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UNIT 7 RIVERS AND STREAMS (Chapter 12 Running Water) Study Guide
(Revised 7/16)
UNIT 7 HOMEWORK worth 10 points
WEB HIT: WORK ON RIVER RESEARCH PAPER HOMEWORK – see page 11/12
For any Unit Web Hits, go to the “DMC HOME” website; in Search box –type “Geology”, select “Vernon
Kramer”, scroll down to GEOL 1303, select “Syllabus”, select “Web Hit Links”, click on icon of interest for web sites
OR: go to DMC Home website, select “Degrees, Certificates, Courses”, scroll down to Natural Sciences and select
“Geology”, select “Faculty Listings”, select “Walter Vernon Kramer”, find “Geol 1303”, select “Syllabus”, and there
you can find the” web hit links” click on icon of interest for web sites
[IF NONE OF THE WEB SITES COME UP, YOUR COMPUTER PROBABLY NEEDS TO BE REBOOTED (RESTARTED)
SEE PAGES 12 & 13 FOR RIVER RESEARCH PAPER
General
- Landscapes without a hydrologic system will change very little over time. For example, the Moon
surface has changed very little over the last billion years.
Erosion: the removal of rocks and soil by ground water, running water, waves, glaciers or wind
- There are many large “river channels” that have deeply cut the surface of Mars. Surprisingly, the
water that cut these channels did not come from rainfall, but from “groundwater”.
- Recent satellite pictures show channels that were carved by rivers of liquid methane on the Saturn
moon of Titan. Thus we know of river channels on two planets and one moon.
- River and stream valleys dominate the appearance of the Earth’s surface as impact craters dominate
the lunar surface.
Erosion
River erosion: surface removal and transport of rocks and soils by flowing water
- River and stream valleys dominate the appearance of the Earth’s surface as impact craters dominate
the lunar surface.
- There are more than 11,240 rivers in Texas alone that cause erosion and shape our landscape!
Truth is stranger than fiction, but it is because fiction is obliged to stick to possibilities; truth isn’t.
Mark Twain
Landforms Can be Created by Rivers
- Landforms (hills and valleys) shaped by running water (rivers) produce the most significant erosional
landforms on Earth. The Grand Canyon is a prime example of this.
- River networks can even dominate landscapes in both humid and desert environments.
Water Supply
- Rivers and lakes provide 50% - 60% of the US public water supply, even though rivers and lakes
contain about 2%-3% of Earth’s water.
- Some have suggested that the creation of millions of large and small lakes has prevented a rise in sea
level. These lakes are preventing the water from returning to the oceans.
Basic River Components
- What is a river? Any large body of water that flows downhill in a well-defined channel (water that
flows under gravity to progressively lower levels).
2
Headwaters: The source area for the beginning point of rivers and streams.
River bed or river channel: An elongated depression or passageway containing (or had contained)
flowing water.
River banks: The ground bordering both sides of a river that serves to confine the water to the natural
channel during its normal course of water flow.
Tributary: A stream or smaller river that joins a larger river. This larger river can be a tributary if it
joins an even larger river.
River mouth: The final point of water discharge for a river (usually where a delta forms).
River system: a river channel and all its tributaries
GENERAL CHARACTERISTICS OF A RIVER SYSTEM
(Remember the Gonsalves painting that compares river drainage systems to a large tree with many
branches)
- Again: a tributary is a smaller river that joins a larger river
1) The number of tributaries decreases downstream. (Like the number of branches that decrease as you
go down from the very top of the tree)
2) Tributary length increases downstream. (Individual tree branches get longer as you go down the top
of the tree.)
3) The river gradient (steepness) generally decreases downstream. (Water runs downhill.)
4) River channels are wider and deeper downstream. (Just like tree branches get bigger as you go
down from the top of the tree.)
5) Valley size is proportional to river size and increases downstream. Generally - larger the river, the
larger the river valley.
The tragedy of life doesn't lie in not reaching your goal. The tragedy lies in having no goals to
reach. Benjamin Mays
3
Reported “Speeds of River Flow
1. River Discharge velocity: The “calculated” volume of water of a river as it moves past a specified
line per unit of time (i.e. 4,000 cubic feet of water/second).
- A common number reported by TV news reporters during times of floods.
2. River water velocity (in the US commonly reported as feet/sec) within a river channel
3. The steeper the river gradient (from high elevation to low elevation), the faster the water will flow
The surest way not to fail is to determine to succeed.
Richard B. Sheridan
Relative Water Speeds of Various Types of Channels
Straight River Channel verses Curved River Channels Velocities: In any channel, moving water speed
is affected by friction on the sides and the bottom of the channel
- Even the surface air presents a weak friction force on the river’s surface to slow down the water
movement.
