The third planet from the solar system to the solar system. m

in #geography6 years ago

The world

The third planet from the solar system to the solar system: image
The third largest planet, according to the distance from the Sun, is the world's fifth largest planet in eight solar systems. It is one of the four solid planets in the Solar System. The world's other name is "World" or "Nilgah". The Greek name known as "Earth", known in English as Gaia (Γαῖα) [n 5], is the Latin name of the planet "Terra".
The world is home to billions of species of people including humans. The world is the only cosmic place where the existence of life is revealed. [25] Earth was formed 454 billion years ago. Within a billion years, life on earth arises. [26] Earth's biosphere has brought significant changes in the atmosphere and other inorganic conditions of this planet. This resulted in the increase of the aerobic organisms on the one hand, on the other hand the level of weight was formed. Together with the magnetic field of the Earth, this weight level has widened the way in which the life cycle of life has been expanded by blocking harmful solar radiation. [27] Earth's natural resources and its geological history and orbits have helped in the survival of life in this age. It is believed that more than 50 billion years of life will be in the condition of life. [28]

The surface of the Earth is divided into several hard strings. These are called crustaceous plaques. For billions of years, they have been deposited on the earth's surface. About 71% of the world's surface is covered by the ocean of saline water. [29] The remnants are composed of continents and numerous islands. There are also numerous ocean lakes and other water sources in the area. These are formed in the world's waterways. Essential fluid water for livelihoods is not available in parallel anywhere in the planet's crust. Earth's perennially covered ice (Antarctic ice sheets) or sea ice (Arctic ice cap) is covered. Earth's interior is always functional. This part is composed of a relatively thick layer of solid mantle, a fluid center (which forms a magnetic field) and a strong iron core center.

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