CHAPTER VIII

GEYSIR

“Where the cauldron of the North

Spouts his boiling waters forth,

From the caverns far beneath,

Where they ever lie and seethe,

And with steam, and hiss, and boom,

Send a tremor through the gloom,

Till, above, the solid ground

Vibrates with a dull rebound,—

In that place I stood and saw

Things that filled my soul with awe.”

—_Miss Menzies._

Morning dawned with a gentle rain. Hour after hour it fell with no

promise of abatement until ten, when the clouds were rifted, the sun

shone through and the dripping plain glistened. We decided to set out for

the long ride to _Geysir_. The ponies had been in readiness for an hour

in anticipation of an earlier start.

We turned into the trail leading across the plain, along the border of

the lake towards _Hrafnagjá_, Johannes following with the train at some

distance. When we reached the rift we halted to examine it until Johannes

arrived. This chasm is longer than the _Almannagjá_ but not so deep

and surely not so impressive. It lacks the beautiful waterfall and the

historical associations of the latter. It extends along the side of the

mountain which we were about to climb. Many blocks of basalt have tumbled

into it in one place and over these a suitable and safe passage has been

constructed. As we crossed the chasm the rain began to fall, likewise the

temperature. Long before we had reached the summit of the mountain pass

the rain was pouring upon us and rolling off in rivulets from horse and

rider. This was a good test of our specially made waterproof clothing

and it stood the test. Never a drop penetrated save up the sleeve of the

bridle hand.

At the summit, the clouds scattered again; this time in earnest and we

experienced no more rain during the long trip. It was just one long and

glorious summer day and we wandered care-free in full enjoyment of the

wonderful country. Near the summit we passed a lonely little farmhouse

and the people being absent in the hayfield the lonesome dog came out to

make our acquaintance.

At this place the trail winds through an exceedingly rough area of

lava, tangled and twisted. It was my first experience with recent

volcanic products and it was with absorbing interest that I examined

this material, as the ponies climbed the steep gradient and threaded the

narrow path through the labyrinth of angular blocks. Above our heads

rose a line of peaked and jagged volcanoes, _Kálfstindar_, Calf-Peaks.

This place has been the center of considerable volcanic activity as

evidenced by the different forms of lava, i. e. lava of different periods

of eruption also by the weathering piles of tufa and conglomerate. Near

the trail there is a peculiar formation, a _tintron_. This is a volcanic

chimney, rising about nine feet out of the lava plain. The opening at the

top is in the form of an ellipse and the tube extends forty feet down

into the solid lava. The sides are blistered and it has the appearance

of having been a blow-hole from which thin lava was thrown upward in the

form of a fountain as water from the nozzle of a hose. There are several

of these unique formations in the north which will be discussed when we

reach _Mývatn_.

Soon after leaving the _tintron_, the trail wound downward along

the side of the mountain and under projecting cliffs of tufa and

brought us suddenly in view of the fair valley of _Laugardalr_,

Valley-of-the-Hot-Springs. An entrancing panorama was spread out at our

feet. The luxuriant green of the valley contrasted strangely with the

scorched and blistered barriers over which we had been climbing. In the

distance a smiling lake of no mean proportions cut a large space out

of the meadows. On the nearer and the farther shore of _Laugarvatn_,

Hot-Spring-Lake, rose columns of steam in slender spirals quivering in

the breeze and vanishing in the upper air. Numerous sheep and cattle

marked the valley with dots of white and brown. Besides the nearer hot

springs clustered a group of farm buildings and the distance caused their

turf roofs to appear like tiny hillocks. This lake and valley appear like

a monstrous chrysoprase in a grand setting. The valley is enclosed by the

needle spires of the volcanoes which are red, brown, yellow and gray and

streaked with a mixture of all these colors on their naked slopes where

the melting snows have swept down many an avalanche of ash and cinder.

