5TH GRADE SCIENCE • EARTH'S SYSTEMS

Earth's Water Reservoirs

Discover where all of Earth's water is stored — and why most of it isn't available for us to drink.

The Phenomenon: A Planet of Water You Can't Drink

ANCHORING PHENOMENON

How can a planet that is covered in water have problems getting enough of it to drink? Where is all of Earth's water actually stored, and why can't we simply use it all?

THINKING QUESTIONS
  • If most of Earth's surface is water, why do some places have water shortages?
  • Where do you think most of Earth's water is located — and what type of water is it?
  • What would you want to find out about how water is distributed across the planet?

What Scientists Know: Earth's Water Reservoirs

A reservoir (say: REZ-er-vwahr) is any place where a large amount of water is stored for a period of time. Earth has several major water reservoirs, and understanding where water is stored helps scientists explain why fresh water can be so hard to find. Let's explore the main ones.

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Oceans

The oceans hold about 97% of all water on Earth. That is an enormous amount — but it is salt water, which means humans, most land animals, and crops cannot drink or use it directly. The five major oceans (Pacific, Atlantic, Indian, Southern, and Arctic) are all connected and form one global body of salt water.
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Glaciers & Ice Caps

About 2% of Earth's water is frozen in glaciers (slow-moving rivers of ice) and ice caps (thick sheets of ice covering land, like in Antarctica and Greenland). This water is fresh, not salty — but it is locked in solid form and very difficult for people to access.
3

Groundwater

Water that seeps into the soil and fills tiny spaces between underground rocks is called groundwater. It makes up a significant portion of Earth's fresh water — less than 1% of the total. People access groundwater by drilling wells. It is one of our most important sources of drinking water.
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Lakes, Rivers & Atmosphere

Surface fresh water — found in lakes, rivers, and streams — makes up only a tiny fraction (about 0.03%) of all water on Earth. Water in the atmosphere (as vapor and clouds) is even less. These reservoirs are small, but they are the most accessible for daily human use.
KEY TAKEAWAY
KEY TAKEAWAY

Let's Investigate: Modeling Earth's Water Distribution

Scientists build models to represent things that are too big or complex to observe directly. Earth's water distribution is one of those things — you can't see all the water on Earth at once. So let's build a simple model to visualize how water is divided among reservoirs.

INVESTIGATION SPOTLIGHT

Question: If you had 1,000 mL of water to represent all the water on Earth, how much would go in each reservoir?

Materials

  • 1-liter (1,000 mL) measuring cup filled with water
  • 4 clear containers (labeled: Oceans, Ice, Groundwater, Surface/Atmosphere)
  • A small dropper or teaspoon
  • Sticky notes and markers for labels

Procedure

  • Pour 970 mL into the "Oceans" container. (That's almost all of it!)
  • Pour 20 mL into the "Ice" container.
  • Pour about 9.7 mL into the "Groundwater" container.
  • Using the dropper, squeeze just 0.3 mL (about 6 drops) into the "Surface/Atmosphere" container.
  • Observe the containers. Which has the most? Which has the least?

What you would observe: The "Oceans" container is nearly full, while the "Surface/Atmosphere" container barely has anything in it — just a few drops. This shows why fresh surface water is so precious.

What We Discovered: A Closer Look at Each Reservoir

The investigation model makes one thing very clear: the oceans dominate Earth's water supply. But to fully understand why water shortages happen, we need to look more carefully at what makes each reservoir different and how accessible its water is.

Salt water vs. fresh water is the single biggest distinction. Salt water contains dissolved salts and minerals, which means it cannot be used for drinking, irrigation, or most industrial processes without expensive desalination (removing the salt). Of Earth's roughly 3% fresh water, most of it is not in liquid form — it is frozen in glaciers and ice caps. That leaves groundwater and surface water as the main sources humans can realistically use.

Groundwater is hidden beneath our feet. Rain and snowmelt seep through soil and rock until they reach a layer of rock that water cannot pass through. The water collects above this layer in spaces called aquifers. Groundwater moves very slowly — sometimes just a few meters per year — and some aquifers took thousands of years to fill. When people pump groundwater out faster than rain can refill it, the aquifer shrinks. This is happening in many places around the world right now.

Lakes and rivers are the most visible reservoirs, but they hold only a tiny share of total water. They are constantly being replenished by rainfall and snowmelt, which is why the water cycle — the continuous movement of water through evaporation, condensation, and precipitation — is so important. Without the water cycle, lakes and rivers would eventually empty.

