Erosion and Deposition by Flowing Water
Lesson Objectives
Explain how flowing water causes erosion and deposition.
Describe how runoff, streams, and rivers change Earth’s surface.
Identify features caused by groundwater erosion and deposition.
Vocabulary
alluvial fan
cave
delta
deposition
erosion
floodplain
levee
meander
oxbow lake
saltation
sinkhole
suspension
traction
Introduction
Erosion and deposition are responsible for many landforms. Erosion is the transport of sediments. Agents of erosion include flowing water, waves, wind, ice, or gravity. Eroded material is eventually dropped somewhere else. This is called deposition.
How Flowing Water Causes Erosion and Deposition
Flowing water is a very important agent of erosion. Flowing water can erode rocks and soil. Water dissolves minerals from rocks and carries the ions. This process happens really slowly. But over millions of years, flowing water dissolves massive amounts of rock.
Moving water also picks up and carries particles of soil and rock. The ability to erode is affected by the velocity, or speed, of the water. The size of the eroded particles depends on the velocity of the water. Eventually, the water deposits the materials. As water slows, larger particles are deposited. As the water slows even more, smaller particles are deposited. The graph in Figure below shows how water velocity and particle size influence erosion and deposition.
Flowing water erodes or deposits particles depending on how fast the water is moving and how big the particles are.
Water Speed and Erosion
Faster-moving water has more energy. Therefore, it can carry larger particles. It can carry more particles. What causes water to move faster? The slope of the land over which the water flows is one factor. The steeper the slope, the faster the water flows. Another factor is the amount of water that's in the stream. Streams with a lot of water flow faster than streams that are nearly dry.
Particle Size and Erosion
The size of particles determines how they are carried by flowing water. This is illustrated in Figure below and at the link below:
Minerals that dissolve in water form salts. The salts are carried in solution. They are mixed thoroughly with the water.
Small particles, such as clay and silt, are carried in suspension. They are mixed throughout the water. These particles are not dissolved in the water.
Somewhat bigger particles, such as sand, are moved by saltation. The particles move in little jumps near the stream bottom. They are nudged along by water and other particles.
The biggest particles, including gravel and pebbles, are moved by traction. In this process, the particles roll or drag along the bottom of the water.
How Flowing Water Moves Particles. How particles are moved by flowing water depends on their size.
Deposition by Water
Flowing water slows down when it reaches flatter land or flows into a body of still water. What do you think happens then? The water starts dropping the particles it was carrying. As the water slows, it drops the largest particles first. The smallest particles settle out last.
Erosion and Deposition by Surface Water
Water that flows over Earth’s surface includes runoff, streams, and rivers. All these types of flowing water can cause erosion and deposition.
Erosion by Runoff
When a lot of rain falls in a short period of time, much of the water is unable to soak into the ground. Instead, it runs over the land.
Gravity causes the water to flow from higher to lower ground. As the runoff flows, it may pick up loose material on the surface, such as bits of soil and sand.
Runoff is likely to cause more erosion if the land is bare. Plants help hold the soil in place. The runoff water in Figure below is brown because it eroded soil from a bare, sloping field. Can you find evidence of erosion by runoff where you live? What should you look for?
Erosion by Runoff. Runoff has eroded small channels through this bare field.
Much of the material eroded by runoff is carried into bodies of water, such as streams, rivers, ponds, lakes, or oceans. Runoff is an important cause of erosion. That’s because it occurs over so much of Earth’s surface.
Erosion by Mountain Streams
Streams often start in mountains, where the land is very steep. You can see an example in Figure below. A mountain stream flows very quickly because of the steep slope. This causes a lot of erosion and very little deposition. The rapidly falling water digs down into the stream bed and makes it deeper. It carves a narrow, V-shaped channel.
Mountain Stream. This mountain stream races down a steep slope. It mainly erodes the bottom of its channel. It carries the eroded rock downstream.
How a Waterfall Forms
Mountain streams may erode waterfalls. As shown in Figure below and at the link below, a waterfall forms where a stream flows from an area of harder to softer rock. The water erodes the softer rock faster than the harder rock. This causes the stream bed to drop down, like a step, creating a waterfall. As erosion continues, the waterfall gradually moves upstream.
[Insert a link to an animation that shows how a waterfall forms where a stream flows from harder to softer rock.]
How a Waterfall Forms and Moves. Why does a waterfall keep moving upstream?
Erosion by Slow-Flowing Rivers
Rivers flowing over gentle slopes erode the sides of their channels more than the bottom. Large curves, called meanders, form because of erosion and deposition by the moving water. The curves are called meanders because they slowly “wander” over the land. You can see how this happens in Figure below and at the link below.
[Insert a link to an animation showing how a meandering river moves over the surface.]
