Sunday, April 15, 2012

Questions about the Moon

It was a simple query: "What questions do you have about the Moon?" A group of savvy and intelligent 8th graders (my students) pondered this question and came up with the following comprehensive list:
NASA: A New Map of the Moon

Physical Characteristics and Features
  • How big is the Moon compared to the Earth?
  • What is the diameter of the Moon?
  • What is the Moon’s mass?
  • Is the Moon smaller than Pluto?
  • Why is the Moon a sphere?
  • How far away is the Moon?
  • Why are there craters on the Moon?
  • How do craters on the Moon form?
  • What is the largest crater on the Moon?
  • Why is the Moon gray/white?
  • What is the Moon’s temperature?
  • What is the temperature difference between light and dark sides of the Moon?
  • Does the Moon have a moon?
  • Does the Moon have an atmosphere?
  • What is the Moon’s atmosphere like?
  • Is there oxygen on the Moon?
  • Why isn’t there oxygen on the Moon?
  • Does the Moon have weather?
  • Does the Moon have wind?
  • How much gravity is on the Moon?
  • Does the Moon have a magnetic field?
  • How strong is the Moon’s magnetic field?
  • How high can you jump on the Moon?
  • Can you make a fire on the Moon?
  • Can you cook on the Moon?


Orbital Data
  • Does the Moon rotate?
  • How long does it take for the Moon to rotate?
  • Does the Moon revolve around the Earth?
  • How long does it take for the Moon to revolve around Earth?
  • Why does the Moon orbit the Earth?
  • Why do we only see one side of the Moon?
  • Why are there phases of the Moon?


Lunar Composition
  • What is inside the Moon?
  • What is the Moon made of?
  • What type of rock is the Moon made of?
  • Does the Moon have layers like the Earth?
  • How many layers does the Moon have?
  • What’s in the Moon’s core?
  • Is the core of the Moon the same as the core of the Earth?
  • Does the Moon have landforms?
  • Does the Moon have natural disasters (like, earthquakes, etc.)?
  • Are there any fossils on the Moon?
  • Is there life on the Moon?
  • Does the Moon have water?
  • Does the Moon have tectonic plates?
  • Does the Moon have earthquakes?
  • Is there lava on the Moon?
  • How old is the Moon?


Lunar Formation
  • How was the Moon formed?
  • How did the Moon get there?
  • How has the Moon changed over time?


Lunar Exploration
  • How many people have landed on the Moon?
  • Who else landed on the Moon?
  • How many missions have we had to the Moon?
  • How long does it take to get to the Moon?
  • How much fuel does it take to visit the Moon?
  • Where are the flags on the Moon?
  • What have we accomplished by landing on the Moon?
  • When did we first discover the Moon?
  • Who hit the golf ball on the Moon?
  • Will the Moon have livable conditions on the future?


Philosophical Questions
  • What is the Moon’s purpose?
  • What if we had no Moon?
  • Who owns the Moon?
  • Why is it called “Moon”?



Question for educators, boards of education, policy makers, textbook publishers, et al.:
  • Do your standards, curriculum, and educational materials reflect the innate curiosity and learning desires of our students?

Saturday, April 7, 2012

Plate Tectonics — Putting It All Together

Why does the Earth's surface look the way it does? Why do Africa and South America look like they could fit together, like pieces of a puzzle? How could these pieces fit together? How do we know? What evidence do we have?
Earth's Tectonic Plates

One hundred years ago, plate tectonics was more of a crazy idea than a rock-solid scientific theory that explains why the Earth's surface looks the way it does. Helping students navigate how the theory was assembled bit-by-bit exposes them to both a deeper understanding of geology as well as the oft-messy nature of science itself. Theories are not always well-received when first proposed, and overwhelming evidence is needed for a fanciful idea to become a scientific theory. This is how science works.

In the classroom, we engage in a plate tectonics research map project to better understand how all of the geologic puzzle pieces fit together to complete the plate tectonics picture. Using primary and secondary internet resources, maps, posters, textbooks, and other artifacts, students add layer upon layer of geologic data and evidence onto a world map to see the patterns and mechanisms which work together in plate tectonics theory. In three to five days, students build evidence for the grand theory of geology that took more than half a century to initially develop. On the shoulders of giants we stand...

