The interaction of earth-orbiting and Sun-orbiting planetesimals (very large chunks of rocks like asteroids) early in the history of the Solar System led to their breakup. The Moon condensed from this debris.
Astroids are like the planeteseimal theory but instead a large creature named mark hanson pushed the particles together glued them but he sadly ate the remaining glue and couldn't finish the planets (astroids)
Large planetesimals have gravitational pull and attract smaaller ones.
Increasing the concentration of the reactants will increase the rate of collisions, but will not change the fact that most of the time particles are in motion and not colliding.
Cause you started with Pangaea a large super continent which slowly broke apart and each one started drifting. Now plate tectonics is how the collisions occur and when and WHY. WHY are they colliding?, because they have drifted away from each other and are now colliding back together again. And also each individual plate will break and come together again.
Accretion
dust and gas
The fission theory, the capture theory, the condensation theory, the colliding planetesimals theory and the ejected ring theory.
The fission theory, the capture theory, the condensation theory, the colliding planetesimals theory and the ejected ring theory.
Viktor Safronov
There are six different stages in the condensation theory. These include the formation of a nebula cloud, the formation of a sun, the formation of planetesimals, the expulsion of gases from the forming sun, the growth of the planetesimals, and the formation of larger planets from planetesimals.
Large planetesimals have gravitational pull and attract smaaller ones.
The theory is that the tectonic plates have faults and are colliding, moving away, or going by each other. ~Toria, 12
No. Stars are many times larger than planetesimals.
In theory, tectonic plates. http://www.ucmp.berkeley.edu/geology/tectonics.html
Planetesimals made from ice and sometimes rock are called comets.
The Fission Theory: The Moon was once part of the Earth and somehow separated from the Earth early in the history of the Solar System. The present Pacific Ocean basin is the most popular site for the part of the Earth from which the Moon came.The Capture Theory: The Moon was formed somewhere else, and was later captured by the gravitational field of the Earth.The Condensation Theory: The Moon and the Earth condensed together from the original nebula that formed the Solar System.The Colliding Planetesimals Theory: The interaction of earth-orbiting and Sun-orbiting planetesimals (very large chunks of rocks like asteroids) early in the history of the Solar System led to their breakup. The Moon condensed from this debris.The Ejected Ring Theory: A planetesimal the size of Mars struck the earth, ejecting large volumes of matter. A disk of orbiting material was formed, and this matter eventually condensed to form the Moon in orbit around the Earth.
As earth formed, most planetesimals were attracted by the earth's gravity and coalesced with earth.
Kinetic theory is when a high number of particles such as temperature, viscosity and volume that move randomly colliding in different directions. The speed of particles has an impact on temperature and gas pressure.