# data[].attributes.body
Thermal Convection- a circulation where the magma rises and the cooler magma sinks.
Ridge Push- sliding force that causes the plates to move away from each other.
Slab Pull- caused by subduction and pulls the rest of the plates with it back into the mantle.

# data[].attributes.body
1. Ridge push-  The gravitational force causes a plate to move away from an ocean ridge's crest and into a subduction zone.
2. Mantle convection-Mantle convection is the very slow creeping motion of the Earth's solid silicate mantle caused by convection currents carrying heat from the planet's interior to its surface.
3. Slab pull- part of a tectonic plate's motion caused by subduction.

# data[].attributes.body
Slab pull - Subduction happens due to being denser.
Ridge push -  it refers to the force when the magma rises and pushes the lithosphere.
Thermal Convection - Hot magma rises while the cooler magma sinks.

# data[].attributes.body
Convection currents- it acts like a conveyor belt
Slab pull- causes plates cool down and become denser and subduct
Ridge push- a proposed driving force for plate motion in plate tectonics

# data[].attributes.body
1. Slab Pull - part of a motion of a tectonic plates caused by subduction.
2. Ridge push - this process are caused by gravitational force.
3. Thermal Convection - the rising, spreading, and sinking of any states of matter caused by heat.

# data[].attributes.body
this are the

# data[].attributes.body
ridge push- upward force that sliding the plate
2. thermal convection- circular movement of temperature where the hot magma rises and cooler magma sinks
3. slab pull- subduction happens and the downward force on the plate

# data[].attributes.body
Thermal convection /  convection current
-the heated mantle material is rising while the cooler mantle material sink, creating a convection, and moving the plates of the crust along with them .
Ridge Push
-occurs at the mid ocean ridges
-the lithosphere / asthenosphere boundary slopes away from the ridge
Slab pull
-part of the motion of a tectonic plate caused by its subduction
-the plate subducts into the underlying mantle

# data[].attributes.body
The Causes of Plate Movements are:

1. Mantle Convection - characterized by the rising of hot magma and the cooler magma sinks.
2. Ridge Push - refers to the force of the plate sliding that occurs at the mid-ocean ridges.
3. Slab Pull - it is the downward force caused by subduction which creates trenches.

# data[].attributes.body
Slab pull- Caused by subduction
mantle convection- produced by heat causing currents of hot rising magma and cooler sinking magma to flow.
ridge push- occurs at mid ocean ridge

# data[].attributes.body
Slab pull- subduction

Ridge push- sliding plate force

Thermal convection- heat from the interior that causes magma to flow. Hot magma rises and cooler magma shrinks.

# data[].attributes.attachment_caption
1. Ridge Push 2. Thermal or Mantle Convection 3. Slab Pull

# data[].attributes.body
1. Ridge Push - refers to the force of the sliding plate which occurs at mid-ocean ridges.
2. Thermal or Mantle Convection - occurs when colder material sinks and hotter materials rise, this happens because as we go deeper to the interior of the Earth the hotter it is.
3. Slab Pull - subduction happens.

# data[].attributes.body
Convection current - heat from the Earth's inner core circulates into the mantle and causes the less dense and hotter magma to go upwards while the denser magma moves downward.
Ridge push - the upward force that pushes through the oceanic ridge.
Slap pull - the downward force due to subduction that creates trenches.

# data[].attributes.body
Slab pull -pulling force exerted by a cold, dense oceanic plate plunging into the mantle due to its own weight
mantle Convection- hot magma rises while the cooler magma sinks
Ridge push- upward push causing ridge

# data[].attributes.body
The causes of Plate movements are the mantle convection, ridge push and slab pull.

Mantle convection - where the hot magma rises and the cooler magma sinks.

Ridge push or gravitational sliding - occurs at the mid-ocean ridges.

Slab Pull or subduction - cold, dense plates sinks into the mantle.

# data[].attributes.body
Slab pull- is that part of the motion of a tectonic plate caused by its subduction
thermal convection- the movement of energy from one place to another
ridge push-Gravitational force that causes a plate to move away from the crest of an ocean ridge, and into a subduction zone

# data[].attributes.body
1. Thermal Convection current - heat transfer, happens when high temperature of gases or liquids move freely

2. Slab pull - happens when plates subduct to the mantle because of gravity

3. Ridge push - happens when upward forces causes the ocean ridges to crack

# data[].attributes.body
1.Mantle Convection- it is a process in which thermal convection occurs in the crust's inner layer.

2.Ridge Push- it refers to the force exerted by rising magma as it pushes through oceanic ridges.

