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Brooke's Notes
Brooke's Chapter notes
Question | Answer |
---|---|
Scientific Method | set of steps used to solve problems |
variables | are factors that can change in an expirement |
how many variables can be tested at one time? | one |
independent variable | the one being tested |
dependent variable | variable being measured |
constants | variables that do not change |
control | standard in which results are compared |
technology | use of science discoveries for practical purposes |
is technology transferable??? | WELL DUH!!!!! |
meteorology | study of weather |
rain guage | first intrument of weather |
scientific theory | an explanation backed by results of many tests |
scientific law | describes how things work in nature |
ethics | deals with moral values about what is good or bad |
bias | personal opinion (best to prevent these) |
matter | made up of atoms |
element | substances that contain only one type of atom |
proton | positive charge |
electron | negative charge |
neutron | no charge |
atomic number | tells the number of protons and electrons in an atom |
atomic mass number | tells the number of protons + neutrons in an atoms nucleus |
isotopes | atoms of the same element that have different neutrons |
ions | electrically charged atoms |
bond | force that holds atoms together |
minerals | naturally occuring, inorganic solid that has a definate chemical composition and an orderly internal atomic structure |
naturally occuring | formed by processes inside or on earth, not man made |
inorganic | not made from living things |
crystal | solid with atoms arranged in repeating patterns |
magma | hot melted rock |
magma cools slowly | large crystals are formed |
magma cools quickly | smaller crystals are formed |
mineral groups | are defined by their composition |
silicates | contain the element silicon and oxygen and one or more other elements |
hardness | is the measure of how easily a mineral can be scratched |
luster | way a mineral reflects light |
metallic luster | looks like metal |
non-metallic luster | doesnt look like metal |
specific gravity | ratio of a minerals weight to the weight of an equal volume of water |
streak | the color of a mineral in its powdered form |
break | the way a mineral breaks |
cleavage | minerals that break along smooth, flat surfaces |
fracture | minerals that break with uneven, jagged surfaces. |
gems | are rare and beautiful minerals that are highly prized. |
ores | mineral or rock containing a substance that can be mined for a profit. |
vein mineral | when metallic elements dissolve and form mineral deposits in cracks and crevices of rock |
rock | a mixture of minerals, volcanic glass, organic matter and other materials |
rock cycle | model showing the processes that create and change rock |
igneous rock | forms when magma cools |
lava | magma that has reached the earths crust |
intrusive igneous | slowly cooled magma inside the earths crust;small crystals will form. |
extrusive igneous | quickly cooled magma outside the earths crust;large crystals will form. |
metamorphic rock | formed from heat, pressure, and hot fluids. |
foliated | when mineral grains flatten in parallel layers |
nonfoliated | when mineral grains rearrange and do NOT form layers |
sedimentary rock | form from compaction and cementation of sediments |
detrial | form from small rock particles |
chemical | form from dissolved minerals |
organic | formed from remains of once living plants or animals |
mechanical weathering | physical process that breaks rocks into sediments |
plant roots | grow and expand rock, causing it to break |
ice wedging | water enters crevices, freezes, and expands causing it to break |
crystal growth | solutions enter, water evaporates, forms crystals that push the rock apart. |
wind and water | constant pounding of wind and water that breaks rock particles. |
chemical weathering | chemical reactions dissolve minerals and rocks breaking them down. |
oxidation | chemical process that breaks down iron. |
carbonic acid | CO2, react with minerals breaking them down. |
continental drift | hypothesis stating all continents were once connected but have moved to their current locations. |
pangaea | large landmass formed by connected continents |
Alfred Wergener | formed the |