In the research project, students use the following websites to gain background knowledge about the scientific theory of plate tectonics and gather data for their world maps:
Using these websites and other resources, students layer the following data and information onto a world map:
  • prevalent earthquakes and volcanoes
  • hot spots
  • mid ocean ridges
  • ocean trenches
  • plate boundaries with their direction of movement
  • plate names
Additionally, students are asked to illustrate the three major types of plate boundaries and how they work as well as assemble a Pangaea puzzle onto the back of their map. Finally, students are asked to explain in their own words what the scientific theory of plate tectonics is, how it works, and what evidence we have to support the theory. Along the way, students discover the story of Alfred Wegener—who first proposed the plate tectonics idea—and how he struggled and persevered throughout his short life to develop his ideas (which we fully accept today).

Sunday, March 25, 2012

Saturday, March 17, 2012

Earth System Science Project

Image courtesy of Microsoft Clipart
I've been pondering the idea of a comprehensive, collaborative science project in which students piece together all of the elements of the Earth system. I envision a giant interconnected, interdependent collage/infographic that weaves the myriad perspectives, voices, and creative talents of my students into one vision of what Earth science is all about...

Hear are a few broad guidelines and parameters for the project:

The Earth system is characterized by interactions among the following components:
  • atmosphere—the gaseous envelope surrounding Earth
  • hydrosphere—the liquid and ice water portions of Earth 
  • lithosphere (geosphere)—the solid portion of Earth
  • biosphere—the living portion of Earth

Matter and energy cycle among the living and nonliving components of the Earth system via different pathways and over varying amounts of time:
  • weather cycle and atmospheric circulation
  • climate cycle
  • carbon cycle
  • Earth’s energy budget
  • water cycle and oceanic circulation
  • rock cycle
  • weathering, erosion, and deposition
  • fossils and geologic time
  • plate tectonics
  • astronomical factors

Students will create the ultimate, illustrated Earth system mural/diagram showing:
  • the different components of the Earth system
  • the cycling of matter and energy throughout the Earth system
  • macro to micro interconnections among cycles of the Earth system
  • temporal/spatial fluxes across the Earth system
  • the contributions that people in different cultures and at different times in history have made to advance our understanding of the Earth system

Of course, one of the largest challenges is orchestrating such a project. I'm still puzzling over that part—maybe it could look like a giant puzzle...

Saturday, March 10, 2012

Reflections — Fossils 3

In 2010, I was nominated for the Presidential Award for Excellence in Math and Science Teaching—a prestigious honor for math and science teachers in the United States. The rigorous application process provided me with an excellent opportunity to reflect deeply on my classroom practice. Although I was not selected as a finalist, I value my experience in the process. Over the next three blog posts, I would like to share some of what I wrote for my application, which centered around a geologic unit on fossils.

The PAEMST application requires a written narrative on several dimensions of outstanding teaching, including the following areas:

  • Dimension 1: Mastery of Science Content
  • Dimension 2: Instructional Methods and Strategies
  • Dimension 3: Effective Use of Student Assessments

In this entry, I would like to share Dimension 3, Effective Use of Student Assessments...



I effectively use student assessments to evaluate, monitor, and improve student learning... 

Image courtesy of MorgueFile
Recall the essential learning questions for this project: 
  • What are fossils? 
  • How do fossils form? 
  • What can fossils tell us about past life? 

For this project, students are assessed on the quality and depth of information communicated on their individual fossil ID cards. Specifically, each student is assessed on the following essential learning skills: 
  • collecting detailed information from fossil “interviews;” 
  • inferring geologic, environmental, and biological change through time based on fossil evidence; 
  • interpreting rocks and their fossil content to determine past conditions; 
  • describing how fossil evidence can be linked to environmental conditions and biological adaptations of the past.

Over the years, I have refined the “interview” questions to help students maximize their interpretation of clues. The questions have gotten more detailed and specific to better help students uncover the fossil’s life story. What originally began as an exercise in basic fossil identification many years ago has become a quest to understand the life story of a fossil through careful interpretation of evidence—asking essential questions to gain enduring understandings.



I routinely assess and guide student learning... 

One-on-one discussions: These are individual conversations with students where I ask clarifying questions, ask students to explain their thinking to me, or have students show me a particular science skill. Emphasis is placed on meaningful responses that answer “how” and “why” rather than simply “who, what, when, where.” Example: “Tell me your thinking about… or, Show me how you did… or, What did you observe when…? or, What is your evidence for…?”

Table discussions: Usually conducted at the beginning of class, I ask students to discuss a particular topic or question among their table peers while I walk around listening to (or sometimes joining in with) their conversations. The purpose is to promote peer collaboration as well as check for understanding and/or misconceptions. Example: “With your table group, have a two-minute discussion: What do you think are some physical characteristics that all minerals have in common?”

