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Our Sun - STEMpire Central
Our Sun - STEMpire Central

... A. visible “surface” of the Sun B. the “graininess” of the Sun’s surface, evidence of the lava lamp effect C. dim layer of the Sun’s atmosphere, seen as a pink band during an eclipse D. thin atmospheric layer where temperatures skyrocket E. cooler, darker regions of the Sun’s surface F. outer layer ...
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... • One light year is how far light travels in one year (based on distance NOT time) • We see all night stars as they were when the light we see left each star ...
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... • Once a star is formed there will be a debris orbiting around it. • This debris may join together to form planets, again due to the gravitational attraction between the particles. • This is the most common explanation to explain the formation of our solar system. • We are all made of stars. ...
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... • The Sun’s surface features vary in an 11-year cycle • This is related to a 22-year cycle in which the surface magnetic field increases, decreases, and then increases again with the opposite polarity • The average number of sunspots increases and decreases in a regular cycle of approximately 11 ye ...
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Formation and evolution of the Solar System



The formation of the Solar System began 4.6 billion years ago with the gravitational collapse of a small part of a giant molecular cloud. Most of the collapsing mass collected in the center, forming the Sun, while the rest flattened into a protoplanetary disk out of which the planets, moons, asteroids, and other small Solar System bodies formed.This widely accepted model, known as the nebular hypothesis, was first developed in the 18th century by Emanuel Swedenborg, Immanuel Kant, and Pierre-Simon Laplace. Its subsequent development has interwoven a variety of scientific disciplines including astronomy, physics, geology, and planetary science. Since the dawn of the space age in the 1950s and the discovery of extrasolar planets in the 1990s, the model has been both challenged and refined to account for new observations.The Solar System has evolved considerably since its initial formation. Many moons have formed from circling discs of gas and dust around their parent planets, while other moons are thought to have formed independently and later been captured by their planets. Still others, such as the Moon, may be the result of giant collisions. Collisions between bodies have occurred continually up to the present day and have been central to the evolution of the Solar System. The positions of the planets often shifted due to gravitational interactions. This planetary migration is now thought to have been responsible for much of the Solar System's early evolution.In roughly 5 billion years, the Sun will cool and expand outward many times its current diameter (becoming a red giant), before casting off its outer layers as a planetary nebula and leaving behind a stellar remnant known as a white dwarf. In the far distant future, the gravity of passing stars will gradually reduce the Sun's retinue of planets. Some planets will be destroyed, others ejected into interstellar space. Ultimately, over the course of tens of billions of years, it is likely that the Sun will be left with none of the original bodies in orbit around it.
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