| 1. | More rarely, clasts are cognate material from the magma chamber.
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| 2. | Dacite clasts cover the inward-sloping walls of the rampart.
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| 3. | The form of a clast can be described by using four parameters:
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| 4. | Larger, heavier clasts in suspension settle first, then smaller clasts.
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| 5. | Larger, heavier clasts in suspension settle first, then smaller clasts.
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| 6. | The larger clasts settled out first, followed by the finer ones.
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| 7. | Deposits of ephemeral streams exhibit little rounding with angular clasts.
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| 8. | Shungite may also occur as clasts within younger sedimentary rocks.
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| 9. | The meteoric iron occurs in clasts instead of a matrix.
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| 10. | The 3D orientation of the clasts is called the fabric of the rock.
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