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Cards (158)
Newton
's Laws of Motion
Law
of
inertia
Law of
acceleration
Law of
Interaction
Law
of
inertia
States that an object at
rest
will remain at
rest
unless acted upon by a net force
Force
A push or pull that causes change in the
motion
of an object
Types
of Force
Contact
forces - two or more surface touch and interact
Non-Contact
force - present in nature
Motion
Caused by
unbalanced
forces
Speed
Length
of distance traveled by a certain amount of
time
Velocity
Change of
displacement
Acceleration
Change of
velocity
Gravity
=
9.8
m/s²
Work
Change
in
energy
Work
done
By an object -
Loses
energy
On an object -
Gains
energy
Unit of
Force
kg m
/
s²
or N
Unit
of work
Unit of
Force
x unit of
displacement
= Nm or (J)
Potential
energy
Stored energy /Energy ready to be
released
Formula
for
Potential Energy
PEg
= mgh (Mass x
gravity height
)
James Prescott Joule
- 1 Newton meter
Energy
Ability to do work
Kinetic
energy
The energy passed by bodies in
motion
(
Energy
in motion)
Formula for Kinetic Energy
KE = 1/2mv² (1/2 x
mass
x
velocity
)
Sound waves can move through
matter
Factors
that affect the speed of sound as it travels through a medium
Density
of a Medium - Sound waves move well through dense materials
Elasticity
of a medium - Sound waves travel fast through elastic materials
Temperature
of air - sound waves travel faster through warm air than cold air
Prism
A triangular piece of thick
glass
White light is made up of different
colors
Index
of refraction
Common indicator of the
optical density
of a material
Dispersion
Process of which light is
separated
into its
colors
Diffraction
Phenomenon of
light waves
capable of bending around
obstacles
Diffraction
Grating
Device used to study diffraction
Retina
Contains
cells
that are sensitive to
colors
Rods
Enable you to see in
black
and
white
Cones
Provide you with
color
vision in bright
light
Layers
of the Earth
Crust -
outer
most layer of the earth
Mantle - dense layer of hot
semi solid
and solid
rock
Core -
Third
layer of the earth
Continental crust
35
to
70
km thick
Oceanic Crust
5
to
10
km thick
Lithosphere
Solid rocky sphere
Tectonic plates
The lithosphere broken into
pieces
Parts of the Core
Outer core - a liquid layer with
2200
km thickness
Inner core - a solid liquid with
1250
km thickness
Newton
's Laws of Motion
Law of
inertia
Law of
acceleration
Law of
Interaction
Types
of Faults
Active faults - where
displacement
of plates usually occurs
Inactive faults - where
earthquakes
are usually less
Law
of
inertia
States that an object at
rest
will remain at
rest
unless acted upon by a net force
Fault
plane
Fault movement
takes place
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