Name CHAPTER 15 Class Date River Systems 2 Stream Erosion SECTION KEY IDEAS As you read this section, keep these questions in mind: • How does a river develop? • What factors affect a river’s ability to erode its channel? • How do erosive factors affect the development of a river channel? • What are the parts of a river system? What Are the Parts of a Stream? A stream is a body of water that flows over the land. A stream has three main parts: a channel, banks, and a bed. Part Description Channel the narrow groove in the ground in which a stream flows Banks the edges of the channel that rise above the water level Bed the part of the channel below the water level There are three main characteristics of streams that affect the stream’s ability to erode land. These three factors are stream load, stream discharge, and gradient. As it flows downhill, a stream carries soil, pieces of rocks, and dissolved minerals. These materials that a stream carries are called the stream load. The larger a stream’s load is, the greater the stream’s ability to erode its channel is. Stream load has three parts: suspended load, bed load, and dissolved load. Suspended load is made up of fine sand and silt. These fine particles do not sink because the water is moving so quickly. Bed load is made up of heavier materials, such as coarse sand, gravel, and pebbles. Dissolved load is the minerals that are carried in liquid solution. The volume of water that moves along the stream bed in a given time period is called the stream’s discharge. The faster a stream flows, the higher its discharge is. The greater a stream’s discharge, the heavier a load it can carry. A fast-moving stream carries more sediment and larger particles than a slow-moving stream does. The speed of the stream also affects how the stream widens its channel. Fast-moving streams erode their channels more quickly than slow-moving streams do. READING TOOLBOX Outline Before you read this section, write each of the headings in your notebook. As you read, use the headings to create an outline of the section. READING CHECK 1. List What are the three main stream erosive factors? READING CHECK 2. Compare How is dissolved load different from suspended load? Copyright © Holt McDougal. All rights reserved. Holt McDougal Earth Science 227 River Systems Name SECTION 2 Class Date Stream Erosion continued Critical Thinking 3. Predict A particular stream flows at a very high speed. What kind of gradient does the stream most likely have? Math Skills 4. Calculate You can use the following equation to calculate the discharge of a stream or river: discharge = speed of the water × cross-sectional area of the channel Suppose a river moves 1.5 m/s through a crosssectional area of 520 m2. What is the discharge of water that the river carries? Express your answer in cubic meters per second (m3/s). STREAM GRADIENT The speed of a stream affects the stream load and how quickly the stream erodes its channel. The speed of a stream depends mainly on gradient. Gradient is the steepness of the stream’s slope. Near the headwaters, or beginning of a stream, the gradient is generally steep. Near the mouth, or where the stream enters a larger body of water, the gradient is flatter. A flatter gradient makes the stream slower. A flatter gradient also decreases the stream’s ability to erode its channel. How Does a River Channel Develop? Over time, a stream channel erodes and becomes wider and deeper. When a stream becomes longer and wider, it is called a river. MEANDERING CHANNELS A river that has a low gradient typically has more bends than a river with a steep gradient has. As gradient decreases, the speed of the water decreases. When water speed decreases, the river is less able to erode into its bed. Instead, the energy of the water flowing through the channel erodes the banks. Erosion of the banks produces a winding pattern of wide curves called meanders. The figure below shows how meanders form. Direction of water flow When a river flows around a bend, the speed of the water on the outside of the bend increases. The fast moving water erodes the bank. LOOKING CLOSER 5. Analyze Diagrams On the diagram, label the area where water is moving fastest and the area where water is moving slowest. The speed of the water on the inside of the bend decreases. The decrease in speed causes the river to deposit sediment on the inside of the bend. The deposited sediment is called a bar. Over time, erosion and deposition make the bends in the river sharper. Copyright © Holt McDougal. All rights reserved. Holt McDougal Earth Science 228 River Systems Name SECTION 2 Class Date Stream Erosion continued BRAIDED STREAMS Most rivers have a single channel. However, under certain conditions, sediment bars between a river’s banks can divide the river into several channels. The water in the separate channels may join around the sediment bars. A stream or river made up of multiple channels that divide and rejoin is called a braided stream. In general, a high gradient and a large sediment load can cause a braided stream to form. What Are the Parts of a River System? A river system is made up of a main stream and smaller streams that feed into it. The figure below shows a general river system. Water runs off land and into the tributaries. The land from which water runs off into a stream is a watershed. READING CHECK 6. Identify What are the main factors that cause a braided stream to form? Ridges or elevated areas that separate watersheds are called divides. Watershed LOOKING CLOSER 7. Describe Relationships What is the relationship between a tributary and a stream? A small stream that feeds into the main stream is called a tributary. River River systems change continuously because of erosion. In a process called headward erosion, channels become longer at their upper ends. They branch out where runoff enters the streams. Erosion of slopes can make a watershed larger. A stream in a watershed with a high rate of erosion may capture a stream from another watershed. This process is called stream piracy. The stream that has been captured drains into its new river system. Copyright © Holt McDougal. All rights reserved. Holt McDougal Earth Science 229 River Systems Name Class Date Section 2 Review SECTION VOCABULARY braided stream a stream or river that is composed of multiple channels that divide and rejoin around sediment bars discharge the volume of water that flows within a given time gradient the change in elevation over a given distance meander one of the bends, twists, or curves in a low-gradient stream or river stream load the materials other than the water that are carried by a stream tributary a stream that flows into a lake or into a larger stream watershed the area of land that is drained by a river system 1. Summarize Relationships Complete the concept map below to describe streams and river systems. Use the following terms in your concept map: braided stream, stream load, suspended load, dissolved load, bed load, meander, stream gradient, tributaries, and watershed. A stream is fed by runoff from the land in a stream’s and water from At the stream’s headwaters, is generally steep, and water speed is high. Under these conditions, a The greater the water speed, the larger the which is made up of that the stream can carry. Where gradient flattens, a may form 2. Explain What are the effects of stream discharge and gradient on the ability of a river to erode its channel? Copyright © Holt McDougal. All rights reserved. Holt McDougal Earth Science 230 River Systems
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