CHAPTER XX.

CHANGING COURSE OF STREAMS--DEWPONDS--A WET HARVEST--WEATHER

PHENOMENA--WILL-O'-THE-WISP--VARIOUS.

"There rolls the deep where grew the tree.

O Earth, what changes hast thou seen!"

--_In Memoriam_.

"With many a curve my banks I fret

By many a field and fallow,

And many a fairy foreland set

With willow-weed and mallow.

"I chatter, chatter, as I flow

To join the brimming river,

For men may come and men may go,

But I go on for ever."

_The Brook_.

Living so many years in one place I had unusual opportunities, as my

rounds nearly always took me beside my brooks, of watching their

slowly changing courses. The roots of the pollard willows helped to

keep them to their regular path by holding up the banks, but sometimes

when an old tree fell into the water it had an opposite result. A

fallen tree, reaching partly across the stream, has the immediate

effect of damming the flow of the water on the side of its growth and

diverting the current towards the opposite bank in a narrowed but more

powerful advance, so that the bank is worn away and the beginning of a

bend is formed. As the breach increases, the water, momentarily

retarded there by the new concavity, rushes forward again in the

direction of the bank from which the tree fell. So that a second

concavity is produced on that side some little way below the tree,

resulting in the slow formation of an extended S-like figure, or hook

with a double bend. The collection of rubbish and sediment retained by

the fallen tree helps to form a new bank on that side, extending

further into the stream than the bank on which the tree originally

stood.

As this process continues it is easy to see that a straight stretch of

stream will in time assume a winding course, and the stream will be

continually altering its path, so that large areas of flat meadows

will be formed, every part of which has at times been the stream's

course. How many ages, then, must it have taken to produce the level

meadows we see extending for immense distances on either side of our

big rivers, and even those adjoining quite small streams? The level

surface thus created by the river or brook's course perpetually

deflected and reflected, is finally completed by the floods bringing

down a deposit of soil in solution, which is precipitated and settles

into any surface irregularities left by the wanderings of the stream.

A faint conception of an absolutely illimitable cycle of years, during

which the whole extent of visible flat meadow has been again and again

eroded and restored, is thus conveyed.

Confirmation of this alteration of their courses by streams is

afforded when we cut a main drain through one of these meadows, to

carry the water from the connected furrow drains of adjoining arable

land. The alluvial soil can be found as deep as the depth of the

present brook, free from the stones found in the arable land, and

containing, to the same depth as the brook, fresh water shells similar

to those in the brook to-day. There was a bend in course of formation

in one of my brooks, where the stump of a tree, whose fall was the

starting-point, could be seen standing in the newly-formed ground, a

yard or more from the stream when I left, though I can remember when

it was so near as almost to touch the water.

If we form an S from a piece of wire, and pinch it together from top

to bottom, the loops become so flattened, [S], that one of them may

almost unite with the central curve. The same thing often happens in

the loops of a brook, and, in time, the stream will complete the

junction, forming a short circuit.[2] Thus an island may be formed; or

when the old loop opposite the short circuit gets filled up with

deposit or falling banks--the water preferring the short circuit--a

piece of land may be cut off from one of the former sides of the brook

and transferred to the other, so that where the brook is a boundary

between two owners or parishes one owner or parish may be robbed and

the other owner or parish becomes a receiver of stolen goods. There

was an instance of this on the farm I owned and occupied adjoining the

Aldington Manor property, and the owner and the tenant of the piece

transferred to my side could not reach it without walking through the

brook. In this case, however, the tenant had wisely planted the ground

with withies, which he managed to get at for lopping when its turn

came round every seven years. Thus we have an example of the necessity

of the ancient practice of beating the bounds, which, at least before

the days of ordnance surveys, was not merely an opportunity for a

holiday.

Another proof of the creation of new land by the meanderings of a

stream is found in the ancient "carrs" of North Lincolnshire, near

Brigg, where the hollowed-out logs of black bog oak, which formed the

canoes of the ancient inhabitants, are sometimes discovered many feet

below the surface, and long distances from the present course of the

Ancholme. These having sunk to the bottom of the river in past ages,

and gradually become covered with alluvium, were left behind as the

river changed its course. In some cases however these canoes may have

sunk to the bottom of the water when it formed a lake, and the lake

having gradually silted up, the river receded to something like its

present width.

The floods in the Vale of Evesham from the Avon and even from my

brooks, often converted the adjoining flat meadows into lakes, and

they rose so suddenly after heavy rains or the melting of deep

snowfalls on the hills, that they were attended with danger to the

stock.