- Straight river channel:
a) Slower water velocity rate: is found along the river bottom, along river edges (banks) and
along the top of the water (air surface)
b) The fastest water velocity rate is found at the center of the river channel, slightly below the
surface;
water velocities in straight and curved channels; darker is faster - Curved river channel: When the water of a river enters a curved river channel, centrifugal forces take
over and the water mass begins to rotate.
a) Slower water velocity rates are found on the inside of a curve; here sand will be deposited as
sand bars. This also presents a shallow river area that is safer to play and wade.
b) Faster water velocity rates are found toward the outside of curves; here erosion occurs by
undercutting the banks (cut-banks). This is a dangerous area to swim because the water speed
could sweep you under the eroding river banks.
Channel Components Along the River
- Most natural rivers do not flow very far in a straight line; river channels are noted by their curved-
shaped patterns. Whenever you see very straight, long river channel – it was probably man who
prepared these channels.
Meanders: Broad, looping bends in a river that can form a sinuous (winding) pattern
Cut banks: A river bank eroded on the outside curve of a river channel meander
4
Point bars: A crescent-shaped accumulation of sand and gravel deposited on the inside of a river
channel meander
Natural levees: A broad, low embankment built up along the banks of a river channel during floods
Oxbow lakes: A temporary lake formed in the channel of an abandoned meandering river or stream
- The creation of oxbow lakes can cause land ownership problems if the title uses the river channel as a
property boundary instead of using “surveyed points”. The formation of oxbow lakes can also create
problems for state and international boundaries that use only the river bank for a boundary instead of
surveyed points.
River sketch: cut banks, point bars, meanders, oxbow lakes
We must be vigilant in our quest to prevent the “death of consequences” such as:
-You find it acceptable to fail a class and don’t feel that you wasted your time and money
River Systems and Drainage Basins
River system consists of a main channel and all its tributaries – all within a single drainage basin.
- Any water (precipitation as rain or snow) that falls within a certain drainage basin is confined to that
river system or drainage basin.
5
Drainage basins of Texas
Drainage Divides
Drainage Divide: A boundary that separates one drainage basin (river system) from another
- Water from rainfall within one drainage basin (watershed) will not enter another drainage basin
(watershed).
US Continental Divide
Continental Divide
Continental Divide: The main “divide” (an imaginary line) of any continent that separates rivers that
empty into different ocean basins
US Continental Divide: The US continental divide runs along the crest of the Rocky Mts. from Canada
to Mexico, and divides the US into two large drainage basins.
- The US Continental Divide separates the rivers; one set of rivers drains water westward to the Pacific
Ocean and the other set of rivers drains water to the east and southward to the GOM and the Atlantic
Ocean.
River Systems - General
River Systems may be divided into three subsystems with gradational boundaries:
1. Erosion Subsystem - mostly eroding sediments at headwaters of rivers
2. Transporting Subsystem – mostly transporting eroded sediments along the rivers
3. Deposition Subsystem – mostly deposition of sediments at the end of a river system
6
1. EROSION SUBSYSTEM – rivers as agents of erosion of rocks and sediments
- A network of headwater tributaries that funnels water and eroded sediments into a larger channel
- River systems commonly form a dendritic (tree-like) drainage patterns that extend upslope to the
eroding edge of the drainage basin.
- We have found dendritic drainage patterns on Mars and the moon Titan
- Dendritic channels and valleys generally have V-shaped valleys.
- There are other types of drainage patterns, but these patterns are not very extensive.
- Typically, headwaters have clearer stream or river waters like we find in the upper Frio River.
- River erosion processes on Earth operate at a faster pace in areas that have large, major river systems
(more water available).
- Erosion will proceed at a much slower pace within areas with minor river systems such as within
deserts (less water available).
Rivers – Erosional Processes – Changing Landscape
- There are three processes that a river system uses to erode and change the landscape
A. Removal of regolith (regolith is loose soil and rock on top of solid rock)
- Regolith can be washed or can slide into a river channel and can be removed from the area
B. Downcutting of the river channel (which broadens and deepens the river valley)
C. Headward erosion uses several processes to expands the drainage basin
A. Removal of Regolith
- The loose regolith will be washed down slope (hydraulic action) and transported down slope into the
river channels.
B. Downcutting of River Channels by Abrasion
Abrasion: In swift moving water, colliding individual rocks and sand will grind out of the bottom and
sides of the river channel
- In swift moving rivers, you can often “hear” the noise made by the grinding action
Down-cutting of river channels by abrasion occurs mostly during floods results in deeper channels
Incised channel – river channel cut into solid rocks (which form canyons)
7
Pothole: Cone-shaped hole or depression formed in a river bed by swirling and grinding action of
individual rocks and gravel.
