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Show 33G NAM( TIM'- DIHECTIOlS : Carefully r2.d t he cr'ob Lem ,- ..,!!ovn (1 \ ariswe r a ...... d L l-'n"'" ,,,eo, ..11 1-' . (3) steps sc use correct i errt i f i,c ari L'Ci!':etic no t a'ti on numo r Lca I (L\)' \ r n; si '" p r cpe r , 'r> grd.f i.ca '" , rce I dUI,O),<=:; t ,, - f'ac a. t d-::._"'...gram 'a (5" unit I ", ' (2) procedural '-." ,- an n swe r Ln': . :;:>']"'lYS1'" ,6a-ranh<...... 0""', c. -. - . '" ,.., L p fu 1 • ' and C nar t s -:::... . • younge s t rock c;_:;::r)inr.r til t e d f'au Lt b Lock v. j,:lom1tcUTlS 18 Li .ime st one corrtn i ni.nz -,. 0 ,,'1 da u.ted {O rraIllon verc 13 -p f O"'vlS The I'lme S t OTIC 1 alcr ' ..... as separa t e d 20GO m + by a no rma L fault be I,'.-feen the t,.-lO t i I t e d b l.oc\... ks An'lce a,::,e J < ak e f OITI8d ce l;' .;ecn the ,1 1 1 OvKS '>rr'l I.i e ft a :.1. l..."). ve cu t o terrace 10m h.i g"er on on e b L oc=( t·,n.an on t 'I.. he other It d i sappea red 10,01)0 yp.;:>_rs az'o If f'au l. f..'; l'was un i f'oz-m ;:_, .J..I., now 1 ong a f,t er t'ne Irmstone -.. _"+ d dOd' l tn::: faul t.Lnz ce c i n (+0 +h" near e "''' vas d e po s i "e. s t rIl L'I' _lon years )? ':" ,.(1 L'", d,;,.. r au r t i ne rate wna .t .La the I{TIJ1r. .l.' s i nce tho ice aEe" : v '/h a t tlmc '-las :::> requlre d to ? separate <; h e layer. Relate this to the age of the coral fossils. The 1. • , - J. - • c;.••• 'J • .' - - cora 1 - • .. - P' - ,..., .. --. - . I ... .1. • ' • . .- ' e. ... '. , '.J _ , 1"· • , , - v .... .... " . v.___ v -- ---. ' . , co , • • :::.> • - . DIAGRAI1: 70,000,000 years 3. About 3000 km of dF}0 _Q oc e an se:9e.'c-"te La::-rador from Sc.andanav i.a , but recent remnant Ta[:91etism studies indicate they wre once joined together and oved apart " rock s amp l e s from both ar-eas appear to be of simi "Ba.semerrt about 1. 5 ern a ye2.:r. than of lar geologic age because they all corrt a i n about 3 times more at oms of is of ura.nium a50ut half life and the 4 uranium. vas once Lead he all t lead If billion years, how lJ1any times older is the "shield" area than the Atla!1tic Ocean? \·rhat half life HINT: HOI., could d i s t anc e and rate help de t e rmi ne when it separated.? U28 •. :":B:: t);:l:?\.:(: A:r;lntfBl l-!- I" is near i ng 6 billion. 4. \'!orld population th2.t.. TJ:: .. , It doubles about every 37 years and life both populate the ext enertion o:iginaJ, a.l"} expe c t ancy is about hlice of Lnhab i table dry land on 'l'here a s about 120 IiUl110n km earth at the same t i me Lorize r would it take to produce a how many years 2 D2.rents, from earth Startl-nf:" 0 '... 2 t h an 11. l; t' 0 "9rO d uce vcu Id't axe m "s t and i ng room on'l y" population of 1 person per technology, factors eV01ution? w, the present population? Keglect , • • - v For calculating and the Row many is required to reach 6 • 37.1 sit;nificant figures. would be only" popul2.tion? How ma.ny generations How Compare. yea.rs? room"? many reach "standing fires to two final time HINT: DIAGR.>.H: uch"as rate_an OnglvlY. cont@:t reroauctlon oe Sl11flcant flgure and assume a to ccnveince, rod ofr pO?Ulatlon flgures disease famine, pollution, '!sta:-lding ,,"s. r'ooc billion, to [; __ 2 4- - 8 fTC. • 200 lO 400 40 80 800 |