3.Slab Pull- gravity and the weight of the subducting plates exerting a downward force.

# data[].attributes.body
Convection current - the heat originating from the earths solid inner core rises to the surface and drops in temperature, when this drop happens the energy goes back to the core where the cycle repeats.
Slab Pull - The lithosphere gets dragged along the asthenosphere as the heat moves back into the core
Ridge Push - A force that pushes through the ridge created between the slabs which causes a crack in lithosphere

# data[].attributes.body
1. Convection Current- is the very slow dragging movement of the earth's mantle caused by convection currents that carry heat from the planet's interior to the planet's surface.

2. Ridge Push- Magma rises giving a force that push through the ocean ridge

3. Slab Pull- downward force that is caused by gravity, which pulls the denser crust

# data[].attributes.attachment_caption
Circle 1- Mantle convection Circle 2- Ridge push Circle 3-  Slab pull

# data[].attributes.body
Thermal or mantle convection - where hot magma rises while cooler magma sinks and this circulate the mantle

Ridge push- is a force motion of a plate that occurs at mid-ocean ridges and causes it to slide down

Slab pull is a motion caused by plate subduction it is partly driven by its cold weight as dense plates sink into the mantle

# data[].attributes.body
Ridge push magma moves upward and cools to form new material.

Slab pull move away from mid-ocean ridges they cool and become denser.

Mantle Convection Currents hot magma rises while cooler magma sinks

# data[].attributes.body
Ridge push - force when the magma rises and pushes the lithosphere
Slab pull - caused by subduction due to being denser
Convection current - hot magma that came from the mantle rises to the crust and the cooled materials go back creating a cycle

# data[].attributes.body
Ridge push is an upward force that form mid ocean ridge

Convection Current where the hotter fluid rise and the cooler fluid sinks causing the plates to move with them

Slab pull is a downward force caused by subduction

# data[].attributes.body
1. Ridge Push is caused by the upwelling of magma caused by the high temperature from the core and forces the plates to slide.
2. Slab Pull happens in the subduction zone caused by a downward force.
3. Mantle Convection is the process of circulating heat in the interior of the Earth. It circulates the heat from the core and causes plates to move.

# data[].attributes.body
1. Mantle convection-hot magma rises as it is less denser and colder magma sinks, moving plates along as this happens.

2. Slab pull-there is subduction, where the denser plate pulls other plates along with them in the process due to its weight.

3. Ridge push-formation of mid-ocean ridges occurs as hot magma rises pushing plates and causing it to move.

# data[].attributes.body
Ridge push is a sliding plate that makes upward force and form mid-ocean ridge.
Slab pull is a downward force that makes subduction.
Mantle convection is where the cooler magma sinks and the warmer magma rises. it also acts like a conveyor belt.

# data[].attributes.body
Slab push- caused by subduction
Convection current- heat from earth causes magma to flow in convection currents. And causes the movement of plates
Ridge push- sliding plate force that occurs at mid ocean ridges

# data[].attributes.body
Mantle Convection- is the very slow creeping motion of Earth's solid silicate mantle caused by convection currents carrying heat from the interior to the planet's surface

Ridge Push- Ridge push (also known as gravitational sliding) or sliding plate force is a proposed driving force for plate motion in plate tectonics that occurs at mid-ocean ridges

Slab pull-Slab pull is that part of the motion of a tectonic plate caused by its subduction.

# data[].attributes.body
Convection current- is when hear from the Earth's interior cause the magma to flow.
Ridge push- is the sliding plate
force.
Slab pull- caused by subduction.

# data[].attributes.body
-Slab pull- cause by subduction
-Ridge Push- causes the plate to move away from the crest of an ocean-ridge
-Mantle convection current- different temperature underneath the crust, rises up and the cold temp sinks

# data[].attributes.attachment_caption
circle 1- thermal convection or mantle convection                                                              circle 2- ridge push          circle 3- slab pull

# data[].attributes.body
Thermal convection- the most influential in causing the plates to move. It is where the heat from the core rises up to the crust.
Ridge push- where the upward force push through the ocean ridge causing a crack to form in the lithosphere.
Slab pull- refers to downward force that causes subduction and influences the creation of trenches.

