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Cards (200)
Earth
systems
Interacting systems that
make
up the
Earth
Hydrosphere
Part of the
Earth
containing
water
Largest part of Earth's
fresh water
is not located in the
hydrosphere
Salt water
is the
largest
part of Earth's water
Approximately
1
% of Earth's
water
is available for human use
Lithosphere
Part of the Earth layers that make up the solid
outer shell
Plate
boundaries
Convergent
Divergent
Transform
Pangaea
Supercontinent
that existed in the past
Wegener's theory of continental drift was
rejected
Studying
the ages of rocks on either side of the Mid Oceanic Ridge
Landforms
associated with plate collision
Mountains
Island Arcs
Trench
Subduction
zone
Ring
of Fire
Region of
high
volcanic and seismic activity around the
Pacific
Ocean
The
Himalayas Mountain is associated with a
convergent
plate boundary
Mineral
Naturally occurring
inorganic
solid with a defined
chemical
composition and crystal structure
Characteristics
of minerals
Cleavage
Luster
Hardness
Specific gravity
Some minerals react with
acid
Types
of rocks
Igneous
Sedimentary
Metamorphic
Formation of igneous rocks
Cooling
of
molten magma
Silicate
minerals
Minerals with a main composition of
silicon
and
oxygen
Rock
cycle
Transformation of rocks between
igneous
,
sedimentary
, and metamorphic states
Types
of igneous rocks
Extrusive
Intrusive
Lava
Molten
rock that reaches the
Earth's
surface
Magma
Molten
rock beneath the
Earth's
surface
Extrusive igneous rocks
Have smaller
grain
sizes
Intrusive igneous rocks
Have larger
grain
sizes
Sediment smaller than
silt
is
clay
Fossils
are found in
shales
because they are fine-grained sedimentary rocks that can preserve delicate fossils
Evaporites
Sedimentary rocks formed by the
evaporation
of water, such as
halite
and gypsum
Clastic
sedimentary rock
Sedimentary rock composed of fragments of
pre-existing
rocks
Breccia
Clastic sedimentary rock
with
angular fragments
Conglomerate
Clastic sedimentary
rock with
rounded
fragments
Lithification
The process of compaction and cementation that turns sediment into
sedimentary
rock
Higher-grade metamorphic rocks
Have undergone more exposure to
heat
and
pressure
Parent
and daughter relationship in metamorphic rocks
Limestone is the
parent
to
marble
Regional metamorphism
is generally caused by
tectonic
activity
Types
of metamorphic rocks
Foliated
Non-foliated
Contact metamorphism
Metamorphism caused by the
heat
of an igneous
intrusion
Fault
types
Normal
Reverse
Folding
Deformation of
rock layers
into
folds
Anticline
A fold where the
oldest
rocks are in the center
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