Lab table talk: As students are working on a lab investigation, I circulate throughout the room and visit each table regularly. I ask clarifying questions as needed and ask students to share what they are doing and thinking. I listen and look for evidence of the science process: 

  • setting up safe, controlled laboratory experiments; 
  • recording detailed observations; making precise measurements; 
  • collecting high quality data; discussing observations and evidence; 
  • and analyzing results. 

Lab investigations: At the end of a lab investigation, I will often collect and grade my students’ lab reports to assess their learning. Many of my investigations use an Experiment Planning Guide, which helps students organize and formalize the process of science. I evaluate these planning guides according to the quality and completeness of scientific writing and thinking, particularly whether students can connect their observations, data, and written conclusions to the original learning goal or research question. Example: “An excellent conclusion restates the original purpose (the research question) and summarizes the results of the experiment in a logical, concise manner. An excellent conclusion also includes supporting details and evidence from the data. An excellent conclusion does not speculate on the unknown...”

Quizzes: During each major unit of study, I give one or two quizzes to further evaluate student mastery of science concepts and learning goals. These quizzes ask students to apply what they have learned during the course of a few interconnected lessons and usually involve short written response, data analysis and interpretation, and/or short performance task. Students may use their lab notes and resources during these quizzes, as I feel that using resources is an essential aspect of the scientific process. Example: “Identify two of the minerals from the mineral collection on the front lab table and fully describe the three convincing properties that led you to your identification.”

Projects: Students engage in longer lab investigations (e.g., fossil identification lab) or projects (e.g., physical oceanography research project) once or twice a trimester. I evaluate these projects against holistic “standards of excellence” that clearly define the criteria necessary for excellent learning.




References

Saturday, March 3, 2012

Reflections — Fossils 2

In 2010, I was nominated for the Presidential Award for Excellence in Math and Science Teaching—a prestigious honor for math and science teachers in the United States. The rigorous application process provided me with an excellent opportunity to reflect deeply on my classroom practice. Although I was not selected as a finalist, I value my experience in the process. Over the next three blog posts, I would like to share some of what I wrote for my application, which centered around a geologic unit on fossils.

The PAEMST application requires a written narrative on several dimensions of outstanding teaching, including the following areas:

  • Dimension 1: Mastery of Science Content
  • Dimension 2: Instructional Methods and Strategies
  • Dimension 3: Effective Use of Student Assessments

In this entry, I would like to share Dimension 2, Instructional Methods and Strategies...



I employ a variety of instructional approaches to help students understand fossils...

Rock cycle video and diagram
Students watch a locally-produced video about the Rock Cycle, which identifies the three main rock families, explains how they were formed, and shows many local examples from each family. Students collaborate after the video to complete a blank rock cycle diagram with terms about rock products and the geologic processes that created them.

Rock identification lab
Students engage in a hands-on process of rock identification to learn the various physical properties and characteristics involved in identifying rocks by family and name. As part of the identification process, students must provide convincing evidence to go along with their identification.

Law of Superposition activity
Students infer the relative ages of rock layers in a vertical rock profile by examining and discussing various clues. They discover that, in general, the oldest rocks and rock layers are at the bottom of a rock profile—the Law of Superposition.

Traces of Tracks activity
Students analyze an image of fossilized animal tracks and reconstruct the story of an encounter between predator and prey. Students collaborate to infer the story from the trace fossil evidence.

Finding Clues to Rock Layers activity
Students analyze fossil clues and data contained in rock layers to determine the relative ages of the layers as well as the physical environment in which the organisms lived. In general, the deeper the rock layer the older the fossils buried within. Additionally, various geologic processes, such as weathering and erosion, can expose fossil layers at the Earth’s surface. 

Fossil ID Cards
Over the course of several days, students “interview” various fossils to infer the life story of once-living, but now fossilized, organisms, and create a detailed fossil identification card for each fossil interviewed. This hands-on, inquiry-based lab allows students to fully engage in the process of science by observing fossil specimens; asking key questions; gathering evidence from physical clues and inference; using a variety of scientific resources such as fossil identification books, posters, and diagrams; learning to avoid bias by following the fossil evidence; sharing data and ideas through peer collaboration; and hypothesizing and theorizing about the past geologic environments in which the fossil lived. Students display their fossil cards on large posters for the rest of the school to enjoy. 

Examples of interview questions include:

  • What are the fossil’s physical characteristics? 
  • How did this fossil move? 
  • What did it eat? 
  • In what environment or habitat did this fossil live? 
  • What was its niche or purpose in life?



