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By M. R. House, A. S. Gale

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K. 1988. Flood hydroclimatology. In: BAKER, V. , KOCHEL,R. C. & PATTON,P. C. (eds) Flood Geomorphology. John Wiley & Sons, New York, 27-49. HooKE, R. L. 1968. Steady-state relationships of arid region alluvial fans in closed basins. American Journal of Science, 266, 609-629. HOWARD, A. D. 1982. Equilibrium and time scales in geomorphology: application to sand-bed alluvial streams. Earth Surface Processes and Landforms, 7, 303-325. INGLES, O. G. & GRANT, K. 1975. The effect of compaction on various properties of coarse-grained sediments.

The easterly and westerly limits of the fans are less well constrained but Fig. 5. Correlation of basin-fill sequences as recorded in the two main study sections, illustrated by logged sandstone content (smoothed using a spline function). Note that the CSF variations in sandstone content are more 'rapid' fluctuations (P4 cycles) with a periodicity of c 700 m (in addition to the relatively short-term P1, P2 and P3 cycles illustrated in Fig. 4). These pulses are thought to reflect long-term climatic change due to cyclical variations in the eccentricity component with a periodicity of 2100 ka.

Canadian Society of Petroleum Geologists, Memoir, 14, 589-600. HAQUE, M. I. & MAHMOOD,K. 1986. Analytical study of steepness in ripples and dunes. Journal of the Hydraulics Division, Proceedings of the American Society of Civil Engineers, 112, 220-236. HARLAND,W. , ARMSTRONG,R. , COX, A. , GRAIG, L. , SMITH, A. G. & SMITH, D. G. 1989. A Geologic Time Scale. Cambridge University Press, Cambridge. HARMS, J. C. & FAHNESTOCK,R. K. 1965. Stratification, bedforms and flow phenomena (with an example from the Rio Grande).

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