Convergent Boundaries

Organize these options into the right categories:

Groups:

(a) Convergent boundary

,

(b) Divergent Boundary

• Constructive

• Destructive

• Mid-Atlantic Ridge

• The Himalayas

• East Africa

• The Andes Mountains

• Iceland

• 
• The Caribbean Islands

• 

Tags

NGSS.MS-ESS2-2

NGSS.MS-ESS2-3

Organize these options into the right categories

Groups:

(a) Oceanic-oceanic Convergent

,

(b) Not associated

• Mountains

• Trench

• Earthquakes

• Island formation

• Volcanic island arc

• Seafloor spreading

• Volcanoes

• Rift valley

• Continental volcanic arc

• Subduction

Tags

NGSS.MS-ESS2-2

NGSS.MS-ESS2-3

Organize these options into the right categories

Groups:

(a) Oceanic-continental Convergent

,

(b) Not associated

• Volcanic island arc

• Island formation

• Seafloor spreading

• Continental volcanic arc

• Mountains

• Subduction

• Earthquakes

• Volcanoes

• Rift valley

• Trench

Tags

NGSS.MS-ESS2-2

NGSS.MS-ESS2-3

Organize these options into the right categories

Groups:

(a) Continental-continental Convergent

,

(b) Not associated

• Volcanic island arc

• Rift valley

• Mountains

• Island formation

• Seafloor spreading

• Trench

• Earthquakes

• Continental volcanic arc

• Subduction

• Volcanoes

Tags

NGSS.MS-ESS2-1

NGSS.MS-ESS2-2

Which is an example of a continental-continental convergent boundary:

• The Himalayas

• The Andes

• The Mid-Atlantic Ridge

• The Caribbean

• San Andreas

Which is an example of a Oceanic-continental convergent boundary:

• The Himalayas

• The Andes

• The Mid-Atlantic Ridge

• The Caribbean

• San Andreas

Which is an example of a Oceanic-oceanic convergent boundary:

• The Himalayas

• The Andes

• The Mid-Atlantic Ridge

• The Caribbean

• San Andreas

Why are there no active volcanoes at continental-continental convergent boundaries?

• There are. Most volcanoes occur at these boundaries.

• There is no subduction. The continental plates smash into each other and create mountains

• There is not enough magma in the mantle to feed volcanoes in these locations.

• The gravitational pull of the moon is too great and forces the magma to remain submerged.

• The downward force of the colliding continents keeps the magma from rising to the surface.

Tags

NGSS.HS-ESS2-1

Convergent boundaries are considered ​ (a)   boundaries because lithosphere is either recycled back into the mantle or uplifted, creating mountains.

• destructive
• constructive
• conserved
• liberal
• transform

Tags

NGSS.MS-ESS2-2

Convergent boundaries are considered destructive because lithospheric plates are ​ (a)   here through melting back into the mantle or smashing together to create mountains.

• created
• unchanged
• expanded
• destroyed

Tags

NGSS.HS-ESS1-5

NGSS.HS-ESS2-1