A list of these features will run very much as follows:--

(1) The road will attempt the shortest passage of the valley floor,

the breadth being more or less of an obstacle, according as the soil

is more or less low, covered, or damp.

(2) It will seek for a ford.

(3) Other things being equal, it would naturally cross a river as high

up as possible, where the stream was likely to be less difficult to

ford.

(4) It would cross in as immediate a neighbourhood as possible to that

height upon which survey could be made of the opportunities for

crossing.

(5) The nature of the bottom at the crossing would influence it

greatly, whether that bottom were gravel and sand, or treacherous mud.

Moreover, a primitive road would often leave evidence of its choice by

the relics of good material thrown in to harden the ford.

(6) A point of so much importance would probably be connected with

religion, and almost always with some relic of habitation or weapons.

(7) It would often preserve in its place-name some record of the

crossing.

(8) It would (as we had found it at Dorking and at Otford) choose a

place where a spur on either side led down to the river.

To these eight points may be added the further consideration, that

whatever was the more usual crossing in early historic times affords

something of a guide as to prehistoric habits, and, finally, that

where a tidal river was concerned, the motives which were present on

any river for seeking a passage as far up stream as possible would be

greatly strengthened, for the tide drowns a ford.

Now, in the light of what the map tells us, and of these principles,

let us see where the crossing is most likely to be found, and having

determined that, discover how far the hypothesis is supported by other

evidence.

To begin with Cuxton:

At Cuxton the firm land of the hills comes upon either side close to

the river. An ancient track-way upon either side leads very near to

the point of crossing and cannot be followed, or at least nothing like

so clearly followed further down the valley. At Cuxton, moreover, as a

constant tradition maintains, the crossing of the river by pilgrims

was common.

On the other hand there is nothing approaching a ford at this place.

The bottom is soft mud, the width of the river very considerable, the

tidal current strong, and of all the points at which the river might

have been crossed, it is the most distant from the direct line;

indeed, compared with the next point, Lower Halling, a traveller would

add five or six miles to his journey by choosing Cuxton.

Now, consider Aylesford, the other extreme; the highest up as Cuxton

is the lowest down the river of the four points. Aylesford has many

powerful arguments in its favour. It has produced one of the most

interesting and suggestive prehistoric relics in England: I mean that

'Aylesford pottery' which is an imitation, or possibly even an import,

of the pottery of northern Italy in the first or second centuries

before our area. It has furnished a mass of other antiquities:

armillae of gold have been found in the river and British coins and

graves on the northern bank. It preserves in the last part of its name

the tradition of a ford, and though 'ford' in place-names by no means

always signifies a ford any more than 'bridge' signifies a bridge, yet

in this case we have historic knowledge that a ford existed; and (as

is most frequently the case) the ford has been bridged.

A further argument, and in its way one of the strongest that could be

adduced, is the position of the place in the earliest of our annals.

Whether 'the Horse and the Mare,' Vortigern, and the rest are wholly

legendary or not, cannot be determined. Certainly the texture of the

story is fabulous, but Bede and 'Nennius' have both retained the

memory of a great battle fought here, in which the British overcame

the Pirates, and what is most significant of all, the legend or memory

records a previous retreat of the Saxons from a defeat at Otford. We

know, therefore, that a writer in the seventh century, though what he

was writing might be fable, would take it for granted that a retreat

westward from Otford would naturally lead along some road which passed

the Medway at Aylesford. We get another much later example of the same

thing when Edmund Ironside, after his great victory at Otford over the

Danes, pursued them to Aylesford, and was only prevented from

destroying them by their passage over the river under the cover of

treason.

This is very strong evidence in favour of Aylesford, and when one

remembers that the manor was ancient demesne, its antiquity and

importance are enhanced.

But against Aylesford there are three strong arguments. They are not

only strong, they are insuperable. The first is the immense width of

valley that would have to be crossed to reach it. That is, the immense

tract of uncertain, wooded way, without a view either of enemies or of

direction.

The second is the clay. A belt of gault of greater or lesser width

stretches all along the Downs just below the chalk. Here it is

particularly wide, and no straight line can be taken from Wrotham to

the Aylesford gravels without crossing nearly two miles of this

wretched footing, which, throughout its course, the road has most

carefully avoided. That a ford of great antiquity was there; that the

men of the sandy heights used it; that the Romans used so admirable a

ford (it is gravel near the river on either side), that they bridged

it, that they made a causeway over the clay, and that this causeway

and that bridge were continuously used after their time, I am willing

to believe; but not that the prehistoric road along the chalk hills

could have waded through all that clay to reach it, and have gone out

of its way into the bargain.

Thirdly, there is the clinching fact that a number of prehistoric

remains, Kit's Coty House and the rest, lie to the _north_ of such a

crossing, and that to reach Boxley itself, a site indubitably

dependent upon the prehistoric road, a man crossing at Aylesford would

have to turn _back_ upon his general direction.

It must further be remembered that by the seventh century some of the

valleys had acquired firm roads, inherited from the old civilisation,

and that in the rout after a battle, an army making for a tidal river,

and not able to choose their own time of crossing (as can a wayfarer),

would certainly make for a point as far up the stream as possible and

for a bridge.

If Cuxton and Aylesford, then, are to be neglected (as I think they

certainly must be), there remain only Lower Hailing and Snodland.

At first sight the weight of argument is for Lower Halling, and if the

various parts of such an argument as I adduce have different

proportions from those I lend them, one might conclude that at Lower

Halling was the original passage of the Medway.