In the summer of 1879 one of these sudden floods occurred, and people

standing on Evesham bridge, saw fallen trees and hay-cocks floating

down the stream. A pollard willow was noticed with a crew of about

twenty land rats, which had found refuge there until the tree itself

was lifted by the rising water and carried down the stream; and a

floating hay-cock supported a man's jacket, his jar of cider, and his

"shuppick." The local word "shuppick," a corruption of "sheaf-pike,"

means a pike used for loading the sheaves of wheat in the harvest

field on to the waggon, and is the "fork" in general use at

hay-making. During another summer flood the whole of the pleasure

ground at Evesham, beside the Avon, was under water several feet deep;

the water poured in at the lower windows of the adjoining hotel, and

the proprietor's casks of beer and cider in the cellars, ready for the

regatta, were lifted from their stands and bumped against walls and

ceilings.

Every parish has its Council in these days, and in country places

almost every other person one meets is a councillor of some sort, and

inclined to be proud of the distinction. These Councils are excellent

safety-valves for parochial malcontents who thus harmlessly let off

superfluous steam which might otherwise ruffle the abiding calm of

peaceful inhabitants, but their powers are really very limited. In a

village in Worcestershire where an approach road crossed a brook by a

ford, during floods the current was sometimes so strong as to

constitute a danger to horses and carts. The village pundits

therefore, in council duly assembled, considered the matter, and after

an extended debate the following resolution was carried unanimously,

"That a notice board be erected on the spot bearing the inscription:

When this board _is covered with water_ it is dangerous to attempt to

cross the ford."

The numerous brooks in the Vale of Evesham supply ample water for the

stock, but in more elevated parts, especially on the chalk Downs of

Sussex, Hants, Wilts, and Dorset, provision is made for an artificial

water supply by what are called "dewponds." A shallow saucer-shaped

depression is dug out on the open Down, the bottom being made

water-tight by puddling with a well-rammed layer of impervious clay.

The first heavy rainfall fills the pond, and, the water being colder

than the air, the dew or mist condenses on its surface sufficiently,

in ordinary weather, to maintain the supply. In a dry time the sheep

can always reach the water, the pond having no banks, by the shelving

formation of the bottom. Sometimes a few trees are allowed to grow

round it; they also act as condensers, and their drip helps to fill

the pond. It is only in an abnormal drought that these dewponds really

fail, and a thunderstorm, followed by ordinary weather, will soon

refill them. Gilbert White, in _The Natural History of Selborne_,

refers to these ponds in a very interesting letter on the subject,

including details of condensation by trees, in which he gives an

instance of a particular pond, high up on the Down, 300 feet above his

house, and situated in such a position that it was impossible for it

to receive any water from springs or drainage, which "though never

above three feet deep in the middle, and not more than thirty feet in

diameter, and containing, perhaps, not more than two or three hundred

hogsheads of water, yet never is known to fail, though it affords

drink for three hundred or four hundred sheep, and for at least twenty

head of large cattle besides."

The natural well-water in the Vale of Evesham is exceedingly hard, and

in the town and some villages was formerly much contaminated. After

great opposition from obstructive ratepayers, a splendid supply was

obtained from the Cotswolds above Broadway, about six miles away, of

much softer and really pure spring water. It comes in pipes by

gravitation, so there is no expense of pumping; but it was difficult

to get recalcitrant ratepayers to lay the water on from the mains to

their houses, as that part of the cost had to be borne by them

individually; and, before compulsion could be resorted to, the Council

had to prove contamination of the wells and close them. To get the

evidence samples were submitted to a London analyst, and they were

invariably condemned. One of the Councillors suggested sending, with a

number of well samples, a sample of the new supply "for a fad." The

samples were numbered, but had no other distinguishing mark, and in

due course the usual condemnations were received, including that of

the new town supply!

During the wet harvest of 1879, when what was called by townspeople

the agricultural depression, was becoming acute, it was impossible to

get a whole day on which wheat could be carried. The position was

serious, because the grain was sprouting in the sheaves in the field,

and time after time a fairly dry Saturday would have allowed carrying

the following day, though Monday was always as wet as ever. At last at

Aldington we faced the situation and decided to proceed with the work

whenever possible, Sunday or no Sunday. A fine drying Saturday

occurred, and my bailiff told the men what we proposed, adding that we

did not wish anyone to help who had scruples as to the day. They all

appeared on Sunday morning, a brilliant day, except one "conscientious

objector," who, as I heard later, spent most of the day at the

public-house. We got up two ricks from about ten acres, which

eventually proved to be some of the driest wheat we had that year, and

which I was able to sell for seed at a good price, to go into

districts where no dry seed wheat could be found.