- These resemble grinding bowls produced by earlier Native Americans.
C. Headward Erosion
Headward Erosion - Upriver Migration of Waterfalls
- Erosion and down-cutting of waterfall ledges can cause these rocky ledges to locally collapse.
This results in a new waterfall ledge.
With this process, we can witness the head-ward (upriver) migration of a waterfall over time, as
exemplified by the ever-moving location of Niagara Falls.
Headward Erosion – Extending Drainage Basin
- Erosion that can extend the reach of a drainage basin
Headward Erosion – River Piracy
Stream Piracy: The diversion of the waters of one stream into another stream (modifies and
changes the drainage basin of more than one river).
- The Pecos River system of West Texas provides a good example of stream or river piracy. As
the Pecos River eroded “head-ward”, it encountered other river channels. Because the Pecos
River channel had a lower elevation than the river it encountered, the captured channel water was
diverted into the Pecos.
Then 3-D Presentation of Eroding Canyons
We must be vigilant in our quest to prevent the “death of consequences”, such as:
-You take money from grants, parents, scholarships and feel it is acceptable to earn less than an A
and it is acceptable to later quit your education
2. TRANSPORTING SUBSYSTEM - rivers as agents for transporting rocks and sediments
- River channels through which water and sediment flows from the eroding area toward an ocean or a
basin.
- Depending upon sediment size and location, it may take thousands of years or longer to move from
its eroded site to a transporting river
- Rivers associated with transporting systems generally have U-shaped valleys.
8
- Erosion and deposition both occur but are generally balanced in a transporting subsystem.
Sediment Load: rocks and soil, etc. that is carried along by the water movement
A) Suspended load involves fine particles (such as mud) carried at same rate as the water
velocity. This load represents the largest fraction of transported sediment that will be
deposited within oceans, lakes, or basins.
B) Bed load represents coarse particles (such as sand and gravel) that is moved along the river
bed by rolling, etc.; the water velocity controls the grain size of the bed load; during floods
bed loads can represent 50% of the total sediment load
C) Dissolved load: dissolved minerals, acids, ions, gas, and pollutants from areas of heavy
vegetation, shale and igneous rocks; in jungles and swamps is represented by dark-colored
river waters FYI: usually involves 4 cations [Ca+2, Na+1, Mg+2, K+1] and 3 anions [HCO3-1,
SO4-1, Cl-1].
Dams Affecting Sediment Transportation
- Dams also can severely impact river systems and people; sometimes in a very negative way by
upsetting biologic “cycles” and sediment “cycles” that prevent sediment from maintaining and
expanding deltas.
3. DEPOSITIONAL SUBSYSTEM - rivers as agents for depositing rocks and sediments - The dispersion of the sediments from the river is a deposition system – i.e. – the sediment load is
dropped to fill in a basin, which is generally an ocean basin.
- Rivers with the largest active deposition of sediments into the oceans: Ganges River, Amazon River,
Mississippi River.
9
Deposition within an Erosion Subsystem (filling a non-ocean basin)
- Not all sediment reaches an oceanic basin
Alluvial fan: Accumulation of sediment in a dry basin. The sediment will form fan-shaped deposits
especially in dry, mountainous areas.
Alluvial fan sketch
Deposition in the Transporting Subsystem (filling a non-ocean basin)
Alluvium: Any sediment deposited by the recent action of rivers (most sediment is deposited by
floods)
Floodplain: The flat, occasionally flooded area that borders a river or stream (filled with alluvium)
The Depositional Subsystem
Delta: a low, nearly flat alluvial area near the mouth of a river, formed by sudden drop in water
velocity and dumping of its sediment load
- There are many types of delta classifications
- The Mississippi River delta is classified as a “bird-foot delta” because of its unique shape
- Large swamps are an integral part of most deltas.
Delta Creation
Deltas evolve by 2 mechanisms: 1) Distributary Channels, 2) Avulsion
1. Distributary Channel: numerous stream channels in a delta that disperse water and sediment
2. Avulsion: This represents a shift in the main course of a river to a totally new and different
channel that results in forming a new delta in a new location.
Flooding
- Floodplain stages:
1) Normal stage: river water level that is below its bank or natural levee
2) Bank-full stage: river water level that stays about even with its banks or levee
3) Flood stage: the water in the river that overflows its river banks and the water submerges the
local area (flooding)
We must be vigilant in our quest to prevent the “death of consequences” such as:
-You convince yourself that it is ok to fail exams and that you don’t have to change your study
methods
10
Floods
Floods: Rivers overflowing their natural levee. Floods are not a rare event but a seasonal occurrence.
- Floods have possibly been the cause of the greatest “natural” loss of human life in recorded history.