We descended by a steep path to the lower level, passing many a towering

pile of conglomerate of soft texture and wading through many a talus of

ash and sand where the myriads of zeolites glistened. The masses of rock

protruding from the tufa cliffs give them the appearance of huge plum

puddings. Reaching the verdant plain we changed ponies and while waiting

for them to graze, we explored a small cavern in the base of the cinder

pile. This cave has long been used as a retreat for the sheep in times

of storm. It has since been cleaned, a turf dwelling erected before its

entrance and it now forms the home of a young Icelandic couple who have

set up their housekeeping here since our visit. Remounting we sped away

over the meadow, crossing many small brooks and arrived at the farm

by the hot springs. This place has many signs of prosperity, such as

the quality of the buildings, the numerous flocks around the lake, the

abundance of hay and the thrifty patch of potatoes in its special turfed

enclosure. We were cordially welcomed, taken to the guest room and served

with hot coffee, milk, pastry and delicious griddle cakes, large in

area and quite thin, buttered while hot, sprinkled with sugar and then

rolled tightly. We found these griddle cakes at many of the farms and

can cordially recommend them to a dainty appetite. At the close of the

lunch we repaired to the hot springs which always had for us an unfailing

interest. They are at the very edge of the lake and have formed small

mounds of silicious scinter mingled with lime and alum. Wherever the hot

water has fallen upon the land there is an incrustation of fantastic

form. Most of the water boils over into the cold water of the lake. The

spring furnishes hot water for all domestic purposes and is a great

conserver of fuel. The clothes are washed in tubs beside the springs and

then rinsed in the lake. Here the wool is cleansed before shipment. In

the hot ground the bread is baked, the dough being enclosed in earthen

jars. In a fuelless country it is a gift. It is a strange contrast this

pouring out of boiling water in the margin of the cold lake.

We hastened across the meadow along the border of the lake to regain

the trail leading to _Geysir_. Hasten is the correct word. No air was

stirring and the clouds of tiny _mý_, midges, that rose out of the long

grass as the ponies disturbed them, simply smothered us. They filled the

ears of the ponies, crowding in with the long hair and swarmed in patches

upon their flanks and legs. Instances are related where the midges so

tormented the ponies that they rushed into the water, in spite of the

protestations of the riders, that they might get rid of their tormenters.

No horse of my knowledge has his ears so completely filled with hair

as the Icelandic pony. Doubtless this is an adaptation for a special

purpose and I believe that purpose was to protect these delicate organs

from these stinging insects. We drew forth our fly veils and put them on

with some relief, but as we did it while at a full gallop they were not

securely fastened and some of the pests got under the netting. Here they

were happy, for we could not drive them away. In desperation I pulled

off my veil, for the express purpose of giving all the midges an equal

chance. It needed no urging to put the ponies to their best paces, for

they well understood that the insects would leave us when we had attained

an elevation above the meadow.

We entered a tract of scrubby willow and dwarf birch. Some of the birches

were as high as our shoulders while we were on horseback and thus we rode

with our heads protruding above the Icelandic forest and there was some

free advice given about getting lost in the woods. There are two or three

larger forests in the north which we shall visit later. We passed several

good farms and every one, men, women and children were busy with the hay

harvest. Two hours riding took us to _Miðdalr_, Middale, church, which is

close to the famous _Brúará_, Bridge-River. Many streams rush out of the

mountain gullies and unite up this side valley. Here the _Brúará_ comes

foaming down its shelving bed in a passion. Near the crossing it spreads

out in a wide sheet over the lava which is full of ugly crevasses. One

great rift, of unknown depth, and five feet wide extends through the

center of this lava and the river tumbles into it from both sides.

Tumbling into lava rifts is a characteristic of Icelandic rivers, some of

them entirely disappear. Until the coming of King Frederick in 1907 the

traveller rode his pony through the water for about one hundred feet,

carefully avoiding the cracks, with the water well up the flanks of the

pony. When the rift was reached it was crossed on planks bolted to the

rock and often with the water flowing over them. When safely across the

“bridge” another passage of one hundred feet through the water brought

the traveller once more upon dry ground. This is why it is called “bridge

river.” A suspension bridge now spans the stream and the view up the

river is excellent. In former days it required some steadiness of purpose

to thread this tangled maze of cracks beneath the white water and ride

the plank over the foaming stream, and yet, I am sure, I would prefer it

to the crossing of the _Ölfusà_ which we made two weeks later.

Here we encountered a large party of Icelanders with numerous pack ponies

laden with provisions, timber, and strangest of all, huge piles of fish

heads with attached vertebrae. The party had been down to the coast to

dispose of their wool and were returning with their supplies for the

summer. When the fish are dressed the heads and backbones are cut out and

hung upon the fences to dry. In the interior they are pulverized and used

for food whenever provisions are short. In the spring when hay becomes

scarce fish are often fed to the livestock.

Passing the farm, _Utlið_, the _out-folk_ or the people beyond, we wound

around the shingly side of _Bjarnafell_, Bear-Mountain,[2] and descended

to the plain which proved to be a bog saturated with the recent rain.

Lord Dufferin in his _Letters from High Latitudes_ calls this place

“an Irish bog.” The crossing was anything but pleasant for the ponies.