My old vicar was somewhat scandalized at this Sunday work, and some of

my neighbours fancied themselves shocked, but a day or two later I

happened to meet another clergyman friend, who farmed a little

himself. "I was _so_ pleased," he said, "to hear that you were

carrying wheat last Sunday; when I was preaching I was strongly

disposed to conclude by telling my people--'Now you have been to

church, go home to your dinners, and then off with your jackets and

carry wheat for the rest of the day.'" Next Sunday all my neighbours

were busy with their wheat, but I had managed to complete my harvest

during the previous week, on the 8th of October, quite a month or six

weeks later than usual, and an extraordinary contrast to the very dry

year 1868, when all the corn on the farm, I was told, was carried

before the last day of July.

I attended a neighbour's sale that autumn; the wet seasons and the low

prices had been too much for him, and he was leaving for the United

States; his rick-yard was empty, all the corn sold, and nothing but

straw left. I heard him remark, "Folks are saying that I'm very

backward with my payments, but I'm very forward with my thrashing,

anyway!" Before the following spring nearly all the rick-yards were

empty, and wheat-ricks, it was said, were as scarce as churches--one

in each parish. The situation was summed up later in a phrase which

passed into a proverb: "In 1879 farmers lived on faith, in 1880 they

are living on hope, and in 1881 they will have to live on charity."

The attitude of the towns was one of apathy and indifference, like

that of the General in _Bracebridge Hall_, which, published in 1822,

proves how history repeats itself in agricultural as in other matters:

"He is amazingly well-contented with the present state of things, and

apt to get a little impatient at any talk about national ruin and

agricultural distress. 'They talk of public distress,' said the

General this day to me at dinner, as he smacked a glass of rich

burgundy and cast his eyes about the ample board: 'They talk of public

distress, but where do we find it, sir? I see none; I see no reason

anyone has to complain. Take my word for it, sir, this talk about

public distress is all humbug!'"

At Evesham, long before the depression grew into a debacle, the

shadows of coming events could easily be detected. There was the

disappearance of the long rows of farmers' conveyances at the inns in

the town on market-days; there was the eclipse of shops--for other

than necessities--such as a little fish shop, opposite the corner at

the cross roads; a corner where much business was formerly transacted

in the open street, and where I myself have sold by sample some

thousands of sacks of wheat. A tempting little shop it used to be,

displaying shining Severn salmon; and it was here that the farmers,

after the market, obtained the supplies commanded by the missus at

home.

And there was the abandonment of the Corn Market proper, for the class

of farmers who survived hated to transact their business indoors. The

attendance of millers and dealers, except of those who had cargoes of

foreign corn at Gloucester or Bristol to dispose of, became irregular.

Sales of farm stock and implements took place in every village on

farms which had passed from father to son for generations, coupled

with the sacrifice of valuable implements and machinery for want of

buyers. There followed the stage when landowners who could find no

tenants, and had heavily mortgaged estates, essayed to make the best

of them by laying away the arable land to pasture, undertaking the

management themselves with, perhaps, an old broken-down tenant as

bailiff. The politicians and the general public did not apprehend the

danger of the situation, in spite of innumerable warnings, until the

German submarines were sending our foreign food supplies to the bottom

of the sea; and now that the immediate danger of starvation has

passed, they appear already to have lapsed again into an attitude of

apathy.

We hear the blessed word "reconstruction" on every side, but the only

official propositions for the permanent establishment of agricultural

prosperity that I have heard are utterly inadequate. It is ridiculous

to suppose that a few thousand acres of special crops, like tobacco,

for instance, only possible in favoured spots, can in any way

compensate for the loss of millions of acres of arable land under

rotations of corn and green crops. Under present conditions nothing is

more certain than the abandonment of arable land as such; and it is

folly to talk of novel systems of transport for a dwindling output, or

of building labourers' cottages at an unjustifiable cost, which are

never likely to be wanted by a dying industry.

Among my experiences of abnormal weather, I have a note of a

remarkable summer flood on July 21, 1875, when my hay was lying in the

meadows beside the brooks, and had to be removed to higher ground in

pouring rain to prevent its disappearance with the current. On the

following day, July 22, the highest flood since 1845 occurred at

Evesham.

October 14, 1877, was memorable for the most terrific south-west gale

that happened in all the years I passed at Aldington; thirteen trees,

mostly old apple trees and elms, were blown down, including the

splendid veteran "Chate boy" pear tree at Blackminster, an exceedingly

sad and irreparable loss. The gale blew hardest in special tracks, the

course of which could be followed by the destruction of trees and

branches in distinct lanes, cut through woods and plantations.

