251.8-251.9 D.E #5

Sample contains well dispersed clasts ranging from small to medium in size. They are sub-angular to sub-rounded in shape. Organic rich domains can be seen throughout the sample with clear boundaries. It also contains water escape structures, seen mainly through clay. Lineations are also present.

HG 295.70-295.80 Thin Section

This sample contains two different domains; a coarse grained domain with well dispersed clasts, and a fine grained domain that potentially contains organics. The coarser grained domain contains comet structures, lineations and minor rotation without a central grain.

HG 297.25-297.35a Thin Section

Brown sediment with well dispersed clasts. Clasts range from small to medium in size and sub-angular to sub-rounded in shape. Alternating domains can be seen (light and dark). Darker domains appear organic rich. Lineations can also be seen throughout the sample.

293.9-294.0 DE # 7

Brown sediment with well dispersed clasts. Clasts range from small to medium in size and angular to sub-rounded in shape. Some appear to have been weathered. Water escape structures can be seen, mainly in finer, clay rich sediment. Lineations can also be seen throughout the sample. Minor grain stacking and crushing are also present.

HG 473.45-473.55

Light brown, coarse grained sediment with a few patches of a finer grained domain. Clasts range from small to medium in size. The finer grained domain mainly contains small sized grains that are very well dispersed. Clast shape ranges from angular to sub-rounded. Edge-to-edge grain crushing is common in the coarser domain, with a few grain stacks. The finer grained domain contains a few lineations.

HG 82.50-82.65

Dark brown sediment with well dispersed clasts ranging from small to medium in size. Clast shape ranges from sub-angular to sub-rounded. Lineations can commonly be seen throughout the sample. Comet structures can also be seen in minor amounts.

ARTHUR 3

Dark brown sediment, almost appears black. This may be due to organic material. Clasts are very well dispersed and range from small to medium in size. The clast shape ranges from angular to sub-rounded. Lineations can be seen in this sample. There are also a few examples of grain crushing that can be seen.

PB #2B

Dark brown sediment that appears almost black. This may be due to organic content. Clasts are well dispersed and range from small to medium. The clast shape ranges from angular to sub-rounded. Lineations can be seen throughout the sample. Grain crushing can also be seen in minor amounts.

PB 3 (Y) KZ

Dark brown sediment, almost black due to organic material. Mainly structure-less with a few well dispersed clasts. Grains range from small to medium in size and sub-angular to rounded in shape.

PB 1C(z)

Dark brown sediment with well dispersed clasts. The clasts are mainly small and range from sub-angular to rounded in shape. This sample is mainly structure-less but does contain lineations.

PB4

Dark brown sediment with well dispersed clasts. Clasts are mainly small and range from sub-angular to rounded. Not many structures are present in this sample, aside from some lineations.

PB14

Dark brown sediment with a few well dispersed clasts. Grains are small, and range from angular to sub-rounded. This sample is mainly structure-less with a few lineations.

PBURWELL #1-87

This sample contains two main domains. One is a light brown sediment domain with mainly small clasts which are clustered together. Only a few larger clasts can be seen in this domain. The other one is dark brown with well dispersed clasts. The light brown domain contains clasts that range from sub-angular to sub-rounded in shape. Lineations can be commonly seen in this domain. Grain crushing is also common with minor amounts of rotation. In the dark brown domain, clasts range from small to medium in size. They range from sub-angular to sub-rounded in shape. A few lineations and rotation structures can be seen in this domain.

PBURWELL #5-87

Brown sample with two domains. One domain contains many small grains that are clustered together. The other domain is a darker brown and contains clasts that are well dispersed. The clasts range from small to large, and are angular to sub-rounded in shape. Lineations are commonly seen throughout both domains. A few rotation structures can also be seen in the well dispersed domain. Some grain crushing/ stacking can also be seen throughout the sample.

TvD PB #61

Brown sediment with well dispersed clasts ranging from small to large. Clast shape ranges from angular to sub-rounded. Lineations can be seen throughout the sample. There is one small patch of another domain present. This domain is light brown, and contains clasts that are clustered together. Grain crushing is abundant in this domain, as well as in other areas of the sample.