–€€@LƒÌ}ˬð5 _­¬Š$ŽŠ%Ž l0¬±$)ªÈ$ð±$Hȱ$ UhšŠL"©À š`©€e$…$æ%`­…$­…%` Œ ©R @©P €Š!àÐ( L¹(©Œ©1© ©€  ­ YäÎ ðŠI˜` ­ d  LÇd M  Œ* €@ ÿ­ …$­ …%­ …C¢©C ‘$¥$)¥%1© U©dÊߥ$9¥%:¬ ¢ˆ˜!0 SèàÐñ¥$ç¥%è©š™Èúš¹ð ÉDðÈÈÈÀÐð©D™©Ë™©™` ­ }œJ‚)ðLr 윂Éd M  Œ* €@ ÿ­ …$­ …%­ …C¢©C ‘$¥$)¥%1© U©dÊߥ$9¥%:¬ ¢ˆ˜!0 SèàÐñ¥$ç¥%è©š™Èúš¹ð} ÉDðÈÈÈÀÐð©D™©Ë™©™` ­ }œJ‚)ðLr 윂ÉðÉðJÉ ð É ð ¥š(°(°  p LÇ ¥ª(°ù¬¹ƒ)ð  ‘ JŽœ}‹L= ¥¬(° Á ¬L ­ 0q A­ ­  ‘¬¢ © ™ÈÊùŠI©Bƒ J¬™œ‹™©C™©™™¢œ;É?ð™Èèà ð D W ¶}©€… ‚ÐLLÇ ¥©©…­ ©‡` W ¬¹ƒ)„¹‹¹ŒLꍜA…! ­¬ ¹Éß°©…"œ‚)ð-Œ‡˜Ý† p°" }ä  °±$þ‡­‘G©@……LÇL ¥ˆœ…08`©©Q¥")ð<Ð2Q­0 â°- ±G‘$Ș݆õ UL# ; p8¥(ý†…(°Æ)¥(0Ê¥)ÐÆNQ`  }±$‘GȘ݆õ‡LU ­œ‚)ðL­ œ‡݆ ë âðLà š±GȘ‡Œ‹ÐŒŒР݆©L¯LÇ ­œ‚)ðW>…Z ‡  œHœHœ‚)ðœƒH }p hƒ âûœ‹œŽŒ Ž¬hy™hy™œƒ™ D ”©‚LÂ>…ó ËLñ œJJ    ! LA© *ˆÐù` ­œBÉþðFÉ }ýð7É'°8é  š¹M H¹N H` 8 € Z ß â  \LdÃÊòÃJóóœJЩ!¢ð©"ªŽ¥!¢ ÉðG¥F¥E @­F (À‹Ð®ð©!ÍÐÑL¯ }ÀÐù ©ÿÑEÐÈÑEðì ¥­¢­É!𢩠‘EˆÐûœ^ èœ^ ‘EÈÀÐõ  ©‘E©ÿÈÌÐö 7©‘EÈ©‘E® d‘E Š©/‘EÈ©‘E ”©š™Èú© DÎ }ø .L } ‰¢ œ;FÊ÷ d  ‚¢Ž¬œ;É?ÐÎÝFÐ7œFÉ?ð™Èèà Ðá(Ð . ‚Ð ®œŒ Z D­ð ü®LÂLè d Á ‚}Ð . D üí ”L ‘¬  ©€™ p  âø ˜‘E`© ,© d¬¹)ß ™ D üêL¬¹) ðÑ ¥§œ…0BœM݊ÐœL݉ðœ…}ð Ë©…œMŒœL‹ ê° œN݆ð ¥Š‡LÇ ¥«œ‡Nœ‰LœŠMLÇ ì[ T Š±E qEHȱE ‹qEªhšŠ¢Ž 0 Š‘GÈ¹Ô ‘GÈÀÐö} HLǬLà ±GîɛÐéÀ°©€L ü°¥ ä LÇFREE SECTORS® © ‘Gœ) ð©*‘GÈ© ‘GÈœ‘GèÈÀ õ© ‘GȌ®¥*jœj ˆ©>‘G} ©<‘GŒœ¢d R¢ R¢ R¢ ˜ð¢+ ©›‘G Œ`Ž¢ÿ…D„Cè8¥C횥Déà ÐêŠ 0¬‘Gî¥D€C` ±$ˆ0dÉ:Ð÷ÈÈ©¢±$É.Ð àÐÈ© Ðî},É*Ð ©?ì°%$É?ðÉ0É:)ßÉAÉ[ © à ð© ÐÈìð¹;èг­;É ðŠI` ¥¥©ÿ ©pî­iî©ÍðN A©š¹}ð#0!)CÉð)ÐÏ¢œ;É?ðÙÐÁèÈà Ð ­ ­ ­ ¹0œ8ŠI` } ì°`L€œ…0  … Ë0"Lâ Jœ‡ ‘GœŒ }‘GÈœ‹}‘G Ë ©‚­L¯þÐþ Õ©‹Œ‡©}†`8œŠŒ‰Lœ‹‰œŒŠ`œ…ðLpœ‹ŒÐ8` Õ Ì04 }±G)ü݁Ð,±G)ŒȱG‹ȱG}Hœ„Ðh0©})Hh†©‡` œœBÉ!ð ¥€8`8­iiš(¢©ÐZ ±EÐ6€!©JÀðŒ©S Sä©d¬ê©Š€!™ Ì ê ‘E š û` T©} ‘E ê8 š û8LÌ¥FŠE hŒ  Œ Ž r9ÀƒðLœ ¥£­)© © ¥Eiª¥Fi(L¶ d±E™î©‘EÈÀÐò`¬  d¹î‘EÈÀÐö`œ‰H)}šhŠð/¹×Hœ‰ ^ŠjˆÐùi šhE‘EÀd  Š±Ei‘EȱEi‘E`  ÈÌ°W±Eðö¢ÿè üœ×QE‘EŠHŠI˜8é ‹©À‹*°úŒh‹‹Àd   Šœƒ)¿ }ƒ8±Eé‘EȱEé‘E ˜‘EœŒ` ¥¢†IºèèŽ Š!ŽÊœ)…Eœ1…Fœð5ŠIŒˆÐ¹! ÈÀö ¥¡©€™!Șˆˆ˜JH©jm9…Ghm:…H` ¥ Œˆ𠈩}ˆ™!`ŠGŽŠHŽLlŒ‰œŠ Z dLÇ©© ŒÈ©8 l­I€0î¬ ÌÐä`Œ©ÐÌ _©}† ; ¥$Í ¥%í ° pLl`¢¬¹}ݚÐÈèà ÐòŠI(`DOS SYSh…Ch…D ±C® šŠICš­`­0íŠI ©Ðä „B®ß0ŠäðüŒÔx …D­Ó)ãDÓ`}Need DOS2.5,type Y ÒÅÔÕÒ}Λd÷  €€ddJ€ÿþýüûì\Ì|DOS SYSCOPY130 COM}B€}B€}-}CDOS SYS}­ …C­ C*ɐ( ‹Ð> Ë¥C8jJ…3©j…2­…C­…D ( ±C‘2ˆù0±2‘Cˆù© Þ ÀŒÔ „BXÈ` N ©1?©ñ¢ l© ¢LlD:RAMDISK}.COM›©LÍu ÐL¥1©©í¢ ÍL ¥;ÐLê˜HL³ê³êºŽ  T `ºŽ  ” `8©ž©Ÿ… ©… ­œêɐР© ©  àêêê¥Ð Ø`TŽU “©À } ŠL’­ð­žð ? . “ t䩍`…ðöÿàá©€Ÿ©Gà©á¢©B©J Œ©Ð~¢©ôD©E©H©I ©B Vä0d©ÿÍôÐVÍõ!}ÐQ¢© D©E©H©I VäFÀˆÐ9 ’,ž0 ©,ŸŸ0 s0hhLž­Ð ©¢ ŠL©ª` ’©Ð÷˜H ’hšÐ DH­¡EšhÈКÈЭ"}¢ ­£¡©¢D©E©L­¢8í H­£í¡I­¡É4ê°­£Éê° ­ 0©€ ŸŸþHÐþI,Ÿ0­ 0Î  9© .¢©Gâ©ã VäLO#},ž0 L÷ɐÉ4*IJ`lâlàD1:AUTORUN.SYS›NEED MEM.SAV TO LOAD THIS FILE.›D8:MEM.SAV› ’©J y08© B©|D©E©ŠH©I$} Vä0 ’0 `©B©;D©ELŒ`­?<0LV䠐`@ÿ¢ŽžŽŸʆ v s©…ð? F0Ξ05©:¢ Š©[¢ Š©B©D©E©H©I%} Vä­ÉYÐ8©…¢ © B Vä¥ œ¥ ©@… ©… ©/¢D©E ŒžˆŒ €`E:›D8:DUP.SYS›ERROR-SAVING USER MEMORY ON DISK›TYPE Y TO &}STILL RUN DOS› œ©B©;D©E© J Œ œ(`©ð 9¢ Vä©ðî ­âÇ­ãÈ©âªÃ© ï©ðàÇ­áÈ©àªÃ© ï ’­ž-'}”ðî”LLu ÄèŽÅÆ¢©ÃD©E©H©ILVä 9© .lú¿ 9© .l­œ… ­… `­žÐ` s©…ð$©B Œ©B©ŠH©(}I©|D©E Vä© BLVä n䢩B©,D©E© JLVä© ¢B Vä¢ © BLVäDŽE¢ŽIÊ© BêꭝðåLÿÿÿàáu • óœ}ÿÿ 3E:›}DISK OPERATING SYSTEM II VERSION  ²®µ COPYRIGHT 1984 ATARI CORP.››A. DISK DIRECTORY I. FORMAT DISK›B. RUN CARTRIDG*}E J. DUPLICATE DISK›C. COPY FILE K. BINARY SAVE›D. DELETE FILE(S) L. BINARY LOAD›E. RENAME FILE M. RUN AT ADDRES+}S›F. LOCK FILE N. CREATE MEM.SAV›G. UNLOCK FILE O. DUPLICATE FILE›H. WRITE DOS FILES P. FORMAT SINGLE›L˜ !N'Æ,}#"&Ÿ)æ)9(Ð&©*)/h)¬'ú'-Ê&¢ÿ؆莟©…R©'…S¥ €…Ò v­ŸÉLð/©©Ë¢ ÍLŒ }Insert DOS 2.0s, type Y ÒÅÔÕÒΛ©ô©x…© …©-}D©E©fH©I ž1¢ÿšèŽ#©q¢! Š©@Ÿ y0ɛðÏ8éA0,Íô' š±ȅ±… ±ªˆ± °1 ¶1¥i…æl©d¢! °1L!NO SUCH ITEM›SELECT.} ITEM OR ÒÅÔÕÒÎ FOR MENU›õ! Ê0 ¿.®œzÉ:Щ*{}©.|èè莩›{Ž¢ Ø1 ã0 ¿0©¢J©BŽþ é1­8íÉðLš%®œ|ÉDÐóL¶/}%DIRECTORY--SEARCH SPEC,LIST FILE?›[# Ê0 ¿0 ž&­|ÉDð©3¢" °1L!NOT A DISK FILE›¢­žÉNÐ ©!B é1L!©E¢# °1©¢ ©!B©ñD©0}E©Dñ©:ó­}É:Щ1ò¢©B©J©|D©E é1©ôD©E©B©¢©H©I é1­õÉ Ðhî­Í0ߢ ¹ôÉ ð ôèÈà0ð©.1}ôè  ¹ôôÈèÀ 0ôŽ©?ô詛ô©ñ¢ °1 y0ÉYЛ­®©›ô¢ é1 ;#LŠ" ;#L!¢© BLé1TYPE "Y" TO DELETE...›DELETE FILE SPEC2}›COPY--FROM, TO?›OPTION NOT ALLOWED›697 FREE SECTORS›› COPYING---D8:COPY32.COM››l# Ê0­­|ÉDТ Ò.ðL/%©€#©3}#©‘#¢©J©B©|D©E é1©B©H©I©’D©#E é1­’#É0É:° © B é1L!­#͑#ðî‘#ÐÁî#© B é1 ¹œ#Ùc$Јõ0‰SY4}S 1­}É:𚌳#¢ œ’#É ð™²#Èèà Ððœ’#É ð©.™²#Èœ’#É ð™²#Èèà Ð𩛙²#©Š¢# °1,#P¢©²D©#ELJ- <.¢©B©J©²D©#EŽþ é5}1¢ Ø1­H­H ã0hh®œ|ÉDðLš% 1œ}É:ðšÌ³#Ð ’LŸ%¢ Œ³#©²D©#ELÞ%¢ Ø1 ã0® è.® Ò.Ð0©O¢% °1L!WILD CARDS NOT A6}LLOWED IN DESTINATION› ¿0 <.­|ÉKð<ÉCð8ÉEТŽþLš%ÉSð(¢©B©JŽþ é1®œ|ÉKð ÉEЩÿLõ%©|¢# °1 ’L!ÉCðﮞàAÐÉDÐä© 7}Щ¢ J©BŽÿ é1©K©®þ¬ÿB© ™B¥D™D¥E™E®þ­H­I VäŒø®ÿ¬þ¹HH¹IIHð é1­øÌɈðLñ1®þ𩠝B8} Vä®ÿ𩠝B Vä®ÿЩI¢' Š,#Lì#L!œ& Ê0 Õ0 ¿0 ž&© ¢B é1L!RENAME - GIVE OLD NAME, NEW› ­}É:ð)šŒöLS)'©ýÐ'©þ9}' 70 ¹2i0H'K' ¿0©0¢' °1 y0ÉYЭ' ! 