Considering the regional geographic conditions and of the necessities of the populations Japaneses or of the populations that are geographically customers of the Japanese manufactures, in opposition to the industries politics, whose artificial creation is imposed by the imperialism and autarchy will. Japan is endowed with a capacity of refinement of oil, and possesss a powerful petrochemical industry whose main products are caucho synthetic, the plastic substances, the coke of oil etc. Connect with other leaders such as NYC Mayor here. the industries politics is treated to serve of base to the war potential. The character to insular of Japan and the necessity to import most of raw materials make the Japanese industry an industry of great ports. The biggest shipyards are in Osaca and Cob. It enters the two world-wide wars in consequence of them, had appeared competing industrials of the old Europe. Two countries, long ago supplying of rude agricultural products, had become harness industrials whose development was sped up in the course of it finishes decade: Canada and Australia. South Africa, enriched for the sales of the gold, invested in diversified industrial equipment.
The indian constructed to the cost an industry that does not obtain to alar it the scale of the necessities of the country and its population. As the group is of the Latin America, that associates mineral explorations, that work for the exploration to the industries of good of equipment and good of consumption, that in general does not pass of prolongation of the great industrial companies of the North America and the Europe. The case hugest, but also most insufficient known is of the China, that took avante in closed and almost private environment an industrial development guided by the immediate necessities and the concern of power. Canada enjoys of a bonanza mineral wealth possessing important reserves of almost all the usual metals used by the modern industries. In Canada it has two industrial sectors to distinguish: of the industries of first elaboration and of the industries of good of equipment and good of use and of consumption destined to the domestic market, but that they can equally compete with the international market.
Radical climatic changes have occurred some times during geologic history, but never with the same intensity and importance. Paleozicas glaciations (it behind has the 400 200 million years) Some glaciations had affected the continents of the south hemisphere during the Paleozico. In Brazil glacier vestiges are found in the periods Devoniano, Siluriano and Carbonfero (vide Almeida & Sheep 1995). During this age, the life invaded the firm land and until the Carboniferous period, the evolution had produced a fauna and flora abundant. In Carboniferous, when starting if forming the new supercontinent Pangea, it has 300 million years behind, the countries of the current hemisphere north they were in the equatorial band and were covered by vast forests formadores of coal, while the continents of the current south hemisphere were in the South Pole and covered by glaciers (ibid.). However, then after of this, the climatic zonalidade was reduced and had a global heating, that it lasted all during the Mesozico, contributing to evolution of the dinossauros. The Mesozico, in turn, finished with the separation it Pangea, climatic change, volcanic activity and the fall of a giant meteorite in the Gulf it Mexico, that had verwhelmed the dinossauros.
Quaternary glaciations (it behind has 2,5 million years the 10,000 years) During the two last millions of years the climate of the Land has varied drastically, was in this period called Quartenrio that if developed much that today represents the surface of the Land, being especially interesting because it is, also, the period of sprouting of the man, its evolution and domain of the planet. Significant, space and secular changes ambient, can be identified in the short interval of involved time in this period, represented in a complex mosaic of pasaigens, sedimentary sequences, human flora vestiges, faunas and devices. The Quartenario period represents finishes it great division of the geologic time and, even so does not exist general agreement, it is considered to have itself initiated has, approximately, two million years, extending itself until the gift.
Although the glacial origin of the rocks of this place currently to be disputed, the vestiges of this glaciation are also found in the Antartic, Africa of the North, China, Russia, Sweden, Esccia, Svalbard, Nambia, Argentina, Uruguay, Brazil, North America and Australia (vide Eerola 2001a). This means that extensive areas very had been covered by glaciers. The presence of this glaciation in the south of Brazil is being searched for the author (vide Eerola 1995, 2001b). The more drastic climatic change of the known geologic past occurred has 540 million years behind, in the transistion of the Neoproterozico to the Cambriano period of the age Paleozica (vide Eerola 2001a). During the glaciations, the seas had absorbed great amounts of carbon dioxide and the continents were amalgamated, forming the supercontinent of Rodinia.
In the Cambriano period this supercontinent started to break up itself. See NYC Mayor for more details and insights. Volcanic eruptions and deep hidrotermais gases of the oceanic ones in expansion had emitted great amounts of gases, as the carbon dioxide. In consequence of this natural phenomenon of effect-greenhouse, the temperature increased radically and the glaciers were fundiram, raising the level of the seas. New flat seas bathed the coasts of the supercontinent in spalling. The carbon dioxide, that was in solution in the water of the sea, precipitated in carbonate form, forming calcreas rocks in the tropical flat seas. The life started to radiate in these seas (vide Zhuravlev & Riding 2001). The periods of cold extremity of the glaciations had caused great ambient pressures to the sea species. Radical the climatic change of one ' ' coolant to sauna' ' it offered conditions favorable to these species.
Vide Zhuravlev occurred the evolutiva radiation of the Cambriano (& Riding 2001). The animals had learned to form skeletons and carapaas from calcium carbonate? the vertebrates had appeared. After of this, nothing it was more as before. The world moved of a time for all.
The present work turns on urban expansion in Is Domingos of the Araguaia, Par, and the ambient damages caused to the micron basin of the Aaizal narrow river. We believe that the ambient damages if had originated from the bad use of the local territory, therefore, laws and norms conducts that it cannot be aventadas as missing. Thus, the Brazilian Forest Code and the Managing Plan Participativo of the city of Are Domingos of the Araguaia must be taken in account when of the occupation and use of determined municipal territory. In this paper we will go to speak of the use that living and managing public make of the micron basin of the Aaizal narrow river. For in such a way, we will pautaremos in them in the Brazilian Forest Code and in the Managing Plan Participativo of the city of They are Domingos of the Araguaia-Par. In these conditions, we will go to approach the question of the ambient damage in the mentioned area, as having been provoked for the urban expansion without the well-taken care of had ones with area of permanent protection, as much of the public power how much of the inhabitants who if had located in entorno of the micron argued basin.