The winter of 1880-1881 was very severe, the mean temperature of

January, 1881, being 27.8 degrees F., the coldest January since 1820.

Ten years later, 1890-1891, another very prolonged winter occurred:

the frost began on the 6th of December, and, with scarcely a break,

continued till well into February. The feature of this frost was the

fine settled weather, and the warmth of the midday sun in the

brilliant air, when skaters could sit on the river banks and enjoy

their rest and lunch in its rays. I took my elder daughter back to

school at Richmond at the end of January, and in London we saw the

Thames choked by huge hummocks of ice, on which people were crossing

the river. An ox was roasted whole on the Avon at Evesham, and, when

the frost broke up, the ice on our millpond was 17 inches thick.

Another great frost happened in 1894-1895, beginning late in December,

and lasting till the end of February, with a single intervening week

of thaw; and in March the ground, in places, was too hard to plough.

It was the only time that I was completely at a loss to find work for

my men; all the carting was finished in the early days of the frost,

and all the thrashing possible followed; ploughing and all working of

the land, or draining, were impracticable. The men, seeing that there

would be no employment for them until the frost broke up, told me that

if they might get what wood they could from fallen trees in the brook,

and if I would lend them horses and carts to get it home, they would

be glad to work in that way for themselves for a time. Just as they

had cleared both brooks from end to end of the farm which occupied

them about ten days, the thaw came and I was able to find them plenty

to do.

We suffered very little from droughts at Aldington, the land was

naturally so retentive of moisture, but 1893 was a dry year, not

easily forgotten; no rain fell from early in March to July 13; the hay

crop was the lightest in remembrance, and straw was so short and

scarce that the hay-ricks of the following year, 1894, had to go

unthatched until the harvest of that year provided the necessary

straw.

The spring of 1895 was remarkable for a plague of the caterpillars of

the winter-moth, due to the destruction of insect-eating birds by the

great frost; the caterpillars devoured the young leaves of the

plum-trees, so that whole orchards were completely stripped. The

balance between insectivorous birds and caterpillar life was destroyed

for a time, and the caterpillars conquered the plum-trees. In 1917,

during the persistent north-east blasts of February, March, and part

of April, the destruction of birds was terrible; all the tit tribe

suffered greatly, and the charming little golden-crested wren, which

here in the Forest was quite common, has scarcely been seen since.

Caterpillars again were a plague in my apple trees that spring, but

were not really destructive, and in the autumn the apples escaped

their usual punishment from the birds and wasps. Tits are often very

troublesome; they peck holes in the fruit, apparently in search of the

larvae of the codlin moth, leaving an opening for wasps and flies. I

find the berries of the laurel, which is a species of cherry, very

attractive to blackbirds, and as long as there are any left they seem

to prefer them to the apples. In 1895 cuckoos came to the rescue of my

young plum orchard; there were dozens of them at work on the nine

acres at once, and they must have cleared away an immense number of

the grubs.

The most remarkable season we have had since I left Aldington was the

great drought of 1911. There was no rain here worth mention from June

22, the Coronation of King George V., until August 30, and the

pastures on this thin land were burnt up. On August 30 we had some

friends for tennis, and we had not been playing long before a mighty

cloud-burst occurred; the rain fell in torrents. "It didn't stop to

rain, it tumbled down," as my men used to say, and in about half an

hour the lawn was a sheet of water, the ground being so hard, that it

could not soak away. It was all over in an hour, and a neighbour with

a rain-gauge registered 0.66 of an inch of rain, equal to 66 tons on

an acre, or 330 tons on my five acres.

One of my ambitions has always been to see a Will-o'-the-wisp, and I

am still hoping; but that hot summer, had I known it at the time, they

were quite common within an easy walk of my house in the New Forest.

There was some correspondence on the subject in _The Observer_, and

the following is extracted from one of the letters:

"As none of your correspondents seem to be aware of a comparatively

recent instance, I write to say that there were enough indubitable

Will-o'-the-wisps to convince the most incredulous during the

extremely hot weather of July, 1911.

"From July 18 to 22 I was at Thorney Hill in the New Forest, some

seven miles behind Christchurch. Owing to the abnormal drought the

bogs and bog-streams at the foot of the hill westward were all but

dry; a dense mist, however, sometimes rose from them at night. On July

19, and the three following nights, the Will-o'-the-wisps were in

great form over the bog. They were like small balls of bluish fire,

which projected themselves with hops and jerks across the most

inaccessible parts of the bog, starting always, so far as could be

told, from where a little stagnant moisture still remained. They moved

with an erratic velocity, so to speak, appearing and reappearing at

distances of several hundred yards. There wasn't the slightest doubt

of their authenticity.

