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Encounter Hypothesis
This hypothesis suggests that a large celestial object (like another star) passed close to the Sun in the early days of the solar system. Its gravity pulled out gas and dust from the Sun. That material spread along the object's path, cooled down, and eventually condensed into planets.
Protoplanet Hypothesis
A near collision between the Sun and another star caused ejected materials to form tiny particles called planetesimals which collided and struck together to form planets
Nebular Hypothesis
The solar system started as a giant cloud of gas and dust. This proves why planets have different sizes, orbit in same direction, and flat plane.
Encounter, Protoplanet, Nebular
3 Hypothesis
Sun
There is an undergoing nuclear fusion in this core.
Convert hyrdogen to helium
How to produce the sun’s energy?
74
% of hydrogen in the sun?
24
% of helium in the sun?
Radioactive Zone
Energy from the core moves out slowly through radiation
Convection Zone
Outer layer of the sun’s interior where hot gasses rise and cooler gasses sink
Terrestrial Planets
Planets that are composed of rocks with a molten heavy metal core. Features valleys, volcanoes, and craters. (Fewer moons)
Jovian planets
These planets are hydrogen and helium. Gas; outer layer. Liquid; inner layer
Must orbit the sun, clear its orbit, spherical in shape
Criteria to become a planet (3)
Rotation
Planet movement around axis
Revolution
Planet movement around sun
Major axis
Minor axis
Aphelion
Perihelion
Equal Areas
As a planet orbits the sun, it moves faster when its closer to the sun and slower when farther from the sun.
Harmony
The square of the planet’s orbital period is proportional to the cube of its average distance from the sun
Asteroids
Rocky and airless remnants left over from the early formation
Comets
Cosmic snowballs of frozen gasses, rock, and dust that orbit around the Sun