Streams and Rivers.

Slides:



Advertisements
Similar presentations
Erosion and Deposition
Advertisements

The transport of weathered materials…
How Do Rivers Change the Land?
Stages of a River Stage:Upper Course 1. Source 2. Waterfall
Unit 2: Erosion and Deposition by Water
Running Water.
HYDROLOGIC CYCLE Precipitation Runoff or infiltration(groundwater flow and plant uptake) Flow to and/or gather in basin Evapotranspiration into air Condensation.
Erosion The transport of earth materials from one place to another.
Objectives Describe how surface water can move weathered materials.
Rivers are formed by erosion due to Running Water.
By the end of the lesson I should know:
A.Erosion – The transportation of weathered sediments 1. Agents of Erosion or Transport Systems: a. Running water b. Wind c. Glaciers d. Waves & Tidal.
WHAT CAN YOU REMEMBER? ocean land 2) _________ 3) _________
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.
Stream Development.
Erosion By Water and Wind.
Running Water & Groundwater
Chapter 13 Surface Water.
Stream Erosion & Deposition
Chapter 13 Notes.
Surface Water Chapter 9. Water Cycle Also the hydrologic cycle Driving force is the sun Review: condensation, precipitation, transpiration, evaporation,
13 Surface Water 13.1 Streams and Rivers
EROSION- The transport of weathered materials….
Section 13.1 Streams and Rivers
Stream Erosion and Transport
The transport of weathered materials…
Surface Water Stream landscapes, erosion and deposition
What is the long river profile? The gradient is less steep than in the upper course. The valley gets wider and flatter. Erosion is more lateral (or.
STREAMS & RIVERS Chapter 6.
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
What happens to rainfall when it hits earth????
EROSION- The transport of weathered materials…. Major Erosive Agents: Running Water GLACIERS WIND OCEAN CURRENTS AND WAVES MASS WASTING (GRAVITY!)
AIM: What are the parts of a stream/river?
A river system is made up of a main stream and tributaries – Tributary: a stream that flows into a lake or into a larger stream.
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.
STREAMS & RIVERS Chapter 6. REVIEW…. The Water Cycle.
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.
AIM: What is a stream/river? Do Now: Answer the following questions in your notebooks. Where does the water come from that fills streams and rivers? Where.
Hosted By Mrs. Shook Types of Landforms Water CycleChanging Landforms Other Landform Terms
Stream Erosion & Deposition Chapter 6 sections 1 and 2.
Chapter 2: The Flow of Freshwater. Draw the water cycle diagram in your daybook and label it in your own words. p.41 in your text.
Water Erosion Can Cause the Formation of New Landforms
TRANSPORTATION & DEPOSITION in a Stream System.
Dworshak Dam, Clearwater River, holds 12,384,000 acre- feet of water Idaho has 93,000 miles of rivers and streams.
Surface Water.
Erosion and Deposition
STREAMS & RIVERS Chapter 6 1.
Erosion of rock by moving water
AIM: What is a stream/river?
Surface Water. Surface Water Surface water notes: Where is all the water? 97.5% in Oceans 1.8 % in Ice .63% in groundwater .007% in salty lakes and.
Chapter 13 Surface Water.
DO NOW Pick up notes and Review #30. Have your turned your lab in?
River System Development
Erosional/Depositional Systems
Chapter 6.1 Running Water.
The life cycle of a river
Stream Erosion.
Surface Water Chapter 9.
Section 2: Stream Development
stream, river, lake, wetland, or ocean
Most soil in New York State is made from
Water Cycle, Groundwater, Aquifers, Caves
Surface Water. Surface Water Surface water notes: Where is all the water? 97.5% in Oceans 1.8 % in Ice .63% in groundwater .007% in salty lakes and.
Surface Water. Surface Water Surface water notes: Where is all the water? 97.5% in Oceans 1.8 % in Ice .63% in groundwater .007% in salty lakes and.
Rivers and Running Water
Erosion Weathered rock particles are transported Agents of erosion
The Flow of Freshwater.
Running Water Earth Science Chapter 6
Erosion.
Presentation transcript:

Streams and Rivers

Streams and Rivers Definitions Tributary: A stream that runs into another stream or river River System: A river and all of its tributaries Watershed: includes all of the land that drains into the river Tributary: A stream that runs into another stream or river River System: A river and all of its tributaries Watershed: includes all of the land that drains into the river

Floodplain: a nearly flat area along a stream or river that is naturally subject to flooding.

Streams and Rivers Continued Oxbow: a bow-shaped bend in a river Oxbow Lake: a bow-shaped lake formed in a former channel of a river. Floodplain: a nearly flat area along a stream or river that is naturally subject to flooding. Oxbow: a bow-shaped bend in a river Oxbow Lake: a bow-shaped lake formed in a former channel of a river.

Deltas Delta: a nearly flat plain of alluvial deposit between diverging branches of the mouth of a river, often triangular Alluvial Deposit: clay, silt or gravel carried by rushing streams and deposited where the stream slows down 

Characteristics of Streams and Rivers Meander: to take a winding or indirect course Velocity: The distance that water travels in a given amount of time. Gradient: The slope of a stream (vertical distance/horizontal distance) Meander: to take a winding or indirect course Velocity: The distance that water travels in a given amount of time. A fast moving river can erode material more quickly and can carry larger particles Gradient: The slope of a stream- the steeper the slope, the faster the river, the more it can carry

Rivers with Many Meanders

Formation of a Cutoff and Oxbow Lake

Characteristics Continued Discharge: the volume of water that passes a certain point in a given amount of time Channel: The path through which the water flows. The size and shape effects the velocity- the more sources of friction the slower the river travels Discharge: the volume of water that passes a certain point in a given amount of time Channel: The path through which the water flows. The size and shape effects the velocity- shallow, winding streams with many boulders has a great deal of friction to slow it down (slowest river scenario)

Diagram

Water Velocity Streams flow fastest in the middle, just below the surface The surface is slower because air provides a little friction The bottom is slower because the ground provides friction The sides are slower because the edge/shore provides friction

From Above From Within X marks the area of highest velocity

ESRT (pg 6)

Most youthful river valleys are V-shaped V-Shaped Valleys Most youthful river valleys are V-shaped V-shaped valleys are found in regions where there is enough rain to erode the sides of the valley

The Yellowstone River Is an Example of a V-Shaped Valley

Visualizations How Sediment is Transported Meanderings

Erosion occurs on the outside of the bends where the water is moving the fastest Deposition occurs on the inside of the bends where the water is moving the slowest

Erosion by Wind When small, loose sediments like sand are available, erosion by wind is possible Arid regions are the most common places for wind erosion to take place

Ventifacts: wedge-shaped rocks formed by wind erosion, often pitted.

Sand dunes are hills of sand deposited by wind Found wherever there are strong winds and loose sand Have long, gentle slope on windward side Have shorter, steep slope on leeward side