@masonbhodgson: Zara are coming different with these water repellents rn 🌂 @ZARA #zara #fyp #fashion

masonbhodgson

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Thursday 10 September 2026 18:13:36 GMT

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2.ko0by.2 :

How Tall and what size ?

2026-09-11 17:10:42

3

Ⓜ️ :

Code Bro

2026-09-11 12:00:20

2

MF13 :

You got the code ?

2026-09-11 09:45:45

1

Ben :

Code?

2026-09-11 11:49:59

2

Cocktails&reading :

Love that !

2026-09-11 06:49:15

3

23 :

Flip its for men

2026-09-11 18:12:29

0

Mickthebrick62 :

❤️❤️

2026-09-11 04:47:34

1

fourwards_ :

💙💙💙

2026-09-10 22:00:14

1

.. :

😁😁😁

2026-09-11 15:26:40

0

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This is how Our Moon affects ocean tides😲🌊 wait till end🙌 Video credits : @drmadness3d This is graphical representation made for educational purpose. The Moon and Earth exert a gravitational pull on each other. On Earth, the Moon’s gravitational pull causes the oceans to bulge out on both the side closest to the Moon and the side farthest from the Moon. These bulges create high tides. The low points are where low tides occur. Rising and ebbing tides happen as Earth’s landmasses rotate through the tidal bulges created by the Moon’s gravitational pull. Our observer sees the tides rise when passing through the bulges, and fall when passing through the low points. Of course, in reality the Earth isn’t a smooth ball, so tides are also affected by the presence of continents, the shape of the Earth, the depth of the ocean in different locations, and more. Twice a month, when the Earth, Sun, and Moon line up, their gravitational power combines to make exceptionally high tides, called spring tides, as well as very low tides where the water has been displaced. When the Sun is at a right angle to the Moon, moderate tides, called neap tides, result. From our view on Earth, these tides coincide with certain lunar phases since they occur when the Moon reaches specific positions in its orbit.

This is how Our Moon affects ocean tides😲🌊 wait till end🙌 Video credits : @drmadness3d This is graphical representation made for educational purpose. The Moon and Earth exert a gravitational pull on each other. On Earth, the Moon’s gravitational pull causes the oceans to bulge out on both the side closest to the Moon and the side farthest from the Moon. These bulges create high tides. The low points are where low tides occur. Rising and ebbing tides happen as Earth’s landmasses rotate through the tidal bulges created by the Moon’s gravitational pull. Our observer sees the tides rise when passing through the bulges, and fall when passing through the low points. Of course, in reality the Earth isn’t a smooth ball, so tides are also affected by the presence of continents, the shape of the Earth, the depth of the ocean in different locations, and more. Twice a month, when the Earth, Sun, and Moon line up, their gravitational power combines to make exceptionally high tides, called spring tides, as well as very low tides where the water has been displaced. When the Sun is at a right angle to the Moon, moderate tides, called neap tides, result. From our view on Earth, these tides coincide with certain lunar phases since they occur when the Moon reaches specific positions in its orbit.

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