• Shuffle
    Toggle On
    Toggle Off
  • Alphabetize
    Toggle On
    Toggle Off
  • Front First
    Toggle On
    Toggle Off
  • Both Sides
    Toggle On
    Toggle Off
  • Read
    Toggle On
    Toggle Off
Reading...
Front

Card Range To Study

through

image

Play button

image

Play button

image

Progress

1/111

Click to flip

Use LEFT and RIGHT arrow keys to navigate between flashcards;

Use UP and DOWN arrow keys to flip the card;

H to show hint;

A reads text to speech;

111 Cards in this Set

  • Front
  • Back
CHAPTER 1
CHAPTER 1
astronomy
the study of objects beyond Earth's atmosphere
meteorology
the study of the air that surrounds our planet
geology
the study of materials that make up Earth and the processes that form and change these materials
oceanography
the study of Earth's oceans
lithosphere
the rigid outer shell of the planet and includes the crust and the mantle
asthenosphere
partially molten, plasticlike, flowing layer located below the solid part of Earth's mantle
hydrosphere
the water in Earth's oceans, seas, lakes, rivers and glaciers, and the water in the atmosphere
atmosphere
the blanket of gases that surrounds our planet
biosphere
all organisms on Earth as well as the environments in which they live
independent variable
the factor that is manipulated by the experimenter
dependent variable
a factor that can change if the independent variable is changed
control
used in an experiment to show that the results of an experiment are actually a result of the condition being tested
Le Systeme International d'Unites (SI)
a system that is a modern version of the metric system
law
a basic fact that describes the behavior of a natural phenomenon
scientific notation
a type of shorthand used to express the number as a multiplier and a power of ten
theory
an explanation based on many observations during the repeated experiments
CHAPTER 2
CHAPTER 2
cartography
the science of mapmaking
equator
that imaginary line that lies at 0 degrees latitude and circles Earth midway between the north and south poles
latitude
the distance in degrees north or south of the equator
longitude
the distance in degrees east or west of the prime meridian
prime meridian
imaginary line representing 0 degrees longitude, running from the north pole, through Greenwich, ENgland, to the south pole
International Date Line
180 degress meridian and serves as the transition line for calendar days
topographic maps
show changes in elevation of Earth's surface
contour line
connect points of equal elevation
contour interval
the difference in elevation between two side-by-side contour lines
map legend
explains what the symbols represent on a map
map scale
the ration between distances on a map and actual distances on the surface of Earth
remote sensing
the process of collecting data about Earth from far above Earth's surface
electromagnetic spectrum
the arrangement of electromagnetic radiation according to wavelengths
frequency
the number of waves that pass a particular point each second
Landsat satellite
information-gathering satellite that uses visible light and infrared radiation to map Earth's surface
Topex/Poseidon satellite
data-gathering satellite that uses radar to map features on the ocean floor
Global Positioning System (GPS)
Satellite-based navigation system that permits a user to pinpoint his or her exact location on Earth
sonar
the use of sound waves to detect and measure objects underwater
CHAPTER 3
CHAPTER 3
element
a substance that cannot be broken down into simpler substances by physical or chemical means
atom
the smallest particle of an element that has all of the characteristics of that element
nucleus
made up of protons and neutrons
protron
a tiny particle that has mass and a positive electrical charge
neutron
a particle with about the same mass as a protron, but it is electrically neutral, has no electrical charge
atomic number
the number of protons in an atom's nucleus
mass number
the combined number of protons and neutrons
electron
has little mass, but has a negative electrical charge that is exactly the same magnitude as the positive charge of a proton
energy level
represents the area in an atom where an electron is most likely to be found
valence electrons
electrons in the outermost energy level
isotopes
atoms of the same element have different mass numbers
atomic mass
average of the mass numbers of the isotopes of an element
radioactivity
the spontaneous process through which unstable nuclei emit radiation
compound
a substance that is composed of atoms of two or more different elements that are chemically combined
chemical bonds
the forces that hold the elements together in a compound
covalent bond
the attraction of two atoms for a shared pair of electrons that holds the atoms together
