Ground and Surface Water: Effects On Landscapes

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  • 0:05 Ground and Surface Water
  • 1:21 Effects of Groundwater…
  • 2:39 Effects of Groundwater…
  • 3:45 Effects of Surface Water
  • 5:22 Lesson Summary
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Lesson Transcript
Instructor: Sarah Friedl

Sarah has two Master's, one in Zoology and one in GIS, a Bachelor's in Biology, and has taught college level Physical Science and Biology.

In this lesson, you will learn how groundwater and surface water form features on Earth and cause changes in landscapes. You will also learn about the different types of features formed by each type of water.

Ground and Surface Water

Our Earth is mostly water - about 70%, in fact. Water is important on Earth not only because it supports life in a variety of ways, but it is also responsible for forming and changing much of Earth's surface. Both groundwater and surface water shape the landscape and create landforms, but they do so in different ways. In order to understand how Earth is shaped by water, we need to understand what these two types of water are.

Groundwater is water below Earth's surface, in what is called the saturated zone. The saturated zone is the region underground where water completely fills any open spaces. Water below Earth's surface also exists as soil moisture, which is found in the unsaturated zone. The unsaturated zone is located just above the saturated zone. This area is not completely saturated with water, and there's still a significant amount of air in the soil.

Surface water is what most people see as streams and rivers. Rivers are really just larger, faster-moving streams, so for simplicity, we're going to call all surface water 'streams.' Streams are dynamic systems that transport water and provide energy and nutrients through this movement.

Effects of Groundwater - Human-Influenced

Even though groundwater is moving slowly underground, it can still cause some pretty drastic changes in landscape. Some of these changes are caused by humans, but most of the time, the changes are caused because gravity causes movement of the water.

One way that humans can cause landscape changes through groundwater movement is by pumping it from the ground. Many people use wells to get the water they need for drinking, showering, and other household uses. When too much groundwater has been pumped from the ground, the land actually lowers because gravity pulls it down into the space that the groundwater occupied previously. When this happens, the land has subsided.

There are some famous examples of land subsidence, such as the Leaning Tower of Pisa. The tower was built on unstable ground, and as the ground compacted from extreme groundwater pumping, the tower began to sink with the land and then tilt. Another example of extreme land subsidence is in the San Joaquin Valley of California. Too much groundwater was pumped for agricultural irrigation and the land surface sank down about 27 feet. Even though the groundwater is now being recharged in this area, the land subsidence is a permanent feature because the land became so compacted as it sank.

Effects of Groundwater - Natural Features

Natural changes in the landscape from groundwater often come from the interaction of groundwater and limestone. Groundwater comes from rainwater that has soaked into the ground, and the rainwater is naturally acidic because it reacts with carbon dioxide in the air. As it meets with limestone in the ground, it partially dissolves the rock, and as this happens, unique features are formed.

Sinkholes are cavities in the ground caused by erosion of limestone. They are usually funnel-shaped and open to the sky. A sinkhole is formed because the groundwater caves in on itself, but they can also be formed from excessive groundwater removal.

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