes of Tchivira and Bonga, belonging to the Mesozoic alkaline massifs of ultrabasic rocks, a rift valley system that occurs during the Early Cretaceous. In this forth excursion day, due to the huge dimensions of these two carbonatite structures it will be visited, only, the Complex of Bonga, namely the outcrops of the northern part of the structure and secondary deposits on the boundary on the southern part of the of the Complex. The last two excursion days, September 9th and September 10th, are to observe the Cretaceous Basin of Namibe. On September 9th, the northern part of Namibe Basin will be visited to observe the volcanic basic rocks of Namibe as well as the interesting paleontological site of Bentiaba. On September 10th, the destination is the southern and more recent part of Namibe Basin, where on the Namib Desert, the exotic plant Welwitschia mirabilis can be observed, as well as Arco, an oasis in the desert. This last excursion day, ends up at the dunes of Tombwa near the mouth of Curoca river and the beautiful bay of Tombwa, where can be observed heavy minerals in their beach sands.

Tectonic evolution of Variscan Iberia: Gondwana–Laurussia

An integrated interpretation of the late Paleozoic structural and geochronological record of the Iberian Massif is presented and discussed under the perspective of a Gondwana-Laurussia collision giving way to the Variscan orogen. Compressional and extensional structures developed during the building of the Variscan orogenic crust of Iberia are linked together into major tectonic events operating at lithosphere scale. A review of the tectonometamorphic and magmatic evolution of the IberianMassif reveals backs and forths in the overall conver- gence between Gondwana and Laurussia during theamalgamation of Pangea in late Paleozoic times. Stages dom- inated by lithosphere compression are characterized by subduction, both oceanic and continental, development of magmatic arcs, (over- and under-) thrusting of continental lithosphere, and folding. Variscan convergence re- sulted in the eventual transference of a large allochthonous set of peri-Gondwanan terranes, the Iberian Allochthon, onto the Gondwana mainland. The Iberian Allochthon bears the imprint of previous interaction be- tween Gondwana and Laurussia, including their juxtaposition after the closure of the Rheic Ocean in Lower De- vonian times. Stages governed by lithosphere extension are featured by the opening of two short-lived oceanic basins that dissected previous Variscan orogenic crust, first in the Lower-Middle Devonian, following the closure of the Rheic Ocean, and then in the early Carboniferous, following the emplacement of the peri-Gondwanan allochthon. An additional, major intra-orogenic extensional event in the early-middle Carboniferous dismem- bered the Iberian Allochthon into individual thrust stacks separated by extensional faults and domes. Lateral tec- tonics played an important role through the Variscan orogenesis, especially during the creation of new tectonic blocks separated by intracontinental strike-slip shear zones in the late stages of continental convergence.

Tracing the Cambro-Ordovician ferrosilicic to calc-alkaline magmatic

U–Pb geochronological study of zircons from nodular granites and Qtz-diorites comprising part of Variscan high- grade metamorphic complexes in Gredos massif (Spanish Central System batholith) points out the significant presence of Cambro-Ordovician protoliths among the Variscan migmatitic rocks that host the Late Carboniferous intrusive granitoids. Indeed, the studied zone was affected by two contrasted tectono-magmatic episodes, Car- boniferous (Variscan) and Cambro-Ordovician. Three main characteristics denote a close relation between the Cambro-Ordovician protholiths of the Prado de las Pozas high-grade metamorphic complex, strongly reworked during the Variscan Orogeny, and other Cambro-Ordovician igneous domains in the Central Iberian Zone of the Iberian Massif: (1) geochemical features show the ferrosilicic signature of nodular granites. They plot very close to the average analysis of themetavolcanic rocks of the Ollo de Sapo formation (Iberia). Qtz-diorites present typical calc-alkaline signatures and are geochemically similar to intermediate cordilleran granitoids. (2) Both Qtz-diorite and nodular granite samples yield a significant population of Cambro-Ordovician ages, ranging between 483 and 473 Ma and between 487 and 457 Ma, respectively. Besides, (3) the abundance of zircon inher- itance observed on nodular granites matches the significant component of inheritance reported on Cambro- Ordovician metagranites and metavolcanic rocks of central and NW Iberia. The spatial and temporal coincidence of both peraluminous and intermediate granitoids, and specifically in nodular granites and Qtz-diorite enclaves of the Prado de las Pozas high-grade complex, is conducive to a common petrogenetic context for the formation of both magmatic types. Tectonic and geochemical characteristics describe the activity of a Cambro-Ordovician arc-back-arc tectonic set- ting associated with the subduction of the Iapetus–Tornquist Ocean and the birth of the Rheic Ocean. The exten- sional setting is favorable for the generation, emplacement, and fast rise of subduction-related cold diapirs, supported by the presence of typical calc-alkaline cordilleran granitoids contemporary with ferrosilicic volcanism.