Meanders form because water erodes the outside of curves and deposits eroded material on the inside. Over time, the curves shift position.
As meanders erode from side to side, they create a floodplain. This is a broad, flat area on both sides of a river. Eventually, a meander may become cut off from the rest of the river. This forms an oxbow lake, like the one in Figure above.
Deposition by Streams and Rivers
When a stream or river slows down, it starts dropping its sediments. Larger sediments are dropped in steep areas, but smaller sediments can still be carried. Smaller sediments are dropped as the slope becomes less steep.
Alluvial Fans
In arid regions, a mountain stream may flow onto flatter land. The stream comes to a stop rapidly. The deposits form an alluvial fan, like the one in Figure below.
An alluvial fan in Death Valley, California (left), Nile River Delta in Egypt (right).
Deltas
Deposition also occurs when a stream or river empties into a large body of still water. In this case, a delta forms. A delta is shaped like a triangle. It spreads out into the body of water. An example is shown in Figure above.
Deposition by Flood Waters
A flood occurs when a river overflows it banks. This might happen because of heavy rains.
Floodplains
As the water spreads out over the land, it slows down and drops its sediment. If a river floods often, the floodplain develops a thick layer of rich soil because of all the deposits. That’s why floodplains are usually good places for growing plants. For example, the Nile River in Egypt provides both water and thick sediments for raising crops in the middle of a sandy desert.
Natural Levees
A flooding river often forms natural levees along its banks. A levee is a raised strip of sediments deposited close to the water’s edge. You can see how levees form in Figure below. Levees occur because floodwaters deposit their biggest sediments first when they overflow the river’s banks.
This diagram shows how a river builds natural levees along its banks.
Erosion and Deposition by Groundwater.
Some water soaks into the ground. It travels down through tiny holes in soil. It seeps through cracks in rock. The water moves slowly, pulled deeper and deeper by gravity. Underground water can also erode and deposit material.
Caves
As groundwater moves through rock, it dissolves minerals. Some rocks dissolve more easily than others. Over time, the water may dissolve large underground holes, or caves. Groundwater drips from the ceiling to the floor of a cave. This water is rich in dissolved minerals. When the minerals come out of solution, they are deposited. They build up on the ceiling of the cave to create formations called stalactites. A stalactite is a pointed, icicle-like mineral deposit that forms on the ceiling of a cave. They drip to the floor of the cave and harden to form stalagmites. A stalagmite is a more rounded mineral deposit that forms on the floor of a cave (Figure below). Both types of formations grow in size as water keeps dripping and more minerals are deposited.
This cave has both stalactites and stalagmites.
Sinkholes
As erosion by groundwater continues, the ceiling of a cave may collapse. The rock and soil above it sink into the ground. This forms a sinkhole on the surface. You can see an example of a sinkhole in Figure below. Some sinkholes are big enough to swallow vehicles and buildings.
A sinkhole.
Lesson Summary
Water flowing over Earth’s surface or underground causes erosion and deposition.
Water flowing over a steeper slope moves faster and causes more erosion.
How water transports particles depends on their size. When water slows down, it starts depositing sediment, starting with the largest particles first.
Runoff erodes the land after a heavy rain. It picks up sediment and carries most of it to bodies of water. Mountain streams erode narrow, V-shaped valleys and waterfalls.
Erosion and deposition by slow-flowing rivers creates broad floodplains and meanders.
Deposition by streams and rivers may form alluvial fans and deltas. Floodwaters may deposit natural levees.
Erosion and deposition by groundwater can form caves and sinkholes. Stalactites and stalagmites are mineral deposits that build up in caves as water continues to drip.
Lesson Review Questions
Recall
1. Define erosion.
2. What is deposition?
3. When does flowing water deposit the sediment it is carrying?
4. What happens to the sediment eroded by runoff?
5. Describe how a waterfall forms?
6. What are meanders?
Apply Concepts
7. Make a table that relates particle size to the way particles are transported by flowing water.
8. Create a sketch that shows effects of groundwater erosion and deposition.
Think Critically
9. Explain why mountain streams erode V-shaped valleys.
10. What might be pros and cons of living on the floodplain of a river?
Points to Consider
Ocean waves are another form of moving water. They also cause erosion and deposition.
How do waves erode shorelines?
What landforms are deposited by waves?
Shocking Moment Road Collapses, Disappears During Floods
Lesson Objectives
Explain how flowing water causes erosion and deposition.
Describe how runoff, streams, and rivers change Earth’s surface.
Identify features caused by groundwater erosion and deposition.
Vocabulary
alluvial fan
cave
delta
deposition
erosion
floodplain
levee
meander
oxbow lake
saltation
sinkhole
suspension
traction
Introduction
Erosion and deposition are responsible for many landforms. Erosion is the transport of sediments. Agents of erosion include flowing water, waves, wind, ice, or gravity. Eroded material is eventually dropped somewhere else. This is called deposition.
