Modelo de representación y difusión de cavidades. Cueva de Praileaitz. Deba, Gipuzkoa

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Complexity of rupture propagation in large earthquakes in relation to tectonic environment

Complexity in the earthquake rupture process can result from many factors. This study investigates the origin of such complexity by examining several recent, large earthquakes in detail. In each case the local tectonic environment plays an important role in understanding the source of the complexity.

Several large shallow earthquakes (M_s > 7.0) along the Middle American Trench have similarities and differences between them that may lead to a better understanding of fracture and subduction processes. They are predominantly thrust events consistent with the known subduction of the Cocos plate beneath N. America. Two events occurring along this subduction zone close to triple junctions show considerable complexity. This may be attributable to a more heterogeneous stress environment in these regions and as such has implications for other subduction zone boundaries.

An event which looks complex but is actually rather simple is the 1978 Bermuda earthquake (M_s ~ 6). It is located predominantly in the mantle. Its mechanism is one of pure thrust faulting with a strike N 20°W and dip 42°NE. Its apparent complexity is caused by local crustal structure. This is an important event in terms of understanding and estimating seismic hazard on the eastern seaboard of N. America.

A study of several large strike-slip continental earthquakes identifies characteristics which are common to them and may be useful in determining what to expect from the next great earthquake on the San Andreas fault. The events are the 1976 Guatemala earthquake on the Motagua fault and two events on the Anatolian fault in Turkey (the 1967, Mudurnu Valley and 1976, E. Turkey events). An attempt to model the complex P-waveforms of these events results in good synthetic fits for the Guatemala and Mudurnu Valley events. However, the E. Turkey event proves to be too complex as it may have associated thrust or normal faulting. Several individual sources occurring at intervals of between 5 and 20 seconds characterize the Guatemala and Mudurnu Valley events. The maximum size of an individual source appears to be bounded at about 5 x 10²⁶ dyne-cm. A detailed source study including directivity is performed on the Guatemala event. The source time history of the Mudurnu Valley event illustrates its significance in modeling strong ground motion in the near field. The complex source time series of the 1967 event produces amplitudes greater by a factor of 2.5 than a uniform model scaled to the same size for a station 20 km from the fault.

Three large and important earthquakes demonstrate an important type of complexity --- multiple-fault complexity. The first, the 1976 Philippine earthquake, an oblique thrust event, represents the first seismological evidence for a northeast dipping subduction zone beneath the island of Mindanao. A large event, following the mainshock by 12 hours, occurred outside the aftershock area and apparently resulted from motion on a subsidiary fault since the event had a strike-slip mechanism.

An aftershock of the great 1960 Chilean earthquake on June 6, 1960, proved to be an interesting discovery. It appears to be a large strike-slip event at the main rupture's southern boundary. It most likely occurred on the landward extension of the Chile Rise transform fault, in the subducting plate. The results for this event suggest that a small event triggered a series of slow events; the duration of the whole sequence being longer than 1 hour. This is indeed a "slow earthquake".

Perhaps one of the most complex of events is the recent Tangshan, China event. It began as a large strike-slip event. Within several seconds of the mainshock it may have triggered thrust faulting to the south of the epicenter. There is no doubt, however, that it triggered a large oblique normal event to the northeast, 15 hours after the mainshock. This event certainly contributed to the great loss of life-sustained as a result of the Tangshan earthquake sequence.

What has been learned from these studies has been applied to predict what one might expect from the next great earthquake on the San Andreas. The expectation from this study is that such an event would be a large complex event, not unlike, but perhaps larger than, the Guatemala or Mudurnu Valley events. That is to say, it will most likely consist of a series of individual events in sequence. It is also quite possible that the event could trigger associated faulting on neighboring fault systems such as those occurring in the Transverse Ranges. This has important bearing on the earthquake hazard estimation for the region.

Processes controlling the quantities of biogenic materials in lakes and reservoirs subject to cultural eutrophication

The processes which control the growth, composition, succession and loss from suspension of phytoplankton algae are briefly reviewed, with special reference to function in eutrophic reservoir systems. The ecology of larger algal biomasses supported by high nutrient loading rates are more likely to be subject to physical (wash-out, underwater light penetration, thermal stability and mixing) than to chemical constraints. Sudden changes in the interactions between physical factors temporarily impair the growth of dominant algal species, and advance the succession. Certain algae may be cropped heavily, but selectively, by zooplankton feeding, but they are rarely the species which cause problems in waterworks practice. Grazing, however, does influence succession. A deeper understanding of the operation of loss control mechanism is urgently required. Potentially, manipulation of the physical environment provides an important means of alleviating day-to-day algal problems in eutrophic reservoirs; in terms of cost effectiveness these may prove to be more attractive than reducing nutrient loads at source.