'L!ý¢B©JD©'E˜JLé1WHICH DRIVE TO FORMAT?›TYPE "Y" TO FORMAT DISK 2›D2:›«'¬ý¿:}©ªý¿Íý¿Ð©Uý¿Íý¿Ð Œý¿©Ÿ¢' °1L!­ü¿Ðñª­ý¿ðëÍý¿ÐæèÐó v©¢ä _ \ä©¢ä b \äLNO CARTRIDGE›È' 70 2 ¿0…†­ÉðP vL RUN FROM;} WHAT ADDRESS?›TYPE "Y" TO CREATE MEM.SAV›ß' y0ÉYÐ s0 ©¢( °1 ’L! FõLð1MEM.SAV FILE ALREADY EXISTS›Õ( 70 ¹2 ¿0ö 0+)<}') S)©¢) °1 y0ÉYÐr©ò¢( °1©¢B©*D©)E©J é1¢© B é1¢ œ.{ÊÐ÷­+)}Ž¢ Ø1© Ã©Ä©Å©ùó/©ø/©3ÆH©uà© =}áΟL›/L!DRIVE TO WRITE DOS FILES TO?›WRITING NEW DOS FILES›TYPE "Y" TO WRITE DOS TO DRIVE 2.›D2:DOS.SYS›ERROR - NOT VERSIO>}N 2 FORMAT.› t*­ôÉð ©5¢) °1L!`©) Ê0©®žžàNÐΞ ¿0 ©àðàð˜Lñ1©›¢) °1 ’L!BAD LOAD FILE›LOAD FROM WHAT FILE?›Ó) Ê0 ?}¿0©#¢B é1L!WHAT FILE TO LOCK?›û) Ê0 ¿0©$¢B é1L!WHAT FILE TO UNLOCK?›DUP DISK-SOURCE,DEST DRIVES?›TYPE "Y" IF OK TO US@}E PROGRAM AREA›CAUTION: A "Y" INVALIDATES MEM.SAV.›©…F©ô…E­ö…!©ù +Lð1© ­þþ©© © `*©  70 ¹2ö ¹2ÿA} ¿0­öÍÿð.¢*©Ù °1 y0Î 0)INSERT BOTH DISKS, TYPE RETURN›©^¢, °1 y0©©3­å8逍­æé­Í­í° ©N¢, °1L! Ý,©B}žC, t*­ ù­ ú­û­ü­þýLx+©ž, 0 ©^¢, °1 y0 , ¡,0,ž0 Ç,LŽ+ Í,­I€0î Ÿ,­ÍðV­Í­í°Ç­ž0C}«Îž, 0 ©}¢, °1 y0­C,КîC,­ÿ 0K' !­ "­ H­ H©ý 'h h Lx+­žž­ÿ…!©ô…E©…F 5Lð1L! ¹D,…¹I,…¢¡H¹ùh™ùˆD}孍­` þNOT ENOUGH ROOM›INSERT SOURCE DISK,TYPE RETURN›INSERT DESTINATION DISK,TYPE RETURN›þÎÐôE}þ©­þ`î Ðî `­ö­ÿ8 rLð1`¥ð©-¢* °1©P¢* °1 y0ÉYЩ…ž`hhL!NAME OF FILE TO MOVE?›- Ê0 ¿0­|ÉDðLŸ% <.¢F},©^ °1 70 ¿0 Ò.Щ@Lä#¢ è.¢©B©J é1©  ¢¥D¥E­H­I©B Vä ÀˆðLð1Î ¢,©} °1 70,õL.¢   ­ Рî G}˜J©B©| ,#P©² #D˜E é1 ¢ ©ÙHÐÙI𩠝B¥D¥E¹HH¹II é1© B é1­ Т,©^ °1 70,õ0La-¢© B Vä,#PH}¢,©^ °1 70 ¿0Lì#L!¥ð©-¢* °1©P¢* °1 y0ÉYÐj©…ž©…©3…­å8鍭æé3©©}m©m­Í Ðå­Í°Ý­Ð©I}}͐`­8é}­é`©ô…©…©ú©`œ|èÉ*ð É?ð ɛðÉ,Ðìè`èœ|É:ðèè ¹-)Ý|ÐÈèÀÐò© ¢/ °1L!`DESTINATION CANT BE DOJ}S.SYS›0© Ÿ Ê0­žH®©›{ 2ÃŽÄà4°Δ 2ÅŽÆ8íÍó/ŠíÄ°L!ø/À›ð) 2âŽã ãðΠÀ›ð 2 ¿0àŽá áðΟ©žK}hÉAÐΞ¢©B,ž0©Ð© J é1© B©ÁD©E©H©I,ž©H©ÃD©E é1¢©ùH©IþHÐþI­ÃD­ÄEL“SAVE-GIVE L}FILE,START,END(,INIT,RUN)›©›¢O€Êú©õ S0 ¶1`©B©€D©E©PH©I¢ VäÀ€ÐÎõ`©õ S0­H÷ ¶1­õ ’L!­÷ÉM}0 ©ª¢0 °1L~0­€`PLEASE TYPE 1 LETTER›,õ0`hhL! 70¢ Ø1Lã0©¬®L<1¬®© œ€É,ð;ɛð7œ¥É,ð"ɛð©:ÝŠð1Ý¥ÐÎœ€ÉN}A"©D™|ÈÎÎÝ€ðíΩD™|È©:™|È©žœ€™|èÈɛð,É,ð(É/ð+É.ЩÎÞ©¢1 °1Îõœ€èÉ,ðɛÐôŽŒ`œ€ž蜀™{èéNAMEO} TOO LONG›© B¢ VäÀ€ÐL!` ŠL¶1©ªI© H©1E©ÎDLž1œ©|mD©iE` Vä˜0`˜8éd¢/è8é úi:2Ž2¢2© °1 ’LP}!ERROR- 164›©©®œ€îɛð+É,ð'  20* ..ˆö ÎÓ©r¢2 °1Îõ`š­®`©‚¢2ÐëTOO MANY DIGITS›INVALID HEXAQ}DECIMAL PARAMETER›8é00É 0 8éÉ 0É0©ÿÉ`,õ0'®œ€èÉDðø8é0ð0É Hœ€èÉ,ðɛÐôŽh`Îõ©ð¢2L°1NEED D1 THRU D8›ÿàáuR} ECIMAL PARAMETER›8é00É 0 8éÉ 0É0©ÿÉ`,õ0'®œ€èÉDðø8é0ð0É Hœ€èÉ,ðɛÐôŽh`Îõ©ð¢2L°1NEED D1 THRU D8›ÿàáuÿÿ²­Ð)𠩍!©"`ûó3ö!£ö3ö<öLäóî!¬!ÀwÐ ©!©ä"¹; `POKE 710,0:POKE 709,0:POKE 712,0›DIM SPQP$(1)›IF STRIG(0)=0T} OR PEEK(764)<255 THEN INPUT SPQP$:RUN"D:MENU"›RUN"D:TITLE"›âãàá10,0:POKE 709,0:POKE 712,0›DIM SPQP$(1)›IF STRIG(0)=0H%&æ—­›€DIR€F€T€M€Z€ÄÉÊFLÇÎØËÆÚÙÁAšLšÌÂÃÅL€€€€€€€ V} @@€VVP W}ROGRAMMED BY PETER LOESER WILLITS HIGH SCHOOL, WILLITS, CA 1985›  (}'AAb'AA X}b@-@@@(&‘’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’…(A-@@A('ü Ò Ï Ã Ë Ó  Á Î Ä  Í É Î Å Ò  Y}Á Ì Ó  ü 2@-@@@(&ü                                    ü<@-@@@(&ü     Äåöåìïðåä âù Ðåôåò Ì Z}ïåóåò      üF@-@@@(&ü     Ôèå Åäõãáôïòó§ Áôáòé Ãìõâ      üP@-@@@(&ü                       [}              üZ@-@@@(&ü  Ðáòô Æïõòº Åáòôè Óãéåîãå Óåòéåó   üd@-@@ @(&š’’’’’’’’’’’’’’’’’’’ \}’’’’’’’’’’’’’’’’’ƒn'-@@'( šÁ© MINERALSx1-@@1( šÂ© THE HARDNESS SCALE‚,-@@ ]},( šÃ© IGNEOUS ROCKSŒ0-@@0( šÄ© SEDIMENTARY ROCKS–0-@@0( šÅ© METAMORPHIC ROCKS ) ^}-@@)( šÆ© WEATHERINGª=-@@=(#select letter and then press ÒÅÔÕÒÎÈ—;@,Ò-@ _}@!—Ü —4A% D:MINERALSæ —4B% D:HARDNESSð —4C% D:FIREROCKú —4D% D:SEDIMENT — `}4E% D:METAMORP —4F% D:WEATHERI, —3F @ÿD1:SCIMENU.SYSú —4D% D:SEDIMENT — \"#‹e&x&››››››››››››››››››››››››››››››››››€€ b} € †+"AR@.6‰-@@@‚@R@ƒ@9l0@c}@†0@@  (}-@@22(‰&‰•••••••••••••••••••••••••••••••••• 22(‰&d} ™ 22(‰& M I N E R A L S ™ #22(‰& e} ™ (22(‰&‹Œ --@@222(‰&‘’’’’’’’’’’’’’’’’’’’’’’’’’’’’’f}’’’’’… 722(‰&ü   Ôèéó ðòïçòáí éó ðáòô ïæ ôèå    ü <22(‰&ü  ‘’’’’’’’’’’’’’’’’’’’’’’’’’’’…   ü A22(‰&ü  ü g}Å Á Ò Ô È   Ó Ã É Å Î Ã Å ü   ü F22(‰&ü  ü        Ó Å Ò É Å Ó        ü   ü K22(‰&ü  š’’’’’’’’’’’’’’’’’’’’’’’’’’h}’ƒ   ü P22(‰&ü  äåöåìïðåä âù  Ðåôåò Á® Ìïåóåò   ü U22(‰&š’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’ƒ Z+(+(‰ i} PROGRAMMED IN JULY 1985_-Š-@A Š-AR@d A€n‹%2@A@@3(j} CORRECT !G‚-@APK ‚m2@‚-@AP… ‚‹(}x$‚‰%2@Ak}@@1(WRONG !E‚-@API ‚k2@‚-@Aƒ ‚‰(}Œ$–l}U€;@,;@0,!