Compressed Earth Blocks. Standards by Houben H., Boubekeur S.

By Houben H., Boubekeur S.

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Geography, 93, 11–16. R. , 2013. When did modern rates of sea-level rise start? Global and Planetary Change, 100, 263–277. M. , 2008. A 20th century sea-level acceleration in New Zealand. 1029/2007GL032632. C. and the Subcommission on Quaternary Stratigraphy, 2009. 58 Ma. Journal of Quaternary Science, 25, 96–102. , 2000. The Changing Nature of Physical Geography. Arnold, London, UK. , 2004. An updated analysis of long-term sea-level change in New Zealand. 1029/GRL2003GL019166. Kay, R. , 1999. Coastal Planning and Management.

L Contribution to Rmax Erosion OVERTOP Rmax > Bh Deposition OVERWASH Rmax >> Bh OVERTOP OVERWASH SLUICING OVERWASH CATASTROPHIC OVERWASH Wave action SLUICING OVERWASH Rmax >>> Bh CATASTROPHIC OVERWASH Rmax >>>> Bh ? ? Fig. 16 Conceptual model showing the different stages of barrier response to increasing wave and water-level conditions. Rmax and Bh refer to maximum run-up height and barrier height, respectively. For positive freeboard Rmax < Bh, and for negative freeboard Rmax > Bh. The maximum run-up height is the summation of storm surge and wave run-up, but for long timescales the relative sea-level rise also needs to be taken into consideration.

D. Woodroffe (Eds), Coastal Evolution. Cambridge University Press, Cambridge, UK, pp. 33–86. S. , 1995. Simulation of largescale coastal change using a morphological behaviour model. Marine Geology, 126, 45–61. , 1992. Hierarchies and spatial scale in process ­geomorphology: a review. Geomorphology, 4, 303–318. , 1991. Equilibrium beach profiles: characteristics and applications. Journal of Coastal Research, 7, 53–84. T. , 1988. Non-linear tidal distortion in shallow well-mixed estuaries: a synthesis.

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