The Geomorphology of the Great Barrier Reef: Development, Diversity and ChangeCambridge University Press, 17. 5. 2007. This 2007 book reviews the history of geomorphological studies of the Great Barrier Reef and assesses the influences of sea-level change and oceanographic processes on the development of reefs over the last 10,000 years. It presents analyses of recently attained data from the Great Barrier Reef and reconstructions of the sequence of events which have led to its more recent geomorphology. The authors emphasise the importance of the geomorphological time span and its applications for present management applications. This is a valuable reference for academic researchers in geomorphology and oceanography, and will also appeal to graduate students in related fields. |
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Страница 6
... shallow-water reef limestone was recovered, overlying basaltic (volcanic) foundations. Numerous unconformities marking periods of subaerial exposure also pointed to the major part played by sea level fluctuations in the evolution of ...
... shallow-water reef limestone was recovered, overlying basaltic (volcanic) foundations. Numerous unconformities marking periods of subaerial exposure also pointed to the major part played by sea level fluctuations in the evolution of ...
Страница 15
... shallow($25m) drilling and radiocarbon dating of cores from all areas of the reef (Fig. 1.4) * an Ocean Drilling Program (ODP Leg 133) carried out just off the GBR in 1990 * drilling through the full extent of the northern GBR in 1995 ...
... shallow($25m) drilling and radiocarbon dating of cores from all areas of the reef (Fig. 1.4) * an Ocean Drilling Program (ODP Leg 133) carried out just off the GBR in 1990 * drilling through the full extent of the northern GBR in 1995 ...
Страница 17
... shallow drilling programs, and provides some insight on rates of geomorphological processes through the Holocene. It also makes comparisons between the GBR and other reefs of the world. In Chapter 12 the rapidly changing paleogeo ...
... shallow drilling programs, and provides some insight on rates of geomorphological processes through the Holocene. It also makes comparisons between the GBR and other reefs of the world. In Chapter 12 the rapidly changing paleogeo ...
Страница 18
... shallow(<60m) watersofthecontinental shelfwhich varies from about 250km in width in the south central GBR to lessthan 40km near Cape Weymouth. Whilst fringing reefs occur around many continental islands, some of which are located up to ...
... shallow(<60m) watersofthecontinental shelfwhich varies from about 250km in width in the south central GBR to lessthan 40km near Cape Weymouth. Whilst fringing reefs occur around many continental islands, some of which are located up to ...
Страница 27
... shallow depth between these two locations. The overall influence of basement rocks within the continental shelf on the GBR and its evolution can only be surmised but is likely to have been significant. 2.3 Evolution of the Coral Sea The ...
... shallow depth between these two locations. The overall influence of basement rocks within the continental shelf on the GBR and its evolution can only be surmised but is likely to have been significant. 2.3 Evolution of the Coral Sea The ...
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accretion accumulation appear associated Barrier Reef beach cays central GBR channels Chapter coast complex continental coral coral reefs cores currents cyclone dates Davies deposits depth described detail discussed dominated drilling edge effects energy established evidence example extend Figure Flood foundations fringing reefs front further geomorphological Halimeda higher holes Holocene Hopley identified important increase indicated inner lagoon less limited mainland major mangrove margin maximum morphology northern noted occur outer patches period planar platform Pleistocene possible present processes produced range rates reached recent record reef flat reef growth reef islands region relatively ribbon rise River sand sea level sediment shallow shelf shingle significant similar slope Stoddart structure studies submerged suggested surface Swain Reefs Table tidal tide vegetated wave wide windward zone