How Flowing Water Causes Erosion and Deposition
Flowing water is a very important agent of erosion. Flowing water can erode rocks and soil. Water dissolves minerals from rocks and carries the ions. This process happens really slowly. But over millions of years, flowing water dissolves massive amounts of rock.
Moving water also picks up and carries particles of soil and rock. The ability to erode is affected by the velocity, or speed, of the water. The size of the eroded particles depends on the velocity of the water. Eventually, the water deposits the materials. As water slows, larger particles are deposited. As the water slows even more, smaller particles are deposited. The graph in Figure below shows how water velocity and particle size influence erosion and deposition.
Flowing water erodes or deposits particles depending on how fast the water is moving and how big the particles are.
Water Speed and Erosion
Faster-moving water has more energy. Therefore, it can carry larger particles. It can carry more particles. What causes water to move faster? The slope of the land over which the water flows is one factor. The steeper the slope, the faster the water flows. Another factor is the amount of water that's in the stream. Streams with a lot of water flow faster than streams that are nearly dry.
Particle Size and Erosion
The size of particles determines how they are carried by flowing water. This is illustrated in Figure below and at the link below:
Minerals that dissolve in water form salts. The salts are carried in solution. They are mixed thoroughly with the water.
Small particles, such as clay and silt, are carried in suspension. They are mixed throughout the water. These particles are not dissolved in the water.
Somewhat bigger particles, such as sand, are moved by saltation. The particles move in little jumps near the stream bottom. They are nudged along by water and other particles.
The biggest particles, including gravel and pebbles, are moved by traction. In this process, the particles roll or drag along the bottom of the water.
How Flowing Water Moves Particles. How particles are moved by flowing water depends on their size.
Deposition by Water
Flowing water slows down when it reaches flatter land or flows into a body of still water. What do you think happens then? The water starts dropping the particles it was carrying. As the water slows, it drops the largest particles first. The smallest particles settle out last.
Erosion and Deposition by Surface Water
Water that flows over Earth’s surface includes runoff, streams, and rivers. All these types of flowing water can cause erosion and deposition.
Erosion by Runoff
When a lot of rain falls in a short period of time, much of the water is unable to soak into the ground. Instead, it runs over the land.
Gravity causes the water to flow from higher to lower ground. As the runoff flows, it may pick up loose material on the surface, such as bits of soil and sand.
Runoff is likely to cause more erosion if the land is bare. Plants help hold the soil in place. The runoff water in Figure below is brown because it eroded soil from a bare, sloping field. Can you find evidence of erosion by runoff where you live? What should you look for?
Erosion by Runoff. Runoff has eroded small channels through this bare field.
Much of the material eroded by runoff is carried into bodies of water, such as streams, rivers, ponds, lakes, or oceans. Runoff is an important cause of erosion. That’s because it occurs over so much of Earth’s surface.
Erosion by Mountain Streams
Streams often start in mountains, where the land is very steep. You can see an example in Figure below. A mountain stream flows very quickly because of the steep slope. This causes a lot of erosion and very little deposition. The rapidly falling water digs down into the stream bed and makes it deeper. It carves a narrow, V-shaped channel.
Mountain Stream. This mountain stream races down a steep slope. It mainly erodes the bottom of its channel. It carries the eroded rock downstream.
How a Waterfall Forms
Mountain streams may erode waterfalls. As shown in Figure below and at the link below, a waterfall forms where a stream flows from an area of harder to softer rock. The water erodes the softer rock faster than the harder rock. This causes the stream bed to drop down, like a step, creating a waterfall. As erosion continues, the waterfall gradually moves upstream.
[Insert a link to an animation that shows how a waterfall forms where a stream flows from harder to softer rock.]
How a Waterfall Forms and Moves. Why does a waterfall keep moving upstream?
Erosion by Slow-Flowing Rivers
Rivers flowing over gentle slopes erode the sides of their channels more than the bottom. Large curves, called meanders, form because of erosion and deposition by the moving water. The curves are called meanders because they slowly “wander” over the land. You can see how this happens in Figure below and at the link below.
[Insert a link to an animation showing how a meandering river moves over the surface.]
Meanders form because water erodes the outside of curves and deposits eroded material on the inside. Over time, the curves shift position.
As meanders erode from side to side, they create a floodplain. This is a broad, flat area on both sides of a river. Eventually, a meander may become cut off from the rest of the river. This forms an oxbow lake, like the one in Figure above.
Deposition by Streams and Rivers
When a stream or river slows down, it starts dropping its sediments. Larger sediments are dropped in steep areas, but smaller sediments can still be carried. Smaller sediments are dropped as the slope becomes less steep.
