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Conglomerate
from out side Kerrville, TX, note the very small pebbles molded together.
This rock is similar to breccia except that the fragments are rounded
indicating water erosion. |
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Chert
from the Edwards Plateau near Kerrville, TX. |
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Ironstone from Cedar Hill, TX |
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Low grade Coal from western Louisiana |
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High grade lignite Coal from Colorado |
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Gary unweathered Shale from Cedar Hill, TX. Note
the yellow stains on the shale is sulfur. |
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As with the formation of iron-rich nodules,
other minerals can become segregated during diagnesis and may form
distinct rounded masses. Here a calcareous concretion has developed in
pelitic sediment and shrinkage cracks have been filled with white calcite.
Sample is from Cedar Hill, TX |
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Red Marl from Cedar Hill, TX and Gray Marl from
Ft. Worth, TX |
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Sandy, clay, limestone from Cedar Hill, TX. |
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Chalk from Cedar Hill, TX |