The solar system began to form from a giant molecular cloud of gas and dust particles about 4.6 billion years ago. This cloud most likely experienced a shock wave from a nearby supernova, which could have made it collapse under its own gravity. It then began to spin and flatten into a disk shape due to conservation of angular momentum. Most of the material in this nebula was pulled towards the center, in which formed our Sun. Within the spinning disk, the process of accretion had tiny grains of dust colling that caused them to stick and form larger particles called planetesimals. These planetesimals continued to collide and accumulate to form planets. Close to the Sun, where it is hotter, only rocky materials could condense, leading to the formation of 4 inner terrestrial planets: Mercury, Venus, Earth, and Mars. As you go more towards the outside, the cooler, icy materials are able to condense, allowing for the formation of the outer gas giants: Jupiter, Saturn, Uranus, and Neptune. As the planets formed, they cleared out their paths of orbit, by gravitational attraction. However, some debris remained which led to the formation of asteroids and comets. Asteroids are rocky remnants from the early solar system that never formed into planets, primarily found in the asteroid belt between Mars and Jupiter. Comets are icy bodies composed of dust, rock, and ice that originate from the outer solar system and sometimes head closer to the Sun.
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