Tides
Tides are defined as the periodic rise and fall in sea levels that occur as a result of gravitational forces of the sun and moon. The moon is the primary factor in controlling temporal rhythm and heights of tides because of its close proximity and regular rotation around the earth. The predictability of tides is dependent on the moons orbit around the earth which takes twenty four hours and fifty minutes per rotation. During this time there are generally two low tides and two high tides that rise and fall on the shoreline, depending on the geography of the shoreline. The highest tides recorded on earth occur along the Bay of Fundy, a body of water that lies between Nova Scotia and New Brunswick provinces in Canada. In this region you may observe tidal variations of up to forty two feet high in a twelve hour period.
The influence of the Sun’s gravity on the tides is less than that of the moon because although the diameter of the sun is 400 times that of the moon, it is far, far further away from the Earth. If the moon did not exist there would still be high and low tides because of the sun, however they would only be half the size compared to their lunar counterparts.
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