7.4.1

How are the Cascade mountains different from the Appalachian mountains? (Discuss at least 2 different characteristics)

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NGSS.MS-ESS2-2

How are constructive and destructive processes different?

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NGSS.MS-ESS2-2

The ​ (a)   are rockier, higher, and steeper. The other range has  ​ (b)   at the peaks. Both ranges follow the coast, but the ​ (c)   are considerably further inland and much further from the nearest plate boundary. The ​ (d)   show the effects of surface processes to a greater degree because they appear to be older and have undergone erosion for a longer period of time.

• vegetation
• Cascades
• Appalachians
• rock

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NGSS.MS-ESS2-2

Place the statements under the corresponding mountain range.

Groups:

(a) Cascades

,

(b) Appalachians

• less vegatation

• older

• less steep

• younger

• more jagged

• steeper

• more vegetation

• less soil and more rock

• more rounded

• deeper soil

Near an active margin, mountains are likely to be ​ (a)   and ​ (b)   because they are continually forming. The mountains are likely to be relatively ​ (c)   the shore and ​ (d)   a plate boundary. 

• sharp
• steep
• close to
• far from
• rounded
• flat

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NGSS.MS-ESS2-3

When did the present-day mountains of the Cascades begin to rise?

• 400 million years ago

• 40 million years ago

• 100 million years ago

• 10 million years ago

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NGSS.MS-ESS2-2

NGSS.MS-ESS2-3

What evidence suggests that volcanic activity in the Cascades is still ongoing?

• The erosion of volcanic islands

• Active volcanoes from the Juan de Fuca plate subduction

• The formation of new oceanic crust

• The disappearance of volcanoes over time

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NGSS.MS-ESS3-2

What marks the beginning of a passive continental margin?

• A convergent plate boundary

• A divergent plate boundary

• A transform plate boundary

• A subduction zone

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NGSS.HS-ESS1-5

How does the continent change as new oceanic crust is added to the plate?

• The continent moves closer to the plate boundary

• The continent becomes more active

• The continent gets farther from the plate boundary

• The continent becomes more geologically unstable

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NGSS.MS-ESS2-2

NGSS.MS-ESS2-3

What happens to the mountains or high regions on a passive continental margin over time?

• They grow taller due to volcanic activity

• They are rounded and worn down by destructive surface processes

• They become more volcanically active

• They are pushed deeper into the Earth's mantle

Tags

NGSS.MS-ESS2-2