Groundwater and fresh water supplies
Grade 9 Science Worksheet

Circle the best answer.
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%.
USGS: rivers and lakes hold about 22,300 cubic miles of fresh water, out of about 332.5 million cubic miles of all water. About what percent is that, by Esme's math?
- About 0.67%
- About 6.7%
- About 15%
- About 0.0067%, or 1/150 of 1%
USGS: about 68.7% of fresh water is ice and about 30.1% is groundwater. About what share is left for everything else, by Jun's math?
- About 38.6%
- About 1.2%
- About 31.3%
- About 98.8%
Groundwater trapped between layers of clay or shale is under pressure (USGS). What kind of aquifer is this, by Kira's reading?
- A dry unsaturated zone
- A confined, or artesian, aquifer
- An underground river
- An unconfined water-table aquifer
USGS: a hole dug at the beach fills with water to about the level of the ocean. What does the hole show, by Milo's reading?
Close-up of water between sand grains below the water table. Close-up of water between sand grains below the water table. sand grains water table water - Water rising from deep in the mantle
- Saturated sand below the water table, with water in its pores
- An underground river under the beach
- Sand with no pore space
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 USGS: near a pumping well, the water table dips into a cone of depression. What does the cone show, by Noah's reading?
- An underground river feeds the well
- Pumping raises the water table around the well's pipe
- The aquifer does not respond to pumping
- Pumping lowers the water table near the well
USGS: in parts of the High Plains aquifer, levels fell more than 100 feet. If an example fall of 120 feet took 60 years, what is the average rate, by Pia's math?
Use the picture in question 5.
- About 7,200 feet a year
- About 0.5 feet a year
- About 180 feet a year
- About 2 feet a year
Recharge in, pumping out. USGS: groundwater is drinking water for about half the US population and nearly all of its rural population. What do the decline data suggest, by Ren's reading?
- Groundwater is a small supply that few people use for drinking
- Recharge keeps pace in each area
- Pumping makes more groundwater
- Pumping faster than recharge strains a key supply
Sand with connected pores beside clay with tiny ones. Sand with connected pores beside clay with tiny ones. Sand clay Model data: sand has 30% open space and lets water through fast; clay has 45% but lets it through very slowly. Which makes the better aquifer, by Tala's reading?
- Neither, since both are dry
- Clay, since it holds more water
- Clay, since slow flow keeps water near the well
- Sand, since water moves through it easily
USGS: a dense granite near the surface may yield little water, while a porous sandstone far below may yield hundreds of gallons a minute. What does this show, by Zee's reading?
Use the picture in question 8.
- Porosity and permeability matter more than depth
- Sandstone holds zero water
- Deeper rock yields more water in each case, whatever its type
- Granite is the top aquifer rock
USGS: groundwater may move meters a day or centimeters a century. How many times faster is 3 m a day than 3 cm a century, by Ari's math?
Use the picture in question 8.
- About 3.7 million times
- About 100 times
- About 36,500 times
- About 365 times

