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Authors: Hilaire Belloc
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avoiding the turnpike continued till a date so close to our own time as easily to bridge a gap which, but for that diversion, might have proved impassable. It is not without irony that a system whose whole object was to replace by new and more excellent roads the old rough tracks, proved, indirectly,one of the principal sources of their survival.
The chalk, the third cause of that survival, is of such importance, and that importance is so commonly neglected, that it almost merits an essay of its own.
Consider the various characters which make of this soil the best conceivable medium for the preservation of an ancient road.
Like the sandy heaths and rocky uplands through which other primitive trails would naturally lead, it never paid to cultivate and therefore invited the wayfarer who was not permitted to trespass upon tilled land. But unlike other waste soil, it was admirably adapted to retain the trace of his passage. Long usage will wear into chalk a deep impression which marshy land will not retain, and which hard rocky land will never suffer. Compare, for example, the results of continuous travel along certain of the Yorkshire moors with that which will be produced along the Chilterns above the Thames valley. In the first case very marshy land, perpetually changing, alternates with hard rock. Unless some considerablelabour were expended, as in the making of a causeway, neither of these would retain any record of the road when once it had fallen into desuetude. But on the chalk some trace would rapidly form, and with every succeeding year would grow more obvious.
Chalk is viscous and spongy when it is wet. It is never so marshy as to lose all impression made upon it. It is never so hard as to resist the wearing down of feet and of vehicles. Moreover, those who are acquainted with chalk countries must have noticed how a road is not only naturally cut into the soil by usage, but forms of itself a kind of embankment upon a hillside from the plastic nature of the soil. The platform of the road is pressed outward, and kneaded, so to speak, into an outer escarpment, which would make such a track, for generations after it was abandoned, quite plain along the hillside. Finally, there are, or were until lately, no forces at work to destroy such a record. The chalk was little built upon; it had no occasion to be largely traversed by modern roads; it stood up in steep hills whereonno one would have dreamt of building, until the torture of our modern cities drove men to contrast.
How these hills invited, and almost compelled, the primitive traveller to use them has been already described. Once he began to use their soil, better than any other soil in England, it would retain his memory.
Now since some considerable portion of the Old Road has been preserved, a basis for knowledge is afforded. Patches aggregating in length to just over eighty miles are certain and fixed. It is possible to work from that known thing to the unknown, and the gaps where the Road is lost can be recovered by the consistent pursuit of a certain method; this method when it is described will be seen to lend to a first vague and tentative examination a greater value than it seemed to promise. It permitted us to establish by converging lines of proof so much of what had been lost, that one may now fairly call the full course of the Road established from the north gate of Winchester, whence it originates,to the west gate of Canterbury, which is its goal.
A description of our method is a necessary preliminary to that of the journey upon which it was put to the test.
The reconstitution of such a road is essentially the filling up of gaps. The task would be impossible if a very large proportion did not remain evident to the eye, or recorded by continuous history. The task would be much more difficult if the gaps in question were of very great length, succeeded by equally long unbroken pieces of the existing road. Luckily, the record or preservation of the
The chalk, the third cause of that survival, is of such importance, and that importance is so commonly neglected, that it almost merits an essay of its own.
Consider the various characters which make of this soil the best conceivable medium for the preservation of an ancient road.
Like the sandy heaths and rocky uplands through which other primitive trails would naturally lead, it never paid to cultivate and therefore invited the wayfarer who was not permitted to trespass upon tilled land. But unlike other waste soil, it was admirably adapted to retain the trace of his passage. Long usage will wear into chalk a deep impression which marshy land will not retain, and which hard rocky land will never suffer. Compare, for example, the results of continuous travel along certain of the Yorkshire moors with that which will be produced along the Chilterns above the Thames valley. In the first case very marshy land, perpetually changing, alternates with hard rock. Unless some considerablelabour were expended, as in the making of a causeway, neither of these would retain any record of the road when once it had fallen into desuetude. But on the chalk some trace would rapidly form, and with every succeeding year would grow more obvious.
Chalk is viscous and spongy when it is wet. It is never so marshy as to lose all impression made upon it. It is never so hard as to resist the wearing down of feet and of vehicles. Moreover, those who are acquainted with chalk countries must have noticed how a road is not only naturally cut into the soil by usage, but forms of itself a kind of embankment upon a hillside from the plastic nature of the soil. The platform of the road is pressed outward, and kneaded, so to speak, into an outer escarpment, which would make such a track, for generations after it was abandoned, quite plain along the hillside. Finally, there are, or were until lately, no forces at work to destroy such a record. The chalk was little built upon; it had no occasion to be largely traversed by modern roads; it stood up in steep hills whereonno one would have dreamt of building, until the torture of our modern cities drove men to contrast.
How these hills invited, and almost compelled, the primitive traveller to use them has been already described. Once he began to use their soil, better than any other soil in England, it would retain his memory.
Now since some considerable portion of the Old Road has been preserved, a basis for knowledge is afforded. Patches aggregating in length to just over eighty miles are certain and fixed. It is possible to work from that known thing to the unknown, and the gaps where the Road is lost can be recovered by the consistent pursuit of a certain method; this method when it is described will be seen to lend to a first vague and tentative examination a greater value than it seemed to promise. It permitted us to establish by converging lines of proof so much of what had been lost, that one may now fairly call the full course of the Road established from the north gate of Winchester, whence it originates,to the west gate of Canterbury, which is its goal.
A description of our method is a necessary preliminary to that of the journey upon which it was put to the test.
The reconstitution of such a road is essentially the filling up of gaps. The task would be impossible if a very large proportion did not remain evident to the eye, or recorded by continuous history. The task would be much more difficult if the gaps in question were of very great length, succeeded by equally long unbroken pieces of the existing road. Luckily, the record or preservation of the
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