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MEDWAY , a See also:river in the See also:south-See also:east of See also:England. It rises in the See also:Forest Ridges, S.W. of East Grinstead in See also:Sussex, and, increased by many feeders from these picturesque hills, has an easterly course to the See also:county boundary, which it forms, turning northward for a See also:short distance. Entering See also:Kent near Ashurst, its course becomes See also:north-easterly, and this direction is generally maintained to the mouth. The river passes See also:Tonbridge, receiving the See also:Eden from the See also:west, and later the Teise and Beult from the south and east, all these streams watering the See also:rich See also:Weald (q.v.) to the south of the North See also:Downs. These hills are breached by the Medway in a beautiful valley, in which lies See also:Maidstone, generally much narrower than the upper. valley. The characteristic structure of this See also:part of the valley is considered under the heading Downs. Below Maidstone the valley forms a perfect See also:basin, the hills descending upon it closely above See also:Rochester. Below this See also:city the river enters a broad, winding See also:estuary, passing See also:Chatham, and at See also:Sheerness joining that of the See also:Thames, so that the Medway may be considered a tributary, and its drainage See also:area of 68o sq. m. reckoned as part of that of the greater river. The length of the Medway is about 6o m., excluding its many lesser windings. The estuary is navigable for See also:sea-going vessels See also:drawing 24 ft. up to Rochester See also:Bridge. A considerable See also:traffic is carried on by small vessels up to Maidstone, and by See also:barges up to Tonbridge, the See also:total length of the See also:navigation being 43 M. The marshy lowlands along the course of the river have yielded extensive remains of See also:Roman pottery, a See also:plain See also:ware of dark See also:slate-See also:colour. Additional information and CommentsThere are no comments yet for this article.
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