(};0@@U0@@  2-@@2(PROGRAMED BY PETm}E LOESERªƒ-@A ƒŽ (}ŸEB(:The layer of gases that surrounds the earth is called the:E(È( 1. n}AtmosphereÒ( 2. HydrosphereÜ( 3. Lithosphereæ\6„-@ A0((0( YOUR CHOICE:4…> B'gD„"…o}R6†-†%@\ Að! „…6‡-‡%@! A0úUR(JThe earth's outer layer of rock up to about 100 km in thicknep}ss is called:U(( 1. Atmosphere( 2. Hydrosphere( 3. Lithosphere"\6„-@ A((0( YOUR q}CHOICE:4…> B'gD„"…R6†-†%@\ A,! „…6‡-‡%@! A06C@(8All the bodies of water on the Ear}rth'ssurface is called:C(@( 1. AtmosphereJ( 2. HydrosphereT( 3. Lithosphere^\6„-@ AP((s}0( YOUR CHOICE:4…> B'gD„"…R6†-†%@\ Ah! „…6‡-‡%@! A0r^[(SA substance found in tht}e earth that always has the same properties is called:^(|( 1. A mineral†( 2. A compound( 3. An Elemu}entš\6„-@ A((0( YOUR CHOICE:4…> B'gD„"…R6†-†%@\ A€! „…6‡-‡%@! A0v}®MJ(BThe smallest complete part of a mineral substance is called:M(ž(( 1. An elementÂ( 2. An atomw}Ì( 3. A compoundÖ\6„-@ Ap((0( YOUR CHOICE:4…> B'gD„"…R6†-†%@\ Aà! „…6x}‡-‡%@! A0ê<9(1A substance made up of only one kind of atom is:<(ô( 1. An atomþ( 2. An elementy}( 3. A compound\6„-@ A0((0( YOUR CHOICE:4…> B'gD„"…R6†-†%@\ A! „…6‡-z}‡%@! A0&jg(_A substance made up of two or more kinds of atoms that have joined together is called:j({}0( 1. An atom:( 2. An elementD( 3. A compoundN\6„-@ A((0( YOUR CHOICE:4…> B'g|}D„"…R6†-†%@\ AX! „…6‡-‡%@! A0bSP(HSomething made up of a particular combination of m}}inerals is called:S(l( 1. An atomv( 2. A rock€( 3. A compoundŠ\6„-@ AP((0( YOUR CHOI~}CE:4…> B'gD„"…R6†-†%@\ A”! „…6‡-‡%@! A0žPM(EThe most common element making up the} weight of the Earth's crust is:P(š( 1. Oxygen²( 2. SiliconŒ( 3. MagnesiumÆ\6„-@ A((€}0( YOUR CHOICE:4…> B'gD„"…R6†-†%@\ AÐ! „…6‡-‡%@! A0ÚFC(;Which two elements make-}up almost 75% of the Earth's crust?F(ä( 1. Silicon and Calciumî( 2. Aluminum and Oxygenø( 3. Oxygen and Si‚}licon\6„-@ Ap((0( YOUR CHOICE:4…> B'gD„"…R6†-†%@\ A ! „…6‡-‡%@! Aƒ}0<9(1Small particles that make up an atom are called:<( ( 1. Compounds*( 2. Subatomic matter4( 3.„} Atomic particles>\6„-@ A0((0( YOUR CHOICE:4…> B'gD„"…R6†-†%@\ AH! „…6‡-‡%…}@! A0R1.(&The central part of an atom is called:1(\( 1. Protonf( 2. electronp( 3. Nucleusz†}\6„-@ A((0( YOUR CHOICE:4…> B'gD„"…R6†-†%@\ A„! „…6‡-‡%@! A0Ž‡}1.(&The smallest atomic particles are the:1(˜( 1. Electrons¢( 2. Protons¬( 3. Neutrons¶\6„-@ ˆ}A P((0( YOUR CHOICE:4…> B'gD„"…R6†-†%@\ AÀ! „…6‡-‡%@! A0Êkh(`An area wh‰}ere a certain number of electrons move at a definite distance from the nucleus is:k(Ô( 1. The NucleusÞ( 2. TŠ}he electron shellè( 3. The atomic particleò\6„-@ A((0( YOUR CHOICE;4…> B'gD„"…R6†-†%@‹}\ Aü! „…6‡-‡%@! A0pp(hAn atom that becomes electrically charged as a result of the lossŒ} or gain of electrons is called:(( 1. A molecule( 2. An ion$( 3. An electron.\6„-@ Ap}((0( YOUR CHOICE:4…> B'gD„"…R6†-†%@\ A8! „…6‡-‡%@! A0B63(+Two or more atomŽ}s joined together form:6(L( 1. An ionV( 2. A molecule`( 3. A shellj\6„-@ A0((0( }YOUR CHOICE:4…> B'gD„"…R6†-†%@\ At! „…6‡-‡%@! A0~63(+A mineral form with a defini}te shape is a:6(ˆ( 1. Gem’( 2. Rockœ( 3. CrystalŠ\6„-@ A((0( YOUR CHOICE:4…> B‘}'gD„"…R6†-†%@\ A°! „…6‡-‡%@! A0ºmj(bAn attractive and rare mineral substance t’}hat is hard enough to be cut and polished is a:m(Ä( 1. GemÎ( 2. RockØ( 3. Crystalâ\6„-@ AP“}((0( YOUR CHOICE:4…> B'gD„"…R6†-†%@\ Aì! „…6‡-‡%@! A0ö^[(SThe way in whic”}h light is reflected from the surface of a mineral is called:^(( 1. Color ( 2. Luster( 3. Texture•}\6„-@ A((0( YOUR CHOICE:4…> B'gD„"…R6†-†%@\ A(! „…6‡-‡%@! A0–}2II(AHow heavy a mineral is, compared with how large it is, is called:<(( 1. LusterF( 2. TextureP( 3. —}HeftZ\6„-@ Ap((0( YOUR CHOICE:4…> B'gD„"…R6†-†%@\ Ad! „…6‡-‡%@! A˜}0nQN(FWhen salt is found in its natural state in the Earth it is called:Q(x( 1. Halite‚( 2. QuartzŒ™}( 3. Pyrite–\6„-@ A0((0( YOUR CHOICE:4…> B'gD„"…R6†-†%@\ A ! „…6‡-‡%@š}! A0ª.+(#Silicon and oxygen combine to form:.(Ž( 1. HaliteŸ( 2. QuartzÈ( 3. PyriteÒ\6„-@›} A((0( YOUR CHOICE:4…> B'gD„"…R6†-†%@\ AÜ! „…6‡-‡%@! A0æ30((An œ}uneven break in a mineral is calleda:3(ð( 1. Fractureú( 2. Cleavage( 3. Streak\6„-@ AP}((0( YOUR CHOICE:4…> B'gD„"…R6†-†%@\ A! „…6‡-‡%@! A0"30((A smooth break in až} mineral is called a:3(,( 1. Fracture6( 2. Cleavage@( 3. StreakJ\6„-@ A((0( YOUR CHŸ}OICE:4…> B'gD„"…R6†-†%@\ AT! „…6‡-‡%@! A0^RO(GA method for determining a mineral' }s identification is the use of the:R(h( 1. Hardness Scaler( 2. Streak Test|( 3. Both of these.†\6„-@¡} Ap((0( YOUR CHOICE:4…> B'gD„"…R6†-†%@\ A! „…6‡-‡%@! A0š (}œ¢}=-@@=(#                                   ž=-@@=(#    =£}-@@=(#  YOUR SCORE WAS:  ¢=-@@ =(#   €E-@€}@-(  WRONG ‡?