The Historic Thames | Page 4

somewhat unnatural shape to their boundaries. Thus Fawley in Buckinghamshire has a curious and interesting arrangement of this sort thrusting down from the hills a tongue of land which ends in a sort of wharfage on the river just opposite Remenham church. In Berkshire there are also several examples of this. On the upper river Dractmoor and Kingston Bagpuise are both very narrow and long, a shape forced upon them by the necessity of having this outlet upon the river in days when the life of a parish was a real one and the village was a true and self-sufficing unit. Next to them Fyfield does the same thing. Lower down, near Wallingford, the parish of Brightwell has added on a similar eccentric edge to the north and east so that it may share in the bank; but perhaps the best example of all in this connection is the curious extension below Reading. Here land which is of no use for human habitation--water meadows continually liable to floods--runs out from the parish northward for a good mile. These lands are separated from the river during the whole of this extension until at last a bend of the stream gives the parish the opportunity it has evidently sought in thus extending its boundaries. On the Oxford bank Standlake and Brighthampton do the same thing upon the Upper Thames and to some extent Eynsham; for when one thinks how far back Eynsham stands from the river it is somewhat remarkable that it should have claimed the right to get at the stream. Below Oxford there is another most interesting instance of the same thing in the case of Littlemore. Littlemore stands on high and dry land up above the river somewhat set back from it. Sandford evidently interfered with its access to the water, and Littlemore has therefore claimed an obviously artificial extension for all the world like a great foot added on to the bulk of the parish. This "foot" includes Kennington Island, and runs up the meadows to the foot of that eyot.
The long and narrow parishes in the reaches below Benson, Nuneham Morren, Mongewell, and Ipsden and South Stoke are not, however, examples of this tendency.
They owe their construction to the same causes as have produced the similar long parishes of the Surrey and the Sussex Weald. The life of the parish was in each case right on the river or very close to it, and the extension is not the attempt of the parish to reach the river, but the claim of the parish upon the hunting lands which lay up behind it upon the Chiltern Hills. The truth of this will be apparent to anyone who notes upon the map the way in which parishes are thus lengthened, not only on the western side of the hills, but also upon the farther eastern side, where there was no connection with the river.
There are many other proofs remaining of the chief function which the Thames fulfilled in the early part of our history as a means of communication.
We shall see later in these pages how united all that line of the stream has been; how the great monasteries founded upon the Thames were supported by possessions stretched all along the valleys; how much of it, and what important parts, were held by the Crown; and how strong was the architectural influence of towns upon one another up and down the water, as also how the place names upon the banks are everywhere drawn from the river; but before dealing with these it is best to establish the main portions into which the Thames falls and to see what would naturally be their limits.
It may be said, generally, that every river which is tidal, and whose stream is so slow as to be easily navigable in either direction, divides itself naturally, when one is regarding it as a means of communication, into three main divisions.
There will first of all be the tidal portion which the tide usually scours into an estuary. As a general rule, this portion is not considerably inhabited in the early periods of history, for it is not until a large international commerce arises that vessels have much occasion to stop as they pass up and down the maritime part of the stream; and even so, settlements upon its banks must come comparatively late in the development of the history of the river, because a landing upon such flooded banks is not easily to be effected.
This is true of the Dutch marshes at the mouths of the Rhine, whose civilisation (one exclusively due to the energy of man) came centuries after the establishment of the great Roman towns of the Rhine; it is true of the estuary of the Seine, whose principal harbour of Havre is