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Sia ? 6 years, 4 months ago
Taiwan is not a member of the United Nations. Only about 25 countries recognize Taiwan as an independent country. Due to political pressure from China, Taiwan does not maintain an embassy in the United States, and the United States has not recognized Taiwan since January 1, 1979.
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Maximum insolation is received over the subtropical deserts. Equator receives comparatively less insolation than the tropics due to presence of clouds. Generally, at the same latitude the insolation is more over the continent than over the oceans because more clouds over the oceans reflect sun rays back into space.
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The continuous flow of huge amount of water in a definite direction is reffered as Ocean currents.Ocean currents are like river flow in oceans,representing a regular volume of water in a definite path and direction. The mixing of warm and cold currents help to replenish the oxygen and favour the growth of planktons which is the primary food for fish population.Mainly in these zones,the best fishing grounds of the world exist.
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Yogita Ingle 6 years, 4 months ago
There are three distinct stages in the evolution of the earth :
Stage I : In this stage planetesimals accretion happened and the earth originated. It was a barren, rocky and hot object-with a thin atmosphere of hydrogen and helium.
Stage II : Development of Lithosphere :
(i)The primordial earth was mostly in volatile state. Its density gradually increased, the temperature inside increased. As a result, the material inside started getting separated depending upon their densities.
(ii)The heavier materials like nickel and iron sank towards the centre of the earth and the lighter ones moved towards the surface. Over a period of time it cooled and solidified and condensed into a smaller size which later led to the formation of crust.
(iii)There was a giant-impact on the earth during the formation of the moon which heated it up further which lead to differentiated layered structure of the earth. Starting from the surface of the earth to the central part, distinct layers like crust, mantle, outer core and inner core were formed.
Stage III : Evolution of Atmosphere and Hydrosphere :
There are three stages in the evolution of the present day atmosphere
(a) Loss of primordial atmosphere containing a thin layer of hydrogen and helium as a result of stripping off by solar winds.
(b) The hot interior of the earth : Contributing to the evolution of the earth. The gases were outpoured from the interior of the earth during the cooling of the earth through the process called degassing. This started the evolution of the early atmosphere which largely contained water vapour, nitrogen, carbon dioxide, methane, ammonia and very little of free oxygen.
(c) Finally, the composition of the atmosphere was modified by the living world through the process of photosynthesis.
Formation of Hydrosphere : The continuous volcanic eruptions contributed water vapour and gases to the atmosphere. As the earth cooled, the water vapour released started getting condensed. The carbon dioxide in the atmosphere got dissolved in rainwater and the temperature further decreased causing more condensation and more rains. The rainwater falling onto the surface got collected in the depressions to give rise to oceans. Thus earth's oceans (hydrosphere) were formed within 500 million years from the formation of the earth. The process of photosynthesis was initially confined to oceans only and thus oceans started filling up with the oxygen. Eventually, oceans got saturated with oxygen and the oxygen started to flood the atmosphere.
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