In the inner component of the solar system, just things i m sorry existas a solid in ~ high temperature are easily accessible to be provided as raw products for planetary assembly (so exactly how come thereis so much water ~ above the earth? -- answer later)So in the inner component of the solar system you have the right to only make a rocky planet via acretion the grains.In the outer component of the solar system, ices deserve to exist so friend canmake larger planets (e.g. Uranus and Neptune) the end of the much an ext abundant icesVery big planets like Jupiter and Saturn, whose composition isprimarily Hydrogen and Helum, developed in a manner similar to the Sun,that is no by accretion of structure blocks. Keep in mind that Jupiter can never becomea star. A star is a round of gas sufficiently hot to wake up nuclearreactions . The minimum mass require for this is about 8% themass of the Sun. Jupiter"s fixed is an order of magnitude belowthis limit. Jupiter will never ever be a star.Jupiter has a very huge mass and perturbs orbits of objects near them.There were many these objects scattered between Jupiter and PlutoJupiter redirected few of this cometary material right into the innersolar system and most the the earth"s water was yielded throughcomet bombardment (therefore would we be here without Jupiter?)Steps in the accretion process from small grains to big planetare represented in the complying with sequences:

![]() | action 1: accretion of cm sizedparticles. plenty of numbers the these small particles collide at low relatively velocity and also coalesce right into objects which are a couple of km in diameter |
![]() | step 2: physical Collision on km scale. when these km size objects space formed, they begin to smack right into one another and also stick thus developing fewer new objects of dimension 10-100 km |
![]() | Step 3: Gravitational accretion on10-100 kilometres scale. Once an object gets come a radius the 10-100 km, its cross ar is bigger than the physical overcome section because it exerts a gravitational affect on surrounding smaller bodies and, in essence, sweeps lock up. This process will produce a earth withsignificant gaps between each brushed up up zone. |
![]() | Step 4: Molten protoplanet fromthe heat of accretion . For each protoplanet that forms, there are thousands that left end planetisimal objects. These planetisimals space then accelerated by the relatively big mass the the formed planets and also they begin to relocate at high velocity transparent theinner solar mechanism - numerous of them ultimately impact the surface of thecooling planets. |
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High velocity collisions betweenchunks of rocks cause them to be shattered and also indeed, over thehistory of the solar system, the size of the biggest asteroidsare decreasing. The asteroid belt is thus not the remains of a planetthat was blown increase by the death Star.