Digitale Bibliotheek
Sluiten Bladeren door artikelen uit een tijdschrift
 
<< vorige   
     Tijdschrift beschrijving
       Alle jaargangen van het bijbehorende tijdschrift
         Alle afleveringen van het bijbehorende jaargang
           Alle artikelen van de bijbehorende aflevering
                                       Details van artikel 15 van 15 gevonden artikelen
 
 
  The bedrock topography of the botany basin, New South Wales
 
 
Titel: The bedrock topography of the botany basin, New South Wales
Auteur: Johnson, B. D.
Albani, A. D.
Rickwood, P. C.
Tayton, J. W.
Verschenen in: Australian journal of earth sciences
Paginering: Jaargang 24 (1977) nr. 7-8 pagina's 403-408
Jaar: 1977-12
Inhoud: The bedrock topography of the Botany Basin has been determined from seismic-sparker records made in Botany Bay and Bate Bay, and from seismic-refraction and gravity measurements on the Kurnell Peninsula. Supplementary information has been obtained from boreholes both on land and in the sea. The Cooks and Georges Rivers formerly constituted the main drainage of the Basin and flowed generally southeastwards (beneath the present Kurnell Peninsula) and joined the Port Hacking River east of Cronulla. The depth of the bedrock channel of the former Georges River is 75-80 m b.s.l. at Taren Point, 90-95 m beneath the Kurnell Peninsula and 110-115 m at its junction with the Port Hacking River channel. The bedrock channel of the former Cooks River is about 30 m b.s.l. at Kyeemagh, its present entrance to Botany Bay, and it joined the Georges River at a location now 90 m b.s.l. beneath the Kurnell Peninsula. A second drainage system existed in the north and east of Botany Bay and generated the present mouth beneath which the bedrock is now 110 m b.s.l. This channel followed a southeasterly course parallel to the present northern shore of Botany Bay and was separated from that of the 'Cooks and Georges Rivers' by a bedrock ridge which extended from beneath Sydney Airport to the northern extremity of the Kurnell Peninsula. Over much of its length this divide had a depth of about 30 m b.s.l. The formation of the Kurnell Peninsula tombolo led to the diversion of the 'Cooks/Georges River' through the mouth of Botany Bay and subsequently led to the development of the bay. This change in the drainage system occurred when the sea was less than 30 m below the present sea level.
Uitgever: Taylor & Francis
Bronbestand: Elektronische Wetenschappelijke Tijdschriften
 
 

                             Details van artikel 15 van 15 gevonden artikelen
 
<< vorige   
 
 Koninklijke Bibliotheek - Nationale Bibliotheek van Nederland