ARTh 1B

Brown sediment with clasts ranging from small to large. The clast shape ranges from angular to sub-rounded. Lineations and rotation structures are commonly seen throughout this sample. Edge-to-edge grain crushing and 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.

ARTHUR 6

Dark brown sediment with clasts ranging from small to large. Clast shape ranges from angular to sub-rounded. Necking structures are abundant in this sample, especially between larger clasts. Rotation structures can also be commonly seen in this sample. This sample also contains lineations, comet structures and grain crushing in minor amounts.

HOEK UNIT C (Y)

Light brown sediment with mainly small clasts. The clast shape ranges from sub-angular to sub-rounded. Lineations are abundant throughout the sample. Edge-to-edge grain crushing, as well as crushed grains, can also be seen.

HOEK UNIT C (Z) B3

Light brown sediment with clasts ranging from small to medium in size. The clast shape ranges from sub-angular to rounded. Lineations and edge-to-edge grain crushing can mainly be seen in this sample. There are also a few examples of grain stacking and crushed grains.

HOEK UNIT C 81

Light brown sediment with clast sizes ranging from small to medium. Clast shape ranges from sub-angular to sub-rounded. Lineations are common throughout the sample. Minor amounts of edge-to-edge grain crushing can also be seen.

MB-3-2

Brown sediment with clasts ranging from small to large in size. The clast shape ranges from angular to sub-rounded. Rotation structures are the most commonly seen micro-structure in this sample. Necking structures, comet structures, grain crushing and lineations can also be seen in minor amounts throughout the sample.

MB-3-3

Brown sediment with clasts ranging from small to large. The clast shape ranges from sub-angular to rounded. Rotation structures and necking structures can commonly be seen throughout the sample. Lineations, comet structures, and grain crushing is also present throughout the sample.

P Burwell #2-87

Dark brown sediment with clasts ranging from small to medium in size. The clast shape ranges from sub-angular to sub-rounded. Lineations and grain crushing can be seen throughout the sample.

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.

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.

PBURWELL #6-87

Brown sample with mainly small clasts and a few medium sized grains. Grains range from sub-angular to sub-rounded. Lineations are abundant. There are patches of darker brown organic material throughout the sample. Grain crushing and some comet structures can also be seen.

T van Diik

Light brown sample with clasts ranging from angular to sub-rounded. Clast size ranges from small to large. Lineations are commonly seen throughout the sample. Minor amounts of rotation structures can be seen. Grain crushing is also common.

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.