91.5K
LIBack to talk about more tides 😈 part 2!! #ocean #science #oceanography #astronomy #physics
@liloceanpaige
#Springtides
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トレンドリール
(12)
4.1K
FUThe gravitational pull of the moon affects the Earth’s oceans, causing the phenomenon known as tides. As the moon orbits the Earth, its gravitational force pulls on the water, creating bulges in the ocean’s surface. These bulges result in high tides where the water level is elevated, and low tides where the water level decreases. The alignment of the sun, moon, and Earth also influences the intensity of tides, leading to variations like spring tides (maximum tidal range) and neap tides (minimum tidal range). Overall, the moon’s gravitational effect on ocean water creates a rhythmic pattern of tides that play a crucial role in coastal ecosystems and navigation.
@futuregenspace
1.8K
JU🌕 The Moon's Hidden Pull: The Science of Tides 🌊
Ever wondered why the ocean’s water levels rise and fall like the earth is breathing? You’re witnessing a cosmic tug-of-war known as Tidal Force.
🔭 The Gravitational Tug
Even though the Moon is about 384,400 kilometers away, its gravity is strong enough to pull on Earth’s oceans. As the Moon orbits our planet, its gravitational pull causes the water to "bulge" toward it. This creates High Tide in the areas closest to the Moon.
🔄 The Second Bulge
Surprisingly, there is also a high tide on the opposite side of the Earth at the same time! This happens because the Moon’s gravity pulls the Earth itself slightly toward it, leaving the water on the far side to bulge outward due to inertia. As the Earth rotates, different coastlines pass through these bulges, giving us two high tides and two low tides every day.
🌍 A Balancing Act
While the Sun also exerts gravitational pressure, the Moon’s proximity makes it the primary director of our tides. This rhythmic motion is essential for marine life, circulating nutrients and oxygen throughout the world's oceans.
The next time you see the tide coming in, remember—you're watching the Moon's invisible hands reshaping our world!
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#astronomy #oceanlife #moon #sciencefacts #sometimeslosealwayswin
@jupiter_tv_studio
228
PEThe ocean rises and falls every day.
not because of wind, but because of the Moon. 🌙🌊
Gravity is quietly moving our planet’s water.
#AstroPhysics #CosmicGravity #MoonPower #EarthAndMoon #OceanTides SpaceScience reach
@peak_of_mylife
5.9K
AS🌕 The Moon does rotate!!!!..... we just don’t notice it.
The reason we always see the same face isn’t because the Moon is standing still. It’s because of tidal locking. 🌊
The Moon takes 27.3 days to rotate once on its axis…
and 27.3 days to orbit Earth.
Because those two motions are perfectly synchronized, the same hemisphere always faces us.
Think of it like walking in a circle around a chair while always facing the center. You’re turning as you move, but the same side of you always faces the chair.
Early in the Moon’s history, Earth’s gravity created tidal bulges that slowly adjusted its rotation until it matched its orbit.
We can’t actually see exactly half the Moon from Earth, either slight orbital shifts called libration let us glimpse about 59% of its surface over time.
The true far side wasn’t seen until 1959, when Luna 3 photographed it for the first time.
The Moon rotates.
It’s just perfectly synchronized with its orbit. 🌕
#astronomy #space #moon #science #astrophysics
@astroathens
4.2K
COEarth is, at its core, predominantly iron - roughly 47% of the planet's composition. The moon, by contrast, contains almost none. That discrepancy points directly to the leading theory of lunar formation. Something hit Earth with enough force to eject that volume of material into orbit, where it gradually coalesced into the moon we have today.
However, that first impact left Earth spinning at a rate incompatible with the conditions needed for life. What followed, according to the Double Big Whack theory, was a second impact - arriving from exactly the right direction, at exactly the right speed, hitting exactly the right point on Earth's surface to slow its rotation down to its current dynamics.
Two massive impacts, both precisely calibrated, billions of years apart. Ben doesn't labour the point - but the implication is there. The margin for error on either strike was essentially zero. And yet here we are.
