Desert and water gardens of the Red Sea : $b Being an account of the natives and the shore formations of the coastCrossland, Cyril
Science
Desert and water gardens of the Red Sea : $b Being an account of the natives and the shore formations of the coast
Crossland, Cyril
Coral reefs and islands; Red Sea; Sudan -- Social life and customs
_Plate I_
[Illustration: Fig. 1. Coast of the Anglo-Egyptian Sudan
Sandstone hills shaded, _small_ islands black. Coastline double,
the outer line being the edge of the fringing reef. The thin lines
enclosing roughly oval or elongated areas at sea are the barrier
reefs. Figures on sea represent depths in fathoms.]
DESERT AND WATER GARDENS
OF THE RED SEA
CAMBRIDGE UNIVERSITY PRESS
London: FETTER LANE, E.C.
C. F. CLAY, MANAGER
[Illustration]
Edinburgh: 100, PRINCES STREET
London: WILLIAM WESLEY & SON, 28, ESSEX STREET, STRAND
Berlin: A. ASHER AND CO.
Leipzig: F. A. BROCKHAUS
New York: G. P. PUTNAM’S SONS
Bombay and Calcutta: MACMILLAN AND CO., LTD.
_All rights reserved_
_Plate III_
[Illustration: Fig. 3. A sandstorm seen from among the Barrier Reefs]
=DESERT AND WATER GARDENS
OF THE
RED SEA=
BEING AN ACCOUNT OF THE NATIVES AND THE
SHORE FORMATIONS OF THE COAST
BY
CYRIL CROSSLAND
M.A. Cantab., B.Sc. Lond., F.L.S., F.Z.S.
Marine Biologist to the Sudan Government
Cambridge:
at the University Press
1913
Cambridge:
PRINTED BY JOHN CLAY, M.A.
AT THE UNIVERSITY PRESS
TO MY WIFE
TO WHOSE BRAVE ENDURANCE OF A LARGE
SHARE OF MY EXILE IS OWING MUCH
OF WHATEVER I HAVE ACHIEVED, OR
OF WHAT SUCCESS MAY YET BE MINE
PREFACE
It is my fortune to know intimately a portion of the Red Sea coast,
that between 18° N. and 22° N. on the western side. This must
be one of the least known coastlines of the world. Until 1905,
the Admiralty Chart shewed an area of 25 square miles of reef,
which the surveys run for the approaches to the new town of Port
Sudan have proved to be non-existent. Though a considerable distance
north of this point has now been accurately surveyed, practically no
details of the great barrier system of reefs leading up to the Rawaya
Peninsula, or of the land inside the coastline, have yet been mapped.
As I shall shew later, certain features of the maritime plain are of
the greatest interest, but they have only been hurriedly examined
by Mr Dunn, one of the Sudan Government geologists; and no survey
of the country has yet been made.
Public-domain text, read in full here on John Shaqi.
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