I identify and build on students’ prior knowledge, and incorporate this knowledge in my general teaching strategies...

Image courtesy of MorgueFile
I strive to ensure that my science lessons build logically from point A to point B and that common themes and ideas are continuously woven throughout each unit as well as throughout the school year. My goal is to promote the transfer of understanding from one lesson to another, not just one-time memorization to be forgotten quickly. I regularly ask discussion questions that help activate prior knowledge, that tie different lessons together, and that help students make logical interconnections among various ideas and concepts.
  • “Does anybody have a fossil collection? Tell us a little bit about your fossils.”
  • “Have you ever been to a museum and seen a fossil dinosaur on display? Where did all those bones come from?”
  • “Remember when we watched the rock cycle video? In which rock family would you most likely expect to find fossils? Why?”
  • “You can find fossil sea shells up in the Rocky Mountains. How can that be? What do these fossils tell us about Earth history?”
  • “Suppose you find a fossil of an X. What story can this fossil tell you? What are some clues you can look for to help explain this organism’s life?”
  • “Here is an example fossil. What characteristics do you see? What kind of organism was this? What did it eat? Where did it live? How do you know?”
In the video I produced for my application, I used many of the types of questions outlined above to help students learn how to interview fossils in order to uncover their life story. My goal was for students to develop a non-biased technique for uncovering clues and evidence contained in fossils. For our fossil lessons, it is most important that students learn to “listen” to the fossil evidence with an open mind rather than just try to quickly name the fossil.

The video shows the first day of our fossil lessons, where we worked together as a group to prepare for our in-depth fossil interviews. The following three days after the video, students interviewed fossils, gathered information and evidence from the fossils and various classroom resources, and created detailed fossil identification cards with the inferred life story of each fossil.



I use instructional strategies and techniques to meet the learning needs of all students, challenging those with stronger knowledge while ensuring learning for less accomplished students...

I utilize a variety of strategies to differentiate for the diverse learning needs of my students, and a few of these are outlined below:
  • Creating hands-on, inquiry-based, authentic learning experiences that encourage students to think critically and develop explanations based on evidence
  • Encouraging peer collaboration: students working together, talking science together, sharing data and ideas together
  • Accommodating for different fossil identification skill levels: 
  • Inferring basic to advanced information from fossil clues at increasing levels of descriptive detail
  • Interpreting fossil structures from simple (bones, teeth, shells) to complex (type of bone, purpose of tooth)
  • Working with incomplete vs. complete fossils (incomplete fossils are much more challenging to interpret than complete fossils)
  • Drawing upon multiple intelligences skills and multiple learning modalities: drawing/visualization, writing, questioning, spatial manipulation, kinesthetic/hands-on observations
  • Using effective questioning: engaging students (individually and within small lab table groups) with highly effective questions to encourage deeper meaning




References

Saturday, February 25, 2012

Reflections — Fossils 1


In 2010, I was nominated for the Presidential Award for Excellence in Math and Science Teaching—a prestigious honor for math and science teachers in the United States. The rigorous application process provided me with an excellent opportunity to reflect deeply on my classroom practice. Although I was not selected as a finalist, I value my experience in the process. Over the next three blog posts, I would like to share some of what I wrote for my application, which centered around a geologic unit on fossils.

The PAEMST application requires a written narrative on several dimensions of outstanding teaching, including the following areas:

  • Dimension 1: Mastery of Science Content
  • Dimension 2: Instructional Methods and Strategies
  • Dimension 3: Effective Use of Student Assessments

In this entry, I would like to share Dimension 1, Mastery of Science Content...



There are three essential questions to guide the study of fossils:
  1. What are fossils? 
  2. How do fossils form? 
  3. What can fossils tell us about past life? 
Planet Earth is billions of years old, and during its long history a diversity of life has evolved. Fossils are the remains of living organisms preserved in the geologic record through burial, and they provide valuable evidence for this long Earth history. Students need fundamental understanding of the geologic processes that led to fossil formation, the types of fossils that form as a result, and the types of clues that are found within the fossils that can be used to interpret past history.
Image courtesy of MorgueFile

Three main types of fossils—body, trace, and replacement—form over time periods of thousands to millions of years. Each type of fossil has unique physical characteristics and clues to help us infer past Earth history. Because fossils are found mainly within sedimentary rocks, it is essential that students understand the constructive and destructive processes involved in sedimentary rock formation, which ultimately lead to the preservation of once-living organisms.

