Saturday, April 28, 2012

Making an Impact

Arizona's Meteor Crater
Looking around our solar system, we see evidence of impactors that have cratered the landscapes of Mars, Mercury, our Moon, and even planet Earth. What are the characteristics of impact craters and how are they formed? Using classroom models and simulations, we can investigate the factors the affect impact craters.

One of the best ways to begin a discussion of craters is by dissecting an image of a crater. Arizona's Meteor Crater provides a launching point for a study of craters and the impactors that formed them.

  • How big is this crater? How wide? How deep? What evidence for scale do we see in the image?
  • What are some physical features of this crater? (raised rim, steep walls, ejected material, central uplift)
  • How big was the impactor?
  • How fast was the impactor traveling?
  • At what angle did the impactor hit?
  • When did the impact happen?
  • Where is the impactor?
  • Why is this crater so well preserved?

From a discussion of these questions, we can begin to formulate research questions about the factors that affect impact craters:

  • How does the diameter of an impactor affect the diameter and depth of a crater?
  • How does the mass of an impactor affect the diameter and depth of a crater?
  • How does the speed of an impactor affect the diameter and depth of a crater?
  • How does the angle of an impactor affect the diameter and depth of a crater?

Impact Craters Lab
From our research questions, we can begin to plan our experiment. The lab investigation we conduct is modeled after an activity designed by NASA, outlined in their Exploring the Moon Educator Guide. Materials needed for this lab activity include Moon material (sand), impactors (marbles and golf balls), pans, balances, and metric rulers. Students test their hypotheses under controlled conditions in an attempt to better understand how an impact crater, such as the one in Arizona, could have formed and the energy involved in the impact.

Why is it important for us to understand craters? A study of geologic history reminds us that Earth has been hit by many impactors in the past. The largest of these impactors have repeatedly reset the evolutionary clock on our planet—mass extinctions of species such as dinosaurs are the result of planetary bombardment by rocks from space. It is only a matter of time before the next impactor threatens Earth.

If a large impactor is headed our way, is there anything we can do about it? While Hollywood-style scenarios involving nuclear missiles, massive explosions, and Bruce Willis single-handedly saving the day are exciting on the big screen, these solution just don't work out mathematically in real life (sorry…). For us to be prepared for a large impactor is a two-step process. We must first catalog the threat by surveying the skies around us and accurately tracking potential impactors. NASA and other organizations have begun to do this, but have not yet found everything—it is a massive undertaking. Second, we must be prepared not to simply blow an object out of space, but to gently finesse it into an orbit that harmlessly bypasses our planet. While the Hollywood excitement level is not as high, the chances for success (and the survival of our species) are much improved.

Universe Today has an excellent analysis of the many ways to deflect an asteroid, and Bad Astronomer Phil Plait explains the process of nudging a space rock out of our way should it come to pass close by. Additionally, there are multiple online resources for simulating impacts, including the Impact Calculator and Impact Earth.

Finally, while impacts have altered the landscapes of countless objects in our solar system and have changed the course of evolutionary history on planet Earth numerous times, they have also had one major positive side effect: the next time you look up in the sky and see the beautiful Moon, be awed by the massive impact between Earth and another long-gone planet-sized body that led to the Moon's formation some 4 billion years ago. Goodnight, Moon!

Sunday, April 22, 2012

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