HG 380.85-380.95

Brown sediment with alternating layers of dark and light sediment. Clasts range from small to large, and are sub-angular. Lineations are abundant in this sample, trending mainly in one direction. Some rotation structures are present.

HG 384.60-384.70

Dark brown sediment with scattered amounts of small clasts and medium clasts as well. Clast shape ranges from sub-angular to sub-rounded. Lineations and water escape structures are abundant in this sample.

384.85-385.0 DE # 11

Mainly coarse grained with a separate fine grained clay domain occurring throughout the sample. The coarse grained domain contains clasts that range from small to medium in size. The clast shape ranges from angular to sub-angular. Grain crushing is abundant in this sample, along with lineations, and minor amounts of rotation.

DE # 10 341.20-341.40

Grey sample with clasts that range from small to medium in size. The clast shape ranges from angular to sub-rounded. It mainly contains lineations and grain crushing. A few comet structures are also visible throughout the sample.

HG 388.75-388.85

Dark brown sample with clasts that range from small to large. The clast shape ranges from angular to sub-rounded. Grain crushing is present in this sample along with some lineations. Faint water escape structures can also be seen.

HG 393.60-393.85

Brown sediment with clasts that range from small to large. The clast shape ranges from angular to sub-rounded. Lineations and water escape structures are present. Grain crushing and minor amounts of rotation are also present.

HG 401.70-401.80

Light brown sediment with mainly small clasts. The clasts are sub-rounded in shape. Lineations are abundant. Grain crushing and stacking are also present.

HG 404.20-404.30

Brown sediment with clasts ranging from small to medium in size. The clast shape ranges from angular to sub-rounded. Lineations are abundant in this sample. Faint water escape structures can also be seen as well as grain crushing/stacking.

HG 406.85-406.95

Brown sediment with organic matter and clasts ranging from small to large. The clast shape ranges from sub-angular to sub-rounded. Lineations and grain stacking are the most abundant in this sample. Minor amounts of grain crushing can also be seen.

HG 421.15-421.25

Brown sediment with a coarse grained domain and a fine grained domain. The coarse grained domain contains clasts that are small to medium in size. The clast shape ranges from sub-angular to sub-rounded. The coarse grained domain is abundant in lineations. The fine grained domain contains many faint water escape structures. A few rotation structures can also be seen throughout the sample.

HG 421.50-421.60

Light brown sediment with clasts that range from small to large in size. The clast shape ranges from sub-angular to sub-rounded. Lineations and rotation structures are abundant in this sample. Edge-to-edge grain crushing is present as well. There are areas of light and dark sediment throughout the sample. A few comet structures can also be seen.

HG 427.45-427.55

Brown sediment with grains ranging from small to large. The clast shape of this sample ranges from sub-angular to sub-rounded. Grain crushing can be seen in large amounts, and commonly involves the larger grains. Many of the larger grains are also fractured. Lineations and comet structures can also be seen.

HG 434.40-434.55

Brown sediment with clasts ranging from small to medium in size. The clast shape ranges from sub-angular to sub-rounded. Grain crushing is abundant throughout the sample, and mainly involves medium sized clasts. Lineations can also be seen. A finer, and darker brown domain is also present within the sample.

HG 436.0-436.15

Light brown, coarse grained sample with grains ranging from small to medium in size. The clast shape ranges from sub-angular to sub-rounded. Edge-to-edge grain crushing is present in large amounts throughout the sample. Lineations can also be seen throughout the sample.

HG 437.50-437.55

Light brown sample with clasts ranging from small to large. The clast shape ranges from sub-angular to sub-rounded. Grain crushing is common in this sample and mainly involves the larger clasts. Many grains are also crushed into one another. The larger grains are also fractured. Lineations and faint water escape structures can also be seen. This sample also contains a finer grained domain, darker in colour.