Many deeply worn trails crossed the plain towards _Geysir_. Under

ordinary conditions of dryness any one of these ditches would have been

satisfactory to the ponies, but partly filled with mud the ponies shied

at them and without any warning frequently jumped out of one and into

another before the rider was aware of what was about to happen. It is in

places of this character that the instinct and experience of the pony is

more serviceable than the judgment of his rider. It is in the bog, on

the rough mountain trail and in the foaming river that the true worth

and peculiar qualities of the Icelandic pony is revealed. The ponies

prefer the old ruts which often are worn so deeply that his flanks rub

the turfed edges and the rider must pay special attention to his own

feet if he would not have them jammed into the turf at the angles of the

intersecting trails. Attempt to get the pony out of the rut and on to

what the rider assumes is a better path, the turf, and the mettle of the

steed is immediately aroused. It requires a strong pull upon the rein and

a dig of the heel into the ribs of the pony to get him out of the path he

has chosen. As soon as this is accomplished to the satisfaction of the

rider and he settles down in the saddle conscious of his superior wisdom

over the brute creation, without the least warning the pony takes a side

step which lands him in the bottom of the forbidden trail. After a few

of these unexpected rebuffs the rider is content to let the pony have

the choice of trails providing it leads in the general direction of the

rider’s choice.

In the distance we saw columns of steam rising from a large area and

Johannes assured us that it was from the geysers. It was here that we

met an acquaintance from the _Laura_, Mr. A. V. Manneling, a banker

from Helsingfors in Finland, whose company had been very agreeable on

the voyage from Leith to _Reykjavik_. He informed us that _Geysir_,

(pronounced gáy-sir,) had erupted that noon and would probably give

another exhibition that evening. We bade him good-bye and hastened on in

order to be present during the eruption. A century ago _Geysir_ was quite

constant in the periods of its eruption but owing to recent earthquakes

which have changed the conditions below it is not at all regular and

it is frequently eight days between the displays. We forded several

tributaries of the _Túngufljót_,[3] Tongue-River, rounded the base of

_Laugarfell_, Hot-Mountain, and rode into the midst of the steaming

acres, the site of great _Geysir_ and his satellites, a place of awful

magnificence, where the water,—

“… hot, through scorching cliffs is seen to rise

With exhalations steaming to the skies!”

—_Iliad._

We dismounted at the little inn, which is located in the midst of the

boiling and spouting caldrons, glad to leave the saddle after a ride of

thirty-five miles across a diversified country. It had been our second

day in the saddle but we had become accustomed to the ponies and they had

discovered that the riders were their masters. We had had an exceedingly

pleasant journey with no discomforts except those attendant upon

horseback riding through a rough and roadless country.

This little inn was another creation for the benefit of the King and

again we rejoiced that his visit to Iceland preceded ours. There are

four rooms on the ground floor, one for dining and the other three for

bedrooms. The cooking is done in a little house slightly removed towards

the mountain. Formerly all travellers to _Geysir_ took tents with them

for use at this place or hired them of the farmer at _Haukadalr_,

Hawk-dale. The Inn was crowded. There was a large company of Icelanders

out for a holiday besides several Danes, Germans and those lovers of the

_Laura_, the Swede and the Icelandic maiden. We encountered them several

times during the summer and they were having a happy time. It appeared to

be a honeymoon preceding the bridal. There was a prolonged conversation

between Johannes and the keeper of the Inn in which Johannes expressed

himself quite forcibly if we could judge by the determination in his

voice. He appeared to be the victor, for he came to us with a beaming

face and showed us into one of the corner rooms next to _Geysir_. Our

luggage was brought in, a steaming supper of boiled mutton, potatoes,

milk, coffee and black bread was set before us. That Icelandic coffee!

The berries are freshly roasted every morning, they are of prime

quality, the brewing is expertly done, the cream is real and,—well, it

is delicious. Throughout the country it is the same. Halt at a farmhouse

at any time in the day and you are invited to _Coffee_. It is coffee

with every meal and frequent potations between meals. In that land the

coffee ghost has never risen to be cried down with a score of cereal

concoctions. Prepare it here freshly and expertly as they do and there is

no reason why conscience should peer over the brim of the steaming cup to

bid us beware of the snare of its fragrance.

We were hungry but our curiosity concerning the locality made short work

of the supper. We then learned that the discussion in which Johannes

became so energetic was precipitated by his stipulation that no one was

to use the room except ourselves. In it there were three single beds,

bunks built against the wall, and provisions for several more in the

middle of the room when occasion required them. We did not know the

Icelandic custom, that several men, women and children, whether known to

each other or not, sleep in the same room without any inconvenience.

The inn-keeper did not understand why this custom should be broken to

the inconvenience of the many people who desired shelter that night. We

learned more of this custom as our experiences multiplied and we will

give the reader a full account in a later chapter.

This place is marked on the map of Iceland as _Geysir_. The word is from

the verb _geysa_, “to rush forth furiously, to burst out with violence.”

