Groundwater and fresh water supplies
Grade 9 Science Worksheet

Circle the best answer.
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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: about 2.5% of Earth's water is fresh, and about 30.1% of that is groundwater. About what share of all water is fresh groundwater, by Bo's math?
- About 32.6%
- About 12%
- About 75%
- About 0.76%
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 1.2%
- About 98.8%
- About 38.6%
- About 31.3%
Groundwater trapped between layers of clay or shale is under pressure (USGS). What kind of aquifer is this, by Kira's reading?
- A confined, or artesian, aquifer
- A dry unsaturated zone
- An unconfined water-table aquifer
- An underground river
Why can water rise up an artesian well without a pump, by Luz's reading (USGS)?
Use the picture in question 3.
- The clay layers pump the water
- An underground river flows uphill
- The water table is above the land at each spot
- Pressure in the confined aquifer pushes it up
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 - Saturated sand below the water table, with water in its pores
- An underground river under the beach
- Sand with no pore space
- Water rising from deep in the mantle
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?
- The aquifer does not respond to pumping
- Pumping lowers the water table near the well
- Pumping raises the water table around the well's pipe
- An underground river feeds 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 6.
- About 180 feet a year
- About 2 feet a year
- About 0.5 feet a year
- About 7,200 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?
- Pumping faster than recharge strains a key supply
- Pumping makes more groundwater
- Groundwater is a small supply that few people use for drinking
- Recharge keeps pace in each area
Sand with connected pores beside clay with tiny ones. Sand with connected pores beside clay with tiny ones. Sand clay 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?
- Deeper rock yields more water in each case, whatever its type
- Sandstone holds zero water
- Granite is the top aquifer rock
- Porosity and permeability matter more than depth
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 9.
- About 365 times
- About 100 times
- About 36,500 times
- About 3.7 million times