ReservoirType of Water% of TotalAccessibility
OceansSalt water~97%Not directly usable — requires desalination
Glaciers & Ice CapsFrozen fresh water~2%Locked in ice — melts slowly into rivers
GroundwaterLiquid fresh water~0.9%Accessible via wells — but refills slowly
Lakes & RiversLiquid fresh water~0.03%Most accessible — replenished by water cycle
AtmosphereWater vapor & clouds~0.001%Becomes rain/snow through precipitation

When we put all of this evidence together, the answer to our anchoring phenomenon becomes clearer. Earth is covered in water — but 97% of it is salt water in the oceans, about 2% is frozen in glaciers and ice caps, and less than 1% is liquid fresh water that humans can access. That explains why communities can face water shortages even on a planet that looks blue from space.

Patterns and Connections: Scale, Proportion, and Quantity

One of the most important tools scientists use across all areas of science is paying attention to scale, proportion, and quantity. This crosscutting concept means that scientists always ask: How much? How big compared to what? What proportion? Numbers and proportions help us see patterns that words alone cannot reveal.

In this lesson, the key insight came from looking at the proportions of water in different reservoirs. Just saying "oceans have a lot of water" doesn't convey the full picture. But when you see that oceans hold 97% while all the lakes and rivers in the world hold just 0.03%, the pattern becomes dramatic and clear. The same thinking — looking at proportions — helps scientists understand patterns in other areas, too.

Science TopicHow Scale & Proportion HelpExample
Earth's Water (this lesson)Knowing the proportion in each reservoir explains water scarcity97% ocean, 2% ice, <1% accessible fresh water
Earth's AtmosphereTiny quantities of gases (like CO₂) can have huge effects on climateCO₂ is only 0.04% of the atmosphere but drives global warming
Human BodyUnderstanding the proportion of water in our bodies shows why hydration mattersThe human body is about 60% water by weight
Solar SystemScale comparisons reveal that the Sun contains 99.8% of all matter in our solar systemAll eight planets together are tiny compared to the Sun
KEY TAKEAWAY
KEY TAKEAWAY

Real-World Connections & Engineering

Understanding where water is stored on Earth is not just interesting science — it helps communities and engineers solve real problems. Here are some ways this knowledge is applied every day.

1

Desalination Plants

In places like Saudi Arabia and parts of California, engineers build desalination plants — facilities that remove salt from ocean water to make it drinkable. Since the ocean holds 97% of Earth's water, this technology opens up a huge reservoir. However, it requires a lot of energy and is expensive, so engineers are constantly working to make the process more efficient.
2

Groundwater Management

Scientists called hydrologists study how quickly aquifers refill and help communities plan how much groundwater they can pump without draining it faster than it fills. In parts of India and the western United States, over-pumping of groundwater has caused the land surface to actually sink — a process called subsidence.
3

Glacier Monitoring

As global temperatures rise, glaciers and ice caps are melting faster than they have in thousands of years. Scientists use satellite images to track glacier size over time. This matters because glacier meltwater feeds many of the world's major rivers. If glaciers shrink too much, the river water supply decreases.
4

Water Conservation Engineering

Engineers design systems to reuse and conserve water — from drip irrigation in agriculture (delivering water directly to plant roots with minimal waste) to water recycling plants that clean used water so it can be used again. These solutions are critical because fresh, accessible water is such a tiny proportion of Earth's total supply.

All of these applications depend on understanding where water is stored, how much is in each reservoir, and how it moves between them. The science of water reservoirs is directly connected to the engineering challenge of providing clean water for billions of people.

Key Vocabulary Review

KEY VOCABULARY
  • Reservoir — A place where a large amount of water is stored for a period of time. Earth's major reservoirs include oceans, glaciers, groundwater, and surface water.
  • Fresh water — Water that contains very low levels of dissolved salts. Fresh water is found in glaciers, groundwater, lakes, and rivers, and is the type of water that humans, animals, and plants need.
  • Salt water — Water that contains high levels of dissolved salts and minerals, like ocean water. It makes up about 97% of all water on Earth and is not drinkable without treatment.
  • Glacier — A large, slow-moving mass of ice formed from compacted snow over many years. Glaciers store about 2% of Earth's total water as frozen fresh water.
  • Ice cap — A thick layer of ice that covers a large area of land, such as those found in Antarctica and Greenland.
  • Groundwater — Fresh water that is found underground in the spaces between soil particles and cracks in rocks. People access groundwater by drilling wells.
  • Aquifer — An underground layer of rock or sediment that holds and allows the flow of groundwater. Aquifers are important sources of drinking water.
  • Water cycle — The continuous movement of water through Earth's systems by evaporation, condensation, precipitation, and collection. It connects all of Earth's water reservoirs.

Practice: Test Your Understanding

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What's Next?

WHAT'S NEXT?
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