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!BSTRACT 4HE PROCESS OF FORMATION IS OFTEN TABLE ASWELLASPICTURESOFCORALFROMALLOVERTHE DIFFICULTFORMIDDLESCHOOLSTUDENTSTOCOMPREHEND#ORALISLAND WORLD HADIMMEDIATELYCAPTIVATEDTHESTUDENTS1UESTIONS FORMATIONISADYNAMICPROCESS ANDSTUDENTSSHOULDHAVETHE SUCHASh7HATISCORALMADEOF vANDh(OWCANCORALBE OPPORTUNITYTOEXPERIENCETHISPROCESSINASYNERGISTICCONTEXT PART OF AN ISLAND v CIRCULATED THROUGH THE CLASSROOM4HE 4HE AUTHORS PROVIDE INSTRUCTIONAL GUIDELINES FOR CONSTRUCTING STUDENTSCOMMENTSANDQUESTIONSINCLUDEDSEVERALMISCON ACORALISLAND3TUDENTSPLAYANINTERACTIVEROLEINTHISACTIVITY CEPTIONS SUCH AS ONE STUDENTS THEORY THAT hCORAL ISLANDS WHICH GIVES THEM BOTH VISUAL AND TACTILE EXPERIENCES 4HE AREFORMEDFROMWHITEMETEORSTHATFALLOUTOFTHESKYAND ACTIVITYWASDESIGNEDFORTH GRADESTUDENTS!FTERCOMPLETING INTOTHEOCEANv THEACTIVITY THESTUDENTSCOULDACCURATELYDESCRIBETHESIGNIFICANT 4HE CORALS BEAUTIFUL YET ALIEN QUALITY ALREADY HAD STU COMPONENTSANDPROCESSOFCORALISLANDFORMATION!DDITIONALLY DENTSMESMERIZED4HEIDEATHATTHESEALIENOBJECTSCOULD STUDENTSUNDERSTOODTHATTHISISANONGOINGGEOLOGICPROCESS FORMANISLANDFURTHERPIQUEDTHEIRCURIOSITY4HEFORMATION OFACORALISLANDISTHERESULTOFADYNAMICBUTSLOWPROCESS +EYWORDS CORALISLAND ISLANDFORMATION THAT INVOLVES THE GROWTH OF CORAL ON AN OCEANIC VOLCANO )NQUIRY INTO AUTHENTIC QUESTIONS GENERATED FROM STUDENT ANDTHESUBSEQUENTSUBSIDENCEOFTHEVOLCANOANDCREATION EXPERIENCESISTHECENTRALSTRATEGYFORTEACHINGSCIENCE OF A CORAL ATOLL 'RIGG   )LLUSTRATING THIS PROCESS IN ˆ.ATIONAL3CIENCE%DUCATION3TANDARDS.ATIONAL2ESEARCH THECLASSROOMISAWAYTOCOVERTHESECONDOCEANLITERACY #OUNCIL ESSENTIAL PRINCIPLE BY INVESTIGATING HOW SUBSIDENCE AND EROSIVEPROCESSESCANHELPSHAPE%ARTHSFEATURES.ATIONAL ORALISLANDSAREFORMEDFROMLARGEWHITEMOUNTAINS 'EOGRAPHIC3OCIETYETAL  º THATLIEBENEATHTHEOCEAN vYELLEDONESIXTH GRADE #ORALISLANDFORMATIONISAPROCESSTHATTAKESMILLIONS STUDENT WHEN ASKED HOW CORAL ISLANDS ARE FORMED 4HE OFYEARS)TBEGINSWITHANEWLYFORMEDVOLCANICISLAND VARIOUSKINDSOFCORALSKELETONSONTHESIXTH GRADESTUDENTS THAT RISES ABOVE THE SURFACE OF THE OCEAN!S THE ISLAND STABILIZESANDMAGMASTOPSFLOWINGINTOTHEOCEAN CORAL STARTSTOGROWINTHESHALLOWWATERAROUNDTHEVOLCANIC (%!4(%2!534).ISAN.3& '+GRADUATEFELLOWATTHE5NI ISLAND4HIS NEW FRINGING CORAL