-@6@E( Š=-@@=(#   š¥}G-@@/(  CORRECT †A-@6@G( ª=-@@=(#  Š}  ¬O-@@=(#                                   OAT® ( ° ( ² ( Ž ( ¶ (§} ž ( º ( Œ ( Ÿ ( À ( Â ( Ä ( Æ ( Ì B }ÐÒÏÔÅÃÔ ÅÎÄ ÒÏÕÔÉÎś }Š-@š}A Š} (}}@-@@@(&‘’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’…(}@-@@@(&ü          ©}                          ü2}@-@@@(&ü ÔÙÐÅ §ÒÕΧ ÔÏ ÂÅÇÉΠÐÒÏÇÒÁÍ ÁÇÁÉΠ ü<}@-@@ @(&ü       ª}                             üF}@-@@@(&ü ÔÙÐÅ §ÅÎħ ÔÏ ÆÉÎÉÓÈ ÔÈÉÓ ÐÒÏÇÒÁÍ  üP}@-@@@(&ü    «}                                üZ}@-@@@(&ü ÔÈÅΠÐÕÓÈ [RETURN] ËÅÙ ÔÏ ÅØÅÃÕÔÅ  üd}@-@@@(&ü ¬}                                   ün}@-@@@(&š’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’ƒx}‹;@,(‹‚­}} ‹4END% D:SCIMENU.SYSŒ} ‹4RUN @–}"‹0RUN)‹0END" B ÿ D2:MINERALS‹;@,(‹‚jf›››››››››››››››››››››€€€ †+¯}"AR@.6‡-@@@‚@R@ƒ@9l0@@†0@°} (}-@@22(‡&‰•••••••••••••••••••••••••••••••••• 22(‡& ™ ±}22(‡& S E D I M E N T A R Y R O C K ™ #22(‡& ™ (22(‡&‹²}Œ --@@222(‡&‘’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’… 722(‡&ü   Ôèéó ðòïçòáí ³}éó ðáòô ïæ ôèå    ü <22(‡&ü  ‘’’’’’’’’’’’’’’’’’’’’’’’’’’’…   ü A22(‡&ü  ü Å Á Ò Ô È   Ó Ã É Å Î Ã Å ü   ü FŽ}22(‡&ü  ü        Ó Å Ò É Å Ó        ü   ü K22(‡&ü  š’’’’’’’’’’’’’’’’’’’’’’’’’’’ƒ   ü P22(‡&ü  äåöåìïðåä âù  µ}Ðåôåò Á® Ìïåóåò   ü U22(‡&š’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’ƒ Z.(.(‡ PROGRAMMED IN SEPTEMBER 1985_-ˆ¶}-@A ˆ-AR@d;@,„;@,n= (}#0@@=0@·}xt-@@t(Z1. The small rock pieces and dissolved minerals carried by running water are called:‚ (ž} ( ( (A) liquid gold.Œ(( B) A load.–(( C) land fill.  6.B APªS-@@S(92. Any ¹}substance that settles out of water is called:Ž( ( ((A) Accumulate.Ÿ(( B) Sediment.È((C) Sedimenº}tary rock.Ò 6.B APÜ[-@@[(A3. The smallest rock fragments make up what is commonly called:æ»}( ( ((A) Mud.ð((B) Sand.ú(( C) Gravel. 6.A AP1-@@1(4. Mud is a mixtuŒ}re of:5( ( (5($A) Water, gravel and decayed plants."'('(B) Tuff, concrete and water.,&(&(C) Clay and siltœ} particles.6 6.C AP@<-@@<("5. One fourth of all sediments is:J( ( ((A) mud.T((Ÿ}B) Sand.^(( C) Gravel.h 6.B APrF-@@F(,6. The least common type of sediment is:|¿}( ( ((A) Mud.†((B) Sand.(( C) Gravel.š 6.C AP€p-@@p(V7. A kind of rockÀ} made when a layer of sediment becomes solid is called:®!( ( (!(A) Igneous rock.ž((B) MetamorphÁ}ic rock.Â((C) Sedimentary rock.Ì 6.C APÖV-@@V(<8. When grains of sand become cemented Â} together they form:à( ( (( A) Sandstone.ê((B) Conglomerates.ô(( C) Shale.þ 6.A APdÃ}-@@d(J9. Gravel and large round particles become cemented together to form:( ( (( A) Gypsum.Ä}((B) Conglomerates.&(( C) Shale.0 6.B AP:Y-@@Y(?10. When a lake drys up it leavesÅ} behind a rock called:D( ( (( A) Gypsum.N(( B) Shale.X(( C) Sandstone.b 6.A APlÆ}6-@@6(11. Dissolved minerals form:v%( ( (%(A) Organic sediment.€ ( (B) Chemical sediment.ŠÇ}(( C) Limestone.” 6.B APž^-@@^(D12. Which of the following are not organic sedimentaÈ}ry rocks?š( ( (( A) Limestone.²((B) Coal.Œ(( C) Rock salt.Æ 6.C APÐ ApÚQ…-É}@3†-@`A @I2…†@@M †Q …ä@ †-A€@P6@<2†@Ê}@@ †î7…-@32…7 …ø A p:-@@:(YOU GOT ƒ CORRECË}T OUT OF 12! Aƒ!@ !-@@A(THAT MAKES YOU A FIRST-RATEEƒ!@ !-@@E(GENIUS ABOÌ}UT SEDIMENTARY ROCKS! ]ƒ @*ƒ!@+-@@](-NOT A BAD SCORE, BUT I BET YOU CAN DO BETTER!*;ƒ @Í}!-@@;(BETTER DO THIS AGAIN!4 B RENTER AND CHECK ANSWER›\'( ( ('(CHOOSE THE BEST ANSÎ}WERf((THEN PRESS ÒÅÔÕÒÎp ( „z7 „0-( SORRY, THE ANSWER WAS .7 A „c „46ƒ-ƒ%@(}Ï}/+@%@I0@c0@Ž< „4-@@<(@* NICE ANSWERÐ}!! *˜< „4-@@<(@* * * * * * * * * *¢= „4-@@=(@* Ñ}*¬< „4-@@ <(@* * * * * * * * * *¶< „4-@@<(@* *ÀÒ} „4 A0Ê@ (}#0@@=0@@$Ô€-@A €$Þ$€-@Ó}A €!(}$$}ÐÒÏÔÅÃÔ ÅÎÄ ÒÏÕÔÉÎś }ˆ-@A ˆ} (}}@-@@@(&‘’’’’’’’’’’’’’’’’’Ô}’’’’’’’’’’’’’’’’’’’…(}@-@@@(&ü                                    ü2}@-@@@(&ü ÔÙÐÅ §ÒÕΧ ÔÏÕ} ÂÅÇÉΠÐÒÏÇÒÁÍ ÁÇÁÉΠ ü<}@-@@ @(&ü                                    üF}@-@@@(&ü ÔÙÐÅ §ÅÎħÖ} ÔÏ ÆÉÎÉÓÈ ÔÈÉÓ ÐÒÏÇÒÁÍ  üP}@-@@@(&ü                                    üZ}@-@@@(&ü ÔÈÅΠÐÕ×}ÓÈ [RETURN] ËÅÙ ÔÏ ÅØÅÃÕÔÅ  üd}@-@@@(&ü                                    ün}@-@@@(&š’’’’’Ø}’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’ƒx}‰;@,(‰‚} ‰4END% D:SCIMENU.SYSŒ} ‰4RUN @–}"‰0RUN)‰0Ù}END" B ÿ D2:SEDIMENT‰;@,(‰‚} ‰4END% D:SCIMENU.SYSŒ} ‰4RUN @–}"‰0RUN)‰0&r‡š›››››››››››››››››››››››››€€ € Û} †+"AR@.6‰-@@@‚@R@ƒ@9l0@@†0@@ Ü} (}-@@22(‰&‰•••••••••••••••••••••••••••••••••• 22(‰& Ý} ™ 22(‰& F I R E R O C K S ™ #22(‰& ™ (22(‰&‹Þ}Œ --@@222(‰&‘’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’… 722(‰&ü   Ôß}èéó ðòïçòáí éó ðáòô ïæ ôèå    ü <22(‰&ü  ‘’’’’’’’’’’’’’’’’’’’’’’’’’’’…   ü A22(‰&ü  ü Å Á Ò Ô È   Ó Ã É Å Î Ã Åà} ü   ü F22(‰&ü  ü        Ó Å Ò É Å Ó        ü   ü K22(‰&ü  š’’’’’’’’’’’’’’’’’’’’’’’’’’’ƒ   ü P22(‰&ü  äåá}öåìïðåä âù  Ðåôåò Á® Ìïåóåò   ü U22(‰&š’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’ƒ Z.(.