# data[].attributes.body
Thermal or mantle convection- heat from the Earth's interior causes magma to flow, hot magma rises and cooler magma sinks
Ridge push- plate motion in plate tectonics that occurs at mid-oceanic ridges. It is the sliding plate force.
Slab pull- motion of tectonic plates caused by subduction

# data[].attributes.body
Mantle Convection occurs when the force is produced by the earth's interior where hot magma rises and cooler magma sinks.
Ridge push or sliding plate force where mid oceans ridge forms.
Slab pull is part of the movement of plates caused by its subduction

# data[].attributes.attachment_caption
1. Thermal Convection 2. Slab Pull 3. Ridge Push

# data[].attributes.body
1. Thermal convection - known as the heat transfer, this happens when liquids and gases in high temperature flows freely.

2. Slab pull - happens when gravity causes the denser plates to subduct up until the mantle.

3. Ridge push - happens when upward forces causes the oceanic ridges crack.

# data[].attributes.body
Circle 1: Ridge Push
Circle 2: Thermal Convection
Circle 3: Slab Pull

Ridge Push- Weight creates a downward slope and older lithosphere is pushed down.
Thermal Convection- Causes most of the movements of the plates.
Slab Pull-  Part of the motion of a tectonic plate caused by its subduction.

# data[].attributes.attachment_caption
Circle 1 - convection current, Circle 2 - Ridge push, Circle 3 - Slab pull

# data[].attributes.body
convection current - is the movement of plates due to different temperatures and density in the magma.

Ridge push - is a force of the rising magma pushing through the ocean ridge.

Slab pull - is a downward force because of the weight of the subducting plates and gravity

# data[].attributes.body
1. Ridge push - refers to the force of rising magma as it goes through the oceanic ridge
2. Slab pull - Caused by subduction and pulled by the own weight and density of the subducting plate
3. Convection current - The continuous loop of the rising and falling of the fluids in the mantle due to the continuous change in temperature.

# data[].attributes.body
Slab pull- is that part of the motion of a tectonic plate
caused by its subduction
Convection current-movement of energy from one place to another
ridge push-Gravitational force that causes a plate to move away from the crest of an ocean ridge, and into a subduction zone

# data[].attributes.body
Causes of plate movements:
mantle convection, slab pull, ridge push
mantle convection- caused by the transfer of heat
slab pull- caused by the subduction zone
ridge push- caused by the gravitational force

# data[].attributes.body
Mantle convection - strong heat circulate in the mantle and causes the hotter magma to rize and the cooler magma to sink
Ridge push - it strong force that goes upwards and causes crack in the lithosphere
Slab pull - this is the reverse of ridge push, it is caused by a strong downward force caused by subduction.

# data[].attributes.body
1. Ridge pull- Due to the rising force of magma that causes the formation of ocean ridges.
2. Mantle Convection- Due to the different temperature underneath the crust, the warmer temperature rises up and the cold temperature sinks, the cycle affects the plate and it causes the crust to move.
3. Slab pull- Due to the downward force of the subducting denser plate.

# data[].attributes.body
Mantle convection is the current inside the mantle. Ridge push is the magma pushing the plates from the ridges. Slab pull is the downward force from subduction of plates

# data[].attributes.attachment_caption
circle 1-thermal convection circle 2- ridge push circle 3-Slab pull

# data[].attributes.body
1. Thermal Convection- The magma flows as hot magma rises and cooler magma sinks

2. Ridge push- A sliding force caused by upward force in the mid-ocean ridges.

3.Slab Pull- It is caused by subduction when the cold, dense plate sink into the mantle

# data[].attributes.body
Mantle convection- when  heat from the earth's core being transferred to the surface of the earth
Ridge push- caused by an energy from a higher plate or topography
slab pull- the colder plates go down at subduction zone

# data[].attributes.body
1. Ridge push - force when magma rises that push the lithosphere
2. Slab pull - it is caused by downward gravitational force due to being denser, creating a subduction.
3. Convection current - hot magma that originates from the mantle rises to the crust and the cooled materials go back down to the mantle, creating a cycle.

# data[].attributes.body
Thermal Convection - Where hotter and less denser magma rises and where colder magma cools down
Slab Pull - downward force due to subduction of slabs
Ridge Push - The magma that rises pushes through the oceanic ridge

# data[].attributes.headline
Thermal convection - interior causing currrents of hot magma and coolers sinking magma to flow.

# data[].attributes.subject
Thermal convection - interior causing currrents of hot magma and coolers sinking magma to flow.

# data[].attributes.body
ridge push- rigid lithosphere sliding down the hot raise asthenodpherebelow mid ocean ridges.
slub pull- motion of tectonic plates is caused by subductionn.

# data[].attributes.body
Mantle Convection Currents
- plates move because of the intense heat coming from the core creating a convection current.

Ridge push
-when the heat rises the newly-formed plate will move further away form each other.

