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ERESE Master Document Index: |
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| Teachers Log | Back to index |
| ERESE
Teachers Log |
|
| Lesson
title |
Continental
Drift? |
| Intent
of the lesson |
What
proof do we have that the continents were, in the past, one landmass?
To instruct students in the continental drift theory. |
| Ed.
standards |
Applicable
level and state and national standards Read, construct and interpret data in various forms produced by self or others in both written and oral form. |
| Orientation |
Introduce
available tools and concepts so that students feel safe taking
intellectual risks Dectectives like to solve crimes. The students will be given four maps that they will put together , one at a time, so that they can understand continent drift. |
|
Intent |
Provide
directions to the students on cutting the continents and glueing them
on the construction paper. They will examine the first map and we
will have a questioning period. |
| Procedure | Should
include a description of any activities or lessons you include to get
the students focused on the skills they will use to experience the
provocative phenomenon Look at the edges of Africa and South America. Describe the match of the east coast of South America and the west coast of Africa. Write a testable hypothesis that can explain your observations. |
|
Type of Evidence |
Questioning.
|
|
Teacher profile |
2 What did you notice about the coast line? Why do you think they look this way? What do you think happened to make them "break apart"? |
|
Student profile |
2.5
Students should be able to answer the questions aked of them.
They should be able to make a hypothesis of what might have happened to
South America and Africa. |
| Fieldwork |
Give
students experience to foster their interest and
ownership; provoke students to explore, observe and generate their own
questions about the phenomenon Give students four maps one at a time. They consist of : map 1 -- the continents, map 2 -- the continents with the fossil remains in Africa, South America, India and Antarctica, map 3 -- the continents with the fossil remains and mountain ranges (marked 1-5) , map 4 -- the continents with fossil remains, mountain ranges, and glacial drift. |
|
Intent |
Provide
the students with the second map with data about the location of four
different fossils. These will be cut out and put on construction
paper. |
|
Procedure |
Should
include a detailed instructions, identify the provocative
phenomenon and a list of the anticipated observations This time as the students put the second puzzle together, they notice that not only do Africa and South America fit together but also India, Antarctica, and Madagascar share the same fossil remains. How did the fossils get there? Why is India connected to Africa? What could have happened to break this land area apart? What are these fossils? Are there other fossils that are found on this landmass? Are these fossils found any other place? How can Antartcica have fossils when it's so cold? |
|
Type of Evidence |
Questioning
now is from the students and not from the teacher. |
|
Teacher profile |
2
Focuses the student observations and allows for student questioning |
|
Student profile |
3
Generates the questions that they would like to discover. |
| Debriefing |
Teacher
honors all student
observations, questions and hypotheses in order to identify and discuss
their viability as a research topic. Teacher honors all student observations, questions and hypotheses in order to identify and discuss their viability as a research topic. |
|
Intent |
Facilitates
leaners in asking questions. |
|
Procedure |
Should
include detailed instructions of the process including the anticipated
hypothesis and question, along with a description of any content
lessons necessary to achieve this stage Ask student if they have any questsions about the hypotheses they have identified. |
|
Type of Evidence |
Probing
questions What do you notice about the mountain ranges? How difficult was it to match the mountain ranges? What was easier to match the fossils or the mountain ranges? Describe any differences between this model landmass and your first map. |
|
Teacher profile |
2
Provides the opportunity for the students to generate their own
questions |
|
Student profile |
3
Students will begin to generate their own questions about how the
