Geomorphology of New Zealand Pt I Systematic An Introduction to the Study of
Geomorphology of New Zealand Pt I Systematic An Introduction to the Study of
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Coasts of Submergence and of Emergence. —Movements of the ocean-level (" eustatic "" movements) will produce results similar to uplift and subsidence of the land except that the eustatic Fig. 382. — Coasts of submergence and of emergence (represented in the diagram as though due to fall and rise of sea-level. B. Effect of submergence, or subsidence, and C, effect of emergence, or uplift ; A, pre-existing coast : D and E, sequential forms derived from the initial forms B and C respectively.
move...ments will be world-wide and their effects of equal magnitude over large areas, whereas the amount of submergence or emergence often varies from point to point, and there is sometimes a rapid passage from a coast of submergence to one of emergence, indicating that movement of the land — often diverse movement— has been responsible for the majority of initial coasts.
Coasts due to warping need not be considered separately, for there is no essential difference in form between shore-lines due to regional depression or uplift and those in which the submergence COASTAL OUTLINES.
What to read after Geomorphology of New Zealand Pt I Systematic An Introduction to the Study of?
You can find similar books in the "Read Also" column, or choose other free books by C a Charles Andrew Cotton to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Coasts of Submergence and of Emergence. —Movements of the ocean-level (" eustatic "" movements) will produce results similar to uplift and subsidence of the land except that the eustatic Fig. 382. — Coasts of submergence and of emergence (represented in the diagram as though due to fall and rise of sea-level. B. Effect of submergence, or subsidence, and C, effect of emergence, or uplift ; A, pre-existing coast : D and E, sequential forms derived from the initial forms B and C respectively.
move...ments will be world-wide and their effects of equal magnitude over large areas, whereas the amount of submergence or emergence often varies from point to point, and there is sometimes a rapid passage from a coast of submergence to one of emergence, indicating that movement of the land — often diverse movement— has been responsible for the majority of initial coasts.
Coasts due to warping need not be considered separately, for there is no essential difference in form between shore-lines due to regional depression or uplift and those in which the submergence COASTAL OUTLINES.
What to read after Geomorphology of New Zealand Pt I Systematic An Introduction to the Study of?
You can find similar books in the "Read Also" column, or choose other free books by C a Charles Andrew Cotton to read onlineMoreLess
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