Save
Busy. Please wait.
Log in with Clever
or

show password
Forgot Password?

Don't have an account?  Sign up 
Sign up using Clever
or

Username is available taken
show password


Make sure to remember your password. If you forget it there is no way for StudyStack to send you a reset link. You would need to create a new account.
Your email address is only used to allow you to reset your password. See our Privacy Policy and Terms of Service.


Already a StudyStack user? Log In

Reset Password
Enter the associated with your account, and we'll email you a link to reset your password.
focusNode
Didn't know it?
click below
 
Knew it?
click below
Don't Know
Remaining cards (0)
Know
0:00
Embed Code - If you would like this activity on your web page, copy the script below and paste it into your web page.

  Normal Size     Small Size show me how

Vocabscience90

science vocab- 90 words for final

QuestionAnswer
mineral naturally formed, inorganic solid that has a definite crystalline structure
element substance that can not be separated or broken down into simpler substances by chemical means
compound substance made up of atoms of two or more different elements joined by chemical bonds
crystals solid whose atoms, ions, or molecules are arranged in a definite pattern
silicate minerals minerals that contains a combination of silicon, oxygen, and one or more metals
nonsilicate minerals mineral that doesn't contain compounds of silicon and oxygen
streak the color of the power of a mineral
cleavage splitting of a mineral along smooth, flat surfaces
Fracture the manner in which a mineral breaks along either curved or irregular surfaces
hardness a measure of the ability of a mineral to resist scratching
density ratio of the mass of a substance to the volume of the substance
ore natural material whose concentration of economically valuable minerals is high enough for the material to be mined profitably
reclamation process of returning land to its original condition after mining is completed
streak color of the powder of a mineral
native elements minerals that are composed of only one element.
Carbonates minerals that contain combinations of carbon and oxygen
halides compounds that form when fluorine, chlorine, iodine, or bromine combine with sodium, potassium, or calcium
oxides are compounds that form when a element combines chemically with oxygen
sulfates mineral that contains sulfur and oxygen,SO4, sulfates are used in toothpaste, cement, cosmetics, and paint
sulfides minerals that contain one or more elements such as lead, iron, or nickel
luster way in which a mineral reflects light
special properties some properties are particular to only a few types of minerals
fluorescence calcite and fluorite glow under ultraviolet light
chemical reaction calcite will become bubbly or fizz when a drop of weak acid is placed upon it
optical properties thin, clear piece of calcite placed over an image will cause a double image
magnetism both magnetite and pyrrhotite are natural magnets that attract iron
taste halite has a salty taste
radioactivity minerals that contain radium or uranium can be detected by a Geiger counter
nonmetallic minerals shiny or dull surfaces, light may pass through them, and are good insulators of electricity
metallic minerals shiny surfaces, don't let light go through them, and are good conductors of heat ans electricity
gemstones some nonmetallic minerals, used for beauty and color is most important characteristic
rock cycle series of processes in which a rock forms, changes from 1 type to another, is destroyed, and forms again by geological processes
erosion proces by which wind,water,ice, or gravity transports soil and sediment from one location to another
deposition process in which material is laid down
composition the chemical makeup of a rock; describes either the minerals or other materials in the rock
texture quality of a rock that is based on size, shapes, and position of the rock's grains
igneous rock forms from magma, cools and solidifies. Type; depends on composition of magma and the amount of time it takes to cool
intrusive igneous rock rock formed from the cooling and solidification of magma beneath Earth's surface
extrusive igneous rock rock that forms as a result of volcanic activity at or near Earth's surface
dikes sheet like intrusions that cut across previous rock units
sills sheetlike intrusions that are oriented parallel to previous rock units
batholiths largest igneous intrusions
stocks intrusive bodies that are exposed over smaller areas than batholiths
fissures sometimes lava erupts and flows from long cracks in the Earth's crust
lava plateaus when a large amount of lava flows out of fissures onto land, the lava can cover a large area and form a plain
stratification process in which sedimentary rocks are arranged in layers
strata a single horizontal layer of rock
foliated metamorphic rock texture of metamorphic rock in which the mineral grains are arranged in planes or bands
non-foliated metamorphic rock the texture of metamorphic rock in which the mineral grains aren't arranged in planes or bands
deformation change in the shape of a rock caused by a force put on it
uniformitarianism principle that states that geologic processes that occurred in the past can be explained by current geologic processes
catastrophism principle that states that geologic change occurs suddenly
paleontology scientific study of fossils
paleontology scientific study of past fossil plants
relative dating any method of determining whether an event or object is older or younger than other events or objects
superposition a principle that states that younger rock lie above older rocks if the layers haven't been disturbed
geologic column arrangement of rock layers in which the oldest rocks are at the bottom
unconformity break in the geologic record when rock layers are eroded or when sediment didn't deposit for a long time
disconformity part of a sequence of parallel rock layers are missing
nonconformity found when horizontal sedimentary rock layers lie on top of an eroded surface of older rock
angular unconformity found between horizontal layers of sedimentary rock and layers ofrock that have been folded or tilted
absolute dating any method of measuring the age of an event or object in years
isotope an atom that has the same number of protons as other atoms of the same elements do but that has a different number of neutrons
radioactive decay the process in which a radioactive isotope tends to break down into a stable isotope of the same elements or another element
radiometric dating a method of determining the age of an object by estimating the relative percentages of a parent isotope and a daughter isotope
half-life time needed for half of a sample of a radioactive substance to undergo radioactive decay
fossil remains or physical evidence of an organism preserved by geological process
trace fossil fossilized mark that id formed in soft sediment by movement of an animal
mold mark or cavity made in a sedimentary surface by a shell or other body
cast type of fossil that forms when sediments fill in the cavity left vy a decomposed organism
index fossil fossil that is found in the rock layers of only one geologic age and that is used to establish the age of the rock layers
geologic time scale the standard method used to divide the earth's long natural history into manageable parts
eon largest division of geologic time
era a unit of geologic time that includes 2 or more periods
period unit of geologic time that includes two or more periods
epoch subdivision of a geologic periods
extinction death of every member of species
index mineral estimate the temp., depth, and pressure at which a rock undergoes metamorphism
metamorphic rock Rock that was once one form of rock but has changed to another under the influence of heat, pressure,
sedimentary rock Sedimentary rocks are types of rock that are formed by the deposition of material at the Earth's surface and within bodies of water.
Created by: Emmalou2
Popular Earth Science sets

 

 



Voices

Use these flashcards to help memorize information. Look at the large card and try to recall what is on the other side. Then click the card to flip it. If you knew the answer, click the green Know box. Otherwise, click the red Don't know box.

When you've placed seven or more cards in the Don't know box, click "retry" to try those cards again.

If you've accidentally put the card in the wrong box, just click on the card to take it out of the box.

You can also use your keyboard to move the cards as follows:

If you are logged in to your account, this website will remember which cards you know and don't know so that they are in the same box the next time you log in.

When you need a break, try one of the other activities listed below the flashcards like Matching, Snowman, or Hungry Bug. Although it may feel like you're playing a game, your brain is still making more connections with the information to help you out.

To see how well you know the information, try the Quiz or Test activity.

Pass complete!
"Know" box contains:
Time elapsed:
Retries:
restart all cards