| 11. | Magma probably formed during deglaciation was erupted during the early Holocene, generating the long lava flow.
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| 12. | During deglaciation, the melted ice-water returned to the oceans, causing sea level to rise.
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| 13. | Beginning with the Lic�n Ignimbrite, generated just after the last deglaciation, activity continued in similar fashion.
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| 14. | If present deglaciation trends continue, the Calderone may soon share Corral de la Veleta's fate.
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| 15. | Oxygen isotope values from high latitudes : clues for Permian sea-surface temperature gradients and Late Paleozoic deglaciation.
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| 16. | The lands of Novaya Zemlya attained most of their early Holocene coastal deglaciation approximately 10, 000 years before present.
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| 17. | During deglaciation, the melted ice water returns to the oceans, thus sea level in the ocean increases again.
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| 18. | In the Alps this maximum was in 1850 and since then the region has become ice free due to deglaciation.
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| 19. | After deglaciation, snow and ice melt from the mountain tops can create streams and rivers in U-shaped valleys.
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| 20. | The physical mechanisms by which deglaciation occurs include melting, evaporation, calving, and aeolian processes such as wind scouring.
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