a rock formed from a sedimentary, igneous or other metamorphic rocks that have under gone increased temperatures and pressure over a long period of time.
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sedimentary rock
rock made from compressed sediment
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mineral
a naturally occurring, inorganic substance present in the solid state, made of a specific chemical formula in a definite crystal structure.
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rock
an inorganic, solid, and natural substance without any specific atomic structure or chemical composition.
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what is the rock cycle?
is the process of how rocks become other types of rocks over huge periods of time
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ore
an ore is a mineral with a large amount of useful metal in it.
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what are the 2 ways minerals can form?
through the crystallization of magma, or the crystallization of materials dissolved in solution.
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properties of a mineral
hardness, luster, cleavage, and streak
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hardness
how easily a mineral can be scratched
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luster
the shininess of a surface of a mineral
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cleavage
the tendency of a mineral to break into a number of smooth planes
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streak
the color of a powdered or crushed mineral.
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properties of a rock
weight and density, color, layers, crystals and grain.
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intrusive igneous rock
is an igneous rock found and formed deep within the earth by magma.
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extrusive igneous rock
is an igneous rock found and formed on the surface of the earth by lava.
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difference between intrusive and extrusive igneous rocks.
Intrusive rocks tend to have larger crystals, this is because the magma takes longer to cool, so the crystals have more time to form. Extrusive rocks tend to have smaller crystals, This is because the lava cools much more rapidly so the crystals have less time to form.
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layers of the earth in order.
crust, mantle, outer core, inner core
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lithosphere
is the solid, outer part of the Earth, made of the crust and upper most solid mantle.
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Asthenosphere
is the denser, weaker layer beneath the lithospheric mantle made up of the partly molten section of the upper mantle.
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kinds of tectonic plates boundries
transform, divergent, and convergent.
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transformative boundries
when two tectonic plates slid past each other in opposite directions.
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Divergent boundaries
when two plates spread apart from each other.
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convergent boundaries
when a two tectonic plates go against each other and one goes
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continental drift
is the idea that continents are continually moving and have significantly changed positions over millions of years.
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sea-floor spreading
that the middle of the ocean is spreading apart, moving very slowly in opposite directions.
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energy
energy is a massless entity that causes things to happen. It is the ability of an object to do work.
gravitational potential energy, chemical potential energy, elastic potential energy
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Law of conservation of energy
energy cannot be created or destroyed, it can only be transformed of transferred.
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conduction
passing kinetic energy from one substance to another by direct contact
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convection
is the transfer of heat by the movement of a fluid (gas or liquid) between areas of different temperatures
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radiation
the transfer of heat across space or through another substance without touching it in the forms of waves/rays.
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magma
molten rock underground
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lava
molten rock exposed at the earths surface
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what causes seismic waves?
they are caused by a sudden movement of materials within the earth
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P-waves (primary waves)
they are the fasted wave that travels through the inside of the Earth through solid and liquid. It reaches the seismic station first and moves the rock in a push-pull compressional wave.
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S-waves (secondary waves)
they travel through the inside of the earth through solids only, it reaches the seismic station second. It moves rock up and down perpendicular to the wave.
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what are fossils
is an organism preserved in a rock.
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how do fossils form
fossils form when an organism dies, and it gets covered by sediment then over millions of years, as the sediment builds up, it compacts and cements turning it into a sedimentary rock, which preserves the organism from weathering and predators.
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how do you date fossils
You can date them by using comparative dating, this compares the different layers of the Earths sediments, bottom being the oldest and top being the youngest. Another way to date fossils is using radioactive dating, you do this by measuring the amount of radioactivity left in rocks
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pangea
Pangea was a super-continent, and the idea that the all the continents were once connected.