| 1. | The lineation orientation is a uniform 65 degrees toward 120 degrees.
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| 2. | Today it is generally agreed that glacial flow caused the lineations.
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| 3. | Intersection lineations can also be due to the intersection of two foliations.
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| 4. | The oldest identifiable lineations are M33 to M35 or perhaps even M38.
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| 5. | Parting lineation can also be created in dewatering tidal channels.
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| 6. | Today, it is generally agreed that glacial flow caused the lineations.
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| 7. | Lineations are measured in terms of dip and dip direction, if possible.
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| 8. | Parting lineation forms in very different depositional environments.
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| 9. | Parting lineation has even been described from turbidites.
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| 10. | Often lineations occur expressed on a planar surface and can be difficult to measure directly.
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