BUILDING.) Depth of Water.—The deepening and widening of the Suez canal in recent years has enabled ships of the largest class to trade with eastern ports. The canal has now (1928) been deep ened throughout to 391f t., and it is practicable for ships drawing 33ft. to pass through it. Further improvements in progress in 1928 will provide for a draught of 35ft. and there is no reasonable limitation to the capacity of the canal. Concurrently with the deepening and widening of the Suez canal the more important ports of the Far East have been developed with the object of ac commodating the largest ship capable of passing through it. The opening in 1914 of the Panama canal, having a navigable depth of 4of t., has also had an important bearing on the development of harbours in the Far East and on the Pacific coasts of America. The general result is that, whereas in 190o a navigable depth of 3of t. was considered ample for practically all requirements, a depth of at least 35ft. is now regarded as essential in harbours of the first class and, in special cases, including the ports used by transat lantic liners, depths exceeding 4oft. are aimed at.
Occasionally, when a tidal river has a shallow entrance, docks, formed on its foreshore adjoining the sea-coast, are provided with a sheltered entrance direct from the sea as in the Havre docks at the outlet of the Seine. Many old ports were first established on sandy coasts where a creek, maintained by the influx and efflux of the tide from low-lying spaces near the shore, afforded some shelter and an outlet to the sea across the beach. Some of these, such as Calais, Dunkirk and Ostend, have had their access improved by parallel jetties and dredging; and docks have been readily formed in the low-lying land only separated by sand dunes from the sea.
(See HARBOURS.) In sheltered places on the sea-coast, docks are sometimes con structed on low-lying land bordering the shore, with direct access to the sea, as at Barrow, Hartlepool, Swansea and Bombay. In the Mediterranean open basins have been formed in the sea, by establishing quays along the foreshore, from which wide, solid jetties, lined with quay walls, are carried into the sea at intervals at right angles to the shore. Such basins are sheltered by an out lying breakwater parallel to the coast, and are reached at each end through the openings left between the projecting jetties and the breakwater, as at Marseilles and Trieste, and at the extensions at Genoa (see HARBOURS). In some of these ports additional ac commodation has been obtained by constructing wide quays along the inner face of the breakwater (q.v.) . Where, however, the basins are formed within the partial protection of a bay, as in the old ports of Genoa and Naples, the requisite additional shelter has been provided by converging breakwaters across the opening of the bay, and an entrance to the port is left between the break waters.
The two deep arms of the sea at New York, known as the Hudson and East rivers, are so protected by Staten Island and Long Island that it has been only necessary to form open basins by projecting jetties or piers into them from the west and east shores of Manhattan island, and from the New Jersey and Brook lyn shores, at intervals, to provide adequate accommodation for Atlantic liners and the sea-going trade of New York (Plate I., figs. 4, 5). Somewhat similar conditions obtain in many of the great natural harbours in other parts of the world, as, for instance, in Sydney harbour and at San Francisco.
Venice being situated upon an island of limited area in a lagoon has secured the extension of its dock facilities by the construction of an entirely new port on the adjoining mainland. New York, in view of the congestion of traffic at the piers in the upper areas of the harbour, is developing large districts such as Staten island and Jamaica bay nearer the sea entrance.