1971-72 Varsity Curling

Pictured here from left to right are: Front - John Donald, Greg Reid, Steve Thomas, John Glennie, and Mike Wilder. Back - Ed Davis (Coach). The 1971-72 curling team boasted a number of achievements including being the Niagara Distrcit Major Champions, University of Toronto Bonspiel Champions, and the Ontario University Athletic Association Champions.

1971 - 72 Oarsman of the Year

1971 - 72 Oarsman of the year, Dave Freshwater, receives his award from rowing coach Tony Biernacki.

HG 188.30-188.35

Very fine grained. Organic matter present. Lineations can also be seen throughout, mainly in one orientation suggesting a masepic fabric.

HG 198.20-198.35 Thin Section

Coarse grained brown sediment with angular-sub-angular grains. Contains mainly medium sized clasts with a few smaller aggregates. A dark organic rich domain can be seen within this sample. Grain crushing (edge-to-edge and into one another) can be seen alongside with grain stacks, and silt caps.

HG 216.35-216.45

Brown, coarse grained sample. Clasts range from small to medium in size and sub-angular to angular. Patched of clay rich domains can be seen throughout the sample. Rotation with and without a central grain can be seen throughout the sample. Edge-to-edge grain crushing and grain stacking can be seen throughout the sample.

HG 261.25-261.35 Thin Section

Brown sediment with small clasts, and an occasional medium sized clast. Clasts appear to be sub-rounded in shape. The sample contains many lineations, the majority oriented in the same direction. There are also darker areas present in the sample, they may contain organics.

HG 458.25-458.35

Dark brown sediment, with clasts ranging from small to large. The sample mainly contained smaller clasts. The clast shape ranges from sub-angular to sub-rounded. Lineations were common throughout the sample. It also contained areas with dark organic material, and a few faint water escape structures.

HG 482.15-482.35

Brown sediment with a coarse grained domain and a few finer grained domains throughout the sample. Clasts range from small to large in size and angular to sub-rounded in shape. In the coarser domain, grain crushing is common. A few rotation structures can also be seen throughout the sample, along with lineations.

HG 498.20-498.35

Coarse grained sample with clasts ranging from small to medium in size. Clast shape ranges from angular to sub-rounded. Lineations and rotation structures are common in this sample. Grain crushing and comet structures are also present in minor amounts.

HG 35.0-35.10

Brown sediment with clasts that range from small to medium in size. The grain shape ranges from angular to sub-rounded. Lineations and rotation structures were the most common throughout the sample. Grain crushing/stacking and a few comet structures were also present. Clay material was also dispersed throughout the sample.

HG 77.35-77.45

Brown sediment with clasts ranging from small to medium in size. The clast shape ranges from angular to sub-rounded. Lineations are the most abundant in this sample, along with grain crushing. A few comet structures and rotation structures can also be seen throughout the sample.

HG 87.30-87.35

Dark brown sediment with clasts ranging from small to medium in size. Clast shape ranges from angular to sub-rounded. Rotation structures and lineations are common throughout the sample. Comet structures and grain stacking/crushing can also be seen in minor amounts.