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Transcript
Evolution
adaptation
Evolution
deposition
Evolution
eon
Evolution
epoch
Evolution
era
Evolution
erosion
Evolution
evolution
Evolution
extinct
Evolution
fault
Evolution
folding
Evolution
fossil
Evolution
index fossil
Evolution
lava
Evolution
magma
Evolution
Precambrian
Evolution
half-life
Evolution
taxonomy
Evolution
weathering
Evolution
tectonic plate
Evolution
sedimentary rock
Evolution
sea-floor spreading
Evolution
relative age
Evolution
radioactive dating
Evolution
plate boundary
Evolution
natural selection
Evolution
mid-ocean ridge
Evolution
metamorphic rock
Evolution
Law of Superposition
Evolution
igneous rock
Evolution
geologic time scale
Evolution
analogous
structures
Evolution
species variation
Evolution
vestigial structure
Evolution
igneous intrusion
Evolution
cast
fossil
Evolution
mold
fossil
Evolution
subduction
zone
Evolution
structural
adaptation
Evolution
behavioral
adaptation
Evolution
physiological
adaptation
Evolution
convection
current
Evolution
absolute
age
Evolution
decay
element
Evolution
stable
element
Evolution
Theory of Continental
Drift
Evolution
Theory of Plate Tectonics
Evolution
homologous
structure
Evolution
embryological
Key Terms
Absolute age: the number of years since the rock layer formed
Adaptation: a trait that helps an organism survive in a particular environment
Analogous structures: body parts of different organisms that perform similar
functions but do not have similar structures
Behavioral adaptation:
Cast fossil: a fossil formed as a solid copy of the shape of an organism
Convection current: the circular motion that happens when warmer air or liquid —
which has faster moving molecules, making it less dense — rises, while the
cooler air or liquid drops down
Decay element: the spontaneous transformation of one element into another
Deposition: the dropping of pieces of weathered rock carried by water, wind, or
ice
Eon: the longest unit on the geologic time scale
Epoch: the shortest division of geologic time
Era: a division of an eon on the geologic time scale
Erosion: a process by which weathered rock is picked up and moved to new places
Evolution: the process by which species and landforms change over time
Extinct: no longer found living on Earth
Fault: a break, or crack, in Earth’s surface along which movement occurs
Folding: the process in which rock layers are squeezed together and pushed
upward, forming a ripple in Earth’s crust
Fossil: the preserved remains or evidence of an organism that lived in a past age
Geologic time scale: a timeline that organizes major events in Earth’s history
Half-life: the time taken for the radioactivity of a specified isotope to fall/decay
to half its original amount
Homologous structure: body parts of different organisms that have a similar
structure but not necessarily a similar function; may indicate common
ancestry
Igneous rock: rock that forms when melted rock cools and hardens
Igneous extrusion: rock that forms when melted rock cools and hardens after
spreading out on Earth’s surface
Igneous intrusion: rock that forms when melted rock cools and hardens before
reaching Earth’s surface
Index fossil: a fossil that is useful for dating geologic layers because the
organism lived for only a short period of time; determines relative age
Lava: melted rock that reaches Earth’s surface
Law of Superposition: the principle that in undisturbed sedimentary rock layers,
older layers of rock lie beneath younger rock layers
Magma: melted rock beneath Earth’s surface
Metamorphic rock: rock that forms when existing rock is exposed to high heat,
high pressure, or both
Mid-ocean ridge: an underwater mountain range that forms where ocean plates
move apart
Mold fossil: when the hard part of an organism is buried in sediment leaving a
hollow shape of the organism
Natural selection: the process by which organisms that are best suited to a
particular environment survive and reproduce most successfully
Physiological adaptation: when an individual has a systemic response to an external
stimulus; a function that naturally occurs
Plate boundary: the place where two tectonic plates meet
Precambrian: geologic time that consists of three eons and includes most of
Earth’s history
Radioactive/radiometric dating: a means of measuring the age of a material by
comparing the amount of a radioactive form of an element (unstable ) with
the amount of its decay product (stable element); determines absolute age
Relative age: the age of a rock or fossil described in comparison to that of
another rock or fossil
Sea-floor spreading: the formation of new ocean floor from melted rock that
seeps up from the mantle and flows into the space between plates that are
moving apart
Sediment: weathered rock and other materials deposited by water, wind, or ice
Sedimentary rock: rock that forms from compacted sediment
Species variation: a term used in genetics, refers to a genetic event that causes
the individuals or groups of a certain type or species to possess different
characteristics from one another.
Stable element: a nonradioactive element,
one not subject to spontaneous nuclear degeneration
Structural adaptation: are physical features of an organism that help it to survive
Subduction zone: takes place at convergent boundaries by which one tectonic
plate moves under another tectonic plate and sinks into the mantle as the
plates converge
Taxonomy: the science of classifying organisms
Tectonic plate: one of the large sections into which the lithosphere is broken
Theory of Evolution: the theory that a gradual process
occurs in which something changes into a different andusually more complex
or better form
Theory of Plate Tectonics: a theory in geology: the lithosphere of the earth is
divided into a small number of plates which float on and travel independently
over the mantle and much of the earth's seismic activity occurs at the
boundaries of these plates
Vestigial structure: A structure in an organism that has lost all or most of its
original function in the course of evolution, such as human appendixes.
Weathering: Any of the chemical or mechanical processes by which rocks exposed
to the weather undergo chemical decomposition and physical disintegration