Charged particles come from the sun, especially after sunspot activity and solar flares. They stream through space and are attracted to the magnetic poles of the earth. In the ionosphere they collide with oxygen and nitrogen atoms, which give out green, blue and red light.
This light is known as the Aurora Borealis, or Aurora Australis, the Northern and Southern Lights.
During gel electrophoresis, the smaller particles move faster than the larger ones. The end of the gel where the samples are loaded is called the sample origin. Samples move from the origin toward the opposite electrode according to size. At the end of the run, smaller particles will have migrated farther from the origin and the larger ones will be found closer to the origin
The origin is in the random motions of all the particles that came together under the mutual force of gravity. Suppose two objects approach each other, but don't actually collide. If they come close enough the force of attraction between them causes them to go into an orbit round each other (round their common centre of gravity). In a cloud of particle the same basic process produces a spinning disc which with further compression can eventually produce a star.
The theory for the origin of planetary ring particles suggests that they are remnants of moons or asteroids that were shattered by collisions. Alternatively, they may also be the result of material that never fully coalesced into a moon due to gravitational forces from the planet.
The Northern lights can be seen round the magnetic North pole of the Earth in the Arctic Circle. High energy particles of the Solar wind are guided to Earth down field lines and excite air molecules to glow. The Aurora Australis occurs over Antarctica
Cosmic ray: A ray of radiation of extraterrestrial origin, consisting of one or more charged particles such as protons, alpha particles, and larger atomic nuclei. Cosmic rays entering the atmosphere collide with atoms, producing secondary radiation, such as pions, muons, electrons, and gamma rays. Cosmic rays (and secondary radiation) can be easily seen in a cloud chamber.(American Heritage Dictionary, 2005)
The origin of free oxygen
Cosmic ray: A ray of radiation of extraterrestrial origin, consisting of one or more charged particles such as protons, alpha particles, and larger atomic nuclei. Cosmic rays entering the atmosphere collide with atoms, producing secondary radiation, such as pions, muons, electrons, and gamma rays. Cosmic rays (and secondary radiation) can be easily seen in a cloud chamber.(American Heritage Dictionary, 2005)
I don't know the origin - but I do know it's a song by Atmosphere
Presently, the ejected ring theory best describes the origin of moon.
the plates under the ground banging together
During gel electrophoresis, the smaller particles move faster than the larger ones. The end of the gel where the samples are loaded is called the sample origin. Samples move from the origin toward the opposite electrode according to size. At the end of the run, smaller particles will have migrated farther from the origin and the larger ones will be found closer to the origin
The theory suggesting that the Earth originated from gas and dust particles is known as the Nebular Hypothesis. It was proposed by scientists such as Immanuel Kant and further developed by Pierre-Simon Laplace in the 18th century. This hypothesis states that the solar system formed from a rotating disk of gas and dust around the young sun.
the American medical association called for the protection of earths diversity
The origin of photosynthetic prokaryotes caused an aerobic atmosphere during the history of the earth.
Mendelevium was obtained in 1955 after the bombardment of 253Es with alpha particles in a cyclotron.
When air molecules collide with objects, they can produce sound waves. These sound waves travel through the air and reach our ears, allowing us to hear the sound created by the collisions.
The point on the earth's surface closest to the origin of an earthquake is called the epicenter. This is where the seismic waves generated by the earthquake first reach the surface.