s6e5. students will investigate the scientific view …peachtreems.dekalb.k12.ga.us/downloads/lesson...
TRANSCRIPT
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Lesson Plan
Subject: Earth Science Grade Level: Gifted 6th
2-15-16 to 2-19-16
Content Standard:
S6E5. Students will investigate the scientific view of how the earth’s
surface is formed.
Vocabulary: Weathering, erosion, chemical, physical, exfoliation, ice wedging, thermal, biotic,
oxidation, carbonation
Parallel
Alternative
Station
Team
Independent
Students are grouped by previous Georgia Milestone scores
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Beginning
May include:
Opening, warm up,
review, anticipatory
set, etc
Middle
May include: Instruction,
checking for understanding,
independent or group practice
End
May include: Closing,
assessments, extension
of lesson, etc.
Monday
NO SCHOOL
Tuesday
substitute
What is the rate of
weathering? What
factors affect
weathering
Task 1: student will use
discussion map to answer
textbook questions and construct a
test question(review of questions
from homework last week)
3-2-1
Wednesday
substitute
What is erosion?
Task 1: Students will code the
informational text reading passage
and create a constructed response
question
Did not complete last week
Ticket out the door
Thursday
Quiz and finish weathering lab
Friday
STEM day
Student will create a prototype of
shark tank product
Marzano’s Essential 9 (Highlight Strategies Used)
Identifying Similarities and Difference
Summarizing and Note-taking
Reinforcing Effort and Providing Recognition
Homework and Practice
Nonlinguistic Representations
Cooperative Learning
Setting Objectives and Providing Feedback
Generating and Testing Hypotheses
Cues, Questions, and Advance Organizers
Multiple Intelligence (Highlight Accessed
Intelligences)
Verbal-Linguistic
Logical-Mathematical
Visual-Spatial
Bodily-Kinesthetic
Musical
Interpersonal
Intrapersonal
Naturalistic
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Name: _______________________________Date: _______________Period: ________
Weathering Lab
Purpose: To investigate the processes of physical and chemical weathering.
Materials:
Sugar Cubes (5)
Shaker Bottle
Hot Water
Cold Water
Alka-seltzer
Triple Balance
Blank paper
2 Thermometers
2 250 ml Beakers
2 Stop watches
Part 1 Physical Weathering
1.) Take the mass of 5 sugar cubes together using your triple beam balance. Record
this mass in grams in the data table (attached to this sheet).
2.) Sketch a drawing of what the average sugar cube looks like in the
data table. 3.) Place the sugar cubes in the jar.
4.) Shake the jar 20 times.
5.) Pour the contents of your jar out on your blank sheet of paper. Separate the sugar
cubes and the crumbs.
6.) Take the mass of all your sugar cubes together and sketch the general appearance of
one of the sugar cubes in your data table.
7.) Repeat this four more times.
Analysis Questions
1.) Describe in detail how the sugar cubes have changed throughout the experiment.
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Physical Weathering Data Table
Shaking Trial Drawing of Sugar Cube Mass of Sugar Cubes (g) 0 Shakes
After 20 Shakes
After 40 Shakes
After 60 Shakes
After 80 Shakes
After 100 Shakes
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Part 2 Chemical Weathering
Purpose: Temperature has an effect on the rate of weathering rocks. In a hot, moist
climate chemical weathering occurs rapidly while in a cool, moist climate physical
weathering occurs faster.
1.) You will be given 2 beakers, one with hot water and the other with cold water.
2.) For a minute, take the temperature for both the hot water and cold water. Record
this in the data table.
3.) Drop an alka-seltzer tab in each of the containers. And time how long it takes each to
dissolve. 4.) Record your information in the data table (on the back of this sheet).
5.) Repeat this two more times and record all information in the data table.
Analysis
1.) How does temperature affect the rate of chemical weathering?
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Data Table
Trial Hot water temperature (Celsius)
Hot water time (seconds)
Cold water temperature (Celsius)
Cold water time (seconds)
1
2
3
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Name: Date: Period:_
Graphing Physical and Chemical Weathering
Part 1 Physical Weathering
1.) Create a line graph that demonstrates the relationship between the amount of shakes
and the masses of the sugar cubes.
2.) Label your x axis (horizontal axis) with the number of shakes (0 shakes to 100 shakes)
3.) Label your y axis (vertical axis) with possible masses of your sugar cubes (start low and
increase, provide steady increments).
4.) Draw a line graph that illustrates the change in mass of the cubes after each shake.
Draw this below:
Part 2: Chemical Weathering
1.) Create a double bar graph for the amount of time taken to dissolve the alka-seltzer in
both hot and cold water.
2.) Label the x axis with your three trials.
3.) Label the Y axis with the time (start low and increase, provide steady
increments). 4.) Draw your double bar graph on the back. See the board for
examples.
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Post Lab Questions
Directions: Answer these questions to the best of your ability. These are for a grade, do your
best. You can use your book, your notes, or your lab results for the answers. Work together with
your group to come up with the best answers.
1.) In what type of climate/biome would chemical weathering have the greatest affect on rocks
and why? (2 points)
2.) Describe in detail how weathering and erosion work together as destructive forces to
create geologic landforms. Explain what weathering and erosion are and how they work
together. Finally give a specific example of a landform they created. (4 points).
3.) Explain how ice wedging (frost wedging) and plant roots as a form of physical
weathering can damage a driveway (2 points).
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Erosion National Geographic Education
Erosion is the act in which earth is worn away, often by water, wind, or ice. A similar process,
weathering, breaks down or dissolves rock, weakening it or turning it into tiny fragments. No rock is
hard enough to resist the forces of weathering and erosion. Together, they shaped the sharp peaks of the
Himalaya Mountains in Asia and sculpted the spectacular forest of rock towers of Bryce Canyon, in the
U.S. state of Utah.