Flash Flood: A local and sudden flood of short duration caused by a local large downburst of rain.
Flash floods often occur in valleys in a semi-arid regions and hilly terrain but can also occur in cities
(because of all of the pavement and poor drainage planning). These floods can wash vehicles and
people downstream or flood roads and streets and underpasses.
Some River Generalities
- In Texas, any stream bed wider than 30 feet is public property, regardless if it has flowing water or is
a dry bed. These stream beds are legally navigable streams.
- In January2004, it became illegal in Texas to drive off road vehicles in river beds.
- Nueces Drainage Basin includes the Nueces River, Frio River, Atascosa River and many smaller
tributaries.
- There are two large reservoirs, created by dams, within the Nueces watershed: Choke Canyon Lake
(near Three Rivers) and Lake Corpus Christi (near Mathis).
- Lake Texana is located near Edna, TX on the Navidad River. This reservoir provides almost 50% of
the drinking water for Corpus Christi via the 101 mile long Mary Rhodes pipeline.
ALWAYS ON EXAM - There is a salt water barrier dam on the Nueces River at Labonte Park to prevent high tides (salt
water) from entering the upper reaches of the river system and contaminating our water supply.
The squeaky axle gets the grease
11
LOCAL RIVERS TEAM DISCOVERY PROJECT FOR UNIT #7 RIVER SYSTEMS
(Designed for Written Communication Skills and Critical Thinking Skills
Guadalupe, San Antonio, Nueces River Basins Frio River Basin (Tributary of Nueces
River)
Purpose: Prepare a “tri-folded travel brochure or tour guide” for your selected “local” Texas river
ITEM #1; Each team member must select one of the four (4) possible choices of rivers for a brochure
River Choices: (Only one “river” each student in a group of 4 – thus each group will have 4 different
rivers)
1) Guadalupe River;
2) San Antonio River (tributary to the Guadalupe River);
3) Nueces River;
4) Frio River (tributary to Nueces River)
References to List: at least 3 (list only references used) and include your name at END of brochure
You can create a black and white or colored TRAVEL BROCHURE with a map of the river and
interesting pictures of river features. Do not copy a brochure from the internet – called
plagiarism, as I will check! Get your pictures from the internet or use your own pictures.
Some features that you may want to point out could include: (up to you which to use):
a) location source of the river
b) location of estuary into which it empties or main river that intercepts this river (if a tributary)
c) length of the river;
d) maybe list a few major towns along its banks;
e) maybe mention dams or lakes along its course;
f) maybe list names of public State parks and a few public campgrounds along its course;
g) maybe popular sports/recreation centers along its course;
h) maybe special species of fish, animals, plants found along its course;
i) maybe any special information that you found interesting about the river
For your team members: Print out completed copies for each one; REMEMBER THE DUE DATE
See following page 12 for grading rubrics
12
GRADING RUBRICS for RIVER RESEARCH PROJECT
COMMUNICATIONS SKILLS-(for RIVER RESEARCH PROJECT)
Rubric for Aspect 1 – Written communication:
6 points – Exceeds
Expectations
5 points – Meets
Expectations
2 points – Below
Expectations
0 – Not
Acceptable
Message
appropriate for
purpose,
Exceptionally
appropriate/effective
for purpose, occasion
Content adequately
appropriate/effective
for purpose,
Content inadequate
for purpose,
Failed to meet
assignment
purpose
Clear &
coherent
organizational
structure
Exceptionally clear
organization pattern;
easily followed
Reasonably
organized; logical
progression of ideas
Rambled;
organization difficult
to follow; lacked
unity
Repetitive
ideas;
impossible to
follow
Main points
fully supported
( 10 examples,
figures, etc.)
Multiple examples,
memorable details
that support central
theme
Adequate details
and 10 examples,
to support central
theme
Lacked adequate
number of examples
to support central
theme
No details
provided or
failed to support
central theme
Referenced
web sites
More than 3 websites Referenced 3 websites Referenced 2
websites
No websites
referenced or
listed references
they did not use
CRITICAL THINKING SKILLS (for RIVER RESEARCH PROJECT)
Rubric for Aspect 6 -
2 – Exceeds 1 – Meets 0 – Below 0 – Not
Acceptable
Aspect 6 Synthesis:
Integrate/organize
information in its
functional context
Information is
clearly
organized &
integrated into a
functional
context
Some information
is organized and
integrated into a
functional context
Information is
organized but not
integrated into a
functional context
Ideas are
disjointed and
presented without
a contextual
framework
If you use Microsoft Office and Word:
Open Word Document
Click File
Click New
Depending upon version of Office:
Select Brochures and Booklets
or Tri-fold brochure (remember to use front and back sides)