REEF CONTAINS MANY TINY VERSITYOF/REGONS)NSTITUTEOF-ARINE"IOLOGYIN#HARLESTON /RE GON3HETEACHESMARINEBIOLOGYTOFIFTH ANDSIXTH GRADESTUDENTS ANIMALS CALLEDCORALPOLYPS THATCREATELIMESTONESHELLS AT-ILLICOMA)NTERMEDIATE3CHOOLIN#OOS"AY /REGON4HEFOCUS 4HEPOLYPSGROWANDDEVELOPONANYSOLIDSURFACE BUILD OF HER MASTERS THESIS IS THE PHYSIOLOGY AND ECOLOGY OF THE SEA INGONTHESKELETALREMAINSOFOTHERPOLYPS#ONSEQUENTLY ANEMONE-ETRIDIUMSENILEWITHINTHE3OUTH3LOUGH%STUARY #OOS ACORALREEFISCOMPOSEDOFATHINLAYEROFLIVINGCORALON "AY /REGON 3HE DEVELOPED THIS ACTIVITY WITH SUPPORT FROM THE TOPOFTHELIMESTONEREMAINSOFDEADCORAL$ARWIN .ATIONAL3CIENCE&OUNDATION'+'RANTNUMBER$'%  ANDNUMBER$'% % MAILHAUSTIN UOREGONEDU 'RIGG  /VER MILLIONS OF YEARS THE VOLCANIC ISLAND UNDERGOES !-%,)!%$$ISASIXTH GRADETEACHERAT-ILLICOMA)NTERMEDIATE SIGNIFICANT CHANGES &IRST THE ISLAND MOVES AWAY FROM THE 3CHOOLIN#OOS"AY /REGON3HESERVEDASAN.3& '+SIXTH GRADEMENTORTEACHERDURINGTHEnACADEMICSCHOOLYEAR MAGMAHOTSPOTTHATORIGINALLYCAUSEDITTOGROW SONONEW % MAIL!MELIA% COOS BAYKORUS MATERIAL IS ADDED TO THE ISLAND !S THE MAGMA COOLS THE #OPYRIGHTÚ(ELDREF0UBLICATIONS ROCKS DENSITY INCREASES RESULTING IN SUBSIDENCE SINKING

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OF THE ISLAND 3ECOND THE EROSIVE PROCESSES OF WIND RAIN 0REACTIVITY!SSESSMENT AND WAVES SLOWLY DISINTEGRATE THE ISLANDS SURFACE MAKING "EFORE THE CORAL ISLAND FORMATION ACTIVITY STUDENTS IT SMALLER &INALLY RISING SEA LEVELS RESULTING FROM GLOBAL ANSWEREDQUESTIONSTHATASSESSEDTHEIRUNDERSTANDINGOF CLIMATE CHANGE CAUSE THE ISLAND TO SINK BELOW THE SURFACE ISLAND FORMATION AND CONNECTED THEIR PREVIOUS KNOWL 4HEFRINGINGCORALREEFGRADUALLYSINKSORSUBSIDES WITHITS EDGEOFISLANDSWITHTHEACTIVITY1UESTIONSINCLUDEDTHE ISLAND(OWEVER NEWCORALPOLYPSCONTINUETOGROWONTOP FOLLOWING7HATGEOLOGICPROCESSESARERESPONSIBLEFOR OFTHELIMESTONESKELETONS DEVELOPINGFASTENOUGHTOKEEP THEFORMATIONOFISLANDS 7HATMATERIALSCOMPOSECORAL THESURFACEOFTHECORALREEFATSEALEVEL!LAGOONSTARTSTO ISLANDS (OWDOYOUTHINKCORALISLANDSFORM 4YPICAL FORMBETWEENTHEISLANDANDTHEREEF4HISLAGOONEVENTUALLY STUDENTRESPONSESINVOLVEDCONCEPTSSUCHASTHETECTONIC SURROUNDSTHESINKINGVOLCANICISLAND ANDTHECORALREEFCON SHIFTING OF PLATES THE RISING OF SEA LEVELS THE RISE OF TINUESTOGROWUPAROUNDTHEISLAND BECOMINGABARRIERREEF