plates move and how the continents drifted apart. Why do we only see the mountain ranges at the coasts? How can mountain ranges break apart? |
| Experimental
design |
1. The students will make observations about their first map. If the pieces fit together, why do you think they do? What would cause them to fit together? Make sure you have a key on your map and #1. 2. After the second map is put together matching the fossil remains, answer the following questions? What fossil remains was found in this area? What patterns do you see? What conclusions can you draw from this map? Make sure you have a key for your Map. 4. Put together the third map. Did you have any difficulty with this one? Why do you think you had problems with the mountain ranges? What conclusions can you draw from your map? Make sure you have a key for your map. 5. Put together the fourth map. What conclusions can you come up with for this map? Where are the glacier remains found? What is the climate in these continents today? Why do you think that the glaciers remains were not found in the northern areas? |
| Data
collection |
Define
approach for collecting data The data the students have collected is based on the evidence that scientists have collected. Here are some websites to enforce their conclusions about their maps. [Located under procedure] |
| Intent |
The
last time the students puts this map together, they have looked at the
evidence that scientists have used to give us information about earth's
past. |
|
Procedure |
Should
include detailed instructions of the process and a description of any
content lessons necessary to achieve this stage Put together the fourth map. What conclusions can you come up with for this map? Where are the glacier remains found? What is the climate in these continents today? Why do you think that the glaciers remains were not found in the northern areas? |
|
Type of Evidence |
Questioning
is now coming from the students instead of the teacher. How do scientists know this "stuff"? If this happened in the past, will it happen in the future? |
|
Teacher profile |
2
Provides for the students to generate their own questions |
|
Student profile |
3
Students will begin to generate their own questions |
| Data
analysis |
Define
approach for analyzing data As the students look at their final map, they will see that they have matched up shapes, fossils, mountain ranges, and glacial drift. When they look at that final map (their data) they will reach the conclusion that, yes, the continents were a large landmass. |
|
Intent |
Each
piece of evidence that the students were given is a little bit more of
the puzzle that scientists are trying to put together. We don't
know for sure what happened 250 million years ago but scientists are
trying to understand what did from the evidence that we find today. |
|
Procedure |
Should
include detailed instructions of the process and a description of any
content lessons necessary to achieve this stage Give the students one map at a time to put together and begin to question why scientists think it would be put together that way. The students are using many different observations as evidence to test the hypothesis that the continents were one large landmass. URL: Quick Quiz Animation Story |
|
Typre of Evidence |
The
students are shown the evidence that the scientists have to support the
idea that the supercontinent of Pangea once existed. |
|
Teacher profile |
2
Provides the opportunity of the students to generate their own questions |
|
Student profile |
3
Students will begin to generate their own questions. |
| Presentation |
Teacher
provides students an opportunity
to prepare and communicate what they have learned. Each group (lab table) will present their findings to the whole class. |
|
Intent |
The
students would be sharing their ideas of the process of putting their
maps together? What they have discovered and what else they would
like to investigate. |
|
Procedure |
Should
include detailed instructions of the process and a description of any
content lessons necessary to achieve this stage What new ideas have you discovered? What else would you like to investigate to make your understanding of the continental drift better? If you talk to a scientist that worked on this theory, what would you ask? |
|
Type of Evidence |
Since
the students have put the four maps together, they have seen that the
Earth is not always the same and these changes have occured over
