All About Our Planet Earth

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The Earth is a relatively small celestial object. It is the third planet orbiting an average star, our Sun, located in the Orion arm, sometimes called the Orion Spur; it is a minor arm located in between the Sagittarius Arm and the Perseus arm of the Milky Way, a barred spiral galaxy. Our solar system orbits the central bulge of our galaxy at a radius of 1.7 billion AU and our period of galactic revolution is 230 million years at a tangential velocity of 828,000 km/hr relative to the center. Our solar system has one main sequence star, 4 inner rocky planets, the asteroid belt, 4 outer large gaseous planets, the Kuiper Belt of small icy objects, and the outermost Oort Cloud of icy objects made of water, ammonia, and methane. It extends from about 2000-5000 AU to an outer distance of as much as 100,000 AU.

The Earth completes one rotation every 23 hrs 56 min. and completes 365.25 rotations (days) during one revolution around the Sun, or 1 Earth Year. The Earth’s average orbital velocity is 29.8 km/s and its rotational velocity is about 460 m/s. The average radius of Earth’s solar orbit is 149,587,817 km, or about 1 AU. About 1320 Earths would fill Jupiter’s volume and around 1,300,000 would fill the Sun’s. It has a density of 5.5 g/cm3, similar to the other rocky inner planets that are composed of heavy elements, but much greater that the outer planets that are mostly hydrogen and helium. Its mass is 5.97×1024 kg. It has a slightly greater equatorial circumference then polar, this is due to Earth’s rotation on its axis and the Sun’s gravitational pull during the Earth’s early molten stage.

Over 4.6 billion years ago, a large molecular cloud located within one branch of the Milky Way galaxy had been the site of the formation ...

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...nd the debris orbiting Earth also accreted into the Moon. As the number of planetesimal collisions diminished, the Earth began to cool. A solid crust had formed by about 3.8 billion years ago. The crust thickened to form one large landmass called Pangea. Then, the crustal plates began to move due to the convective mantle. As they pulled apart, a new, thin ocean floor formed. The Earth’s atmosphere formed by outgassing, or the release of gas trapped within the interior of the planet by volcanic activity. The Earth’s oceans were formed when water vapor in the atmosphere condensed and fell as rain to form the oceans. Light elements like He and H escaped to space, leaving behind an early atmosphere of volcanic compounds like NH3, CH4, N and S compounds, water, and carbon dioxide. As of about 3.5 billion years ago, the Earth’s surface was set for the origin of life.

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