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 13
... outer reefs (e.g., Hopley, 1977). A higher mid-Holocene relative sea level for the inner shelf of North Queensland was established from these studies. Seismic reflection survey of inter-reefal areas was also being introduced into the ...
... outer reefs (e.g., Hopley, 1977). A higher mid-Holocene relative sea level for the inner shelf of North Queensland was established from these studies. Seismic reflection survey of inter-reefal areas was also being introduced into the ...
Страница 16
... shelf of north-east Australia, describingthe sediments and featuresof the inter-reefal areas. The next three ... outer shelf reefs (Chapter 9). However, each has its own particular theme. Fringing reefs are examined in terms of the ...
... shelf of north-east Australia, describingthe sediments and featuresof the inter-reefal areas. The next three ... outer shelf reefs (Chapter 9). However, each has its own particular theme. Fringing reefs are examined in terms of the ...
Страница 22
... outer shelf in the far north (Fig. 2.3). These are almost certainly of Pleistocene age (Stephenson et al., 1980). Uplift and denudation of the Eastern Highlands over the last 50 million yearshas provided much of the material which has ...
... outer shelf in the far north (Fig. 2.3). These are almost certainly of Pleistocene age (Stephenson et al., 1980). Uplift and denudation of the Eastern Highlands over the last 50 million yearshas provided much of the material which has ...
Страница 30
... shelf remained a stable block beneath the coastal escarpment, the outer shelf was also formed from a series of rift basins which were filled initially with fluvial and colluvial sediment. (2) 24–15Ma – the major marine transgression of ...
... shelf remained a stable block beneath the coastal escarpment, the outer shelf was also formed from a series of rift basins which were filled initially with fluvial and colluvial sediment. (2) 24–15Ma – the major marine transgression of ...
Страница 32
... shelf is related to the onshore structural features (Fig. 2.1) some of which may have continued activity well into ... outer shelf of the central GBR. WhilsttheGBRshelfistectonicallystableitdoesexperiencesomeearthquake activity ...
... shelf is related to the onshore structural features (Fig. 2.1) some of which may have continued activity well into ... outer shelf of the central GBR. WhilsttheGBRshelfistectonicallystableitdoesexperiencesomeearthquake activity ...
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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