To kiss or it is learned, it is not an ability with which one is born and it is good or no, is possible to be learned and to be improved, like any other ability the more. And, doubtless, it is an extremely important art at the time of finding pair. Many men commit the error to think that they are good besadores by nature, although is not absolutely certain. Nevertheless, for many women it is important to be with a man who kisses well, otherwise although he is charming, attractive perhaps and funny they do not return it to call more. Certainly, the kisses can get to transmit fantastic and unpublished sensations for both sexes. However, there are slight differences on the form how men and perceive them to women. For the man, the kiss is tactics strategic to reach the following level of approach and a form to increase the probabilities of intimar with the woman with whom it is.
For this reason, in first stage of the relation the men usually are more active kissing. In phases more outposts of the relation they usually use them more as it forms of to trench and to solve conflicts, although also in the sentimental relations long play the kiss is used like an indicator that evaluates the degree of complicity and union with the pair and as a form to conserve the existing connection. Some investigations reveal that they are not so selective at the time of choosing to whom to kiss and with whom to go away to the bed and that they attribute to minor importance to them as the relation continues. On the contrary for many women the act to kiss well is a requirement fundamental to look for pair. According to realised investigations, a 20% of the women would be arranged to leave with men who were good besadores although they were not so attractive.
When historically one analyzes the familiar aspects of a society, becomes essential that if it has led in consideration, social points as the etnia, temporality, groups, regional sort, economic contexts, in order to equalize subject to the o its time and space, not to commit andinos errors in elapsing of the study. She is necessary to understand the family as a situated phenomenon, historically subject to alterations, in accordance with the changes of the relations of production established between the men … Is evident that the functions of the family go to depend on the place that it occupies in the social organization and the economy. (SPIDER, 1989, P. 75). As the aspect shows in the gotten understanding when it perceives that some historiografias of the Brazilian family still are tied in the prebalance of cultural characteristics, more than what the social attitudes and/or conditions, beyond the segregated regionalistic study, where the lack of information concerning the classrooms and the favored localities is observed less.
When dealing with the family as a microscopical representation the social order. These authors had failed in the focus on the dynamics in the formation and organization of the familiar life. The result was a study of the cultural attitudes more than what of the social conditions. The tipologia of the national character only represents the dominant culture, and excludes a variety of familiar experiences, among others groups. … other places, as the cattle hinterland northeastern also had been practically forgotten in its historical and regional especificidades, however fit in a world vision littoral-northeastern, however perceived as a half wild world, if wants different of the coast.
Important feature is the provision of modern ideas about what the main tectonic stresses acting horizontally in the crust and many times the power of stress on the weight of the rock, which is good confirmed by field measurements in the mines. Modern shift the Earth's surface always occur along active tectonic faults. Tectonic fault – a zone of discontinuity crustal suture separating breed array into two blocks. Tectonic faults are present in every mountain range in any territory and has long been studied by geologists. If a building is erected on a tectonic fault, displacement and strain in the zone tectonic suture can be passed to the supporting structure and lead to a breach of the stability and accidents. Given the wide spread of local tectonic disturbances in the surface of the earth's crust, the likelihood of a tectonic zone at the base of the engineering facility is extremely high. It should be noted that the presence of the fault does not always lead to deformations of the building.
To this effect the combination of certain factors, in particular – the intersection of several faults under the foundation and defined the orientation of the faulting in the field of acting stresses, ie depends on the direction of the force. The normative Documents on the engineering survey, most of which are copied documents from the Soviet period, published 30-40 years ago, the geological environment is considered as a static structure. Engineers Geologists study only lithological difference between the ground and gravity processes, ie processes occurring under the influence of gravity. In the surveys do not take into account the tectonic stress state of the geological environment with a predominance significant horizontal stress and ignored her mobility. That is why the deformation of the next building standard methods of studying the causes of this process useless. Speculation on the impact of sediment and soil compaction on the occurrence of cracks in foundations and walls of buildings often do not withstand scrutiny. The modern buildings of reinforced concrete have increased strength and had to be less sensitive to such processes.
However, experience shows that the concrete tower blocks pop no less than the prefab houses. In addition, the precipitation characteristic only of loose soil and, therefore, the buildings constructed on solid rock grounds should have no deformations. But here the opposite is true. In the Urals – an area where major developments are rocky ground, a huge number of deformed monolithic skyscrapers. Moreover, deformation is often localized in those parts of the buildings which stand on a solid bedrock, which excludes the possibility of precipitation and condensation. This is probably due to the fact that the modern shift in the zones of active tectonic faults are passed through hard rocky ground on concrete structures. Deformation take place abruptly, without mitigation, with the formation of cracks and breaks. Buildings standing on a bed of loose sediment on the contrary more protected from the dynamic effects of the tectonic faults. Thus, it is clear that the problem of identifying and exploring moving tectonic faults requires special attention. High rates construction, large-scale construction of high-rise buildings and the active development of underground space requires a more thorough analysis of engineering geological conditions and geodynamic hazard of the geological environment. A considerable amount of information about the dynamic effects of tectonic zones in the engineering objects, accumulated by a number of independent researchers, requires careful analysis in order to develop an effective system prevent these negative effects. In the future it will require substantial changes in the regulatory documentation to conduct geotechnical studies.
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