and comsnintion. avea, ty o Oy 3 Cr 8 dust inside this vides is a particularly flat . ba CAN faa 4 apt chat ar] It wuns about £00 foot in width and a solid paveomont. g3 generally consicored as one of the areans G? 4 "3 bie ou | ns 3 “yep mann oyen de it is a pavement, eng not hore Zt is honucyesmsed uncernocath eelarst (indicating) but in ae reel not for avay asmo of tho honoyecubod areas break throunsh so that you havo rolls holes that yeu find only these forms which aro ca themselves vovy therougaly acadast the battrorins eaanm 4: OF agen nw . mys You have enerysting forms of coral and you Yhave sz = © e+ Ja mee Bt To clans and soma of“4 tho soa urchins waieh hang on Qe. me OY USAR GvVazy r. y Ps In sone areas, an area the sise ofTt Ty this twta t (indicating) wi the welativitys eqnite hich, As we move clong here (indicating) which is about 39 fest wido, we run into a boulder area, This boulder area is raised scnewnat over thse gencral reef surface so that it is exposed at very low tida, We have rot made any studics in this aroa. \ It is way out on the roof in the Isiand, and it is very cdizticult to get to, and it is rot a particularly ri eh aroa froma our point of view. Just inside, we have what has been called @ coral zone. This aren oven at low tide,“? whicth,is cov erad fest of water--you have a rich crowth of coza alae with 2 te 4 a is ae 52 e144 aa es Si ee -?