(‰ PROGRAMMED IN SEPTEMBERâ} 1985_-ˆ-@A ˆ-AR@d;@,„;@,n= (}#0@@=0@ã}@ xa-@@a(G1. A piece of the Earth that is usually made up of two or more‚88(0 miä}nerals mixed together is called:Œ( ( (( A) An atom.–(( B) A rock. !(!(C) An atomic particle.å}ª 6.B A ŽR-@@R(82. Rock formed when molten materials cool is called:Ÿ%( ( (%(A) Meæ}tamorphic rock.È((B) Igneous rock.Ò((C) Sedimentary rock.Ü 6.B A æ4-@@4(3. Thç}e word éçîåïõó means:ð%( ( (%(A) Coming from fire.ú((B) Formed in layers.(( C) Changed. 6.A è}A ]-@@](C4. Molten material reaching the Earth's surface is called:"( ( (( A) Magmaé}.,((B) Volcanic matter.6((C) Lava.@ 6.C A J>-@@>($5. When lava cools quickly iê}t forms:T( ( (( A) Pumice.^((B) Volcanic glass.h((C) Tuff.r 6.B A |9-@@ë}9(6. A kind of volcanic glass is:†( ( (( A) Pumice.((B) Tuff.š(( C) Obsidian.€ 6.C A ì}®r-@@r(X7. As volcanic ash piles up on the ground and is squeezed together it forms:ž( (í} (( A) Pumice.Â(( B) Obsidian.Ì((C) Tuff.Ö 6.C A àZ-@@Z(@8. When gas bubblesî} are trapped in hardened lava it forms:ê( ( (( A) Pumice.ô((B) Volcanic ash.þ(( C) Obsidian.ï} 6.A A U-@@U(;9. Rock formed when lava comes to the surface is called:+( ( (+(A) Exð}trusive igneous rock.&%(%(B) Intrusive igneous rock.0$($(C) Igneous surface stone.: 6.A A Dd-@ñ}@d(J10. Igneous rock formed underground in cracks that cut across layersN''( of existing rock is calò}led:X( ( (( A) A dike.b(( B) A sill.l((C) A batholith.v 6.A A €e-@@e(Kó}11. Igneous rock formed underground in cracks that run parallel with Š99(1 layers of existing rock is ô}called:”( ( (( A) A dike.ž(( B) A sill.š((C) A batholith.² 6.B A Œa-@@aõ}(G12. A large body of igneous rock formed underground is called:Æ( ( (( A) A dike.Ð(( B) A sill.Úö}((C) A batholith.ä 6.C A î A ø ‡-@6@2@%@‡ ÷}ˆ-@@  ˆ ‡ %%2* A 4:-@@:(YOU GOT ƒ CORRECø}T OUT OF 12!>Aƒ!@ !-@@A(THAT MAKES YOU A FIRST-RATEHAƒ!@ !-@@A(GENIUS ABOù}UT IGNEOUS ROCKS!R]ƒ @*ƒ!@+-@@](-NOT A BAD SCORE, BUT I BET YOU CAN DO BETTER!\;ƒ @ú}!-@@;(BETTER DO THIS AGAIN!f B „ENTER AND CHECK ANSWER›Ž'( ( ('(CHOOSE THE BEST ANSWERû}˜((THEN PRESS ÒÅÔÕÒ΢ ( „¬7 „0-( SORRY, THE ANSWER WAS .7 A@¶c „46ƒ-ƒ%@(}/+ü}@%@I0@@ c0@À< „4-@@<(@* FANTASTIC ! ý}*Ê< „4-@@<(@* * * * * * * * * *Ô= „4-@@=(@* *Þþ}< „4-@@ <(@* * * * * * * * * *è< „4-@@<(@* *ò „4ÿ} A`ü& (}#0@@ &$€-@A €$$€-@A €!(}$$$€-@}A €!(}$$}ÐÒÏÔÅÃÔ ÅÎÄ ÒÏÕÔÉÎś }ˆ-@A ˆ} (}}@-@@@(&‘’’’’’’’’’’’}’’’’’’’’’’’’’’’’’’’’’’’’’…(}@-@@@(&ü                                    ü2}@-@@@(&ü ÔÙÐÅ §Ò}ÕΧ ÔÏ ÂÅÇÉΠÐÒÏÇÒÁÍ ÁÇÁÉΠ ü<}@-@@ @(&ü                                    üF}@-@@@(&ü ÔÙÐÅ} §ÅÎħ ÔÏ ÆÉÎÉÓÈ ÔÈÉÓ ÐÒÏÇÒÁÍ  üP}@-@@@(&ü                                    üZ}@-@@@(&ü Ô}ÈÅΠÐÕÓÈ [RETURN] ËÅÙ ÔÏ ÅØÅÃÕÔÅ  üd}@-@@@(&ü                                    ün}@-@@@(&}š’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’ƒx}Š;@,(Š‚} Š4END% D:SCIMENU.SYSŒ} Š4RUN @–}"Š0}RUN)Š0END" B ÿ D2:FIREROCKŠ;@,(Š‚} Š4END% D:SCIMENU.SYSŒ} Š4RUN @–}"Š0,f_r›››››››››››››››››››››€€€ l+}"AR@.6‡-@@@‚@R@ƒ@9l0@@ (}-@@ }22(‡&‰•••••••••••••••••••••••••••••••••• 22(‡& ™ 22(‡& M E T A M O } R P H I C R O C K ™ #22(‡& ™ (22(‡&‹Œ  }--@@222(‡&‘’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’… 722(‡&ü   Ôèéó ðòïçòáí éó ðáòô ïæ ôèå    ü <2 }2(‡&ü  ‘’’’’’’’’’’’’’’’’’’’’’’’’’’’…   ü A22(‡&ü  ü Å Á Ò Ô È   Ó Ã É Å Î Ã Å ü   ü F22(‡&ü  ü        Ó Å Ò  }É Å Ó        ü   ü K22(‡&ü  š’’’’’’’’’’’’’’’’’’’’’’’’’’’ƒ   ü P22(‡&ü  äåöåìïðåä âù  Ðåôåò Á® Ìïåóåò   ü U2}2(‡&š’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’ƒ Z.(.(‡ PROGRAMMED IN SEPTEMBER 1985_-ˆ-@A ˆ-A}R@d;@,„;@,n# (}#0@@xl-@@l(R1. Rock that has change}d by the action of heat or pressure without melting is:‚!( ( (!(A) igneous rock.Œ((B) sedimentary rock.–}((C) metamorphic rock.  6.C A`ª/-@@/(2. Metamorphic means:Ž%( ( (%(A) formed w}ith heat.Ÿ((B) changed in form.È!(!(C) formed by pressure.Ò 6.B A`Ü@-@@@(&3. Met}amorphic rocks can be formed by:æ( ( (( A) pressure.ð((B) heat.ú((((C) both by pressure and heat. }6.C A`d-@@d(J4. The endless process by which rocks are formed, destroyed, and formed88(0 } again in the Earth's crust is called:"#( ( (#(A) the Rock Cycle.,((B) the Earth Cycle.6(( C)} evolution.@ 6.A A`JM-@@M(35. Quartzite is the metamorphic rock made from:T( ( ((}A) clay.^(( B) Sandstone.h(( C) limestone.r 6.B A`|H-@@H(.6. Slate is a metamor}phic rock made from:†( ( ((A) clay.(( B) shale.š!(!(C) both clay or shale.€ 6.C A`}®1-@@1(7. Marble is made from:ž#( ( (#(A) clay, or shale.Â(( B) sandstone.Ì(( C) lime}stone.Ö 6.C A`à@-@@@(&8. Gneiss differs from marble because:êE( ( (E(4A) it has a strea}ked or banded appearance.