@cosmicsummit2025
18.2K
QUThis visualization shows how the Moon influences Earth’s oceans through gravity. The Moon’s gravitational pull draws water toward it, creating a high tide on the side of Earth facing the Moon. At the same time, another high tide forms on the opposite side due to the Earth–Moon system’s motion.
As the Earth rotates, coastal regions move through these tidal bulges, producing the regular cycle of high and low tides experienced around the world.
A simple cosmic interaction shaping our oceans every single day.
Follow @quantumxparadoxx for more
#Moon #OceanTides #Gravity #Astronomy #earthmoonsystem
@quantumxparadoxx
66.1K
THDid you know?👨🚀 High tides and low tides are caused by the moon. The moon’s gravitational pull generates something called the tidal force. The tidal force causes Earth—and its water—to bulge out on the side closest to the moon and the side farthest from the moon. These bulges of water are high tides.
@thedeepastronomy
19.0K
QUThe Moon's gravitational pull causes Earth's oceans to bulge, resulting in high and low tides. This daily phenomenon occurs as the ocean's water is pulled strongest at high tide and weakest at low tide.
@quantumxparadoxx
2.3K
OUThe gravitational pull of the moon affects the Earth’s oceans, causing the phenomenon known as tides. As the moon orbits the Earth, its gravitational force pulls on the water, creating bulges in the ocean’s surface. These bulges result in high tides where the water level is elevated, and low tides where the water level decreases. The alignment of the sun, moon, and Earth also influences the intensity of tides, leading to variations like spring tides (maximum tidal range) and neap tides (minimum tidal range). Overall, the moon’s gravitational effect on ocean water creates a rhythmic pattern of tides that play a crucial role in coastal ecosystems and navigation.
© all the rights and credits are reserved to the respective owners.
Caption by: @interstellarsciencee
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#science #physics #astronomy #cosmology #blackhole
@ourvisualvibes1
109
SMWatch this video to learn about what causes tides?
@smartkidstips
4.6K
STTides: Earth's Angular Momentum Pump To The Mool
Are Tides Higher During The Full Moon?
Prepare to have your minds blown with this post. Let's go for a ride
The tides aren't really "higher during full moon" in the way pop explanations often imply — they're dramatically amplified in range (higher highs + lower lows) during both full moons and new moons. The full moon just happens to be the visually spectacular version of the same geometry.
Today I strip away the textbook diagram of "Moon pulls water toward it + fake bulge on the other side" and look at what actually makes the phenomenon mind-blowing when you zoom out.
In this video Neil deGrasse Tyson nails this topic repeatedly in his explanations (from StarTalk episodes to quick clips and posts)—and it aligns perfectly with the deeper view I'm going to talk about. He consistently debunks the romantic/magical notion that the full moon itself has some extra gravitational mojo.
He also loves flipping the everyday perception: tides aren't the water "coming in and out" toward the Moon; Earth is spinning underneath fixed tidal bulges (one toward the Moon, one away), so we rotate into and out of them twice a day. His take strips away the cliché mysticism while keeping the awe: the full moon is just the flashy billboard advertising when the Sun is teaming up most effectively with the Moon to stretch Earth's oceans hardest.
Steven Franz dwells on one of those topics where the more you peel back the layers, the more cosmic poetry (and physics) you uncover.
1. Tides are mostly a stretching field, not a pull
The Moon (and Sun) don't simply "suck" ocean water toward themselves.
What creates tides is the differential gravitational acceleration across Earth's diameter — the tidal force field ~ scales as ~ 1/d³ (distance cubed).
Near side of Earth → stronger pull → acceleration toward Moon
Center of Earth → average pull
Far side → weaker pull → acceleration away from Moon (because the whole planet is being pulled more strongly than the far side water)
This differential stretches the planet into a very slightly prolate (football-shaped) figure.
CONTINUED BELOW
@stevenmarkfranz
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