VOLCANOES ANDTHEAMALGAMATIONOFSKELETONSOFSMALL /VERTIME THEENTIREVOLCANICISLANDSINKSBELOWTHESURFACE ANIMALS CALLED POLYPS3TUDENTSALSOMADECONNECTIONS OFTHEOCEAN LEAVINGANATOLL ARINGOFGROWINGCORALWITHAN BETWEENTHERISEOFVOLCANICISLANDSANDTHEFORMATION OPENLAGOONINITSCENTER$ARWIN'RIGG  OFCORALREEFS "ECAUSETHEPROCESSOFCORALISLANDFORMATIONENCOMPASSES ABSTRACTGEOLOGICPROCESSESLIKEANDSUBSIDENCE ITCAN /BJECTIVESOF#ORAL)SLAND&ORMATION!CTIVITY BE HARD TO COMPREHEND #OMBINING BOTH VISUAL AND TACTILE EXPERIENCESASSTUDENTSCONSTRUCTTHEIROWNCORALISLANDISAN 3TUDENTSCANDISTINGUISHBETWEENDIFFERENTISLANDTYPES EFFECTIVEWAYTOHELPMIDDLESCHOOLSTUDENTSLEARNABOUTCORAL 3TUDENTSCANDESCRIBEHOWACORALISLANDFORMSANDWHAT ISLANDFORMATION!SSTUDENTSBECOMEINVOLVEDINTHEFORMATION CREATES THE ATOLL USING VOCABULARY SUCH AS BARRIER REEF PROCESS THEY SYNTHESIZE DIFFERENT COMPONENTS AND STAGES OF FRINGINGREEF SUBSIDENCE ATOLL ANDLAGOON CORALISLANDFORMATIONANDSEEHOWEACHSTAGECONTRIBUTESTOTHE 3TUDENTS CAN EXPLAIN HOW THE FORMATION OF THEIR ISLAND OVERALLPROCESS5LTIMATELY THISACTIVITYINCREASESTHESTUDENTS MODELSTHATOFANACTUALCORALISLAND SCIENTIFICLITERACY ENABLINGTHEMTODESCRIBE EXPLAIN ANDTEACH THISPROCESSTOOTHERS.ATIONAL2ESEARCH#OUNCIL  -ATERIALS

"ACKGROUND vCoral skeleton set (can be purchased from Carolina Bio- logical Supply) ,ESSON#ONTEXT vFive pictures of coral islands or from around the 3IXTH GRADE STUDENTS PARTICIPATED IN THE FOLLOWING INTRO world (e.g., Tuamotu Islands, Caroline Islands, , DUCTORYLESSONTOGAINSOMEBACKGROUNDONCORALISLANDFOR Laccadive Islands, Chagos Archipelago); images can be MATIONBEFOREBEGINNINGTHEHANDS ONACTIVITY4OHELPTHEM found online or in old calendars such as the National BEGINTHINKINGABOUTISLANDS STUDENTSWORKEDINGROUPSOF Geographic Islands calendar THREETOOBSERVEVARIOUSOBJECTSTYPICALLYFOUNDONISLANDS vSchematic for the initial setup of the coral island activity SUCHASFISHBONES SHELLS SAND ANDCORAL ASWELLASPICTURES (for the teacher; see Figure 1) OFDIFFERENTTYPESOFISLANDS!FTERTHISOBSERVATION EACHSTU vThree Coral Island Formation worksheets for each stu- DENTWROTEHISORHEROWNDEFINITIONOFANISLANDANDSHAREDIT dent (see Figures 2–4) WITHTHECLASS4HETEACHERLEDADISCUSSIONOFTHESEIDEAS AND vOverhead on coral island formation (see Figure 5) STUDENTSVOTEDONTHEBESTDEFINITION!FTERTHEDISCUSSION