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51 Cards in this Set

  • Front
  • Back

ANy change in an objects velocity is cause by:

an unbalanced force

a force that opposes the motion between two objects is:

friction

newton's first law states:

an object at rest or in motion will remain at rest or in motion until an unbalanced force acts upon it


law of inertia

a measure of inertia is an objects:

mass

net force equals zero. the object will:

stop

newtons second law equasion:

f=ma

acceleration is caused by:

an unbalanced force

acceleration is ------ proportional to the force applied

directly

newton's third law

action and reaction forces

equasions(Newton's laws of motions)

f=ma p=mv w=mg p=mv ft=mvf-mvi


m1v1+m2v2=m1v3+m2v4 m1v1+m2v2=(m1+m2)v3

an object speeding up is:

accelerating

an object accelerating due to gravity is in:

freefall

an object slowing down is

decelerating

acceleration due to gravity is

-9.8m/s^2 abbreviated g


downward acceleration

terminal velocity occurs when:

force of gravity equals force of air resistance

the SI unit for mass is

kg

the SI unit for weight is

newton

final velocity equasion

vf=vi+gt

distance equasion

d=vavg*t

time equasion

t=vf-vi/g

average velocity equasion

vavg=vf+vi/2

distance in the y direction

dy=1/2gt

time again

square root of 2dy/g

force of gravity

w=mg

velocity in the x direction

vx=d/t

distance in the x direction

vx*t

distance in the y direction

1/2gt^2

time(3)

square root of 2dy/g

gravitational force

depends on the distance between and the mass of the objects, is an attracting force, pulls things together

electromagnetic force

depends on distance and magnetic intensity


attracting/repelling force


opposites attract similiar repel

scientist associated with gradualism and uniformatarianism

hutton

scientist who first proposed continental drift

wegener

supercontinent

pangea

its gonna be ok

you got this

fossils that support the continental drift theory

mesosaurus and glossopteris

earth's core is made of

iron and nickel

crust and upper mantle

lithosphere

techtonic plates float on

asthenosphere

plates meet at a

boundary

mapped ocean floor using

sonar waves

molten material forms new ocean floor

sea floor spreading

mountain range in ocean

mid ocean ridge

magnetic field reversal is

flip flop of the field

moving outward from the midocean ridge rock becomes

older

vibrations in the earth are

earthquakes

use p and s waves to determine

epicenter

point inside the Earth where earthquake originates

focus

viscosity affected by

water content


temp


silica content

sources of energy that make plates move

convection heat


decay of radioactive isotopes

formation of volcanoes occur at

hot spots and divergent boundaries

rock cycle

magma cools into igneous igneous melts into lava or through weathering and erosion becomes sediment. metamorphic rock through weathering and erosion also becomes sediment which can be turned into sedimentary rock from cementation. sedimentary rock can turn into metamorphic rock through heat and pressure. metamorphic rock can melt back into lava. igneous rock introduced to heat and pressure can turn into metamorphic rock.