Ash-Flow Tuffs: Their Origin, Geologic Relations and - download pdf or read online

By Clarence S. Ross (Author), Robert L. Smith (Author)

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Additional info for Ash-Flow Tuffs: Their Origin, Geologic Relations and Identification and Zones and Zonal Variations in Welded Ash Flows

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Beaches in the exponential category had the narrowest beachface (13–18 m), whereas those in the convex-curvilinear group were widest (36 –53 m) for all sites (Table 2). Dimensions of the sub-tidal terrace also varied between profile groups and between study sites. 388). Modal sediment size also varied between profile sites for each study environment. 5 mm), with coarsest sediment associated with sites in the vicinity of Hanover Bay and finer grains characterizing beaches in Shoal Bay in the SE of the Harbour.

1994. Sedimentary processes and the evolution of the distal bayside of Long Point, Lake Erie. Canadian Journal of Earth Science, 31, 1461–1473. Davidson-Arnott, R. G. D. & Fisher, J. D. 1992. Spatial and temporal controls on overwash occurrence on a Great Lakes barrier spit. Canadian Journal of Earth Sciences, 29, 102– 117. Davies, J. L. 1980. Geographical Variation in Coastal Development, 2nd edn. Longman, Harlow. DEP. 1996. Southern Metropolitan Coastal Waters Study 1991–1994: Final Report (1).

In accordance with variation in the wind regime, wave climate varied systematically around Cockburn Sound with aspect and exposure. The most energetic conditions for all fetch directions occurred in the SW around Rockingham, followed by Buchanan Bay and Sulphur Bay. The least energetic conditions for all key wind characteristics under consideration occurred at Mangles Bay on Garden Island. In keeping with results from Albany, attenuation of wave height by the sub-tidal terrace accentuated the disparity between highest and lowest wave sites, with Mangles Bay, with a long, low subtidal terrace, experiencing the greatest reduction in wave height and Rockingham the least.

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Ash-Flow Tuffs: Their Origin, Geologic Relations and Identification and Zones and Zonal Variations in Welded Ash Flows by Clarence S. Ross (Author), Robert L. Smith (Author)

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