Information about the environments in which fossilized organisms lived can be inferred from fossil clues when students rigorously apply the process of science. Making careful, detailed observations using different scientific tools (such as hand lenses and microscopes), asking a variety of probing “interview” questions about each fossil, referencing fossil identification guides and charts, and collaborating with other student scientists are all key to interpreting fossil clues in a non-biased, open-minded manner to unlock the information about their past environments.

Fossil evidence helps us infer geologic, environmental, and biological changes through time. By examining fossils and reconstructing the story they tell, students fine tune their “process of science” skills and develop a better understanding of the 3.5+ billion-year life history of planet Earth. Specifically, students engage in making detailed observations of fossils and asking questions in order to infer information about the geologic past.Students will apply what they learned during fossil identification to a future plate tectonics research project. The skills and knowledge developed in this lesson will be applied to understanding spatial and temporal changes of Earth’s tectonic plates—fossil evidence gives us clues that Earth’s crustal plates move and that continents were once connected.

This particular lesson on fossils contributes to the “Six Facets of Understanding”—a lesson planning tool I use to develop deep, engaging learning activities—as outlined below: 
  • Explanation: Students address the following conceptual questions: 1) What are fossils? 2) What the different types of fossils? 3) How do fossils form? 4) How can we infer information about past environments from examining fossils?
  • Interpretation: Students observe and “interview” fossils to determine the physical characteristics of organisms and infer the past environment in which they lived.
  • Perspective: Students make connections between life and conditions on planet Earth today and life and conditions during geologic eras and periods of the past.
  • Self-Knowledge: Students may inquire about or begin to assemble their own fossil collection, or seek opportunities to learn more about fossils (for example, museum visits).
  • Empathy: Students consider why geologists study fossils and develop a better understanding about the difficulties involved in fossil interpretation and reconstruction.
  • Application: Students engage as fossil scientists and create their own fossil identification cards that show physical characteristics and inferred information about past environments.


A variety of misconceptions and misunderstandings about fossils can arise in the science classroom. Here is a summary:

All rocks contain fossils.
Fossils are found mainly in sedimentary rocks. For an organism to become a fossil, a protective layer of sediment, such as sand or mud, must quickly cover up its remains. Otherwise, the remains are likely to be eaten, to decompose, or to be destroyed before fossilization can occur. Probing questions to ask students: 
  • Why don’t we find fossils inside rocks like granite, basalt, gneiss, or schist?
  • Why do we find fossils inside rocks like sandstone, shale, and slate?
Fossils are actual pieces of dead animals and plants, rather than preserved impressions of the original organisms. 
During the fossilization process, the living remains of organisms decay and are replaced by minerals, leaving behind an impression of the original organism. Exceptions to this include insects that are fully preserved in fossilized tree sap (amber). However, most organisms are preserved in an altered state during the fossilization process. Probing questions to ask students: 
  • Petrified wood, a fossil, is not wood anymore. What happened to the wood?
  • If you have a fossil shell or leaf imprint, what happened to the original organism?
All living organisms leave behind fossils, and the fossil record is complete. 
Hard structures such as bones, teeth, shells, and exoskeletons are more likely to be preserved during the fossilization process than soft body materials such as tissues, organs, and/or hair/feathers, which decay more readily. It is estimated that only 1% to 3% of organisms have fossilized and/or been described. While our fossil record keeps growing as we explore more and more of Earth’s crust, we will never have a 100% fossil record because not all species leave behind fossils and not all fossils can ever be found or recovered. Probing questions to ask students: 
  • Why do scientists keep looking for fossils, even today?
  • Why don’t we find fully preserved, fully intact organisms (like dinosaurs) buried in the ground? Why do we usually just find skeletons, bones, teeth, etc.?
  • When an organism dies, what parts decay and what parts are preserved, and why? 
Geologic time is short, and fossils are relatively young. 
Geologic time is vast. The fossilization process, which occurs during the sedimentary rock formation process, can take thousands and millions of years to occur. Various dating techniques allow scientists to accurately determine the ages of rocks and fossils. Fossils are thousands, millions, and in some cases, billions of years old. Probing questions to ask students: 
  • How do you think fossilized seashells got to the top of the Rocky Mountains?
  • What does finding fossilized seashells in the Rocky Mountains tell us about the past?
Few species have gone extinct during Earth’s history. 
More than 99% of all species (which number in the millions) that ever lived on planet Earth have gone extinct. The fossil record leaves us evidence of species that are no longer alive and what the environments in which they lived were like. Probing questions to ask students: 
  • Have you ever seen an organism like this (show pictures of extinct organisms)?
  • What happened to these organisms?


References