THE vOne can of white shaving cream, labeled “ TEACHERGAVESTUDENTSAFORMALDEFINITIONOFANISLANDALAND mix,” for each group MASS SMALLERTHANACONTINENT ENTIRELYSURROUNDEDBYWATER  vOne empty soda can for each group 3TUDENTSWROTETHISDEFINITIONNEXTTOTHEIROWN vOne 7.6 s 12.7 cm (3 s 5 in.) index card per group; 4HETEACHERTHENUSEDPICTURESANDOVERHEADSTOINTRODUCE fold each card into the shape of a cone and tape to top VOLCANIC BARRIER AND CONTINENTAL ISLANDS 3TUDENTS ASKED of can QUESTIONSANDRECORDEDBASICDEFINITIVEFEATURESOFEACHTYPE vOne tub of water for each group (water level should be OF ISLAND INCLUDING THE MATERIAL FROM WHICH THE ISLAND IS 2.5–5.0 cm from the top, so the water will not overflow COMPOSED HOWTHEISLANDFORMS ANDWHEREISLANDSOFTHIS when the can displaces water) TYPEAREFOUND%ACHGROUPOFSTUDENTSTHENPICKEDONEOFTHE vOne blue paper plate for each group with a hole cut from THREEISLANDTYPESTORESEARCHINGREATERDETAIL/VERTHENEXT the center (the hole should be the exact diameter of the FEWDAYS STUDENTSCREATEDPOSTERSLISTINGTHEIRISLANDTYPES soda can, so the can barely fits through), and labeled SPECIFICCHARACTERISTICS DETAILSABOUTITSPROCESSOFFORMATION “ocean” in large letters with a permanent marker ANDDESCRIPTIONSOFWHEREITCANBEFOUND%ACHGROUPHAD v60 marbles for each group MINTOPRESENTITSFINISHEDISLANDPOSTERTOTHECLASS vPaper towels (for cleaning up spilled water) &ALL 3#)%.#%!#4)6)4)%3 

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0ROCEDURE 4HEACTIVITYTAKESAPPROXIMATELYMIN!CLASSROOM WITHANOVERHEADPROJECTOR TABLES ANDSINKISIDEALFOR THISACTIVITY  0LACE STUDENTS IN GROUPS OF THREE AND ASSIGN EACH STUDENTALETTERFORTHEACTIVITYSTUDENT! STUDENT" AND STUDENT#  (ANGPICTURESOFDIFFERENTCORALISLANDSFROMAROUND THE WORLD ON THE BLACKBOARD AND WALLS OF THE CLASSROOM !SKEACHGROUPTODISCUSSTHEPICTURESANDPREDICTHOWTHEY &)'52%3TAGE))#ORAL)SLAND&ORMATIONWORKSHEETKEY THINK A CORAL ISLAND IS FORMED BASED ON THEIR OBSERVATION  3#)%.#%!#4)6)4)%3 6OL .O

