By James P. M. Syvitski, David C. Burrell, Jens M. Skei (auth.)
ISBN-10: 1461246326
ISBN-13: 9781461246329
ISBN-10: 1461290910
ISBN-13: 9781461290919
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Additional resources for Fjords: Processes and Products
Example text
1981). The Mecatina coast of southern Quebec is fronted by a series of infilled fjords and overlapping deltas: only one, the Saguenay Fjord, remains to be infilled. 4). 3). Given below is a brief but important scientific snapshot of these coasts. Details and exceptions as related to processes are described throughout the remainder of the book. 1 Greenland Fjords The fjords of Greenland are geomorphologically similar to Norwegian fjords (Ahlmann, 1941), that is, fronted by a plateau-presumably a Late .
MAN·S INPUT ~ FJORD OUTPUT ~:.. ' . ' . > . - , ,": .. ". ,--=-----{.. . . . .. :', . 14. Primary sediment inputs to a nonglaciated fjord (cf. Fig. 30). , 1984b). , 1980). Additionally, fjord rivers supply terrestrial organic matter such as leaves, twigs, humic substances, etc. (Glasby, 1978b). The latter source is relatively more important in fjords situated at lower latitudes, where the vegetation cover of the catchment area is dense. The grain size of the fluvial sediment will vary according to the parent material, the extent of erosion, the inclination of the river, the energy of the river water, and the filtering effect of lakes.
I .. MODERATE WAVE ENERGY . I. P. ------------------------------------------------------------~-----------. --- -.......... -- -. ~ STRAWBERRY ISLANDS LOWER LI MIT OF EROSION 10 ,000 YA. P. """--J_--_ \ /PRESENT SEA LEVEL ........ --------- ......... LIMIT OF EROSION CONFORMABLE COVER UN IT OUTER BAY -_ - ......... ....... 19. Longitudinal profile of Makkovik Bay, Labrador, showing the facie s development as a result of sea-level lowering and increase in the effect of seafloor wave erosion (Barrie and Piper, 1982).
Fjords: Processes and Products by James P. M. Syvitski, David C. Burrell, Jens M. Skei (auth.)
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