LIVE INTERACTIVE LEARNING @ YOUR DESKTOPNSDL/NSTA Web SeminarBeyond Penguins and Polar Bears: IntegratingScience and Literacy in the K-5 Classroom-Physical Science from the PolesWednesday, October 29, 20086:30 p.m. to 8:00 p.m. Eastern time
Agenda:1. Introductions2. Tech-help info3. Web Seminar tools4. Presentation5. Evaluation6. Chat with the presentershttp://nsdl.org
Supporting the NSDLPresenting Team is For additional Tech-helpcall:Elluminate Support,1-866-388-8674 (Option 2)http://nsdl.orgJeff LaymanTech SupportNSTAjlayman@nsta.org703-312-9384
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How many NSTA webseminars have you attended?A. 1-3B. 4-5C. More than 5D. More than 10E. This is my first web seminarUse the letters A-E located atthe top left of your actualscreen to answer the poll
How many NSTA web seminarshave you attended?A. 1-3B. 4-5C. More than 5D. More than 10E. This is my first NSTAweb seminar
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What grade level do youteach?A. Elementary School, K-5.B. Middle School, 6-8.C. High School, 9-12.D. I teach college students.E. I am an Informal Educator.http://nsdl.org
LIVE INTERACTIVE LEARNING @ YOUR DESKTOPNSDL/NSTA Web SeminarBeyond Penguins and Polar Bears: IntegratingScience and Literacy in the K-5 Classroom-Physical Science from the PolesWednesday, October 29, 2008
Today’s NSDL ExpertsJessica Fries-Gaither, Beyond Penguins andPolar Bears Project Director and ElementaryResource Specialist, Ohio State UniversityDr. Carol Landis, Education OutreachSpecialist, Byrd Polar Research Center,Ohio State l.org
Overview of Presentation1.Physical properties of ice2.Geography of ice3.Teaching strategies and K-5 resourcesfrom Beyond Penguins and Polar Bearshttp://nsdl.org
http://beyondpenguins.nsdl.orgToday’s presentation: Featuring materialrelated to Issue 5: Water, Ice, and Snow,August 2008http://nsdl.org
States of matter: Solid, Liquid, GasPhoto by Chris Linder,Woods Hole Oceanographic Institutionhttp://nsdl.orgPhoto by C. Landis,Byrd Polar Research Center
Change in state (or phase) of waterAddition or loss of heat is required tochange from one state to another.boilingGasTemperature 1006/Fall00 night/H20 heating curve.JPGhttp://nsdl.org
States of matterStamp your answers.A change of state does not mean a change in mass.TrueFalseSolids can only melt with heat.Truehttp://nsdl.orgFalse
Misconceptions:States and Changes of MatterFormative Assessment: Massconservation“Ice Cubes in a Bag” (Vol. 1)Blue Ice Melt:Ice can melt with pressure.http://nsdl.org
Admiring snowflakesLiquidwaterSolidwaterPidwirny, M. (2006). "Physical Properties of Water". Fundamentals ofPhysical Geography, 2nd Edition. Date viewed: October 16, /8a.htmlhttp://nsdl.orghttp://www.classzone.com
Stamp your answerDoes the size of an ice cubeaffect the temperature at whichit freezes?Yeshttp://nsdl.orgNo
Misconception: The more water thereis to freeze, the lower thetemperature is required to freeze it.Formative Assessment:“Freezing Ice” (Vol. 2)Instead: The temperature of the freezing pointis independent of the amount of liquid.http://nsdl.org
Density is the mass perunit volume of asubstance.Photo: www.dkimages.comBuoyancy is the force of aliquid pushing up to keepsomething afloat.http://nsdl.org
True or False: Stamp your answerWater expands as it freezes becausethe molecules become larger.Truehttp://nsdl.orgFalse
Misconceptions aboutDensity & BuoyancyFloating or sinking is based on an object’s weight.Water expands as it freezes because themolecules become larger.Instead:Floating or sinking is based on an object'sdensity.Water expands as it freezes because themolecules are locked into place in a crystallinestructure.http://nsdl.org
Formative Assessment:“Floating Logs” & “Floating High andLow” (Vol. 2)Model and read about waterand icehttp://nsdl.org
Let’s pause forquestions fromthe audience .http://nsdl.org
Ice formationIce on land is usually fromprecipitation, unless it is freezingwater that is present in saturatedsoil.Ice forming on water develops atthe liquid surface of thewater and therefore on thebottom of any ice layer at thesurface.http://nsdl.org
Geography of IceLand-based ice: ice sheet ice field glacier ice streamA glacier in the Transantarctic nsdl.orgIce on/in the ocean: ice shelf ice floe sea ice icebergRoss Sea ice edge, 1957http://photolibrary.usap.gov/index2.htm
GlaciersPhoto: Glenn Grant, NSFDiagram: http://www.answers.com/glacierhttp://nsdl.org
Studying Ice CoresPhoto: Robert R Stewart,Texas hy-book/evidenceforwarming.htmhttp://nsdl.orgIce Cores: Trap gases and windblown materials Can show layering,especially dust layersin dry seasons Some date back toalmost 800,000 yearsbefore present
Effects on sea level: Land ice vs. sea iceLand-based ice is perched above sealevel. If it melts, the water drainsdownward, potentially adding water intothe ocean. The water that reaches theocean will thereby raise sea level.Photo: JasonBox, Byrd Polar Research CenterSea ice is already floating(displacing its mass) and it wasformed from sea water. Meltingof sea ice will not raise sea levelappreciably.Photo: Zee Evans, NSF
Which comes first?Concrete,hands-onexperienceAbstract orreal-worldapplicationsStamp one of the boxeshttp://nsdl.org
Activities: States & Changes of MatterHands-on investigationsand content area readingWater and IceStudents in grades K-2 observewater as it changes states.Heat Energy and WaterStudents in grades 3-5 investigateheat's effect on water.http://nsdl.org
Activities: States & Changes of MatterPolar Connections:glaciers, icebergs, sea iceHow Do Snowflakes Become Ice?Model glacier formation with marshmallows.Do It Yourself Iceberg ScienceCreate icebergs with film canisters.Sea Ice SetA collection of images and video.http://nsdl.org
Tie to the global Water CycleDon’t forget about ice and snow!Beyond Penguins and Polar Bears Issue 5(August 2008): Water, Ice, and Snowhttp://nsdl.org
Density and Buoyancy: Grades K-2Sink or Float?Students determine whether objects sink or float inwater. Include ice in various shapes and sizes!Do It Yourself Iceberg ScienceCreate icebergs with film canisters, watch themfloat.
