Rip 💀 |FAKE COLLAB| (Join pls!) #roblox #robloxanimaion #animation

Rip 💀 |FAKE COLLAB| #roblox #robloxanimaion #animation
pls join

[Eliotte]

For those who dont understand:

Nuclear fission is a reaction in which the nucleus of an atom splits into two or more smaller nuclei. The fission process often produces gamma photons, and releases a very large amount of energy even by the energetic standards of radioactive decay.

Induced fission reaction. A neutron is absorbed by a uranium-235 nucleus, turning it briefly into an excited uranium-236 nucleus, with the excitation energy provided by the kinetic energy of the neutron plus the forces that bind the neutron. The uranium-236, in turn, splits into fast-moving lighter elements (fission products) and releases several free neutrons, one or more "prompt gamma rays" (not shown) and a (proportionally) large amount of kinetic energy.
Nuclear fission was discovered by chemists Otto Hahn and Fritz Strassmann and physicists Lise Meitner and Otto Robert Frisch. Hahn and Strassmann proved that a fission reaction had taken place on 19 December 1938, and Meitner and her nephew Frisch explained it theoretically in January 1939. Frisch named the process "fission" by analogy with biological fission of living cells. In their second publication on nuclear fission in February 1939, Hahn and Strassmann predicted the existence and liberation of additional neutrons during the fission process, opening up the possibility of a nuclear chain reaction.
For heavy nuclides, it is an exothermic reaction which can release large amounts of energy both as electromagnetic radiation and as kinetic energy of the fragments (heating the bulk material where fission takes place). Like nuclear fusion, for fission to produce energy, the total binding energy of the resulting elements must be greater than that of the starting element.
Fission is a form of nuclear transmutation because the resulting fragments (or daughter atoms) are not the same element as the original parent atom. The two (or more) nuclei produced are most often of comparable but slightly different sizes, typically with a mass ratio of products of about 3 to 2, for common fissile isotopes.[1][2] Most fissions are binary fissions (producing two charged fragments), but occasionally (2 to 4 times per 1000 events), three positively charged fragments are produced, in a ternary fission. The smallest of these fragments in ternary processes ranges in size from a proton to an argon nucleus.
Apart from fission induced by an exogenous neutron, harnessed and exploited by humans, a natural form of spontaneous radioactive decay (not requiring an exogenous neutron, because the nucleus already has an overabundance of neutrons) is also referred to as fission, and occurs especially in very high-mass-number isotopes. Spontaneous fission was discovered in 1940 by Flyorov, Petrzhak, and Kurchatov[3] in Moscow, in an experiment intended to confirm that, without bombardment by neutrons, the fission rate of uranium was negligible, as predicted by Niels Bohr; it was not negligible.[3] Despite the possibility of spontaneous fission, it does not play any role for energy production of stars. In contrast to nuclear fusion, which drives the formation of stars and their development, one can consider nuclear fission as neglectable for the evolution of the universe. Accordingly, all elements (with a few exceptions, see "spontaneous fission") which are important for the formation of solar systems, planets and also for all forms of life are not fission products, but rather the results of fusion processes.
The unpredictable composition of the products (which vary in a broad probabilistic and somewhat chaotic manner) distinguishes fission from purely quantum tunneling processes such as proton emission, alpha decay, and cluster decay, which give the same products each time. Nuclear fission produces energy for nuclear power and drives the explosion of nuclear weapons. Both uses are possible because certain substances called nuclear fuels undergo fission when struck by fission neutrons, and in turn emit neutrons when they break apart. This makes a self-sustaining nuclear chain reaction possible, releasing energy at a controlled rate in a nuclear reactor or at a very rapid, uncontrolled rate in a nuclear weapon.
The amount of free energy released in the fission of an equivalent amount of 235
U is a million times more than that released in the combustion of methane or from hydrogen fuel cells.[4]
The products of nuclear fission, however, are on average far more radioactive than the heavy elements which are normally fissioned as fuel, and remain so for significant amounts of time, giving rise to a nuclear waste problem. However, the seven long-lived fission products make up only a small fraction of fission products. Neutron absorption which does not lead to fission produces plutonium (from 238
U) and minor actinides (from both 235
U and 238
U) whose radiotoxicity is far higher than that of the long lived fission products. Concerns over nuclear waste accumulation and the destructive potential of nuclear weapons are a counterbalance to the peaceful desire to use fission as an energy source. The thorium fuel cycle produces virtually no plutonium and much less minor actinides, but 232
U - or rather its decay products - are a major gamma ray emitter. All actinides are fertile or fissile and fast breeder reactors can fission them all albeit only in certain configurations. Nuclear reprocessing aims to recover usable material from spent nuclear fuel to both enable uranium (and thorium) supplies to last longer and to reduce the amount of "waste". The industry term for a process that fissions all or nearly all actinides is a "closed fuel cycle".

