i's bng aten awa you kno where i's jt a litt bit by ttle bit getng destred. now,he only ting is,he piecof land is lting lonr than t human body c. the onright he is an o fielcanal. ere's one tht passesere. the's one at pass a bit fther, and the's e that pses in the backso you're loing at water oraltwaterntrusion comg from t pipelincanals, and ey destred the getationhat we ud to have.. but, u know, st of th peopleork for e oil cpanies. ey' the on at' puttingood and ying the re and morages andtuff like tha so, as ch as yo hate tm, youave to ke them. dup: isle djean chaes is-- at' the comon sayig?--the cana in the ne fieldwe' eing--or here, call it elative a level se. you have thelobal selevel ri, whch is slht, but out 80% of theea levelise heres cause osubsiden, so we both ssiding a you havthe glol sea lel rise athe same tim so were sinkg by, i thinit'3 milliters a year. idoesn't sound ke much, buyou go io 40 years50 yea, and yostart tnotice dferenceshen yo're ready on slightl abovthe watelike islde jean chaes. brun: in theeginningit was a sloprocess.t was rely