Density and Buoyancy: Grades 3-5Water Molecule PocketsDemonstrate liquid water’s molecular structure witha discrepant event and a model.The Magic Trick with IceA discrepant event – an ice cube floats in water butnot rubbing alcohol.
Nonfiction stories for studentsFeature Story column of themagazineAvailable at three grade levels(K-1, 2-3, and 4-5)Available as text, illustratedbook, and electronic bookhttp://nsdl.org
Let’s pause forquestions fromthe audience .http://nsdl.org
Interested in learning more?Beyond Penguins Web Seminar Series:November 13th--Energy and the PolarEnvironmentBeyond Penguins and Polar Bears ical-science-from-the-poles/Beyond Penguins and Polar Bears,August 2008, Issue 5http://beyondpenguins.nsdl.orghttp://nsdl.org
http://beyondpenguins.nsdl.orgJessica Fries-Gaitherfries-gaither.1@osu.eduDr. Carol Landislandis.83@osu.eduhttp://nsdl.orgTHANKYOU!
Go to http://nsdl.org and click on the K-12audience page to: Download our Seminar Resource List Find resources from archived seminarsLearn about new tools and resources,discuss issues related to science education,find out about ways to enhance your teachingat: p://nsdl.org
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Toshiba/NSTA ExploraVision Awards: How to Submit QualityExploraVision EntriesNovember 5, 2008 NSTA: The Learning Center – Focus on Education LeadersNovember 12, 2008 NSDL: Beyond Penguins and Polar Bears: Energy and thePolar EnvironmentNovember 13, 2008
National Science Teachers AssociationDr. Francis Q. Eberle, Executive DirectorZipporah Miller, Associate Executive DirectorConferences and ProgramsAl Byers, Assistant Executive Director e-LearningNSTA Web SeminarsFlavio Mendez, Senior DirectorJeff Layman, Technical CoordinatorLIVE INTERACTIVE LEARNING @ YOUR DESKTOP
Web Seminar Evaluation:Click on the URL located on theChat Window
A. Elementary School, K-5. B. Middle School, 6-8. C. High School, 9-12. D. I teach college students. . Density & Buoyancy Floating or sinking is based on an object's weight. . Instead: Floating or sinking is based on an object's density. Water expands as it freezes because the molecules are locked into place in a crystalline structure .
the Creation Seminar Series Dr. Kent Hovind CSE Ministry. Table of Content 2004 EDITION / Age of the Earth Seminar One 1 Seminar One B 4 The Garden of Eden Seminar Two 0 Seminar Two B 14 Dinosaurs and the Bibl e Seminar Three 20 Seminar Three B 23 lies in the Textbook Seminar Four 26
Project Report Yi Li Cornell University yl2326@cornell.edu Rudhir Gupta Cornell University rg495@cornell.edu Yoshiyuki Nagasaki Cornell University yn253@cornell.edu Tianhe Zhang Cornell University tz249@cornell.edu Abstract—For our project, we decided to experiment, desig
Cornell University, and the University Corporation for Atmospheric Research (UCAR), NSDL integrates multiple . Biology Teachers (NABT) National Association of Health Sciences Education Partners (NAHSEP) . with the National Computational Science Institute (NCSI) m
The NSTA Reader’s Guide to A Framework for K–12 Sci-ence Education and a series of articles published in NSTA member journals. NSTA Press has assembled the guide and the journal articles into one useful publication, The NSTA Reader’s Guide to A Framework for K–
NSTA Readers Guide to NGSS - Chapter 3 An Overview of NGSS for Principals Reading NGSS Performance Expectations Three Dimensions of the Framework NSTA Article on Engaging in Argument and Explanation Cindy Passmore (2015) NSTA Blog Order the NSTA Reader's Guide to the NGSS
Seminar Topic Assignment Institut of Logic and Computation Knowledge-Based Systems Group www.kr.tuwien.ac.at. Empty Head Seminar Topics Seminars: ä Seminar in Theoretical Computer Science ä Seminar in Arti cial Intelligence ä Seminar in Logic ä Seminar in Knowledge Representation and Reasoning
Aman Agarwal Cornell University Ithaca, NY aa2398@cornell.edu Ivan Zaitsev Cornell University Ithaca, NY iz44@cornell.edu Xuanhui Wang, Cheng Li, Marc Najork Google Inc. Mountain View, CA {xuanhui,chgli,najork}@google.com Thorsten Joachims Cornell University Ithaca, NY tj@cs.cornell.edu AB
IELTS Academic Writing Task 2 Activity – teacher’s notes Description An activity to introduce Academic Writing task 2, involving task analysis, idea generation, essay planning and language activation. Students are then asked to write an essay and to analyse two sample scripts. Time required: 130 minutes (90–100 minutes for procedure 1-12. Follow up text analysis another 30–40 mins .