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About this activity

Test your knowledge of the water cycle in this fun and interactive game! Identify the correct process based on the points shown in the image. Think fast and choose wisely. You only have 3 lives and 6 minutes to complete the challenge. Can you point out every step correctly before time runs out?

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Pin that Process!Online version

Test your knowledge of the water cycle in this fun and interactive game! Identify the correct process based on the points shown in the image. Think fast and choose wisely. You only have 3 lives and 6 minutes to complete the challenge. Can you point out every step correctly before time runs out?

by Mj Servas
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Explanation

Precipitation is water released from clouds in the form of rain, freezing rain, sleet, snow, or hail. Precipitation is the main way atmospheric water returns to the surface of the Earth. Most precipitation falls as rain.

Condensation is the process in the water cycle where water vapor (a gas) cools and changes back into liquid water droplets. It is the opposite of evaporation and is responsible for forming clouds, fog, and dew. This phase change occurs when air cools to its dew point, causing water vapor to coalesce around particles like dust or salt in the atmosphere.

Evaporation is the process by which a liquid turns into a gas. It is also one of the three main steps in the global water cycle.

Collection is the stage of the water cycle where water is temporarily collected and stored. As water returns to the Earth’s surface, it will run-off into our rivers, streams, lakes, and glaciers.

Runoff occurs when there is more water than land can absorb. The excess liquid flows across the surface of the land and into nearby creeks, streams, or ponds.

Transpiration is defined as the process where water evaporates into the atmosphere through plants.

Percolation is the downward movement of water through rock. Percolation occurs beneath the root zone. Groundwater infiltrates through the soil much as water fills a sponge, and percolates from space to space along fractures in rock, through sand and gravel, or through channels in formations such as cavernous limestone.

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