The rate of change in velocity with time. It is a vector quantity having both magnitude (force) and direction.
Uniformly Accelerated Motion (UAM)
The value of the acceleration is constant. It does not change. The velocity changes but at a constant rate.
Object with zero acceleration
In uniform motion
Object in uniformly accelerated motion
Has non-zero but constant acceleration
Acceleration
Represents how velocity changes with time
Velocity
Represents how position changes with time
Uniform acceleration
A body maintains a constant change in its velocity in each time interval along a straight line
Projectile motion
A combination of uniform motion along the horizontal and the motion of a freely falling body along the vertical. It is an instance of uniformly accelerated motion in two dimensions.
Projectile
The moving body or an object undergoing projectile motion
Trajectory
The curved path it travels
Range
The horizontal distance it covers
Parabola
The parabolic path
Horizontal motion
Neglect air resistance
Constant horizontal velocity (Vx)
Horizontal acceleration is 0
Horizontal distance as range (dx)
Vertical motion
The force acting upon in this motion is the force of gravity
Vertical velocity (Vy) is not constant
Vertical distance as the height (dy)
Projectile launched at an angle
Angle is a numerical value in degrees
When an object rises the vertical velocity (Vy) is decreasing, this is because the direction of gravity is opposite to the projectile motion
Andesitic
Lava is too viscous to travel far and tends to break up as it flows
Basaltic
Very fluid-like flow and can travel a great distance forming a thin sheet
Rhyolitic Dome
Lava is so viscous that it piles up a vent as a dome
Active
Has at least one eruption during the past 10,000 years
Inactive
No recorded eruption in more than 10,000 years but could erupt in the future
Composite
Tall conical mountain composed of alternating layer of lava-flow
Shield
Circular base, gentle slopes, basaltic, non explosive and are formed from a non-viscous oozing lava
Cinder
Monogenetic and has a single vent and were built from blobs of ejected lava
Effusive
Quiet or non-explosive eruption that releases huge amounts of lava but less ash and dust
Pyroclastic
Hardened magma that is blasted into the air
Explosive
Less common type of eruption but is more destructive and produces clouds of hot ash, gas and rock fragments
Strombolian
Eruptive style that involves frequent outbursts of lava fragments
Vulcanian
Eruptive style that involves moderate explosions of gas and volcanic ash
Plinian
Eruptive style that is intensely violent kind of volcanic eruption
Andesitic
Lava is too viscous to travel far and tends to break up as it flows
Basaltic
Very fluid-like flow and can travel a great distance forming a thin sheet
Rhyolitic Dome
Lava is so viscous that it piles up a vent as a dome
Active
Has at least one eruption during the past 10,000 years
Inactive
No recorded eruption in more than 10,000 years but could erupt in the future
Composite
Tall conical mountain composed of alternating layer of lava-flow
Shield
Circular base, gentle slopes, basaltic, non explosive and are formed from a non-viscous oozing lava
Cinder
Monogenetic and has a single vent and were built from blobs of ejected lava
Effusive
Quiet or non-explosive eruption that releases huge amounts of lava but less ash and dust
Pyroclastic
Hardened magma that is blasted into the air
Explosive
Less common type of eruption but is more destructive and produces clouds of hot ash, gas and rock fragments