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State Department of Conservation, who had an idea that a spelunker from Pittsfield, Massachusetts, would know about them if anyone did.

   "Miss Kemp had written that "a group of us are planning to visit the east this summer and wish to explore caverns known as 'the East Caves of Syracuse.' These caves are said to be the western entrance to the subterranean passage which extended under the Atlantic Ocean to the British Isles. Parts of the cavern system have collapsed - one as recently as 1928 - so that it is now impossible to travel in them. However, the entrances remain intact."

   "It took but a few minutes of research in the geology department of the State Museum to discover that there actually are some caves east of Syracuse, and that they are curious ones, indeed, and deep and some of them quite long, for in 'The Geology of the Syracuse Quadrangle' by Thomas Cramer Hopkins, published as 'New York State Museum Bulletin 171,' in 1914, there was found not only an elaborate study of the "East Caves of Syracuse," but photographs taken, exteriorly, of some of the odd crevices, with people perched in them.

   "These crevices are in Onandaga limestone, which is the hardest kind found in New York State and which spreads clear across the Syracuse quadrangle, in some areas forming large, level floors of rock swept free of residual matter by glaciers and the wash of water, and with deep clefts in the rock.

   "One of these areas lies along the top of a cliff that borders what is known as the Clark Reservation, a state park, about three miles southeast of Syracuse...

   "This officially confirms Miss Kemp's long-distance tip on caves which, until June, 1947, had completely escaped the attention of present-day geologists, speleologists, and spelunkers as well as the usually alert boosters of the Syracuse Chamber of Commerce,