[SnackCOREDUCK]

"YÆ-"
just beautiful
Edit: HOW THE HECK DID I GET THESE LIKES BRU-

[Astra_Comet]

“It’s a bird! it’s a plane! No that’s my innocence flying away 😔”

[GIH-HUNLOVER]

You can tell Blondie's traumatized

[sigmacat]

The way the daddy walking backward got me laughing😂

[arty-aftn]

Bruh- I got the whole room staring at me I fell out of my chair bruh- 😂🤣

[ejenalifavor]

Nah dad said "erm bye im heading to get milk"💀💀

[Shekiahberns]

Mom:is shock) 😦
Dad:erm i'm going to buy milk 🥛
Little sister: yay!🥰
Brother: 🤨😨

[wiggletime]

not the dad doing the moonwalk while floating😂

[JM-rvws]

I fell out of my chair when kumotta made that suprised face and the father backed out of the room LOL😂💀

[Two_Idiots-ri]

Not the dad backing up like he just got cooked by her own daughter💀💀💀🙏🙏🙏

[Լamborghini]

Dad backing up like he innocent, like he didn’t create a new sibling for their son. The bedroom shake the whole house.

[StubbycAR]

Ain’t no way I played this max volume in a restaurant

[Great_frog]

for anybody who does not understand

Lava is magma that reaches the Earth's surface. While magma refers to molten rock beneath the crust, it is termed lava once it erupts. Lava is composed primarily of silicate minerals and contains various gases such as water vapor, carbon dioxide, and sulfur dioxide. Its temperature typically ranges between 700°C to 1, 200°C (1, 292°F to 2, 192°F), and its composition determines its viscosity, flow rate, and the type of volcanic eruption it produces. Lava originates in the Earth's mantle, the semi-solid layer beneath the crust. When mantle rocks partially melt due to high temperatures, pressure release, or the addition of volatiles, they form magma. This magma accumulates in magma chambers and, under high pressure, forces its way to the surface through volcanic vents. When magma erupts from a volcano, it transforms into lava. The nature of this eruption depends on the chemical composition of the magma. For example, basaltic magma, low in silica, results in relatively gentle lava flows, while andesitic or rhyolitic magma, rich in silica, tends to be more viscous and explosive. There are several types of lava, each with distinct characteristics
Pāhoehoe (pronounced "pah-hoy-hoy") is a smooth, ropey type of basaltic lava. It flows easily due to its low viscosity and forms thin, glossy crusts. Pāhoehoe flows are common in Hawaiian volcanoes and can travel long distances from the eruption site.
ʻAʻā Lava ʻAʻā (pronounced "ah-ah") is a rough, clinkery lava with a jagged surface. It moves more slowly than pāhoehoe due to its higher viscosity and often results in thick, blocky flows. Once solidified, ʻAʻā lava is difficult to walk on due to its sharp fragments. Pillow Lava Pillow lava forms underwater, typically at mid-ocean ridges or undersea volcanoes. As lava cools rapidly upon contact with water, it forms rounded, pillow-shaped structures. These structures are vital in studying oceanic crust formation and underwater volcanic activity Block lava resembles ʻAʻā but is formed from more viscous lavas like andesite and dacite. It consists of large, angular blocks and is typical of continental and subduction zone volcanoes. Lava varies in chemical composition, influencing its behavior during eruptions Basaltic Lava (low silica, ~50%): Low viscosity, fast-flowing, less explosive.