millions of years. |
|
Teacher profile |
2
Provides the opportunity of the students to share their invetigation
and generate their own questions |
|
Student profile |
3
Students will begin to generate their own questions. |
| CP0001 Expedition - Cruise Planning | Back to index |
| M00001 Simple Seafloor Spreading (Reykjanes Ridge) | Back to index |
| Standard | Subject | ||||||
| M00001 | Simple Seafloor Spreading | ||||||
| General Metadata | |||||||
| magnetic
anomalies, seafloor spreading, magnetic stripes, magnetism, magnetic
anomaly, mid-ocean ridge |
|||||||
| Level (L) | Images (I) | Data (D) | Text (T) | ||||
| 1-2 (Elementary) |
Photograph of bar magnet and nearby iron filings | Index Page | |||||
| 3 (Middle School) |
Magnetic Seafloor and Deeper Reversals | Table 1: Le Pichon 1968 | Index Page | Definition of Mid-Ocean Ridge | Index Page | ||
| 4 (High School) |
Age of the Seafloor Along Reykjanes Ridge | Index Page | Cross-Section Formation of Magnetic Anomalies with Geologic Timescale | Index Page | Definition of Seafloor Spreading | Index Page | |
| 5 (College) |
Magnetic Polarities Along Reykjanes Ridge | Index Page | Magnetic Poloraity and Ocean Depth Versus Longitude Along the Reykjanes Ridge | Index Page | Abstract-Heirtzler et al 1966 | Index Page | |
| 6-9 (Graduate & Research) |
Figure 1: Heirtzler et al 1966 | Index Page | Figure 2-Heirtzler et al 1966 | Index Page | Abstract-Heirtzler et al 1966 | Index Page | |
| M00002 Complex Seafloor Spreading | Back to index |
| Standard | Subject | ||||||
| M00002 | Complex Seafloor Spreading | ||||||
| General Metadata | |||||||
| magnetic
anomalies, seafloor spreading, magnetic stripes, |
|||||||
| Level (L) | Images (I) | Data (D) | Text (T) | ||||
| 1-2 (Elementary) |
Seafloor Spreading Animation | Index Page | |||||
| 3 (Middle School) |
Magnetic Particles in Oceanic Sediment | Index Page | Cross-Section Formation of Magnetic Anomalies with Geologic Timescale | Index Page | Text 01 from Vine 1966 | Text 01 from Vine 1966 | |
| 4 (High School) |
Magnetic Anomalies Off the Coast of the Pacific Northwest | Index Page | Geomagnetic-Polarity Epochs and Respective Age of Seafloor | Index Page | Text 04 from Vine 1966 | Text 04 from Vine 1966 | |
| Magnetic Anomalies and the Sea-floor Spreading Rate | Index Page | ||||||
| 5 (College) |
Figure 1-Vine 1966 (Raff & Mason) | Index Page | Table 1. Mid-Ocean Ridge Data Table (Wilson) | Index Page | Chapter 2 Mason - Oreskes | Chapter 2 Mason - Oreskes | |
| Multiple Maps of Diverging Plate Boundary and Cruise Paths | Index Page | Magnetic Profile and Map of Spreading Center | Index Page | ||||
| 6-9 (Graduate & Research) |
Magnetic Anomaly Data for Multiple Seafloor Locations | Index Page | Magnetic Anomlay Data from Multiple Seafloor Locations | Index Page | Chapter 3 Vine - Oreskes | Chapter 3 Vine - Oreskes | |
| Map of Diverging Plate Boundary and Cruise Path | Index Page | Magnetic Profiles and Map of Diverging Plate Boundary | Index Page | ||||
| M00006 Magnetic Reversals | Back to index |
| Standard | Subject | ||||||
| M00006 | Magnetic Reversals | ||||||
| General Metadata | |||||||
| magnetic field reversals, geomagnetic field reversals | |||||||
| Level (L) | Images (I) | Data (D) | Text (T) | ||||
| 1-2 (Elementary) |
Magnetic Reversal Video Along a Spreading Center | Index Page | Magnetic Rock Sample Polarity Data Table | Index Page | Definition of Magnetic Reversal - Elementary School | Index Page | |
| 3 (Middle School) |
Figure of a Normal and Reversed Magnetic Field | Index Page | Magnetic Reversal Data and Timescale | Index Page | Definition of Magnetic Reversal - Middle School | Index Page | |
| 4 (High School) |
Direction of Changing Magnetic Poles based on Basalt Samples in Japan | Index Page | Magnetic Reversal Data Table | Index Page | |||
| Magnetic Profiles | Index Page | ||||||
| 5 (College) |
Magnetic Field Reversal Video | Index Page | Magnetic Profile Data Across the East Pacific Rise | Index Page | |||
| 6-9 (Graduate & Research) |
Magnetic Reversals Based on Dipole and Nondipole Field Strength | Index Page | Paleomagnetic Data of Field Intensity and Polarity | Index Page | Chapter 6 - Oreskes: Morley | Chapter 6 - Oreskes: Morley | |
| M00008 Seamounts | Back to index |
| Standard | Subject | ||||||
| M00008 | Seamounts | ||||||
| General Metadata | |||||||
| Level (L) | Images (I) | Data (D) | Text (T) | ||||
