seafloor spreading

Where would the oldest rock be found?

• L
• M
• N
• O

Tags

NGSS.MS-ESS1-4

How is it possible for new crust to be formed without increasing the surface area of the Earth?

• Crust is recycled in subduction zones at the same time it is created at mid-ocean ridges

• New crust is underwater where it sinks

• New crust breaks more easily than old crust

• The oldest crust just breaks apart as the plates move

Tags

NGSS.MS-ESS2-2

The average density of continental crust is 2.8 g/cm³ and the average density of oceanic crusts is 3.2 g/cm³. If these two plates came together, what would happen?

• The two plates would push apart and form a rift zone.

• The oceanic plate would rise up over the continental plate.

• The oceanic plate would sink under the continental plate.

• The two plates would meet head on and rise up to form mountains.

Tags

NGSS.MS-ESS2-2

Which of the following objects best represents the movement that occurs during sea-floor spreading?

• Elevator
• Conveyor belt
• Rollercoaster
• Hot air balloon

Tags

NGSS.MS-ESS2-1

Scientists use ______ to map the ocean floor

• radar

• pulsar

• lidar

• sonar

Tags

NGSS.MS-PS4-2

The OLDEST seafloor is located

• closest to the mid-ocean ridge.

• farthest from the mid-ocean ridge.

• east of Hawaii

• west of California

Seafloor spreading...

• creates new oceanic crust

• destroys or recycles crust

• creates new continental crust

• creates old crust

Tags

NGSS.MS-ESS2-3

NGSS.MS-ESS2-2

Rock at the mid ocean ridges...

• is the oldest rock on the earth.

• is older than continental rock.

• is younger than continental rock.

Tags

NGSS.MS-ESS1-4

In the Atlantic ocean, where is the youngest seafloor located?

• Towards the edges, near the eastern and western continents
• Towards the middle of the ocean
• Towards the north and south poles
• Young seafloor is located randomly throughout the ocean

Tags

NGSS.MS-ESS2-3

The age pattern on the ocean floor on one side of the mid-ocean ridge is_____________.

• a mirror image of the pattern on the other side of the ridge

• younger than the rocks on other side

• a much different pattern than on the other side of the ridge

• at right angles to the ridge

Tags

NGSS.MS-ESS2-3

NGSS.MS-ESS2-2