Geomorphology of the mouth of the arosa estuary (coruña-pontevedra, spain)...etc.); the littoral morphogenetic system comprised of marine (marine terraces, beaches, tidal bars, tombolos and coastal arrows), transition (marshes, lagoons and fan deltas) and eolian (dune systems) settings; the fluvial morphogenetic system with channelled (alluvial, flood plain and river terraces), transition (alluvial fans and alluvial cones) and sheet flood (pediments and glacis) systems; the gravitational morphogenetic system (colluvium); and the alteration morphogenetic system (sand-alteration)
The trent, glen p.arva and blue anchor formations (upper triassic) of the east midlands and them sulphate deposfls.... Four facies are recognized; (1) sheet flood, (2) red-bed saline mudflat, (3) lacustrine and (4) marginal....
Soil-landform relationships on bullock creek fan, north canterbury... The resultant fan sediments are mainly sandy matrix supported, gravelly to bouldery debris flow deposits and finer, massive or laminated sheet flood deposits.Five...
Geomorphology of mountainous deserts...special interest), does not remain near its source long enough in the earlier stages of erosion to be reduced to very fine texture before (4) it is carried by stream floods or sheet floods toward or to (5) playa basins of rising base-level; but in an advanced stage of the arid cycle (6) the playa surface may be lowered by the wind, whereupon the rock...