ô+(+( B) it is not a metamorphic rock.þ*(*(C) it always is the same color. }6.A A`3-@@3(9. Schist is formed from:( ( (( A) Gypsum.&((B) Conglomerates.0}"("(C) many types of rocks.: 6.C A`De-@@e(K10. In the Rock Cycle igneous rock is chang}ed into metamorphic rock by:N( ( ((A) weathering.X ( (B) heat and pressure.b,(,(!C) heat, pressure and w}eathering.l 6.C A`ve-@@e(K11. In the Rock Cycle sedimentary rock is changed into metamorphi }c rock:€)( ( ()(A) by heat and pressure.Š((B) by weathering.”/(/($C) by weathering, heat and pressure.ž!} 6.A A`šd-@@d(J12. In the Rock Cycle metamorphic rock is changed into igneous rock by:²#("} ( (#(A) chemical means.Œ(( B) melting.Æ(( C) pressure.Ð 6.B A`Ú A€äQ…-#}@3†-@`A @I2…†@@M †Q …î@ †-A€@P6@<2†@@$}@ †ø7…-@32…7 … A € :-@@:(YOU GOT ƒ CORRECT OUT OF%} 12!Aƒ!@ !-@@A(THAT MAKES YOU A FIRST-RATE Eƒ!@ !-@@E(GENIUS ABOUT METAM&}ORPHIC ROCKS!*]ƒ @*ƒ!@+-@@](-NOT A BAD SCORE, BUT I BET YOU CAN DO BETTER!4;ƒ @!-'}@@;(BETTER DO THIS AGAIN!> B \ENTER AND CHECK ANSWER›f'( ( ('(CHOOSE THE BEST ANSWERp(}((THEN PRESS ÒÅÔÕÒÎz ( „„7 „0-( SORRY, THE ANSWER WAS .7 AŽc „46ƒ-ƒ%@(}/+@)}%@I0@@c0@@˜< „4-@@<(@* YOU'RE CORRECT! *¢*}< „4-@@<(@* * * * * * * * * *¬= „4-@@=(@* *¶< „+}4-@@ <(@* * * * * * * * * *À< „4-@@<(@* *Ê „4 ,}A@Ô& (}#0@@&$Þ€-@A €$è$€-@A €!(}$$}ÐÒÏÔÅÃÔ -}ÅÎÄ ÒÏÕÔÉÎś }ˆ-@A ˆ} (}}@-@@@(&‘’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’…(}@-@.}@@(&ü                                    ü2}@-@@@(&ü ÔÙÐÅ §ÒÕΧ ÔÏ ÂÅÇÉΠÐÒÏÇÒÁÍ ÁÇÁÉΠ ü<}@-@/}@ @(&ü                                    üF}@-@@@(&ü ÔÙÐÅ §ÅÎħ ÔÏ ÆÉÎÉÓÈ ÔÈÉÓ ÐÒÏÇÒÁÍ  üP}@-@0}@@(&ü                                    üZ}@-@@@(&ü ÔÈÅΠÐÕÓÈ [RETURN] ËÅÙ ÔÏ ÅØÅÃÕÔÅ  üd}@1}-@@@(&ü                                    ün}@-@@@(&š’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’ƒx2}}‰;@,(‰‚} ‰4END% D:SCIMENU.SYSŒ} ‰4RUN @–}"‰0RUN)‰0END" B ÿ D2:METAM3}ORP‰;@,(‰‚} ‰4END% D:SCIMENU.SYSŒ} ‰4RUN @–}"‰0RUN)‰0END" B ÿ D2:METAM./·o››››››››››››››››››››››››››››››››››››››››››››››A€!5} @ A@€   ªª ÔÉÔÌÅ ÓÃÒÅÅΠªª  ›†+@"AR!6}@.6-@@@‚@R@ƒ@9l0@@@†0@@@-@!7}(( the hardness scale2-@<( of mineralsF-@@P((( developed b!8}y Peter A. LoeserZ--@A -AR@_ A d##  ªª ÍÁÉΠÐÒÏÇÒÁÍ ÂÅÇÉÎÓ ªª  ›nk (}+!9}%AR@?0@@@Y0@@@k-@@xRR(J In this program you wi!:}ll be asked to name all the minerals used in the‚EE(=THE HARDNESS SCALE starting from the softest to the hardest.ŒL(!;}L(A If you don't know an answer, type HELP and push the .–>(>(3 Begin with the softest mineral used be!<}low... -@@ªT(T(I                                      ŽQQ(I   AN!=}SWERS NOT SPELLED CORRECTLY     ARE NOT ACCEPTED!  Ÿ,,($     È++(#     !>}                             æ€;@ ,ð‚;@ ,ú"€€4ENDA0-@@‚‚4H!?}ELPAP&‚4MINERALS A & A"‚0€A€'##  ªª ÃÏÒÒÅÃÔ ÁÎÓ×ÅÒ ÌÏÏРªª  ›,5 (}+@%@!@}50@@@60-@@0 @ *************@0-@@0 @ * *!A}J0-@@0 @ * *T0-@@0 @ * CORRECT *^0-@@0 @!B} * *h0-@@0 @ * *r0-@@0 @ *************|‡-!C}@† ƒ-@6? 2ƒ@@š-@Ž € ƒ®) ‡)2!D}ž AÂAR@̆-@@/0@@@I0@@@!E}| .Name the next hardest mineral of the scale...† A0Ö APà8 (}-@@8 Sorry, that was w!F}rong...êl( (l(^If you can't get it, you can type HELP, but first...ôƒ-@!G}AP ƒþ (}$-@@$( Try again! Ap AP&1 (}-@ @1(The a!H}nswer was €0 A:E-@@;(!What is the next hardest mineral?E A0D APNƒ-@A!I} ƒX= }#0@@@=0@@@b$g  ªª ÄÁÔÁ ÓÔÁÔÅÍÅÎÔÓ ªª  ›l TALC›v GY!J}PSUM›€ CALCITE›ŠFLUORITE›” APATITE›žFELDSPAR›š QUARTZ›² TOPAZ›ŒCORUNDUM›Æ DIAMOND›Ð END›Õ  !K}ªª ÆÉÎÁÌ ÓÃÒÅÅΠªª  ›Ú (}ä((( H A R D N E S S S C A L Eî--(%____________________________________ øFF(> l|!L} Talc |Fingernail scratches it | | easily.LL(D 2| Gypsum |Fingernail barely | | scr!M}atches it. LL(D 3| Calcite |Copper penny just | | scratches it.II(A 4| Fluorite |Steel knife scrat!N}ches | | it easily. LL(D 5| Apatite |Steel knife barely | | scratches it.*<<(4 6| Fel!O}dspar |Scratches glass easily. | |4LL(D 7| Quartz |Scratches steel and | | glass easily.>H!P}H(@ 8| Topaz |Scratches all common | | minerals.H&&( 9| Corundum |Scratches Topaz.R&&(10| Diamond!Q} |Hardest mineral.\+(+( > PUSH SPACE BAR TO CONTINUE <f F:Ad,"AUApp%D:MENU„  ªª ÈÅÌРÌ!R}ÉÓÔ ÌÏÏРªª  ›ŽY (}+-0@@@G0@@@YAR@˜R(R(G HERE IS HO!S}W THE TEN MINERALS IN THE HARDNESS SCALE ARE SPELLED.¢LL(D  | !T} |¬rr(j | CORUNDUM | | GYPSUM | | TALC |!U}¶rr(j | TOPAZ | | CALCITE | | FLUORITE |Àrr(j !V} | FELDSPAR | | APATITE | | QUARTZ |ÊLL(D | DIAMO!W}ND | | |Ô&&( ÙK(K(@However, they are not l!X}isted here in the correct order...Þ@(@(5Push to continue with the program...