molecule
two or more atoms held together by covalent bonds
ion
an atom that gains or loses an electron and is charged
ionic bond
the attractive force between two ions of opposite charge
chemical reaction
the change of one or more substances into other substances
solution
homogeneous mixture whose components cannot be distinguished and can be classified as liquid, gaseous, solid or a combination
acid
a solution containing a substance that produces hydrogen ions in water
crystalline structure
when particles in a solid are arranged in regular geometric patterns
glasses
solids that consist of densely packed atoms arranged at random
evaporation
the process of change from a liquid to a gas
sublimation
the change of state from a solid to a gas without an intermediate liquid state
plasmas
hot, highly ionized, electrically conducting gases
condensation
the change from a gas to a liquid
CHAPTER 4
CHAPTER 4
mineral
a naturally occurring, inorganic solid with a specific chemical composition and a definite crystalline structure
crystal
a solid in which the atoms are arranged in repeating patterns
magma
molten material found beneath Earth's surface
silicates
minerals that contain silicon and oxygen and usually one or more other elements
luster
the way that a mineral reflect light from its surface
streak
the color of a mineral when it is broken up and powdered
hardness
a measure of how easily a mineral can be scratched
cleavage
a mineral that splits relatively easily and evenly along one or more flat planes
fracture
minerals that break with rough or jagged edges
specific gravity
the ratio of the weight of a substance to the weight of an equal volume of water at 4 degrees Celsius
ore
a mineral that contains a useful substance that can be mined at a profit
gems
valuable minerals that are prized for their rarity and beauty
CHAPTER 5
CHAPTER 5
igneous rocks
intrusive or extrusive rock formed from the cooling and crystallization of magma; can be classified as felsic, mafic, intermediate, and ultramafic, according to its mineral composition
lava
magma that flows out onto Earth's surface
extrusive
fine-grained igneous rocks that cool quickly on Earth's surface
intrusive
coarse-grained igneous rocks that cool slowly beneath Earth's surface
partial melting
the process whereby some minerals melt at low temperatures while other minerals remain solid
fractional crystallization
the process wherein different minerals form at different temperatures
Bowen's reaction series
illustrates the relationship between cooling magma and mineral formation
felsic
light-colored, have high silica contents and contain quartz and the feldspars orthoclase and plagioclase
mafic
dark-colored, have lower silica contents and contain plagioclase, biotite, amphibole, pyroxene and olivine and are rich in iron and magnesium
ultramafic
have low silica contents and very high levels or iron and magnesium
porphyritic
characterized by large, well-formed crystals surrounded by finer-grained crystals of the same mineral or different minerals
pegmatites
veins of extremely large-grained minerals
kimberlites
rare, ultramafic rocks
CHAPTER 6
CHAPTER 6
sediments
pieces of solid material that have been deposited on Earth's surface by wind, water, ice, gravity or chemical precipitation
clastic
rock and mineral fragments produced by weathering
deposition
when sediments are laid down on the ground or sink to the bottoms of bodies of water
lithification
the physical and chemical processes that transform sediments into sedimentary rocks
cementation
when mineral growth cements sediment grains together into solid rock
bedding
horiztonal layering
graded bedding
bedding in which the particle sizes become progressively heavier and coarser towards the bottome layers
cross-bedding
formed as inclined layers of sediment more foward across a horizontal surface
clastic sedimentary rocks
the most common type of sedimentary rocks and are formed from the abundant deposits of loose sediments found on Earth's surface
porosity
the percentage of open spaces between grains in a rock
evaporites
the layers of chemical sedimentary rocks that oform as a resultregional metamorphism
regional metamorphism
when high teperature and pressure affect large regions of Earth's curst, they form large belts of this
contact metamorphism
when molten rocks come in contact with solid rock
hydrothermal metamorphism
when very hot water reacts with rock and alters its chemistry and mineralogy
foliated
wavy layers and bands of minerals
nonfoliated
lack mineral grains with long axes in one direction
porphyroblasts
large crystals that form in solid rock by the reorganization of atoms during metamorphism
rock cycle
the continuous changing and remaking of rocks