Andesitic Lava (intermediate silica, ~60%): Medium viscosity, moderately explosive. Rhyolitic Lava (high silica, ~70%): High viscosity, slow-flowing, highly explosive. These compositions result from differences in the source rock, the degree of partial melting, and interactions with the Earth's crust during magma ascentWhen lava emerges, it flows under gravity, spreading over landscapes and creating lava fields. The speed and distance of lava flows depend on slope, temperature, and viscosity. As it cools, lava solidifies from the outside in. A crust forms first, while the interior remains molten longer. Cooling may result in various formations, such as lava tubes, which are tunnels formed when surface lava cools while the interior continues to flow. In some cases, lava solidifies into columnar basalt, creating stunning hexagonal patterns seen in places like the Giant’s Causeway in Northern Ireland. Impact on the Environment Lava has both destructive and constructive effects. On one hand, it can obliterate ecosystems, destroy property, and displace communities. Lava flows bury everything in their path, including forests, homes, and infrastructure. Historical eruptions, such as those of Mount Vesuvius or Mount Etna, demonstrate the devastating potential of lava. On the other hand, lava contributes to the creation of new land. The Hawaiian Islands, for instance, were formed entirely by successive lava flows from underwater volcanoes. Over time, weathering of lava rocks forms fertile soils rich in minerals, which support diverse plant life and agriculture. Lava in Human History and Culture
Throughout history, lava and volcanoes have been subjects of myth, reverence, and scientific curiosity. In many cultures, volcanoes were considered homes of gods or spirits. The Hawaiian goddess Pele, for instance, is believed to live in the Halemaʻumaʻu crater and is associated with fire, lightning, and lava. In modern times, lava remains a critical focus for volcanologists and geologists. Monitoring lava flows helps predict volcanic activity and reduce risks to human populations. Technologies such as satellite imagery, drones, and thermal imaging are now essential in tracking lava behavior and developing evacuation plans. Lava is not unique to Earth. Evidence of past volcanic activity has been observed on other celestial bodies. The Moon’s dark plains, known as maria, are vast basaltic lava flows. Mars has ancient lava plains and the largest volcano in the solar system, Olympus Mons. Venus, too, shows signs of volcanic resurfacing. Studying extraterrestrial lava offers clues to planetary evolution and geological activity across the universe. Lava and Modern Science
Scientists study lava to understand Earth's internal processes and tectonic activity. Lava samples reveal information about the mantle’s composition and temperature. Additionally, artificial lava flows created in laboratories help researchers test theories about flow Lava also plays a role in geothermal energy production. In regions with active volcanism, the heat from lava and magma chambers can beharnessed to generate electricity and provide sustainable energy solutions. Lava is a mesmerizing and multifaceted natural phenomenon that reflects the dynamic processes of our planet’s interior. While it can be a source of destruction, it is also a creator—shaping landscapes, forming new land, and enriching the soil. From the heart of Earth to the surface of distant planets, lava symbolizes the ever-changing nature of planetary bodies. By studying lava, we gain a deeper appreciation for Earth’s geological history and enhance our ability to live safely in harmony with the planet’s fiery forces.

[BestRobloxianedits]

I was using this as my flashlight at night and my son walks through the hallway while this is on full blast😅

[Gojofan-ym]

“Well what I heard is you said no no no and daddy said yes yes yes” got me rolling on the ground 😂😂😂😂😂

[Daisyzs]

I flew away from my bed and all of my toys were looking at me 😭😭😭😭😭-

[Sikepro]

Best video I have ever seen in this whole year

[sirineboussif]

"Is a bird! "
"No is a plane! "
"No is my brain cells flying away... "

[valquiriabarboza]

The dad was like: "nah i cooked"