Alluvial Fans
In arid regions, a mountain stream may flow onto flatter land. The stream comes to a stop rapidly. The deposits form an alluvial fan, like the one in Figure below.
An alluvial fan in Death Valley, California (left), Nile River Delta in Egypt (right).
Deltas
Deposition also occurs when a stream or river empties into a large body of still water. In this case, a delta forms. A delta is shaped like a triangle. It spreads out into the body of water. An example is shown in Figure above.
Deposition by Flood Waters
A flood occurs when a river overflows it banks. This might happen because of heavy rains.
Floodplains
As the water spreads out over the land, it slows down and drops its sediment. If a river floods often, the floodplain develops a thick layer of rich soil because of all the deposits. That’s why floodplains are usually good places for growing plants. For example, the Nile River in Egypt provides both water and thick sediments for raising crops in the middle of a sandy desert.
Natural Levees
A flooding river often forms natural levees along its banks. A levee is a raised strip of sediments deposited close to the water’s edge. You can see how levees form in Figure below. Levees occur because floodwaters deposit their biggest sediments first when they overflow the river’s banks.
This diagram shows how a river builds natural levees along its banks.
Erosion and Deposition by Groundwater.
Some water soaks into the ground. It travels down through tiny holes in soil. It seeps through cracks in rock. The water moves slowly, pulled deeper and deeper by gravity. Underground water can also erode and deposit material.
Caves
As groundwater moves through rock, it dissolves minerals. Some rocks dissolve more easily than others. Over time, the water may dissolve large underground holes, or caves. Groundwater drips from the ceiling to the floor of a cave. This water is rich in dissolved minerals. When the minerals come out of solution, they are deposited. They build up on the ceiling of the cave to create formations called stalactites. A stalactite is a pointed, icicle-like mineral deposit that forms on the ceiling of a cave. They drip to the floor of the cave and harden to form stalagmites. A stalagmite is a more rounded mineral deposit that forms on the floor of a cave (Figure below). Both types of formations grow in size as water keeps dripping and more minerals are deposited.
This cave has both stalactites and stalagmites.
Sinkholes
As erosion by groundwater continues, the ceiling of a cave may collapse. The rock and soil above it sink into the ground. This forms a sinkhole on the surface. You can see an example of a sinkhole in Figure below. Some sinkholes are big enough to swallow vehicles and buildings.
A sinkhole.
Lesson Summary
Water flowing over Earth’s surface or underground causes erosion and deposition.
Water flowing over a steeper slope moves faster and causes more erosion.
How water transports particles depends on their size. When water slows down, it starts depositing sediment, starting with the largest particles first.
Runoff erodes the land after a heavy rain. It picks up sediment and carries most of it to bodies of water. Mountain streams erode narrow, V-shaped valleys and waterfalls.
Erosion and deposition by slow-flowing rivers creates broad floodplains and meanders.
Deposition by streams and rivers may form alluvial fans and deltas. Floodwaters may deposit natural levees.
Erosion and deposition by groundwater can form caves and sinkholes. Stalactites and stalagmites are mineral deposits that build up in caves as water continues to drip.
Lesson Review Questions
Recall
1. Define erosion.
2. What is deposition?
3. When does flowing water deposit the sediment it is carrying?
4. What happens to the sediment eroded by runoff?
5. Describe how a waterfall forms?
6. What are meanders?
Apply Concepts
7. Make a table that relates particle size to the way particles are transported by flowing water.
8. Create a sketch that shows effects of groundwater erosion and deposition.
Think Critically
9. Explain why mountain streams erode V-shaped valleys.
10. What might be pros and cons of living on the floodplain of a river?
Points to Consider
Ocean waves are another form of moving water. They also cause erosion and deposition.
How do waves erode shorelines?
What landforms are deposited by waves?
Shocking Moment Road Collapses, Disappears During Floods
"Even if we were late by two hours, and it was dark in the area, it could have been much worse," said the person who recorded the video
Updated: July 30, 2019 03:23 pm IST
Watch the moment a road disappears during floods in Canada
This is the moment a road collapses in Antigonish, Nova Scotia, Canada, after heavy rainfall leaves road surfaces hazardous for passing cars.
A shocking video has captured moment a road literally collapsed and disappeared into a river during floods in Canada. The incident occurred in the town of Antigonish in Nova Scotia. According to CBC News, it was a section of the Cloverville Road that collapsed on Monday evening as the area experienced heavy rainfall.
A shocking video has captured moment a road literally collapsed and disappeared into a river during floods in Canada. The incident occurred in the town of Antigonish in Nova Scotia. According to CBC News, it was a section of the Cloverville Road that collapsed on Monday evening as the area experienced heavy rainfall.
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