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Lec – History4
Lec – History4

... - will be at rest - or moves at a constant speed, in straight line, forever Second Law (FF = ma) If a net force acts on an object: - it changes its motion (accelerates) - speeds up, slows down, or turns - depends on mass of object - more mass, harder to accelerate ...
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... Once the Earth-Moon becomes tidally locked, only other external tidal forces will affect its configuration. As solar tides will tend to slow the Earth's rotation even more, the tidal bulges due to the Moon will begin to get behind (in the reverse inclination as seen in Fig. 3). Therefore there would ...
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... Question: How about tides due to the sun? The sun’s gravitational force on Earth is 180 times as large as that of the moon’s pull on Earth. So, what about ocean tides due to the sun?? Why are these not 180 times as strong as those due to the moon? Because tides happen due to differences in grav pul ...
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... Moon rocks show signs of all having been melted at some time in the The Moon was formed very hot, possibly entirely molten. ancient past, but this is not typical of Earth’s rocks. Techniques used by scientists to tell the age of ancient rocks reveal that This is evidence of similar origins OR of Moo ...
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Earth's rotation



Earth's rotation is the rotation of the planet Earth around its own axis. The Earth rotates from the west towards east. As viewed from North Star or polestar Polaris, the Earth turns counter-clockwise.The North Pole, also known as the Geographic North Pole or Terrestrial North Pole, is the point in the Northern Hemisphere where the Earth's axis of rotation meets its surface. This point is distinct from the Earth's North Magnetic Pole. The South Pole is the other point where the Earth's axis of rotation intersects its surface, in Antarctica.The Earth rotates once in about 24 hours with respect to the sun and once every 23 hours 56 minutes and 4 seconds with respect to the stars (see below). Earth's rotation is slowing slightly with time; thus, a day was shorter in the past. This is due to the tidal effects the Moon has on Earth's rotation. Atomic clocks show that a modern-day is longer by about 1.7 milliseconds than a century ago, slowly increasing the rate at which UTC is adjusted by leap seconds.
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