| 1-2 (Elementary) |
|||||||
| 3 (Middle School) |
|||||||
| 4 (High School) |
Bathymetric map of the Magellan Seamount Trail including Vlinder Morphology Analysis | Index Page | |||||
| Bathymetry of the Magellan Seamount Trail | Index Page | ||||||
| Ralik and Ratak Seamount Trails | Index Page | ||||||
| 5 (College) |
Map of West Pacific Seamount Province | Index Page | |||||
| Map of the Japanese Seamount Trail | Index Page | ||||||
| WPSP Seamount Trails | Index Page | ||||||
| 6-9 (Graduate & Research) |
West Pacific Seamount Province and the Japanese Seamounts | Index Page | |||||
| Northern and Southern Wake Seamount Trails | Index Page | ||||||
| Euler Pole derivation | Index Page | ||||||
| M00013 Tectonic Plates | Back to index |
| Standard | Subject | ||||||
| M00013 | Tectonic Plates | ||||||
| General Metadata | |||||||
| plate tectonics, tectonic plates, crustal blocks, lithospheric plates | |||||||
| Level (L) | Images (I) | Data (D) | Text (T) | ||||
| 1-2 (Elementary) |
The Earth's Layers | Index Page | Plate Tectonics and Volcanoes | Index Page | Definition of Lithospheric Plates and Plate Tectonics | Index Page | |
| 3 (Middle School) |
The Major Tectonic Plates of the World | Index Page | Map of Tectonic Plates and Their Movement | Index Page | Fill-in-the-Blank Plate Tectonic Exercise | Index Page | |
| 4 (High School) |
Map of the North American Plate and the Eurasian Plate Diverging Over Iceland | Index Page | Geology of Africa and South America | Index Page | |||
| 5 (College) |
Diagram Illustrating Components of Plate Tectonics | Index Page | Movement between Tectonic Plates (Table 5) | Index Page | Chpt 1. -- Oreskes | Index Page | |
| 6-9 (Graduate & Research) |
Rates of Plate Rotation (Table 4) | Index Page | Abstract -- Morgan | Abstract -- Morgan | |||
| M00016 Convergent Boundaries | Back to index |
| Standard | Subject | ||||||
| M00016 | Convergent Plate Boundaries | ||||||
| General Metadata | |||||||
| Level (L) | Images (I) | Data (D) | Text (T) | ||||
| 1-2 (Elementary) |
The Eurasian Plate and Indian Plate Converging to Create the Himalayas | Index Page | |||||
| 3 (Middle School) |
Subduction Zone | Index Page | Relationship of Temperature and Earthquakes in a Downgoing Slab | Index Page | |||
| 4 (High School) |
The Collision of Two Continents | Index Page | Temperature Distribution in a Sinking Lithospheric Plate Compared to Surrounding Mantle | Index Page | Converging Plate Boundaries | Index | |
| Global image of the Pacific Margins | Index Page | ||||||
| 5 (College) |
|||||||
| 6-9 (Graduate & Research) |
|||||||
| M00017 Divergent Boundaries | Back to index |
| Standard | Subject | ||||||
| M00017 | Divergent Plate Boundaries | ||||||
| General Metadata | |||||||
| divergent plate boundary, spreading center | |||||||
| Level (L) | Images (I) | Data (D) | Text (T) | ||||
| 1-2 (Elementary) |
Simple Figure for a Divergent Boundary | Index Page | Simple Definition of Divergent Plate Boundaries | Index Page | |||
| 3 (Middle School) |
Image of a Divergent Boundary | Index Page | Heat Level Data Over Divergent Boundary | Index Page | Definition of Divergent Plate Margins - Middle School | Index Page | |
| 4 (High School) |
Divergent Boundary Between Two Continents | Index Page | Gravity Data Over Oceanic Ridge | Index Page | |||
| 5 (College) |
Topographic Map of a Divergent Plate Boundary | Index Page | |||||
| 6-9 (Graduate & Research) |
|||||||
| M00018 Strike Slip Boundaries | Back to index |
| Standard | Subject | ||||||
| M00018 | Strike-Slip Plate Boundaries | ||||||
| General Metadata | |||||||
transform faults, strike-slip faults |
|||||||
| Level (L) | Images (I) | Data (D) | Text (T) | ||||
| 1-2 (Elementary) |
3-D Image with Arrow Plate Motion | Index Page | |||||
| 3 (Middle School) |
Transform fault at Mid-Ocean Ridge vs. Seafloor Age | Index Page | Definition of Transform Fault | Index Page | |||
| 4 (High School) |
Fig. 1-Wilson 1965: Transform and Transcurrent Faults | Index Page | Text 01-Wilson
1965: Definition of Transform and Transcurrent Faults |
Text 01-Wilson
1965: Definition of Transform and Transcurrent Faults *need to scan & archive* |
|||
| 5 (College) |
Mendocino Transform Fault | Index Page | |||||
| 6-9 (Graduate & Research) |
Fig.3-Wilson 1965: Juan de Fuca Ridge and related faults | Index Page | Table 1-Wilson 1965: Location of points on Figure 3 | Index Page | |||
2004-07-19 09:15 AM