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At the point when the earth and the moons gravity lines up with one another, the impacts of these two gravitational powers turns out to be solid and makes a great many gallons of water move or stream towards the shore making a "high tide" condition. In like manner when the earth and the moon's gravity are at 90o to one another, the impacts of these two gravitational powers are more fragile and the water streams from the shore as the mass of water moves to another area on the earth, making a "low tide" condition. This ebbing and streaming of the tides happen twice amid every time of the turn of the earth with more grounded week by week and yearly lunar cycles superimposed onto these tides. 

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