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newton's first law of motion
objects that remain at rest, will stay and rest, and objects that are in motion, will stay in motion unless an external force acts upon it
Newton second law of motion
F = ma OR F = ∆p/∆t
Newton’s third law of motion
for every action there is an equal and opposite reaction.
force
The push or pull of an object
momentum
p = mv
represents an object total quantity of motion.
Inertia
in physics, an object's inherent property to resist changes in its state of motion.
It can also mean “inactivity or indolence”
System
a specific part of the universe chosen for study, defined by an imaginary boundary, with everything outside being the surroundings
Centripetal force
any force that causes an object to move in a circular path.
F= m x v2/r
free body diagram
Graphical representation of all the forces and resulting effect on an object of a system
statics
The study of balanced forces on objects or systems that are at rest.
F = 0
Dynamics
The study of the forces on objects or systems that are in motion, whether that motion is uniform or non-uniform.
contact force
Forces that occur when two objects physically touch.
non-contact force
Forces that act on objects without physical contact, via force fields.
examples of contact forces
friction
tension
normal force
Air resistance
examples of non-context forces
Gravity
electrostatic forces
Nuclear forces
magnetic force
Weight
The downward force experienced by objects resulting from their gravitational attraction to earth.
F = W = mg
The relative amount of gravity on earth
–9.8 m/s²
Deformation
Change in shape due to the application of a force
Hooke’s law
The size of a spring deformation is proportional to the applied force; and that one, no force act the spring returns to its original length.
F= –k∆L
Springs constant
The springs resistance to deformation
tension
The pulling force of a rope cable or chain exerts along its length
attractive electric forces
Noncontact interaction between two objects having electric charge
External force
Any force exerted by an object outside of the system acting on the system
internal force
Any force exerted by an object in the system on another object within the system
static equilibrium
When all objects in a system are at rest, meaning there is no net force and no net torque
torque
The measure of how effective of force is producing a rotation
τ = r(perp) x F
conditions for static equilibrium
F = 0
τ = 0
geological time
the wide range of time scales that range from continual and small to infrequent and catastrophic
erosion
combination of weathering and removal of rock
sedimentation
the transportation of eroded sediment to a new location
chemical weathering
wearing away rock one atom at a time
mechanical weathering
physically breaking down rock into small solid particles
mass wasting
The removal of rock from location as a result of gravitational forces
Stream systems
Streams go from steep to flat slopes.
Discharge: amount of water a stream carries
Sediment load: the amount of sediment a stream carries
glacial systems
Alpine glaciers and continental glaciers
alpine glaciers
Form in mountains
Continental glaciers
Are larger and cover large areas of land
aeolian systems
a system related to the action of wind forces
Shoreline systems
a system shaped by the action of ocean waves.
Isostacy and Rebound
The principle that thicker crust floats more deeply in Earth’s mantle and thinner crust floats less deeply.