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F r o m W i k i p e d i a , t h e f r e e e n c y c l o p e d i a
The ridge of which the Carlsberg Ridge is a part extends northward from a triple point junction near the island of Rodrigues (the Rodrigues Triple Point ) to a junction with the Owen Fracture Zone . The ridge started its northwards propagation in the late Maastrichtian and reached the incipient Arabian Sea in the Eocene . Then it continued to accrete basalt but did not propagate for nearly 30 Ma . Then, in the early Miocene it started to propagate westwards towards the Afar hot spot, opening the Gulf of Aden.[1]
The Carlsberg Ridge is seismically active, with a major earthquake being recorded by the U.S. Geological Survey at 7.6 on the moment magnitude scale on July 15, 2003.[2]
The submarine ridge was discovered by the Danish research vessel Dana during the Carlsberg Foundation's Oceanographic Expedition around the world (1928–1930), better known as the 2nd Dana Expedition , and named after the Carlsberg Foundation , which funded the entire expedition and subsequent analysis and publication of results.[3] [4]
^ Earth and Space (The Open University, 2007), p. 222 and "NGA: Undersea Features History" . National Geospatial-Intelligence Agency . Archived from the original on 2013-07-09. Retrieved 2013-12-01 .
^ Wolff, Torben (1967). Danish Expeditions on the Seven Seas. Copenhagen: Rhodos.
External links [ edit ]
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R e t r i e v e d f r o m " https://en.wikipedia.org/w/index.php?title=Carlsberg_Ridge&oldid=1177396775 "
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a d d i t i o n a l t e r m s m a y a p p l y . B y u s i n g t h i s s i t e , y o u a g r e e t o t h e T e r m s o f U s e a n d P r i v a c y P o l i c y . W i k i p e d i a ® i s a r e g i s t e r e d t r a d e m a r k o f t h e W i k i m e d i a F o u n d a t i o n , I n c . , a n o n - p r o f i t o r g a n i z a t i o n .
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