Patrimonio cultural subacuático

Con el estudio práctico de este tema, tan rico e interesante, pretendo elaborar una revisión de las normas jurídicas que regulan el régimen del patrimonio cultural subacuático, tanto a nivel internacional (UNESCO 2001) como nacional, parando a analizar un apartado especial dedicado al estudio de esta situación en el País Vasco. Por otra parte, trataré también los aspectos técnico - náuticos en relación con las operaciones de investigación y desarrollo de proyectos, búsqueda, rescate y preservación del patrimonio cultural subacuático describiéndose, a continuación, algunos de los casos más importantes en la materia.

Participación ciudadana, patrimonio cultural y museos: entre la teoría y la praxis

Cap. 1. La Nueva Museología, el patrimonio cultural y la participación ciudadana a debate. Iñaki Arrieta Urtizberea Cap. 2. Museos: del público al ciudadano. Rafael Azuar Ruiz Cap. 3. Los públicos y lo público. De mutismos, sorderas, y de diálogos sociales en museos y espacios patrimoniales. Luz Maceira Ochoa Cap. 4. La restitution du patrimoine: un rôle pour le musée? Études de cas dans les communautés innues du Québec et du Labrador (Canada). Élise Dubuc Cap. 5. El museo de territorio y sociedad, ¿una utopía? el caso del Museo Industrial del Ter. Carles García Hermosilla Cap. 6. El ecomuseo del río Caicena (Almedinilla-Córdoba): un proyecto de desarrollo rural desde el patrimonio histórico-natural, ¿y la participación ciudadana? Ignacio Muñiz Jaén Cap. 7. Mé-tisser les mémoires. Musées indiens du nordeste brésilien. Martin Soares Cap. 8. El patrimonio como proceso social. Intervención, desarrollo y consumo del patrimonio minero en Andalucía. Macarena Hernández Ramírez y Esteban Ruiz Ballesteros Cap. 9. Legislación patrimonial, intervención pública y participación ciudadana en la declaración de un conjunto histórico. Iñaki Arrieta Urtizberea Cap. 10. El castillo de Montsoriu. La participación de la sociedad civil. Joaquim Mateu Gasquet Cap. 11. El patrimonio cultural; espacio de encuentro. Daniel Arnesio Lara Montero

Patrimonios culturales y museos: más allá de la Historia y del Arte

Cap. 1. La reinvención del museo etnológico. Xavier Roigé i Ventura Cap. 2. La mise en patrimoine du catharisme. Enjeux de territoire, enjeux d’identité. Marie-Carmen Garcia. Cap. 3. Más allá del museo. Las activaciones económicas del patrimonio: de los parques naturales a las fiestas temáticas. Agustí Andreu i Tomàs. Cap. 4. La patrimonialización de un territorio a través de los museos etnográficos: el caso de Extremadura. Aniceto Delgado Méndez. Cap. 5. La situación de los museos, colecciones, centros de interpretación y otros equipamientos patrimoniales del Alto Pirineo catalán. Jordi Abella Pons. Cap. 6. Patrimonio, conocimiento y dinamización. Una experiencia de trabajo en el Priorat (Catalunya). Salvador Palomar. Cap. 7. Experiencias de desarrollo local en el Pirineo aragonés basadas en la valorización del patrimonio. Aurelio García Gállego. Cap. 8. Las dimensiones sociales y culturales del patrimonio edificado: una propuesta para su estudio. Iñaki Arrieta Urtizberea.

Cultural methods of detection for microorganisms: recent advances and successes

Most microbiological methods require culture to allow organisms to recover or to selectively increase, and target organisms are identified by growth on specific agar media. Many cultural methods take several days to complete and even then the results require confirmation. Alternative techniques include the use of chromogenic and fluorogenic substances to identify bacteria as they are growing, selective capture using antibodies after short periods of growth, molecular techniques, and direct staining with or without flow cytometry for enumeration and identification. Future microbiologists may not use culture but depend on the use of specific probes and sophisticated detection systems.