were 0.0026 in. or less in diameter, when observed with a microscope
appeared to be perfectly clean grains of quartz; to the eye it looked
like ordinary building sand, sharp, and well graded from large to small
grains. This sand, with a surplus of water, was quick. With the water
blown out of it by air pressure, it is stable, stands up well, and is
very easy to work. It appears to be the same as the reddish quicksand
found in most deep excavations around New York City.

The second material was pronounced "bull's liver" by the miners as soon
as it was uncovered. "Bull's liver" seems to be a common term among
English-speaking miners the world over. It is doubtful, however, if it
is always applied to the same thing. In this case it consisted of layers
of blue clay and very fine red sand. The clay seemed to be perfectly
pure and entirely free from sand. It would break easily with a clean,
almost crystalline, fracture, and yet it was soft and would work up
easily. The layers of clay varied in thickness from 1/16 in. to 1 in.,
while the thickness of the sand layer varied from 1/4 in. to several
inches. The sand was the same as the quicksand already described.

The "bull's liver" was ideal material in which to work a shield. It
stood up as well and held the air about as well as clay, and was much
easier to handle.

The third material was a layer of fine gray sand which was encountered
in the top of all the tunnels for about 400 ft. just east of Blackwell's
Island Reef. It was very open, and had grains of rather uniform size.

During the starting out of the tunnels from the shafts, and for more
than a year afterward, the roof of the working chamber in the caissons
and the locks previously described under the Long Island shafts took the