OFTHECORALATTHEIRTABLEANDTHEPICTURESOFCORALISLANDS  )NSTRUCTSTUDENTSTOLABELTHEPARTSOFTHEIRISLANDONTHE 4ELL STUDENTS TO SAVE THEIR PREDICTIONS FOR THE DISCUSSION 3TAGE))#ORAL)SLAND&ORMATIONWORKSHEET&IGURE  AFTERTHEACTIVITY  4OMODELTHEULTIMATESTAGEINCORALISLANDFORMATION  0LACE TWO DIFFERENT TYPES OF CORAL ONE TUB OF WATER STUDENT#SPRAYSANOTHERLAYERORSOOFSHAVINGCREAMON ONE PAPER PLATE WITH A HOLE CUT OUT ONE SODA CAN WITH TOP OF THE EXISTING LAYERS )F THE CAN HAS NOT SUNK TO THE ATTACHEDCONE SHAPEDINDEXCARD MARBLES ANDONESHAV BOTTOMALREADY STUDENT"CANPUSHTHECANANDTHEPAPER INGCREAMCANLABELEDhCORALREEFMIXvATEACHTABLE&IGURE CONETAPEDTOITSTOP ALLTHEWAYTHROUGHTHEHOLEANDINTO SHOWSASCHEMATICFORTHEINITIALSETUPOFTHEACTIVITY THEWATER4HEPAPERCONEISNOWSATURATEDWITHWATERAND  'IVEEACHSTUDENTACOPYOFTHE#ORAL)SLAND&ORMATION WILLSLOWLYSTARTTOCOMEAPARTINTHETUB)FTHETUBISTOO WORKSHEETS &IGURES n AND TELL THE STUDENTS THAT THEY SMALL HAVESTUDENTSREMOVETHECANANDTHECONEFROMTHE WILLACTIVELYGOTHROUGHTHECORALISLANDFORMATIONPROCESS TUB COMPLETELY BUT REMIND THEM THAT THE ISLAND HAS SUNK TO MAKE THEIR OWN CORAL ISLAND 2EMIND STUDENTS THAT IN BENEATHTHESURFACEOFTHEOCEAN 3TUDENTSSHOULDSEEARING REALITY THIS PROCESS TAKES MILLIONS OF YEARS &OR EXAMPLE OFCORALSHAVINGCREAM WITHALARGEHOLEINTHECENTERTHAT IN (AWAII THE PROCESS HAS BEEN GOING ON FOR THE PAST  ISFILLEDBYTHESURROUNDINGWATER MILLIONYEARS  !SKTHESTUDENTSHOWTHEIRISLANDHASCHANGED7HAT  4ELL STUDENT! IN EACH GROUP TO PLACE THE BLUE PLATE HAPPENEDTOTHEVOLCANICISLAND 7HEREDIDITGO (OW WITHTHEHOLEINTHECENTER ONTOPOFTHEWATERINTHETUB DIDTHISHAPPEN 7HATHAPPENEDTOTHECORALREEF 7HY 3TUDENT"PLACESTHESODACANINTHEHOLESOTHECANANDTHE 7HATISTHISCORALREEFCALLEDNOW 7HATISTHEWATERINTHE PLATEAREFLOATINGTOGETHERONTOPOFTHEWATER3TUDENT# CENTERCALLED SLOWLYSPRAYSATHINLAYEROFSHAVINGCREAMAROUNDTHEBASE  !SKSTUDENTSTOEXPLAINWHATHASHAPPENEDTOTHEIRMODEL OFTHECANSEE&IGURE  ISLAND$URINGTHEDISCUSSION INTRODUCETHECONCEPTTHATWHAT  !SK STUDENTS WHAT THEY THINK THE CAN THE SHAVING ISLEFTOFTHEISLANDISARINGOFGROWINGCORAL CALLEDANATOLL CREAM ANDTHETUBOFWATERREPRESENT!FTERDISCUSSINGTHEIR WITHWATERINTHECENTER ALAGOON4HERINGOFSHAVINGCREAM IDEAS CONFIRM THAT THE TUB OF WATER REPRESENTS THE OCEAN ATTHEWATERSSURFACEREPRESENTSTHEATOLL THEWATERWITHINTHE AND THAT THE CAN REPRESENTS THE NEWLY FORMED VOLCANIC HOLEINTHECENTEROFTHESHAVINGCREAMISTHELAGOON ANDTHE ISLANDPROTRUDINGFROMTHEDEPTHSOFTHEOCEAN4HESHAVING CANTHEFORMERISLAND ISNOWUNDERTHEWATER CREAMREPRESENTSTHENEWFRINGINGREEFFORMINGALONGTHE  !SKTHESTUDENTSHOWLONGTHISACTIVITYTOOK$EPEND SHORE OF THE VOLCANIC ISLAND )T IS