The Cambridge History of the British Empire, Volume 7, Issue 1John Holland Rose, Arthur Percival Newton, Ernest Alfred Benians, Henry Dodwell The University Press, 1933 - Great Britain |
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Page 4
This lowland area may be divided into the northern Artesian Basin and the southern Murray Basin . The artesian basin is the older in origin - for it has been an area of subsidence and infilling since early Mesozoic times , possibly 100 ...
This lowland area may be divided into the northern Artesian Basin and the southern Murray Basin . The artesian basin is the older in origin - for it has been an area of subsidence and infilling since early Mesozoic times , possibly 100 ...
Page 7
Their southern limit in the Commonwealth is about 31 ° S. in January and 22 ° S. in July . The third meteorological belt comprises the great westerly drift of the atmosphere , which is most marked in the southern parts of Australasia .
Their southern limit in the Commonwealth is about 31 ° S. in January and 22 ° S. in July . The third meteorological belt comprises the great westerly drift of the atmosphere , which is most marked in the southern parts of Australasia .
Page 8
However , a large number of cyclones appear to originate in the Southern Ocean where the cold air of the Antarctic mingles with the warmer westerly drift previously mentioned . On this " Polar Front " develop the Antarctic cyclones ...
However , a large number of cyclones appear to originate in the Southern Ocean where the cold air of the Antarctic mingles with the warmer westerly drift previously mentioned . On this " Polar Front " develop the Antarctic cyclones ...
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Bibliographic information
| Title | The Cambridge History of the British Empire, Volume 7, Issue 1 The Cambridge History of the British Empire, John Holland Rose |
| Editors | John Holland Rose, Arthur Percival Newton, Ernest Alfred Benians, Henry Dodwell |
| Publisher | The University Press, 1933 |
| Original from | the University of California |
| Digitized | 3 Feb 2009 |
| Export Citation | BiBTeX EndNote RefMan |