A series of 40 impact tests was conducted on large right-circular cyli
nders (68.5 cm diameter and 25.7 cm thickness) of iceberg ice collecte
d from an iceberg in Labrador. Temperature profiles were also obtained
for the iceberg and the profiles exhibited differences associated wit
h the probe location. Temperatures as low as -15 degrees C were measur
ed at penetration depths of about 8 In. The impact specimens were conf
ined at the perimeter and base by a rigid metallic ring and prate. A s
pherically terminated impactor, with center-mounted pressure transduce
r, was dropped on to the flat top surface of specimens from various he
ights and with various added masses. Impact velocity varied from 1.8 t
o 3.9 m s(-1); impactor mass varied from 155 to 510 kg and the ice-spe
cimen temperature varied from -0.5 degrees to -14.5 degrees C. Peak ce
nter pressures averaged from about 25 MPa at the highest temperature t
o about 41 MPa at the lowest temperature, with the highest recorded pr
essure being 50 MPa. Crater volume increased with increasing impact en
ergy, as expected; however, the specific energy of the ejected materia
l was found to decrease as the energy of impact and crater volume incr
eased. A mechanism for this observed behaviour is proposed.