streams glg 101 - physical geology bob leighty. these lecture notes are very similar to the ones i...

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Streams Streams GLG 101 - Physical Geology GLG 101 - Physical Geology Bob Leighty Bob Leighty

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Page 1: Streams GLG 101 - Physical Geology Bob Leighty. These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are

StreamsStreams

GLG 101 - Physical GeologyGLG 101 - Physical Geology Bob LeightyBob Leighty

Page 2: Streams GLG 101 - Physical Geology Bob Leighty. These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are

These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are loaded with imagery and streamlined text that highlight the most essential terms and concepts. The notes provide a framework for learning and, by themselves, are not meant to be a comprehensive source of information.

To take advantage of the global knowledge base known as the Internet, I have included numerous hyperlinks to external web sites (like the Wikipedia, USGS, NASA, etc.). Follow the links and scan them for relevant info. The information from linked web sites is meant to supplement and reinforce the lecture notes – you won’t be responsible for knowing everything contained in them.

As a distance learning student, you need to explore and understand the content more independently than in a traditional class. As always, I will help guide you through this learning adventure. Remember, email Dr. Bob if you have any questions about today’s lecture ([email protected]).Leave no questions behind!

Explore and have fun!Explore and have fun!

These notes and web links are your primary “lecture” content in this class. Additionally, various articles are assigned each week to supplement this “lecture” information. I believe you’ll have enough information to reference without having to purchase a costly textbook.

Page 3: Streams GLG 101 - Physical Geology Bob Leighty. These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are

Cycling of water due to gravity & solar energy

The Hydrologic CycleThe Hydrologic CycleStreamsStreams

Page 4: Streams GLG 101 - Physical Geology Bob Leighty. These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are

Where’s the Water?Where’s the Water?StreamsStreams

Page 5: Streams GLG 101 - Physical Geology Bob Leighty. These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are

Water flowing in streams, canyons, ravines, etc.

Lakes, ponds, and springs

Intermittent streams = flow only at certain times of the year (e.g., Salt, Gila)

Perennial streams = flow continuously (e.g., Colorado,

Verde)

Arizona’s WaterArizona’s WaterStreamsStreams

Page 6: Streams GLG 101 - Physical Geology Bob Leighty. These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are

Services over 17 million people in 7 states (Colorado River Compact)

Colorado RiverColorado River Arizona portion over 600 miles long

Several hydroelectric dams (& lakes)

Lots of dissolved material (a desalting plant was built in 1993 near Yuma for $484 million)

Arizona’s WaterArizona’s WaterStreamsStreams

Page 7: Streams GLG 101 - Physical Geology Bob Leighty. These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are

Averages 80 ft wide & 16 ft deep

7% lost to seepage & evaporation

Built (1973-1993) to provide an alternative water source 336-mile canal system (Colorado River to Tucson)

costing $3.6 billion

Central Arizona Project (CAP)Central Arizona Project (CAP)

Arizona’s WaterArizona’s WaterStreamsStreams

Page 8: Streams GLG 101 - Physical Geology Bob Leighty. These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are

7 dams (& lakes) on the Salt River & Verde River

Salt River Project (SRP)Salt River Project (SRP)

Arizona’s WaterArizona’s WaterStreamsStreams

Page 9: Streams GLG 101 - Physical Geology Bob Leighty. These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are

Water collects in drainage basins

Streams = all channelized runoff (any size)

How Do Streams Form?How Do Streams Form?StreamsStreams

Fluvial = stream-related process

Page 10: Streams GLG 101 - Physical Geology Bob Leighty. These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are

Highest velocity in upper-center of a straight channel

How Do Streams Flow?How Do Streams Flow?StreamsStreams

VelocityVelocity

Page 11: Streams GLG 101 - Physical Geology Bob Leighty. These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are

At a river bend - highest velocity shifts to outside

How Do Streams Flow?How Do Streams Flow?StreamsStreams

VelocityVelocity

Page 12: Streams GLG 101 - Physical Geology Bob Leighty. These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are

Velocity of stream controls whether it erodes, transports, or deposits material

Most erosion occurs on outside (higher velocity) & most deposition on inside (lower velocity)

How Do Streams Flow?How Do Streams Flow?StreamsStreams

VelocityVelocity

Page 13: Streams GLG 101 - Physical Geology Bob Leighty. These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are

Typically measured in feet per mile

Gradient = the slope of the channel (vertical drop / horizontal distance)

Most streams decrease in gradient (become less steep) downstream (seaward)

How Do Streams Flow?How Do Streams Flow?StreamsStreams

GradientGradient

Page 14: Streams GLG 101 - Physical Geology Bob Leighty. These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are

Steeper gradients = in upper areas of stream (100’s of ft/mile; rapids & waterfalls)

How Do Streams Flow?How Do Streams Flow?StreamsStreams

GradientGradient

Page 15: Streams GLG 101 - Physical Geology Bob Leighty. These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are

Gentle gradients = in lower areas (1’s of ft/mile; “old man river”)