"The inhabitants of Thorney Hill, I believe, regarded these

appearances with alarm, as being, though not exactly novelties,

harbingers of much misfortune. But the drought was quite bad enough,

without having the Jack-o'-lanterns to accentuate it!"

This instance was the more remarkable as I have never succeeded in

finding anyone, even among people who are constantly on duty in the

Forest, who could testify to having seen a Will-o'-the-wisp.

Waterspouts are, I believe, more frequently seen at sea than on land,

but I have an account from my brother, Mr. F.E. Savory, of one he saw

many years ago in Wiltshire. He writes:

"When I was at Manningford Bruce in 1873 or 1874, I saw a dense black

cloud travelling towards the southeast, the lower part of which became

pointed like a funnel in shape, waving about as it descended until, I

suppose, the attraction of the earth overcame the cohesion of the

cloud's vapour, and it discharged itself. I could see it looking

lighter and lighter, from the middle outwards, until it was entirely

dispersed. I heard that the water fell on the side of the Down near

Collingbourne, about five miles off, and washed some of the soil away,

but I did not see that. The weather was stormy, but I do not remember

the time of year or any other particulars."

It would seem that a waterspout is caused by a whirlwind entering a

cloud and gathering vapour together by its rotary action into such a

heavy mass that it descends in the funnel shape described. We are all

familiar with the small whirlwinds that travel across a road in

summer, carrying the dust round and round with them; these are called

"whirly-curlies" in Worcestershire, and are regarded as a sign of fine

weather. I have sometimes seen quite a strong one crossing rows of hay

just ready to carry, cutting a clean track through each row, and

leaving the ground bare where it passed. The hay is often carried to a

great height, and sometimes dropped in an adjoining field.

On a bright morning in summer one often sees, a little distance away,

a tremulous or flickering movement in the air, not far from the

ground, which Tennyson refers to in _In Memoriam_, as, "The landscape

winking thro' the heat"; and again in _The Princess_:

"All the rich to come

Reels, as the golden Autumn woodland reels

Athwart the smoke of burning weeds."

I am told that this appearance is "due to layers of air of different

degrees of refracting power, in motion, relative to one another. Air

at different temperatures will refract light differently." In

Hampshire this phenomenon is known by the pretty name of "the summer

dance."

Since I came to the Forest I have seen two very curious and, I think,

unusual natural appearances. As I was cycling one rather dull

afternoon from Wimborne to Ringwood, I noticed a colourless rainbow,

or perhaps I should say, "mist-bow," for there was no rain, and the

sun was partially obscured. The sun was about south-west, and the bow

was north-east; it was merely a series of well-defined but colourless

segments of circles, close to each other but shaded so as to make them

distinguishable, arranged exactly like a rainbow but without a trace

of colour beyond a grey uniformity. It was on my left for several

miles, perhaps half of the total distance of nine miles between the

two towns.

Cycling another day between Lyndhurst and Burley, I reached the east

entrance of Burley Lodge, which is on higher ground than the farm

spread out to the right in the valley. The whole valley was filled

with thick white mist, as level as a lake, so that nothing could be

seen of the fields. The setting sun was low down at the further

extremity of the valley, and the surface of the mist-lake reflected

its rays in a rosy sheen, with a track of brighter light in the

middle, stretching from the far end of the lake in a broad path almost

to where I was standing; just as we see the track of sunlight or

moonlight, sometimes, on the sea, from the shore. This phenomenon is

not uncommon when one is looking down from the top of a hill in the

sunshine, upon a valley full of mist, but I have never seen it before

from comparatively low ground, as on this occasion.

My summers at Aldington were nearly always too busy to allow me to

take a holiday, except for a very few days, but when the urgent work

of the year was over, the harvest completed, and the hops and the

fruit picked, we always had a clear month away from home, about the

middle of October to the middle of November; and, as we found the

autumn much less advanced in the south than in the midlands, we often

spent the time on the south coast or in the Isle of Wight, and we were

nearly always favoured by fine weather. On one of these occasions,

when we were exploring the whole island on bicycles, I never once

found it necessary to carry a waterproof cape, though in the course of

this visit we rode over 600 miles.

[Illustration: NOTE. THE CHANGING COURSE OF STREAMS.]

Grain and Chaff from an English Manor · 第 20 / 25 章