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The Great Thames Barrage

Chapter 6: The Tidal Thames.
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About This Book

An engineering proposal argues for construction of a barrage across the lower Thames between Gravesend and Tilbury to create a non-tidal inland reservoir and maintain consistent deep navigation to central London, eliminating dredging, tide-waiting, and grounding, and improving safety and loading operations. The pamphlet catalogs complaints about inadequate depth, delays, overlapping authorities, high costs, and hazardous navigation, critiques dredging and administrative reforms as insufficient, surveys analogous international proposals, and advocates dockisation with locks and sluices as a comprehensive remedy while discussing technical, economic, and operational implications.

The Tidal Thames.

To understand clearly the conditions to be dealt with, it is necessary to consider the daily movements of tide, the affluents, the dock and wharf business and the traffic of the river.

The maps (Figs. 2 and 3) show the tidal river and estuary from Teddington to the North Foreland. [Transcriber’s Note: It seems ‘Teddington’ here is an error for either ‘London’ or ‘Southwark’; that’s what the maps show, anyway.]

The river proper—that is, from Teddington to Gravesend—is forty-six miles long, and averages one-third of a mile wide. Its depth at low water varies from 6 ft. at Teddington to 10 ft. at London Bridge and 40 ft. at Gravesend, and the rise of tide at London varies from 17 ft. to 21 ft. and at Gravesend from 15 ft. to 19 ft., the current usually averaging four knots per hour. At London Bridge the Spring tides flow 5 hours and ebb 7½ hours; while at Gravesend they flow 6 hours and ebb 6½ hours.

The river winds about considerably. The straight line distance from Teddington to Gravesend being thirty-three miles, shows that thirteen miles are added to the river in its bends, some of which—as those at Grays, Erith, Blackwall and Limehouse—are short and tortuous.

The longitudinal section (Fig. 4) of the river from Teddington to Gravesend gives graphically all the data necessary for our purpose. Ordnance Datum (O.D.) is the common datum line of the Government maps. Trinity High Water (T.H.W.) is the water datum usually adopted in the river. High and low water, ordinary and Spring tides (H.W.O.T.—L.W.O.T.—H.W.S.T.—L.W.S.T.) are the levels of the respective states of tide in the river at various points. The highest and lowest known tides are also given, as well as the level of the river bottom and the levels of the principal dock entrance sills and of the crowns of the Thames tunnels, showing their depths below the river bottom.