How Do Streams Flow?How Do Streams Flow?StreamsStreams

GradientGradient

Page 16: Streams GLG 101 - Physical Geology Bob Leighty. These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are

Streams cut vertically

Common in areas with high stream gradients

Creates V-shaped valleys, waterfalls, rapids

How Do Streams Erode?How Do Streams Erode?StreamsStreams

DowncuttingDowncutting

Page 17: Streams GLG 101 - Physical Geology Bob Leighty. These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are

Slot canyons result from extreme downcutting

How Do Streams Erode?How Do Streams Erode?StreamsStreams

DowncuttingDowncutting

Page 18: Streams GLG 101 - Physical Geology Bob Leighty. These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are

Stream cuts sideways

Creates meanders, flood plains, wider valleys

Common in areas with low stream gradients

How Do Streams Erode?How Do Streams Erode?StreamsStreams

Lateral ErosionLateral Erosion

Page 19: Streams GLG 101 - Physical Geology Bob Leighty. These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are

Lateral erosion at a meander bend

How Do Streams Erode?How Do Streams Erode?StreamsStreams

Lateral ErosionLateral Erosion

Page 20: Streams GLG 101 - Physical Geology Bob Leighty. These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are

Material moves:

1) along bottom of channel (bed load)

2) by drifting along (suspended load)

3) in solution (dissolved load)

How Do Streams Transport Sediment?How Do Streams Transport Sediment?StreamsStreams

Page 21: Streams GLG 101 - Physical Geology Bob Leighty. These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are

Alluvium = material deposited by stream

Sediment is deposited if stream velocity decreases

How Do Streams Deposit Sediment?How Do Streams Deposit Sediment?StreamsStreams

Page 22: Streams GLG 101 - Physical Geology Bob Leighty. These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are

Channel - Higher velocity water; sand & gravel

Fluvial FeaturesFluvial FeaturesStreamsStreams

Page 23: Streams GLG 101 - Physical Geology Bob Leighty. These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are

Floodplain – Flat area with lower velocity water; mud & silt

Fluvial FeaturesFluvial FeaturesStreamsStreams

Page 24: Streams GLG 101 - Physical Geology Bob Leighty. These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are

Terrace - Remnant of a former floodplain

Fluvial FeaturesFluvial FeaturesStreamsStreams

Page 25: Streams GLG 101 - Physical Geology Bob Leighty. These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are

Delta – Sediment accumulates as streams enter a lake or

ocean,

because of the reduction in water velocity

Fluvial FeaturesFluvial FeaturesStreamsStreams

Page 26: Streams GLG 101 - Physical Geology Bob Leighty. These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are

The Mississippi Delta in the last 6,000 years

Fluvial FeaturesFluvial FeaturesStreamsStreams

Page 27: Streams GLG 101 - Physical Geology Bob Leighty. These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are

Alluvial fan - Similar to a delta “on dry land”

Fluvial FeaturesFluvial FeaturesStreamsStreams

Page 28: Streams GLG 101 - Physical Geology Bob Leighty. These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are

Entrenched meanders – Regional uplift or a drop in base level causes streams to downcut

Fluvial FeaturesFluvial FeaturesStreamsStreams

Page 29: Streams GLG 101 - Physical Geology Bob Leighty. These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are

Slot canyons – Regional uplift or a drop in base level

causes streams to downcut

Fluvial FeaturesFluvial FeaturesStreamsStreams

Page 30: Streams GLG 101 - Physical Geology Bob Leighty. These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are

WWW Links in this LectureWWW Links in this Lecture

> Hydrologic cycle - http://en.wikipedia.org/wiki/Water_cycle

> Colorado River - http://en.wikipedia.org/wiki/Colorado_River

> Colorado River Compact - http://en.wikipedia.org/wiki/Colorado_River_Compact

> Hydroelectricity - http://en.wikipedia.org/wiki/Hydroelectricity

> Central Arizona Project - http://en.wikipedia.org/wiki/Central_Arizona_Project

> Salt River Project - http://en.wikipedia.org/wiki/Salt_River_Project

> Salt River - http://en.wikipedia.org/wiki/Salt_River_%28Arizona%29

> Verde River - http://en.wikipedia.org/wiki/Verde_River

> Drainage basin - http://en.wikipedia.org/wiki/Drainage_basin

> Stream - http://en.wikipedia.org/wiki/Stream

> Alluvium - http://en.wikipedia.org/wiki/Alluvium

> Channel - http://en.wikipedia.org/wiki/Channel_%28geography%29

> Floodplain - http://en.wikipedia.org/wiki/Floodplain

> Stream terrace - http://en.wikipedia.org/wiki/Stream_terrace

> River delta - http://en.wikipedia.org/wiki/River_delta

> Alluvial fan - http://en.wikipedia.org/wiki/Alluvial_fan

> Entrenched meanders - http://en.wikipedia.org/wiki/Entrenched_river

> Slot canyon - http://en.wikipedia.org/wiki/Slot_canyon

StreamsStreams