Worksheets Water Cycle Vocabulary

📆 Updated: 1 Jan 1970
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🔖 Category: Other

The water cycle is a fundamental concept in understanding the Earth's natural systems. To help students grasp the various terms associated with this process, worksheets can be an effective educational tool. These worksheets provide a clear and concise way for students to learn and review vocabulary related to the water cycle. Whether you are a teacher searching for resources to enhance your lesson plans or a student looking to expand your understanding, these worksheets offer a valuable opportunity to delve into the subject matter.



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What is the water cycle?

The water cycle is the continuous process of water movement on Earth, involving evaporation, condensation, precipitation, and runoff. Water evaporates from bodies of water and transpires from plants, condenses into clouds, falls as precipitation, and then flows into rivers, lakes, and oceans, ultimately starting the cycle again. This natural process is essential for maintaining the Earth's water supply and regulating the planet's temperature.

What is evaporation?

Evaporation is the process in which a liquid, such as water, transforms into a gas form by being heated up, usually through exposure to heat from the surroundings. This transformation occurs when the molecules in the liquid gain enough energy to break free from the surface and enter the surrounding air as vapor.

What is condensation?

Condensation is the process by which a gas or vapor turns into a liquid. This occurs when the temperature of the gas or vapor decreases, causing the molecules to slow down and come closer together, leading to the formation of droplets or liquid on a surface.

What is precipitation?

Precipitation is a weather phenomenon where water, in any form, falls from the atmosphere to the Earth's surface. This can include rain, snow, sleet, or hail, and is essential for the water cycle, providing moisture for plants, animals, and human activities.

What is transpiration?

Transpiration is the process by which plants absorb water through their roots and then release it into the atmosphere through their leaves in the form of water vapor. This mechanism helps plants regulate their temperature, control moisture levels, and transport nutrients throughout their tissues.

What is groundwater?

Groundwater is the water found beneath the Earth's surface in crevices and porous spaces within soil, sand, and rocks. It represents a vital source of freshwater for various ecosystems and human activities, as it supplies wells and springs with water that has infiltrated the ground from precipitation or surface water bodies.

What is infiltration?

Infiltration is the process by which water penetrates the soil surface and moves into the ground, often reaching the groundwater table. It is an important component of the water cycle as it replenishes groundwater supplies and contributes to soil moisture content.

What is runoff?

Runoff is the flow of water over the ground surface that occurs when the ground is unable to absorb all of the water from precipitation. This excess water flows over the surface and can pick up pollutants, sediments, and other materials before it eventually reaches streams, rivers, and lakes, potentially causing environmental harm.

What is a watershed?

A watershed is the area of land where all of the water that falls onto it ultimately drains off into a common body of water, such as a river, lake, or ocean. It is defined by the topography of the land, with high points forming boundaries that direct the flow of water into smaller streams and rivers that eventually come together as a larger water body. Watersheds play a crucial role in the water cycle and are important for regulating water quality and quantity in a particular region.

What is a water table?

A water table is the underground boundary between the soil surface and the area where groundwater saturates the spaces between rocks and soils. It represents the upper level of the saturated zone where the soil and rocks are filled with water, representing the level at which the ground becomes saturated.

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