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524 June 8, 2011 Mr. Sindulfo Castillo Chief, Regulatory Section Corps of Engineers San Juan Area Office 400 Fernandez Juncos Avenue San Juan, Puerto Rico, 00901-3299 RE: LSJ, LLC (Little St James Island) Installation of two (2) moorings St Thomas, Virgin Islands Dear Mr. Castillo: Enclosed is an

leading edge of a blowout which is recolonizing with grass species. Halodule beaudettei is present within the blowout in addition to Thalassia and Syringodium. This blow out is much lar t er and is movie L in a northerl direction. The mooring design will limit impact on the seafloor and the surrounding be

rown up by block faulting during the late Pliocene or early Pleistocene. It is oriented generally northeast to southwest, separating St. Croix from Puerto Rico and the other Virgin Islands. Based on shallow focus earthquakes, the Anegada Fault Trough is estimated to be more than 400 miles in length. There

onized area before the bottom begins to become colonized by Syringodiztmfilifonne which slowly grades into a mixed bed of Thalassia testitudium and Syringodium. The exotic seavine Halophila stipulacea is also present. This seavine was not present in 2006. There was a very large intact Acropora cerviconzis

rown up by block faulting during the late Pliocene or early Pleistocene. It is oriented generally northeast to southwest, separating St. Croix from Puerto Rico and the other Virgin Islands. Based on shallow focus earthquakes, the Anegada Fault Trough is estimated to be more than 400 miles in length. There

. faveolata and Dendrogyra cylindrus as well as other coral species. Offshore there are dense seagrass beds consisting of 77u2lassia testudinum and Syringodium fihforme, however these are greater than the 75ft off shore which the barge will extend while moored. There very sparse Syringodium colonization wi