è F:B2y,"@!Y}A ò Aü (} $@-@@ @(&type 'MINERALS' to see list of answers$ÿ D:HARDNESS!Z}A ò Aü (} $@-@@ @(&type 'MINERALS' to see list of answers$ÿ D:HARDNESS #$œ;5N5›››››››››››››››››››››››››››››››››››€€ %\} € l+"AR@.6Œ-@@@‚@R@ƒ@9%]}l0@ (}-@@22(Œ&‰•••••••••••••••••••••••••••••••••• 22(Œ& %^} ™ 22(Œ& W E A T H E R I N G ™ #22(Œ& %_}™ (22(Œ&‹Œ --@@222(Œ&‘’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’… %`}722(Œ&ü   Ôèéó ðòïçòáí éó ðáòô ïæ ôèå    ü <22(Œ&ü  ‘’’’’’’’’’’’’’’’’’’’’’’’’’’’…   ü A22(Œ&ü  ü Å Á Ò Ô È%a}   Ó Ã É Å Î Ã Å ü   ü F22(Œ&ü  ü        Ó Å Ò É Å Ó        ü   ü K22(Œ&ü  š’’’’’’’’’’’’’’’’’’’’’’’’’’’ƒ   ü %b}P22(Œ&ü  äåöåìïðåä âù  Ðåôåò Á® Ìïåóåò   ü U22(Œ&š’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’’ƒ Z+(+(Œ PROGR%c}AMMED IN JUNE 1985_--@A -AR@d€;@,;@0,n A`x—Š-@@%d}+ˆ-@@G2ˆ@@g( C O R R E C T !k ˆo Š‘2—%e}(}‚$Œeˆ-@@032ˆ@@Q( NO ! N0! NO!U ˆ_2‹‹‹‹e(}–$ # (%f}}#0@ªE?(7THE BREAKING OF SOLID ROCK INTO SMALL PIECES IS CALLED:B(E(Ž( 1. INTERFACE(Ÿ%g}( 2. OXIDATION(È( 3. WEATHERINGÒ\6ƒ-@ A((0( YOUR CHOICE?4„> B'gDƒ"„R6…-…%@\%q}Ãÿÿÿÿÿÿÿÿÿÿÿÿÿÿÿÿÿÿÿÿÿÿÿÿÿÿÿÿÿÿÿÿb%DOS SYSb*)DUP SYSbSAUTORUN SYSb UTITLE bMaMINERALS b,®SEDIMENT b-ÚFIREROCK b-METAMORP b'4HARDNESS bl[WEATHERI A Ü! ƒ„6†-†%@! A@æf`(XA ZONE WHERE THE LITHOSPHERE, HYDROSPHERE, OR ATMOSPHERE COME %r}TOGETHER IS:c(f(ð( 1. A WEATHER PLAIN(ú ( 2. AN OXIDATION ZONE (( 3. AN INTERFACE\6ƒ-@ A%s}p((0( YOUR CHOICE?4„> B'gDƒ"„R6…-…%@\ A ! ƒ„6†-†%@! A@"ke(]THE BREAKING %t}OF ROCKS INTO SMALLER PIECES WITHOUT CHANGING THEIR MINERAL MAKEUP IS CALLED:h(k(,( 1. OXIDATION(6"( 2. CHE%u}MICAL WEATHERING"(@( 3. PHYSICAL WEATHERINGJ\6ƒ-@ Ap((0( YOUR CHOICE?4„> B'gDƒ"„R6…-…%%v}@\ A T! ƒ„6†-†%@! A@^XR(JTHE BREAKING DOWN OF ROCKS BY CHEMICALCHANGES IN THEIR MINERALS IS %w}CALLED:U(X(h( 1. OXIDATION(r"( 2. CHEMICAL WEATHERING"(|( 3. PHYSICAL WEATHERING†\6ƒ-@ A%x}((0( YOUR CHOICE?4„> B'gDƒ"„R6…-…%@\ A ! ƒ„6†-†%@! A@š>8(0THE UNION OF A %y}SUBSTANCE WITH OXYGEN IS CALLED:;(>(€( 1. OXIDATION(®"( 2. CHEMICAL WEATHERING"(ž( 3. NATURAL MIXINGÂ%z}\6ƒ-@ AP((0( YOUR CHOICE?4„> B'gDƒ"„R6…-…%@\ A Ì! ƒ„6†-†%@! A@Ö%{}OI(AA SIMPLE PLANT THAT GROWS ON THE SURFACE OF ROCKS IS CALLED:L(O(à( 1. A LICHEN(ê( 2. A PIONEER PLA%|}NT(ô%%( 3. BOTH OF THESE ARE CORRECTþ\6ƒ-@ A((0( YOUR CHOICE?4„> B'gDƒ"„R6…-…%@%}}\ A ! ƒ„6†-†%@! A@<6(.GRANITE IS BROKEN DOWN BY WEATHERING TO FORM:9(<(( 1. LIMESTONE%~}(&( 2. CLAY AND SAND(0( 3. TUFF:\6ƒ-@ Ap((0( YOUR CHOICE?4„> B'gDƒ"„R6…-…%@%}\ A D! ƒ„6†-†%@! A@N=7(/A GOOD EXAMPLE OF PHYSICAL WEATHERING WOULD BE::(=(X( 1. ACID RA%€}IN(b( 2. CAVERN BUILDING(l( 3. FROST BREAKING ROCKv\6ƒ-@ A0((0( YOUR CHOICE?4„> B'%}gDƒ"„R6…-…%@\ A €! ƒ„6†-†%@! A@Ške(]THE SPLITTING OFF OF SCALES OR FLAKES OF ROCK AS A %‚}RESULT OF WEATHERING IS SOMETIMES CALLED:h(k(”( 1. EXFOLIATION(ž"( 2. NATURAL INTERACTION"(š( 3. ATOMI%ƒ}C WEATHERING²\6ƒ-@ A((0( YOUR CHOICE?4„> B'gDƒ"„R6…-…%@\ A Œ! ƒ„6†-†%@%„}! A@Æic([A PILE OF BROKEN ROCK THAT ACCUMULATESAT THE BOTTOM OF A CLIFF OR STEEP SLOPE IS CALLEDf(i(Ð( %…} 1. TALUS(Ú( 2. A LANDSLIDE(ä( 3. A SLUMPî\6ƒ-@ AP((0( YOUR CHOICE?4„> B'gDƒ"„%†}R6…-…%@\ A ø! ƒ„6†-†%@! A@KE(=A SUDDEN MOVEMENT OF LOOSE MATERIAL DOWN A SLOPE IS CALLED%‡}:H(K( ( 1. TALUS(( 2. A LANDSLIDE( ( 3. A SLUMP*\6ƒ-@ A((0( YOUR CHOICE?4„%ˆ}> B'gDƒ"„R6…-…%@\ A 4! ƒ„6†-†%@! A@>*$(A SMALL LANDSLIDE IS CALLED:'(*(H( 1.%‰} TALUS(R( 2. A LANDSLIDE(\( 3. A SLUMPf\6ƒ-@ Ap((0( YOUR CHOICE?4„> B'gDƒ"„R6%Š}…-…%@\ A p! ƒ„6†-†%@! A@zRL(DA SLOW DOWNWARD MOVEMENT OF LOOSE MATERIAL ON A SLOPE IS CA%‹}LLED:O(R(„( 1. TALUS(Ž( 2. A SLUMP(˜( 3. A CREEP¢\6ƒ-@ A 0((0( YOUR CHOICE?4„%Œ}> B'gDƒ"„R6…-…%@\ A ¬! ƒ„6†-†%@! A@¶:7(/A WORD THAT MEANS COMING FROM LIVING THINGS %}IS:(À( 1. NATURAL(Ê( 2. ORGANIC(Ô( 3. PUREÞ\6ƒ-@ A ((0( YOUR CHOICE?4„> B'g%Ž}Dƒ"„R6…-…%@\ A è! ƒ„6†-†%@! A@ò`Z(RMATERIAL IN SOIL THAT COMES FROM THE REMAINS OF PLA%}NTS AND ANIMALS IS CALLED](`(ü( 1. HUMUS((( 2. RESIDUAL SOIL((( 3. WEATHERED \6ƒ-@%} AP((0( YOUR CHOICE?4„> B'gDƒ"„R6…-…%@\ A $! ƒ„6†-†%@! A@.a[(SSMALL%‘} PARTICLES, RANGING FROM MICROSCOPIC SIZE TO ABOUT 2MM, ARE CALLED:^(a(8( 1. GRAVEL(B( 2. SAND(%’}L$$( 3. SILT AND CLAY PARTICLES V\6ƒ-@ A((0( YOUR CHOICE?4„> B'gDƒ"„R6…-…%@\ A %“}`! ƒ„6†-†%@! A@j71()QUARTZ IS THE MOST ABUNDANT MINERAL IN:4(7(t( 1. GRAVEL(~( 2. SA%”}ND(ˆ( 3. SILT’\6ƒ-@ Ap((0( YOUR CHOICE?4„> B'gDƒ"„R6…-…%@\ A œ! ƒ„6%•}†-†%@! A@Š;5(-PARTICLES MOVED BY WIND OR WATER ARE CALLED:8(;(°( 1. RESIDUAL SOIL(º( 2. PAREN%–}T ROCK(Ä( 3. TRANSPORTED SOILÎ\6ƒ-@ A0((0( YOUR CHOICE?4„> B'gDƒ"„R6…-…%@\ A%—} Ø! ƒ„6†-†%@! A@âOI(ASOIL THAT STAYS WHERE IT WAS FORMED AND DOESN'T MOVE IS CALLED:L(O(ì( %˜}1. RESIDUAL SOIL(ö( 2. PARENT ROCK(( 3. TRANSPORTED SOIL \6ƒ-@ A((0( YOUR CHOICE?4„%™}> B'gDƒ"„R6…-…%@\ A ! ƒ„6†-†%@! A@#(RESIDUAL SOIL SITS ON (#((( 1. SUBSO%š}IL(2( 2. TOPSOIL(<( 3. PARENT ROCKF\6ƒ-@ AP((0( YOUR CHOICE?4„> B'gDƒ"„R6…-…%%›}@\ A P! ƒ„6†-†%@! A@Z1+(#A SEPARATE LAYER OF SOIL IS CALLED:.