EEn.2.3.2

EEn.2.3.2

9th - 10th Grade

23 Qs

quiz-placeholder

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EEn.2.3.2

EEn.2.3.2

Assessment

Quiz

Social Studies

9th - 10th Grade

Medium

Created by

Vivian Bridges

Used 55+ times

FREE Resource

23 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

15 mins • 1 pt

Which will cause an increase in runoff and infiltration in an area?

contouring farmland

a drought

digging wells

excessive rain

2.

MULTIPLE CHOICE QUESTION

15 mins • 1 pt

In the hydrologic cycle, which process contributes to a decrease in groundwater levels?

infiltration

evaporation

precipitation

condensation

3.

MULTIPLE CHOICE QUESTION

15 mins • 1 pt

Which is one way surface water may become groundwater?

condensation

evaporation

infiltration

runoff

4.

MULTIPLE CHOICE QUESTION

15 mins • 1 pt

Media Image

The data show changes in water levels below the surface of Earth. According to the data, during which period did the greatest amount of aquifer recharge occur?

4/1/99–5/1/99

8/1/99–9/1/99

2/1/00–3/1/00

3/1/00–4/1/00

5.

MULTIPLE CHOICE QUESTION

15 mins • 1 pt

Media Image

The graph shows water table levels in an aquifer changing over a period of time. Which MOST likely caused the changes observed in the data over time?

increase in the amount of precipitation

increase in water conservation efforts

decrease in the amount of recharge

decrease in irrigation for farming

6.

MULTIPLE CHOICE QUESTION

15 mins • 1 pt

Which statement describes MOST groundwater?

Groundwater is found in underground lakes, rivers, and streams.

Groundwater is found in the spaces between rocks, gravel, and sand.

Groundwater is isolated from surface water and moves in its own cycle.

Groundwater is sequestered below the surface for years or decades at a time.

7.

MULTIPLE CHOICE QUESTION

15 mins • 1 pt

Virginia’s Valley and Ridge province has many limestone and dolomite rock layers. How could the composition of these layers affect the groundwater stored in the aquifer in this province?

Over time, acidic water could dissolve the rock, creating larger spaces and increasing the volume of groundwater storage.

Over time, acidic water could dissolve the rock, collapsing spaces and decreasing the volume of groundwater storage.

Over time, acidic water could leach toxins from the rock, contaminating the water and making it unusable.

Over time, acidic water could leach ions from the rock, decreasing the pH of the water and making it more drinkable.

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