Life Cycle of a Stream Aim: How does a river shape the land over time?

Slides:



Advertisements
Similar presentations
Erosion and Deposition
Advertisements

Characteristics of High Gradient Streams
13.3 River Valleys Key Idea:
Stages of a River Stage:Upper Course 1. Source 2. Waterfall
Topic: Erosion & Running Water
Chapter 9 Water Erosion and Deposition
Running Water.
Surface Water Streams and Rivers Stream Erosion and Deposition
Erosion and Deposition Changing Earth’s Surface
Water Erosion.
Water Erosion Chapter 9 Section 2.
Surface Water Topics: Surface Water Movement Stream Development
Rivers are formed by erosion due to Running Water.
Stream and River Deposits
A.Erosion – The transportation of weathered sediments 1. Agents of Erosion or Transport Systems: a. Running water b. Wind c. Glaciers d. Waves & Tidal.
Fluvial Morphology: Landforms Made by Running Water
RIVER FORMATION EARTH’S GRAVITATIONAL FORCE PULLS OBJECTS TOWARD IT’S CENTER OF MASS. WATER FALLING DOWN A SLOPE IS EVIDENCE OF GRAVITY. AS OBJECTS DROP.
Chapter 11 Rivers & Groundwater.
Chapter River Valleys.
Stream Development.
Erosion and Deposition
Running Water Running water Water as an agent of erosion; water in streams, tributaries (larger streams) and rivers that flow down hill therefore changing.
Chapter 13 Surface Water.
Fluvial Morphology: Landforms Made by Running Water
Running water: The major force of erosion acting on Earth today. If it weren’t for the mountain- building activity of plate tectonics, Earth would be completely.
Chapter 16: Running Water. Hydrologic cycle The hydrologic cycle is a summary of the circulation of Earth’s water supply Processes involved in the hydrologic.
Surface Water.
13 Surface Water 13.1 Streams and Rivers
Rivers 11.1 – Zones in rivers From Miller’s Living in the Environment.
A stream is a body of water that carries rock particles and dissolved ions and flows down slope along a clearly defined path, called a channel. Thus, streams.
Characteristics of Straight, Meandering, and Braided Channels
 Beginning of a stream; high elevation.
Erosion Or... How to make molehills out of mountains.
RIVERS.
Chapter 9 Surface water Mars.
Rivers Almost half of the water that falls to the Earth’s surface eventually ends up in a stream or river (runoff), where it travels overland to the.
11.1 The Active River. Do you think a river can have a source? Describe where you would expect to find a river’s source. The source of a river is where.
 Water is responsible for a majority of all erosion on Earth  Runoff - after rain the water remaining on the surface is called runoff. › As runoff moves.
Stream Channel Geology. Stream Channel Behavior CCCChannel shape and Velocity Less contact with channel = greater velocity Deeper narrow channels.
Water Erosion Chapter 3 Section 2. Standard S 6.2.a – Students know water running downhill is the dominant process in shaping the landscape S 6.2.a.
A river runs through it Erosion & rivers. River-related vocabulary  You may recall the following terms.  A tributary is a small stream that empties.
River systems. Runoff vs. Infiltration Factors determining runoff, or infiltration 1.Soil composition & pore space Coarse-grains & lots of humus = good.
Unit 1.3B_4 River Landforms. Now you know a bout the processes that enable the river to change What does the river look like?
Running water.
River Systems. A river system is an open system. An open system has inputs, processes and outputs. So unlike water in the hydrological cycle, where there.
Stream Evolution Young Mature Old Age. Weathering and Erosion by water Running water on the Earth’s surface is responsible for much of the shaping of.
Surface Water.
Erosion and Deposition
Erosion of rock by moving water
11.1 The Active River.
Rivers & Groundwater.
Ch. 13 Modern Earth Science p
Chapter 6 Running Water and Groundwater
Stages of a River.
River System Development
The hydrologic cycle.
Stages of a River.
Earth’s Changing Surface
The Work of Streams.
The life cycle of a river
Section 2: Stream Development
Characteristics of a Mature Stream
River Systems Part 2 Features of a Meandering River Levees
Rivers & Groundwater.
Stages of a River.
Stages of a River.
The Flow of Water.
Erosion and Deposition
13.3 V shape As they grow they become U shaped How do rivers begin?
Stages in the Development of a River Valley
Presentation transcript:

Life Cycle of a Stream Aim: How does a river shape the land over time?

In the beginning…. A single heavy rain may form a small valley in loose soil along a hill slope When the rain ends, the small valley remains (this is called a gully) These will grow in length, and depth and may cut down far enough to become permanent. (Downcutting)

Youthful Stage During this stage a river may capture the headwaters of another river through the process of headward erosion. This is called stream piracy.

Youthful Rivers Youthful rivers have fairly straight channels and steep gradients

Youthful Stage V-shaped valley –Water erodes the sides of the valley walls and the river cuts down into its channel –The upper valley walls are widened into a v-shape

Youthful Stage Rapids Waterfalls

Maturity When sidecutting (lateral erosion) becomes greater than downcutting The topography becomes less steep with a smoother gradient Floodplains form The stream begins to meander Meandering River

Meander

Floodplains The land between the stream and the steep walls of the valley that is usually covered when the river overflows its banks during a flood Natural levees form along the banks of the river

Manmade levees are built to protect nearby areas when a river overflows its banks

Old Age Meanders become cut off from the river forming oxbow lakes A river officially enters old age when the flood plain becomes wide enough to accommodate all of the meanders

Oxbow Lakes

Summary of Stages