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Show Ocean Encroaching s ons on } IslanLn IslanjEngland on"Tight "Tight Tight " Little Islan Islanj ' Ln England lc.111d lc111d . is gradually gMdunlly . Inthe itlle ! > sinking IDI.Ing IDIIng i to : tlle the sea set 5c ' ' } , , ficcordln according to a n recently lI'1hed lI1hed lished pilishcd ptlI'1hed ptlished ' " pt government "Blue Blue Paper ' B Bkeep Bheep heep keep J ! sour our seats , pIC'1 pIC1 please-the please the please ' e-the e the - the rate ratel rater ; tlie t1le the ratelt1le raterthe suh subsidence ldence is estimated { nInches nlInches at nl ni ) Accordto Acc.ordlto Accordito Inches per hundied hunched hundred vcars ve'lrs velrs vears ' ? ' Acc.ordl Accordl Accordi . ! to the report , tel1"tstoeon Pelivstoue--on Pelivstoue on Pelixstow tel1"tsto\\ tel1"tsto tel1tsto " teast \ e-on e on - e - - on t east cO'lst-Is cO'lst cOlst Is co'ist-is co'ist coist coast ' ' - is sufferln suffering from " ! "t t "tsinking I slnkmg sinking "tlsinking tlsinking nemitwo feehn feeling " It has 11'15 1115 ' sunk ne nemi Itwo ycSThe two ncnitwo inches mches in the past fifteen yea yeaa a The yeaThe heartthe Bank Banb . of ; England Ingland , in the heart the metropolis , is 1 & > over six mC'hes mChes ineheslo inchesIocr inehesloer ' 10 10cr cr er than th'1n th1n ' in 1805 1SGj 1593 < ) St t Paul a s cnthedr catlmedr cnthedron catlmedron cnllieddon . on the other h'm hm hand h'tnd htnd ' , has h'1s h1s ' dropped 0 o three ontlireo othree JThat penodThat periodThat inches Inche , in the ' same 5ame period penod J That tlicie thele theie Is n a definite mcveme moveme mcvemeof movemeof movemeof of the land hnd in relation to the ' moments moments mo moments cojfirmed cofirmed ments of the tide has h'1.9 h1.9 h19 ' . now been bE'en ' co firmed A selsniogiaph elsmoglaph seismograph in the conn corm | connhall connh'lll cormhall h'lll hlll hall ' , , Westminster , displayed dicpla\"ed dicpla "ed ed dicpla"eda dieplaved dieplaveda : ' \ " a mov.ment movment no mo noment momeat ! . ment meat Qf of the building bUlldmg correspondll correcponcll correspondi ; ; correspondiw ' \ w \ ith mth high hgh high ( and low t1de tides < ; ObCUT'ltI ObCUTltI Obscrvatl ObCUT'ltIon Obscrvatlon OburvatKon : ' on Waterloo W'1.terloo W1.terloo W1terloo ' . bridge revealed re\ealed re ealed \ that ttweight t tweight tweight , weight of the water w'1ter w1ter ' c'lu clu caused ' < ; ed th the < > stru strutura struturc tura ture to sink sinle at 'It It ' high tide nnd nncl rI r1 r1again rIng11n riagain ] ng11n again at 'It It ' low tide Railway n'111\\ay n'111 n111 ay Ralhtay ' \ and nail ot1\ ot1 ot1tunnels otl otltunnels oth1tunnels \ tunnels which run beneath benC'1th benC1th bene'ith beneith ' ' t tThames tThames tilThames Thames have 11Re Katie 11R\ 11R \ e been found tp tfl thantheir cl1nn than cl1nnt1wlr chantheir | t1wlr their sliaps shape at high hrgh tide tJel ] ' The TIle c cculnr ccular ccular | culnr cular tunnels tunDelq are nre slightly shghttv flatten flattenbut flattenbut fiattcnbut | but return to their normal chapethe ; shape chape tthe ' the tide trde rece recedesMontreal recedes es es'fontrc'11 -'fontrc'11 'fontrc'11 fontrc11 -Montreal Montreal - ' Montreal ' ITera llera ncral |