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MANHATTAN ISLAND                        45
hattan Island rocks are very rare, or unknown. The follow­ing interesting note of J. Howard Wilson, connected with ex­cavations in Rector Street, is suggestive of a former boreal climate:
" In excavating for the new building for the United States Express Company, on Rector Street, between Sixth and Ninth Avenue elevated, Mr. Daniel E. Moran, C. E., found resting on the bedrock forty feet below the surface a small deposit of Venus shells, fragments of wood and some peaty matter. This deposit was covered by ten feet of glacial drift which, in turn, was buried under thirty feet of sand, probably of post-glacial age. The fossiliferous deposit was apparently protected from the ice action in this spot by a local ledge or shelf of the bed­rock.
The Venus shells resemble very closely those of the recent V. mercenaria Linn., but differ from them somewhat and along a line which seemed to identify them with the variety antiqua of Verrill from the Pleistocene deposits of Sankaty Head, Nantucket. The Manhattan specimens were compared with a number of these in the collections at Columbia University, and the identification was found to be complete. The variety an­tiqua is an unusually massive and strongly sculptured variety."
This shell—a hard-shell clam or quahog—is regarded as symptomatic of cold currents, and has been found in shell beds on Nantucket Island, in which were unmistakably associated species of shells decidedly northern in habit.
Professor William H. Hobbs * has taken pains to investi­gate the underlying rock flooring of Greater New York, and has gathered together a great many records from the en­gineering work carried on in the construction of the East River bridges, the tunnels of the Pennsylvania R. R., the vari­ous municipal bridges connecting Long Island with New York, the Croton aqueduct, the Subway in Manhattan, the Harlem Ship Canal, together with the reports of borings, excavations,
♦The Configuration of the Rock Floor of Greater New York, William Herbert Hobbs, Bulletin 270, United States Geological Survey.