Extensional orogenic collapse captured by strike-slip tectonics:

The late Paleozoic collision between Gondwana and Laurussia resulted in the polyphase deformation and magmatism that characterizes the Iberian Massif of the Variscan orogen. In the Central Iberian Zone, initial con- tinental thickening (D1; folding and thrusting) was followed by extensional orogenic collapse (D2) responsible for the exhumation of high-grade rocks coeval to the emplacement of granitoids. This study presents a tectonometamorphic analysis of the Trancoso-Pinhel region (Central Iberian Zone) to ex- plain the processes in place during the transition froman extension-dominated state (D2) to a compression-dom- inated one (D3).Wereveal the existence of low-dipping D2 extensional structures later affected by several pulses of subhorizontal shortening, each of them typified by upright folds and strike-slip shearing (D3, D4 and D5, as identified by superimposition of structures). The D2 Pinhel extensional shear zone separates a low-grade domain from an underlying high-grade domain, and it contributed to the thermal reequilibration of the orogen by facil- itating heat advection from lower parts of the crust, crustal thinning, decompression melting, and magma intru- sion. Progressive lessening of the gravitational disequilibrium carried out by this D2 shear zone led to a switch from subhorizontal extension to compression and the eventual cessation and capture of the Pinhel shear zone by strike-slip tectonics during renewed crustal shortening. High-grade domains of the Pinhel shear zone were folded together with low-grade domains to define the current upright folded structure of the Trancoso-Pinhel re- gion, the D3 Tamames-Marofa-Sátão synform. Newdating of syn-orogenic granitoids (SHRIMP U\\Pb zircon dat- ing) intruding the Pinhel shear zone, together with the already published ages of early extensional fabrics constrain the functioning of this shear zone to ca. 331–311 Ma, with maximum tectonomagmatic activity at ca. 321–317 Ma. The capture and apparent cessation of movement of the Pinhel shear zone occurred at ca. 317– 311 Ma.

Superposition relations of microfabrics in the northern hanging-wall block

This study reports alternation of D2 extension-related and D3 contraction-related microfabrics in the northern hanging wall block of a gneiss dome-like structure recognized in the Évora Massif (Ossa-Morena Zone). In the Arraiolos – Santo Antonio de Alcorrego traverse high- to low-grade mylonites are dominant. Microfabrics related to D2 ductile deformation and M2 high-amphibolite to greenschist facies characterize an extensional shear zone with telescoping metamorphic isograds. D2 microstructures indicate shear sense with top-to-SE. Superposition of D3 contraction developed under greenschist facies (M3) producing folding of D2 microfabrics, mylonitization of granites along strike-slip shear zones and retrogression of M2 mineral assemblages.

Métodos tradicionais de sondagem e construção de captação de água subterrânea em países em vias de desenvolvimento

Neste trabalho avaliam-se e comparam-se metodologias tradicionais de prospeção e construção de captações de água subterrânea em países em vias de desenvolvimento, neste caso do Sul da Ásia (Butão, Bangladeche, Índia, Nepal e Paquistão). Faz-se uma análise às metodologias do ponto de vista geológico (diversos tipos de aquífero, litologias, graus de fracturação e alteração), mecânico (técnica das metodologias de perfuração e construção das captações), e económico (comparação dos tempos de avanço das sondagens, dos tempos de construção das captações, da produtividade das mesmas e seus custos). Conclui-se que as metodologias de prospeção low cost e tradicionais são semelhantes em âmbito e em cenário de aplicação, e que, ainda que as segundas sejam mais caras, têm custos muito menores em comparação com as convencionais. Conclui-se ainda que as metodologias convencionais de construção de captações estão pensadas para metodologias convencionais de prospeção, e que as low cost são muito semelhantes entre si; Abstract: The present work evaluates and compares traditional methods of borehole drilling and construction for water abstraction in developing countries, particularly South Asia (Bhutan, Bangladesh, India, Nepal and Pakistan). The methods are analyzed in regards to geology (types of aquifers, lithologies, massif fractures and weathering), mechanic (borehole drilling and abstraction technologies), and economic (comparing the progression in drilling and construction of boreholes, productivity and its costs) factors. It is concluded that the traditional drilling methods are similar in scope and application set, and that, though the latter are more expensive, they cost less than conventional methods. It is also concluded that conventional borehole construction is based in conventional drilling methods, and that the diverse low cost methodologies are very similar between them.

EL MACIZO CHIRRIPO, UNA RIQUEZA NACIONAL DEL PACIFICO SUR

Descripción del macizo Chirripó, del parque nacional, sus posibilidades turísticas. Se hacen recomendaciones para el aprovechamiento de estas bellezas escénicas y recursos naturales.   SUMMARY Includes a description of the Chirripó Mountain, Chirripó National Park and the tourism potential. Recommendations are also given for the utilization of its scenic landscape and natural recourses.       RESUME On décrit le massif Chirripó, ainsi que le parc national et ses possibilités touristiques. On fait plusieurs recommandations en vue d’une utilisation beaucoup plus intense des paysages et des ressources naturelles.