701 resultados para Rounded atelectasis


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Coarse grained sample, with generally medium sized clasts. Clasts were sub-angular to sub-rounded. Many rotation structures, as well as large amounts edge-to-edge grain crushing are also present.

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Dark brown sediment with clasts that range from small to large. The clast shape ranges from sub-angular to sub-rounded. Lineations are abundant in this sample. Edge-to-edge grain crushing can also be seen. Darker organic rich domains are also present throughout the sample.

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Coarse grained sediment with clasts ranging from small to medium in size. Clast shape range from sub-angular to sub-rounded. Lineations are present throughout the sample. Edge-to-edge grain crushing, grain stacking, and comet structures can also be seen. Some grains are crushed into one another. Areas of finer sediment can also be seen.

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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.

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Coarse grained sample with clasts that range from small to large in size. The clast shape ranges from angular to rounded, and many grains are fractured. Grain crushing is present in large amounts. This includes edge-to-edge crushing as well as grains that are crushed into one another. Rotation structures are also common among the clasts that are sub-rounded to rounded. Areas of finer sediment can also be seen.

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Coarse grained sample, with small clasts. Clasts range from sub-angular to sub-rounded in shape. Lineations are abundant throughout the sample. Grain stacking and crushing can also be seen in minor amounts.

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This is a coarse grained sample with some very fine grained domains throughout the sample. The clast shape and size range from small to large, as well as angular to sub-rounded. Grain crushing is the most prevalent in this sample. It also contains some rotation structures and minor necking structures. Lineations and grain stacking can also be seen.

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Coarse grained sample, with grains ranging from small to large in size. Shapes range from angular to rounded. This sample is abundant in lineations, and rotation structures can also be seen around larger aggregates. Many large grains are fractured and minor grain stacking can also be seen.

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Coarse grained sample with inclusions of finer grained sediment. Clasts are small to large in size and angular to sub-rounded in shape. Grain crushing is abundant in this sample, and lineations and minor grain stacks can also be seen.

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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.

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Fine grained sample with some small clasts. The small clasts are sub-angular to sub-rounded in shape. Organic materials can be seen throughout the sample (darker areas). Lineations are also present throughout the sample.

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Brown sediment with clasts ranging from small to medium in size. They are sub-angular to sub-rounded in shape. Lineations are abundant throughout the sample. Minor grain stacking and crushing can also be seen.

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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.

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Dark brown sediment with small to large sized clasts. The clasts are sub-angular to sub-rounded in shape. Lineations are the most abundant. Minor amounts of rotation structures and comet structures can also be seen. Grain crushing is also present throughout the sample.

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Dark brown sediment with clasts ranging from small to large. Clasts are sub-angular to sub-rounded in shape. Larger tend to be more sub-rounded in this sample. Lineations and comet structures are present. Minor amounts of rotation structures can also be seen.