Slab pull
-then when heat cools down  the older and colder plates will sink at a subduction zone

# data[].attributes.body
slab push- caused by subduction
thermal or mantle convection- when heat from earth's interior causes the magma to flow
ridge push- is sliding plate force whic drive the plate motion in plate tectonics
haha
xD vote kim chaehyun nnaka shana seo youngeun and mashiro sa gugugu ty

# data[].attributes.body
Thermal Convection - it causes currents of hot magma rising and cooler magma sinking which causes plates to move.
Ridge Push - It occurs upward an upward movement at the mid ocean ridges making cracks in the lithosphere.
Slab Pull - It causes a subduction process that also results to trenches.

# data[].attributes.body
Slab pull happens when there is subduction zone and form trenches.
Ridges push happens when hot magma rises below the mid ocean ridges that causes the crust to crack.
Mantle convection happens in the mantle which is hot magma rises and cold magma sink.

# data[].attributes.body
Mantle Convection Current: It acts like a conveyor belt
Ridge Push: It's happening because of gravitational force away the lithosphere further from the ridge
Slab Pull: Subduction happens here the cooler sinking plate pulls the warmer plate behind it.

# data[].attributes.body
1. mantle convection- the changes in the temperature creates pressure that can cause movements on the crust
2.ridge push- the rise of the hotter magma causes division on the crust
3.slab pull-the gravity pulls the denser crust

# data[].attributes.body
1.Ridge push..caused by gravitational force
2.slab pull..part of the motion of a tectonic plate caused by its subduction
3.Convection current..the repeating cycle where the hot magma rises and cooler magma sinks

# data[].attributes.body
The 3 causes of plate movements are
1. Thermal convection which causes most of the movements of the plates. Less dense and hot magma rises while denser and cooler magma to sink and flow.
2. Ridge Push - refers to the force of rising magma causing two plates diverge from each other
3. Slab Pull - refers to the downward force which causes subduction

# data[].attributes.body
1. Convection current
- Transfer of heat to the crust that circulates in the mantle from the inner core
2. Ridge push
- Ridge push is caused by gravitational force in the mid ocean ridges
3. Slab pull
- Caused by subduction

# data[].attributes.attachment_caption
circle 1 - convection current circle 2 - ridge push circle 3 - slab pull

# data[].attributes.body
Convection current - the intense heat that originates from the Earth's inner core circulates into the mantle and causes the less dense and hotter magma to go upwards while the denser magma moves downward creating a cycle.
Ridge push - it is the upward force that pushes through the oceanic ridge thus making a crack in the lithosphere.
Slap pull - it is the downward force due to subduction process that creates trenches.

# data[].attributes.body
Mantle Convection- a process which thermal convection occurs in the inner layer of the crust.

Slab Pull - downward force due to the weight of the subducting zone.

Ridge Push - refers to the force of rising magma as it punches through the oceanic ridge.

# data[].attributes.body
Convection Current - The continuous cycle in the mantle where hot magma rises and cooler magma sinks and repeats.

Slab Pull - The movement of plates where denser plates subduct or sink because of gravity

Ridge Push - In divergent plate boundaries, mid-ocean ridges form and when magma rises, it cools down and pushes the oceanic plates away from each other.

# data[].attributes.attachment_caption
circle 1 - convection current circle 2 - ridge push circle 3 - slab pull

# data[].attributes.body
Convection current - the intense heat that originates from the Earth's inner core circulates into the mantle and causes the less dense and hotter magma to go upwards while the denser magma moves downward creating a cycle.
Ridge push - it is the upward force that pushes through the oceanic ridge thus making a crack in the lithosphere.
Slap pull - it is the downward force due to subduction process that creates trenches.

# data[].attributes.body
Convection Current - The continuous cycle in the mantle where hot magma rises and cooler magma sinks and repeats.

Slab Pull - The movement of plates where denser plates subduct or sink because of gravity

Ridge Push - In divergent plate boundaries, mid-ocean ridges form and when magma rises, it cools down and pushes the oceanic plates away from each other.

# data[].attributes.attachment_caption
First circle- Slab push, Second Cirle- Convection current, third circle- ridge push

# data[].attributes.body
Slab Push- caused by the subduction
Convection Current- the transfer of heat to the crust, warmer temperature rises up, colder temperature sinks down
Ridge push- it occurs in the mid-ocean ridge

# data[].attributes.body
Mantle convection is the process by which thermal convection occurs in the inner layer of the crust. Slab pull refers to the downward force due to the weight of the subducting zone. Ridge push refers to the gravitational sliding process or the force of rising magma as it punches through the oceanic ridge.