True, there is for the passage at Lower Halling but one evidence that

I can discover, but it is an evidence of the greatest weight, and such

an one as is often permitted alone to establish a conclusion in

archæology. It is this, that there was good surface over the original

soil from the Pilgrim's Way on the hills above, right down to the

river-bank at this point. No clay intervenes between the chalk and

gravel. The primitive traveller would have had fairly dry land all the

way down to the river. Even beyond the river the belt of alluvial soil

is less broad than it is at Snodland; and altogether, if the

geological argument alone were considered, the decision undoubtedly

would be given to this place.

The claims of Snodland are asserted by a number of converging

arguments. I will enumerate them, and it will, I think, be seen that

though each is individually slight, the whole bundle is convincing.

_First._--The spur, which leaves the main range of hills for the river

(such a spur as has elsewhere, at Shalford, and at Dorking, and at

Otford, attracted the Old Road towards the ford it points to), touches

indeed both Snodland and Lower Halling on either side, but with this

great difference--that Snodland is on the south, Lower Halling upon

the north of the ridge. The elevation is not pronounced, the slope is

slight, but a little experience of such ground at various seasons will

determine one that the southern bank would be chosen under primitive

conditions. In such a conformation the southern bank alone has during

the winter any chance of drying, and in a dry summer, it matters

little whether a slope be partly of clay[35] (as is the descent to

Snodland) or of chalk (as is that to Lower Halling). During more than

half the year, therefore, the descent to Snodland was preferable;

during the other half indifferent.

_Secondly._--Immediately before and beyond the Lower Halling crossing

no antiquities of moment have been discovered: a grave, possibly

Roman, is, I believe, the only one. At Snodland, and beyond its

crossing, they are numerous. An ancient and ruined chapel marks the

descent from the hills. The church itself has Roman tiles. Beyond the

river, the Roman villa which was unearthed in 1896 by Mr. Patrick is

precisely upon the road that would lead from such a crossing up to the

Pilgrim's Way upon the hill. Close by the origin of this lane from the

ford to the hillside were discovered the fragments of what some have

believed to be a Mithraic temple; and earlier, in 1848, Roman urns and

foundations were found near the road at Little Culand.

_Thirdly._--The crossing at Snodland is shallower than that at Lower

Halling, and (though I do not pretend that the artifice is

prehistoric) the bottom has been artificially hardened.

_Fourthly._--There stands at Snodland a church, past the _southern_

porch of which goes the road, and when the river is crossed, and the

same alignment followed along the bank upon the further side for a

little way, the track again passes by a church, and again by its

_southern_ porch.

_Fifthly._--The 'Horseshoe Reach'--the reach, that is, between

Snodland and Burham--has always marked the limit between Rochester's

jurisdiction over the lower, and Maidstone's over the upper, Medway.

This is of great importance. All our tidal rivers have a sea-town and

a land-town; the limits up to which the seaport has control is nearly

always the _traditional crossing-place_ of the river. Thus Yarmouth

Stone on the Yare divides the jurisdiction of Norwich from that of

Yarmouth; it is close to the Reedham Ferry, which has always been the

first passage over the river. For London and the Thames we have the

best example of all--Staines.

_Finally_, it is not extravagant to note how the megalithic monument

(now fallen) near Trottescliffe, corresponds to Kit's Coty House on

the opposite shoulder beyond the valley. The crossing at Snodland

would be the natural road between the two.

[Illustration: ROCHESTER]

These seven converging lines of proof, or rather of suggestion--seven

points which ingenuity or research might easily develop into a

greater number--seem to me to settle the discussion in favour of

Snodland.[36]

By that ferry then we crossed. We noted the muddy river, suggestive of

the sea, the Medway, which so few miles above suggests, when it brims

at high tide, a great inland river. It has hidden reaches whose fields

and trees have quite forgotten the sea. We passed by the old church at

Burham. We were in a very field of antiquity[37] as we went our way,

and apart from the stones and fragments it has left, we were

surrounded by that great legend which made this place the funeral of

the first barbarians.

It was already nearly dark when we came to the place where that old

sphinx of three poised monoliths, Kit's Coty House, stands in a field

just north of the lane; the old circle of stones, now overthrown, lay

below us to the south.

We would not pass Kit's Coty House without going near it to touch it,

and to look at it curiously with our own eyes. Though we were very

weary, and though it was now all but dark, we trudged over the plough

to where it stood; the overwhelming age of the way we had come was

gathered up in that hackneyed place.

Whether the name be, or be not, a relic of some Gaelic phrase that

should mean 'the grave in the wood,' no one can tell. The wood has at

any rate receded, and only covers in patches the height of the hill

above; but that repeated suggestion of the immense antiquity of the

trail we were pursuing came to us from it again as we hesitated near

it, filled us with a permanent interest, and for a moment overcame our

fatigue.

When we had struck the high-road some yards beyond, just at the place

where the Pilgrims Way leaves it to reach the site where Boxley Abbey

once stood, our weakness returned. Not that the distance we had

traversed was very great, but that this kind of walking, interrupted

by doubts and careful search, and much of it of necessity taken over

rough land, had exhausted us more than we knew.

With difficulty, though it was by a fine, great falling road, we made

the town of Maidstone, and having dined there in the principal inn to

the accompaniment of wine, we determined to complete the journey, if

possible, in the course of the next day.

The Old Road · 第 45 / 49 题