References - Extreme Events: A Physical Reconstruction and Risk Assessment - page 276

Darienzo, M. and Peterson, C. (1990). Episodic tectonic subsidence of late Holocene
in salt marshes in northern Oregon central Cascadia margin. Tectonics , 9 ,
1--22.
Davies, O. K. (1999). Pollen analysis of Tulare Lake, California: Great Basin-like
vegetation in Central California during the full-glacial and early Holocene.
Review of Palaeobotany and Palynology , 107 , 249--257.
Davies, P. J. (1983). Reef growth. In Perspectives on Coral Reefs , ed. D. J. Barnes. Australia
Institute Marine Science. Manuka: Clouston Publishing, pp. 69--106.
Dawson, A. G. (1994). Geomorphological effects of tsunami run-up and backwash.
Geomorphology , 10 , 83--94.
Dawson, A. G. and Shi, S. (2000). Tsunami deposits. Pure and Applied Geophysics , 157 ,
875--897.
Dawson, A. G., Long, D. and Smith, D. E., (1988). The Storegga slides: evidence from
eastern Scotland for a possible tsunami. Marine Geology , 82 ,271--276.
Dawson, A. G., Shi, S., Dawson, S., Takahashi, T. and Shuto, N. (1996). Coastal
sedimentation associated with the June 2nd and 3rd 1994 tsunami in
Rajegwesi, Java. Quaternary Science Reviews , 15 ,901--912.
Day, S. J., Carracedo, J. C., Guillou, H., et al. (2000). Comparison and cross-checking of
historical, archaeological and geological evidence for the location and type of
historical and sub-historical eruptions of multiple-vent oceanic island volcanoes.
In The Archaeology of Geological Catastrophes , ed. W. G., McGuire, D. R., Griffiths,
P. L. Hancock, and I. S., Stewart, Geological Society of London Special Publication ,
vol. 171 . London: Geological Society of London, pp. 281--306.
Dean, W. (1997). Rates, timing, and cyclicity of Holocene eolian activity in
north-central United States: evidence from varved lake sediments. Geology , 25 (4),
331--334.
Dean, W. E., Ahlbrandt, T. S., Anderson, R. Y. and Bradbury, J. P. (1996).
Regional aridity in North America during the middle Holocene. Holocene ,
6 (2), 145--155.
De Deckker, P. and Correge, T. (1991). Late Pleistocene record of cyclic eolian activity
from tropical Australia suggesting the Younger Dryas is not an unusual climatic
event. Geology , 19 , 602--605.
Deloule, E., Chaussidon, M., Glass, B. P. and Koeberl, C. (2001). U--Pb isotopic study of
relict zircon inclusions recovered from Muong Nong-type tektites. Geochimica et
Cosmochimica Acta , 65 (11), 1833--1838.
Dominey-Howes, D. (1996). Sedimentary deposits associated with the July 9th, 1956
Aegean Sea tsunami. Physics and Chemistry of the Earth , 21 ,51--55.
Dominey-Howes, D. T. M., Papodopolous, G. A. and Dawson, A. G. (2000). Geological
and historical investigation of the 1650 A.D. Mt Columbo (Thera Island)
eruption and tsunami, Aegean Sea, Greece. Natural Hazards , 21 , 83--96.
Donn, W. L. and Balachandrian, N. K. (1969). Coupling a moving air-pressure
disturbance and the sea surface. Tellus , 21 (5), 701--706.
Donnelly, J. P., Roll, S., Wengren, M., et al. (2001a). Sedimentary evidence of intense
hurricane strikes from New Jersey. Geology , 29 ,615--618.