(1(d( 1. A HORIZON(n%œ}( 2. THE BED ROCK(x( 3. A PLAIN‚\6ƒ-@ A((0( YOUR CHOICE?4„> B'gDƒ"„R6…-…%@%}\ A Œ! ƒ„6†-†%@! A@–( TOPSOIL IS:(( ( 1. HORIZON A(ª( 2. HORIZON B(Ž( %ž} 3. HORIZON CŸ\6ƒ-@ Ap((0( YOUR CHOICE?4„> B'gDƒ"„R6…-…%@\ A È! ƒ„6†-†%@%Ÿ}! A@Ò( SUBSOIL IS:((Ü( 1. HORIZON B(æ( 2. HORIZON C(ð( 3. HORIZON Dú\6ƒ-@ % }A0((0( YOUR CHOICE?4„> B'gDƒ"„R6…-…%@\ A ! ƒ„6†-†%@! A@( BED ROCK I%¡}S:((( 1. HORIZON B("( 2. HORIZON C(,( 3. HORIZON D6\6ƒ-@ A((0( YOUR CHOICE?%¢}4„> B'gDƒ"„R6…-…%@\ A @! ƒ„6†-†%@! A@J-'(PARTLY WEATHERED ROCK MAKES UP:*(-(T%£}( 1. HORIZON B(^( 2. HORIZON C(h( 3. HORIZON Dr\6ƒ-@ AP((0( YOUR CHOICE?4„> B'%€}gDƒ"„R6…-…%@\ A |! ƒ„6†-†%@! A@†+%(YOUNG IMMATURE SOIL HAS ONLY:((+(( 1. A AN%¥}D B HORIZONS(š( 2. A AND C HORIZONS(€( 3. B AND C HORIZONS®\6ƒ-@ A((0( YOUR CHOICE?4%Š}„> B'gDƒ"„R6…-…%@\ A ž! ƒ„6†-†%@! A@Â(MATURE SOIL HAS:((Ì ( 1. ALL FOUR %§}HORIZONS (Ö( 2. ONLY A HORIZON(à( 3. B, C AND D HORIZONSê\6ƒ-@ Ap((0( YOUR CHOICE?4„>%š} B'gDƒ"„R6…-…%@\ A ô! ƒ„6†-†%@! A@þYS(KTHE TYPE OF SOIL MOST COMMON IN THE EASTERN %©}PART OF THE UNITED STATES IS:V(Y(( 1. GRASSLAND(( 2. FOREST(( 3. PRAIRIE&\6ƒ-@ A0%ª}((0( YOUR CHOICE?4„> B'gDƒ"„R6…-…%@\ A 0! ƒ„6†-†%@! A@:NH(@THE TYPE OF SOIL M%«}OST COMMON IN THE DRY REGIONS OF THE WEST ISK(N(D( 1. TUNDRA(N( 2. PRAIRIE(X( 3. DESERTb\6ƒ-@%¬} A((0( YOUR CHOICE?4„> B'gDƒ"„R6…-…%@\ A l! ƒ„6†-†%@! A@v]W(OBETW%­}EEN THE EASTERN FOREST AND THE ROCKY MOUNTAINS THE MOST COMMON SOIL IS:Z(](€( 1. GRASSLAND(Š( 2. PRAIRIE%®}(”( 3. TUNDRAž\6ƒ-@ AP((0( YOUR CHOICE?4„> B'gDƒ"„R6…-…%@\ A š! ƒ„6†%¯}-†%@! A@²QK(CTHE NUMBER AND SIZE OF THE OPEN SPACESOR PORES IN A ROCK IS CALLED:N(Q(Œ( 1. PERMEABILITY%°}(Æ( 2. POROSITY(Ð( 3. AQUIFERÚ\6ƒ-@ A ((0( YOUR CHOICE?4„> B'gDƒ"„R6…-…%@%±}\ A ä! ƒ„6†-†%@! A@înh(`A MEASURE OF THE SPEED WITH WHICH WATER CAN MOVE BETWEEN THE PORE SP%²}ACESIN A ROCK IS CALLED:k(n(ø( 1. PERMEABILITY(( 2. WATER TABLE( ( 3. POROSITY\6ƒ-@ A p%³}((0( YOUR CHOICE?4„> B'gDƒ"„R6…-…%@\ A  ! ƒ„6†-†%@! A@*d^(VTHE LEVEL BELO%Ž}W THE SURFACE WHERE ALL THE OPEN SPACES ARE FILLED WITH WATER IS CALLED:a(d(4( 1. AN AQUIFER(>( 2. A SPRING%µ}(H( 3. THE WATER TABLER\6ƒ-@ A p((0( YOUR CHOICE?4„> B'gDƒ"„R6…-…%@\ A \! %¶}ƒ„6†-†%@! A@f?9(1WHEN THE WATER TABLE MEETS THE SURFACEIT FORMS A:<(?(p( 1. AQUIFER(z( 2. %·}CAVERN(„( 3. SPRINGŽ\6ƒ-@ A p((0( YOUR CHOICE?4„> B'gDƒ"„R6…-…%@\ A ˜! %ž}ƒ„6†-†%@! A@¢QK(CA HOT SPRING THAT SHOOTS WATER AND STEAM INTO THE AIR IS CALLED:N(Q(¬( 1. AN AR%¹}TESIAN WELL(¶( 2. A VOLCANIC VENT(À( 3. A GEYSERÊ\6ƒ-@ A p((0( YOUR CHOICE?4„> B'g%º}Dƒ"„R6…-…%@\ A Ô! ƒ„6†-†%@! A@ÞJD( B'gDƒ"„R6…-…%@\ A  ! ƒ„6†-†%@! A@ E?(7A POROUS LAYER OF SOIL UNDER%œ} THE GROUND IS CALLED:B(E($ ( 1. A SPRING(. ( 2. AN ARTESIAN WELL(8 ( 3. AN AQUIFERB \6ƒ-@%Ÿ} A p((0( YOUR CHOICE?4„> B'gDƒ"„R6…-…%@\ A L ! ƒ„6†-†%@! A@V KE(=WHEN WAT%¿}ER DISSOLVES LIMESTONE UNDER THE GROUND IT CAN FORM:H(K(` ( 1. CAVERNS(j ( 2. GEYSERS(t ( 3. SPRINGS~ %À}\6ƒ-@ A p((0( YOUR CHOICE?4„> B'gDƒ"„R6…-…%@\ A ˆ ! ƒ„6†-†%@! A@’ %Á}QK(CLONG ICICLES OF STONE HANGING DOWN FROM CAVERN ROOFS ARE CALLED:N(Q(œ ( 1. STALACTITES(Š ( 2. STALAGMIT%Â}ES(° ( 3. SINKHOLESº \6ƒ-@ A p((0( YOUR CHOICE?4„> B'gDƒ"„R6…-…%@\ A Ä ! ƒ%Ã}„6†-†%@! A@Î f`(XA MOUND OF STONE THAT SEEMS TO BE GROWING UP FROM THE FLOOR OF A CAVERN IS CALLED A:c(%Ä}f(Ø ( 1. STALACTITE(â ( 2. STALAGMITE(ì ( 3. SINKHOLEö \6ƒ-@ A p((0( YOUR CHOICE?4„%Å}> B'gDƒ"„R6…-…%@\ A  ! ƒ„6†-†%@! A@ pj(bWHEN A CAVERN CAVES IN FORMING A DEPRES%Æ}SION ON THE SURFACE OF THE GROUND IT IS CALLED A:m(p( ( 1. STALACTITE( ( 2. STALAGMITE(( ( 3. SIN%Ç}KHOLE2 \6ƒ-@ A p((0( YOUR CHOICE?4„> B'gDƒ"„R6…-…%@\ A < ! ƒ„6†-†%@! A%È}@F (}P 4( (( THERE WERE "6‡-…%†4(‡ QUESTIONS.Z (( YOU MISSED †d !(!(YOU GOT … CORRECT!n%É} B }ÐÒÏÔÅÃÔ ÅÎÄ ÒÏÕÔÉÎś }-@A } (}}@-@@@(&‘’’’’’’’’’’’’’’’’’’’’’’’’’’%Ê}’’’’’’’’’’…(}@-@@@(&ü                                    ü2}@-@@@(&ü ÔÙÐÅ §ÒÕΧ ÔÏ ÂÅÇÉΠÐÒ%Ë}ÏÇÒÁÍ ÁÇÁÉΠ ü<}@-@@ @(&ü                                    üF}@-@@@(&ü ÔÙÐÅ §ÅÎħ ÔÏ ÆÉÎÉÓ%Ì}È ÔÈÉÓ ÐÒÏÇÒÁÍ  üP}@-@@@(&ü                                    üZ}@-@@@(&ü ÔÈÅΠÐÕÓÈ [RETUR%Í}N] ËÅÙ ÔÏ ÅØÅÃÕÔÅ  üd}@-@@@(&ü                                    ün}@-@@@(&š’’’’’’’’’’’’’’%Î}’’’’’’’’’’’’’’’’’’’’’’ƒx}Ž;@,(Ž‚} Ž4END% D:SCIMENU.SYSŒ} Ž4RUN @–}"Ž0RUN)Ž0END%Ï}" B ÿ D2:WEATHERIŽ;@,(Ž‚} Ž4END% D:SCIMENU.SYSŒ} Ž4RUN @–}"Ž0RUN)Ž0END$