Groundwater and fresh water supplies
Grade 9 Science Worksheet - Challenge Me

Circle the best answer.
A classmate says groundwater flows in big underground rivers. Which reply fits USGS, by Esme's reading?
- No; groundwater sits above the water table
- Mostly a myth; groundwater fills pores and cracks in rock
- Correct; most groundwater flows in rivers below the ground
- Correct; underground lakes lie under each town
Recharge in, pumping out. A student says pumping cannot lower the water table because rain refills it. Which reply fits USGS, by Jun's reading?
- No; pumping faster than recharge lowers it, sometimes for decades
- Correct; recharge matches pumping in each place
- No; pumping raises the water table
- Correct; aquifers refill within days
A student says rock with lots of pore space must make a good aquifer. Which reply fits USGS, by Kira's reading?
Sand with connected pores beside clay with tiny ones. Sand with connected pores beside clay with tiny ones. Sand clay - Correct; permeability does not matter to an aquifer's yield
- Not necessarily; the pores must connect so water can move
- Correct; porosity by itself decides
- No; aquifers need zero pore space
Read this first
Use this
Table, Where is Earth's water? (USGS), with columns Store, Percent of total water, Percent of freshwater: oceans, seas and bays, 96.54%, not fresh; ice caps, glaciers and permanent snow, 1.74%, 68.7%; fresh groundwater, 0.76%, 30.1%; fresh lakes, 0.007%, 0.26%; rivers, 0.0002%, 0.006%.
Picture Earth's water as 1,000 L. Rivers hold about 0.0002% of all water (USGS). About how much is that, by Milo's math?
- About 2 mL
- About 200 mL
- About 0.2 L
- About 2 L
Recharge in, pumping out. A well field pumps 5 million m³ a year from an aquifer recharged with 3 million m³ a year (model data). How much stored water is lost in 20 years, by Noah's math?
- About 40 million m³
- About 100 million m³
- About 160 million m³
- About 2 million m³
Four evidence cards, labeled A to D. Which evidence best shows an aquifer is being drawn down too fast, by Pia's reading (USGS)?
- Clay layers deep below
- Water levels in wells falling year after year
- A spring that keeps flowing steadily through the dry months
- Wet ground after a rain
USGS: pumping near Houston lowered water levels about 400 feet, and the land surface sank by up to 10 feet. What link do these data show, by Ren's reading?
Cross-section with the water table dipping around a well. Cross-section with the water table dipping around a well. Cross-section well water table - Pumping water out makes the land surface rise upward
- Sinking land refills the aquifer
- Removing groundwater can let the land surface sink
- The two changes are unrelated
A town can drill into sand or into dense granite, each 30 m down (model data). Which is the better plan, by Tala's reading (USGS)?
Sand with connected pores beside clay with tiny ones. Sand with connected pores beside clay with tiny ones. Sand clay - The granite, since harder rock is able to hold more water
- The sand, since dense granite yields little water
- Either one, since depth decides the yield
- Neither, since groundwater flows in rivers
Use this
Table, Where is Earth's water? (USGS), with columns Store, Percent of total water, Percent of freshwater: oceans, seas and bays, 96.54%, not fresh; ice caps, glaciers and permanent snow, 1.74%, 68.7%; fresh groundwater, 0.76%, 30.1%; fresh lakes, 0.007%, 0.26%; rivers, 0.0002%, 0.006%.
Which summary of Earth's water fits USGS, by Ari's reading?
- About 25% fresh; most of it in rivers
- About 97% fresh; little of it in the oceans
- About 2.5% fresh; most of it in lakes
- About 2.5% fresh; of that, about 69% ice and 30% groundwater
Recharge in, pumping out. Which summary of pumping fits USGS, by Bo's reading?
- Pumping raises the water table over time
- Recharge refills each aquifer at once
- Pumping affects nothing beyond the well's own pipe
- Pumping faster than recharge lowers the water table; wells can go dry