The process of erosion moves bits of rock or soil from one place to another. Most erosion is performed
by water, wind, or ice (usually in the form of a glacier). These forces carry the rocks and soil from the
places where they were weathered. If water is muddy, it is a sign that erosion is taking place. The
brown color indicates that bits of rock and soil are suspended in the water and being transported from
one place to another. This transported material is called sediment.
When wind or water slows down, or ice melts, sediment is deposited in a new location. As the sediment
builds up, it creates fertile land. River deltas are made almost entirely of sediment. Delta sediment is
eroded from the banks and bed of the river.
Erosion by Water Moving water is the major agent of erosion. Rain carries away bits of soil and slowly washes away rock
fragments. Rushing streams and rivers wear away their banks, creating larger and larger valleys. In a
span of about 5 million years, the Colorado River cut deeper and deeper into the land in what is now
the U.S. state of Arizona. It eventually formed the Grand Canyon, which is more than 1,600 meters (1
mile) deep and as much as 29 kilometers (18 miles) wide in some places.
Erosion by water changes the shape of coastlines. Waves constantly crash against shores. They pound
rocks into pebbles and reduce pebbles to sand. Water sometimes takes sand away from beaches. This
moves the coastline farther inland.
The Cape Hatteras Lighthouse was built in 1870, on the Outer Banks, a series of islands off the coast of
the U.S. state of North Carolina. At the time, the lighthouse was nearly 1,000 meters (3,300 feet) from
the ocean. Over time, however, the ocean eroded most of the beach near the lighthouse. By 1999, the
surf endangered the structure. Many people thought it would collapse during a strong storm. The
lighthouse was moved 880 meters (2,900 feet) inland.
The battering of ocean waves also erodes seaside cliffs. It sometimes bores holes that form caves.
When water breaks through the back of the cave, it creates an arch. The continual pounding of the
waves can cause the top of the arch to fall, leaving nothing but rock columns. These are called sea
stacks. All of these features make rocky beaches beautiful, but also dangerous.
Erosion by Wind Wind is also an agent of erosion. It carries dust, sand, and volcanic ash from one place to another. Wind
can sometimes blow sand into towering dunes. Some sand dunes in the Badain Jaran area of the Gobi
Desert in China reach more than 400 meters (1,300 feet) high.
In dry areas, windblown sand blasts against rock with tremendous force, slowly wearing away the soft
rock. It also polishes rocks and cliffs until they are smooth.
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Wind is responsible for the dramatic arches that give Arches National Park, in the U.S. state of Utah, its
name. Wind can also erode material until nothing remains at all. Over millions of years, wind and water
eroded an entire mountain range in central Australia. Uluru, also known as Ayers Rock, is the only
remnant of those mountains.
Erosion by Ice Ice can erode the land. In frigid areas and on some mountaintops, glaciers move slowly downhill and
across the land. As they move, they pick up everything in their path, from tiny grains of sand to huge
boulders.
The rocks carried by a glacier rub against the ground below, eroding both the ground and the rocks.
Glaciers grind up rocks and scrape away the soil. Moving glaciers gouge out basins and form steep-
sided mountain valleys.
Several times in Earth's history, vast glaciers covered parts of the Northern Hemisphere. These glacial
periods are known as ice ages. Glaciers carved much of the northern North American and European
landscape. They scoured the ground to form the bottom of what are now the Finger Lakes in the U.S.
state of New York. They also carved fjords, deep inlets along the coast of Scandinavia.
Today, in places such as Greenland and Antarctica, glaciers continue to erode the earth. These ice
sheets, sometimes more than a mile thick, carry rocks and other debris downhill toward the sea. Eroded
sediment is often visible on and around glaciers. This material is called moraine.
Erosion and People Erosion is a natural process, but human activity can make it happen more quickly. Trees and plants
hold soil in place. When people cut down forests or plow up grasses for agriculture or development, the
soil washes away or blows away more easily. Landslides become more common. Water also rushes
over exposed soil rather than soaking into it, causing flooding.
Erosion control is the process of reducing erosion by wind and water. Farmers and engineers must
regularly practice erosion control. Sometimes, engineers simply install structures to physically prevent
soil from being transported. Gabions are huge wire frames that hold boulders in place, for instance.
Gabions are often placed near cliffs. These cliffs, often near the coast, have homes, businesses, and
highways near them. When erosion by water or wind threatens to tumble the boulders toward buildings
and cars, gabions protect landowners and drivers by hold
“Erosion” is an encyclopedic entry at the National Geographic Education website. It was accessed on July 25, 2012, at this
website address:http://education.nationalgeographic.com/education/encyclopedia/erosion/kd/?ar_a=5&ar_r=3#page=1
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Guiding Question: Using evidence from the article, do weathering and erosion help people or hurt people?
Paragraph # Notes
Check relevant categories below.
can help
people
can hurt
people
no impact
on people
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Question Generation “Erosion”
http://education.nationalgeographic.com/education/encyclopedia/erosion/kd/?ar_a=5&ar_r=3#page=1
Directions: Generate additional questions that are unanswered from your text reading and based on discussion with your partner(s). Record your
questions in the chart and check the relevant category.
Paragraph # Questions
Check relevant categories below.
Impacts Florida
Scientific Fact
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Code Description
W describes where an agent is breaking apart rock (weathering)
E describes where an agent is moving rock, sediment, sand, etc.
(erosion)
+ describes when weathering and erosion are helpful to humans
- describes when weathering and erosion are harmful to humans
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3 Things I Learned Today …
2 Things I Found Interesting …
1 Question I Still Have …