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30 Cards in this Set

  • Front
  • Back

Gamma Rays

High Energy and Frequency


Low Wavelengths

Radio

Low Energy and Frequency


High Wavelengths

Visible Light

400 - 800 nanometers


400=short wavelength


800=long wavelength

Atoms that have gained or lost an electron and have a net charge are called

Ions

Absorption of a photon

Jumps to a higher energy level

Emission of a photon

Jumps to a lower energy level

Absorption line spectrum

Rainbow background, black lines

Blue Shifted

an object is moving towards us (shorter wavelengths)

Red Shifted

Object is moving away from us


(Longer wavelengths)

Earths Twin

Venus

My Very Excellent Mom Just Served Us Noodles

Mercury, Venus, Earth, Mars, Jupiter, Saturn, Uranus, and Neptune

The belt after the terrestrial planets

Asteroid Belt

The belt after the Jovian planets

Kuiper Belt

Oort Cloud

waaaaay past the Kuiper Belt. Most comets come from the Oort Cloud

The biggest rocky planet and the biggest gas planet

Earth, Jupiter

All planets orbit the sun

Counter clockwise

Nebula

A cloud of gas and dust

Bigger Axis Tilt

More dramatic seasons

The frost line is how many AU from our solar system

5 AU

Radioactive Decay

an unstable atomic nucleus loses energy by radiation

Nuclear Fusion

Nuclear fusion is a reaction in which two or more atomic nuclei combine to form different atomic nuclei and subatomic particles.

Order of Sun Layers


Charming Rabbits Celebrate Parties, Carrots, and Cuddles!

1. Core -energy is generated here


2. Radiative zone


3. Convective zone


4. Photosphere


5. Chromosphere


6. Corona

Fission

Large nucleus splits into daughter particles

Solar Thermostat

Self regulating temperature mechanism of the sun. Temp rises-nuclear reactions increase-energy output increases-outer layers expand and core temperature drops

Accretion:

Objects collide converting gravitational energy to kinetic energy then to thermal energy

Differentiation:

Denser materials sink to the core and the same energy conversion takes place as with accretion

Radioactivity

isotopes inside the planet decay into more stable elements releasing thermal energy

Convection

Hot rock rises and cooler rock falls

Conduction

Heat transfers from the warm mantle through the lithosphere to the surface

Radiation

Surface emits IR radiation into space