IMPORTANT TO NOTE THAT INGONTHESIZEOFTHECLASS ANSWERSWILLVARYFROMMIN THE ACTUAL VOLCANIC ISLAND DOES NOT FLOAT LIKE THE CAN BUT TO  MIN 4ELL STUDENTS THAT EACH MINUTE THAT THEY WERE IS CONNECTED TO THE BOTTOM OF THE OCEAN -AKE SURE EACH FORMINGTHEIRCORALISLANDREPRESENTEDROUGHLYMILLION STUDENT UNDERSTANDS THIS SO IT DOES NOT BECOME A LASTING YEARSOFACTUALCORALISLANDFORMATION(AVETHEMWORKOUT MISCONCEPTION HOW MANY MILLIONS OF YEARS THEIR n MIN TIME PERIOD  )NSTRUCTSTUDENTSTOLABELTHEPARTSOFTHEIRISLANDONTHE REPRESENTS%MPHASIZEHOWSLOWTHISPROCESSIS 3TAGE)#ORAL)SLAND&ORMATIONWORKSHEETSEE&IGURE   (AVESTUDENTSLABELTHEPARTSOFTHEIRNEWCORALISLAND  !FTER STUDENTS COMPLETE THEIR WORKSHEET STUDENT ! ON THE 3TAGE ))) #ORAL )SLAND &ORMATION WORKSHEET SEE DROPS  MARBLES INTO THE CAN!S THE CAN BEGINS TO SINK &IGURE  4HIS IS A GOOD TIME FOR A TEACHER TO USE PAPER THROUGHTHEHOLEINTHEPLATE STUDENT#SPRAYSTHREEMORE TOWELSTOMOPUPANYSPILLEDWATERFROMTHETABLES LAYERS OF SHAVING CREAM AROUND THE CAN WHILE STUDENT "  4O SOLIDIFY LEARNING AND ASSESS UNDERSTANDING ASK SIMULTANEOUSLYPUSHESTHECANDOWNTHROUGHTHEHOLEUNTIL STUDENTSTOEXPLAINTHETHREEDIFFERENTSTAGESOFCORALISLAND ONLYTHECONETAPEDTOTHETOPISVISIBLEONTHEPLATE FORMATIONINTHEIROWNWORDS  !SKSTUDENTSHOWTHEIRISLANDHASCHANGED7HATHAS  2EVIEWCORALISLANDFORMATIONUSINGTHEOVERHEADSEE HAPPENED TO THE ISLAND (OW DID THIS HAPPEN 7HAT HAS &IGURE ANDPICTURESOFTHECORALISLANDS HAPPENEDTOTHECORALREEF 7HATDOTHECAN SHAVINGCREAM &OR A FINAL ASSESSMENT HAVE STUDENTS WRITE THEIR ANDTUBOFWATERREPRESENTNOW OWNDESCRIPTIONOFCORALISLANDFORMATIONUSINGPERTINENT  #ONFIRM THAT THE CAN REPRESENTS THE SUBSIDING SINK VOCABULARY ING VOLCANICISLAND THATTHENEWLYAPPLIEDSHAVINGCREAM REPRESENTSTHEGROWTHOFNEWCORALONTOPOFTHELIMESTONE %VALUATION REMNANTSOFDEADCORAL ANDTHATTHEREEFATTHISSTAGEISNOW !FTERCOMPLETINGTHEACTIVITY ASSESSSTUDENTSONTHEBASISOF CONSIDERED A BARRIER REEF AS IT CONTINUES TO GROW UPWARD THEFOLLOWINGCRITERIA AROUNDTHESINKINGVOLCANICISLAND4HETUBOFWATERREPRE SENTSTHEOCEAN!SKSTUDENTSWHATPROCESSESHAVECAUSED  PARTICIPATIONINTHEACTIVITY THE CHANGE IN THE ISLAND 4HIS ALLOWS FOR A DISCUSSION OF COMPLETION OF THE THREE CORAL ISLAND FORMATION SUBSIDENCEANDEROSION IFTIMEPERMITS WORKSHEETS &ALL 3#)%.#%!#4)6)4)%3 

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