It is not applied to all the spouting springs of boiling water as is

_geyser_, the geological term, but is the name of the king of all the

spouting springs in Iceland. Scores of these springs are located in this

place but each has a special name which is appropriate to some physical

peculiarity, such as _Strokr_, the churn, the tube where the water rises,

falls and boils vigorously as the cream rose and fell with a frothy

splutter in the ancient dash churn. When we think of the geysers of

New Zealand, the Yellowstone National Park or any place in Iceland we

must remember that they took this name from _Geysir_. There is only one

_Geysir_.

The area dominated by the springs is directly at the foot of

_Laugarfell_, indeed the south side of this mountain once formed a

portion of the hot section. This portion of the mountain is void of every

trace of vegetation, it is marked by ruined geyser mounds, smeared with

sticky clay of many colors, punctured with tiny fumaroles whence issue

wavering wands of steam, while in many places rivulets of hot water break

through the pasty crust. The area of real activity is about 3,000 feet

by 1,800 feet. The place is strewn with fragments of geyserite and bits

of wood, straw and metal, thinly encrusted with the mineral deposit from

the springs. Cast a stick, a straw or a bit of paper where the spray will

fall on it and in a day it will have become petrified and cemented to

the rock beneath. The entire substratum is intensely heated, the ground

is in a constant tremor which often accelerates to a gentle quake. Far

down below these hissing, silicious tubes there is unknown latent heat.

For ages the thermal capacity of this place has been sufficient to eject

untold millions of tons of superheated water, at frequent intervals, in

large installments from these stupendous safety valves.

We roamed over the section several times with our attention always fixed

on _Geysir_ and ready at the slightest warning to dash madly towards it

should it condescend to favor us with a manifestation of its power. In

the meantime we plugged the tube of a little geyser with turf and then

stood aside to listen to the heavy gurgle of reproach which rattled in

its throat and to witness the vomiting of boiling water to a height of

twenty-five feet. As soon as it got relief we plugged it up again and

as often as we administered the turf so often did it eject it. It was

midnight and Mrs. Russell had long since retired, but the weirdness of

the place held sleep aloof from my eyes. In company with a German I

wandered over the area again, stood on the rim of _Geysir_ to watch our

shadows in its depths hoping for the occasion to arise for us to chase

those shadows headlong up the mountain slope. We returned to the little

spouter and played like a couple of boys. As a parting shot we decided

to give it an extra amount of turf and to ram it down the barrel with

a pole. We did this with so much success that we waited long for the

discharge but there was none. We had loaded it too well. The tube of

our gun was too strong to burst, the wadding was packed too tightly for

the powder to blow it out. Silently we sat by it for an hour when my

companion said,—

“Geyser schlaft.”

To which I replied,—“Ich will schlafen.”

The day after the following it burst out with a fine jet of water at six

in the morning and spouted without interruption till nine when we rode

away. As we passed over the ridge we looked back and the last sight we

had of this place was the top of a column of water pouring from this

tube. The extra charge of turf was well worth the trouble.

Morning came but _Geysir_ had not erupted. Its surface betrayed no

signs of past disturbances and gave no promise for the future. From the

neighboring farms we collected seventy pounds of bar soap which we cast

into the center of the basin, where it immediately sank. We were told

that during the day there would certainly be an eruption. The soap is

kept here expressly for sale for this work. Ask an Icelander what the

agency of the soap is and he will reply,—

“I do not know, it always does it and does it thoroughly.” I venture the

following explanation. Recalling that the accepted idea of the interior

of a geyser is that of a large chamber of heated rock nearly filled with

water and that below the water line there is a tube which bends down

then upward into a chamber in the rock. The water becomes superheated.

The steam and other gases in the dome of the chamber are under terrific

pressure on account of the great heat and the weight of the column of

water above, (if one thinks of the geyser tube connecting the underground

basin with the surface as the letter J). When the pressure in the dome

over the water becomes greater than the downward force of the water in

the long arm of the tube then there is an upward movement through the

tube. The expanding steam throws out some of the water. This reduces the

pressure on the superheated water in the basin and some of the water

bursts into steam to continue the action. This process goes on till

basin, tube, underground chamber and connecting tubes are empty. Distant

and cooler underground waters now rush in freely to refill the system

and time produces a repetition. It is easy to construct glass apparatus

in the laboratory to demonstrate this phenomenon. But what of the soap?

This substance is composed of materials which quickly break down into

hydrocarbon gases and increase the pressure in the chamber, just like oil

spurted into the superheater of a water gas machine.

Many of the boiling springs, spurting jets and fumaroles are alike in

this locality but three of them deserve special notice.

_Blesi_, Blaze, as the white stripe in a horse’s face, is a charming

grotto. It is a double basin connected with a tunnel just beneath a

narrow bridge near the surface. These basins are about thirty feet deep.

One is eighteen by twelve and the other thirty by twenty feet in the

longest and shortest diameters respectively. The water is wonderfully

transparent and the white silicious lining of the grottoes reflects from

the sky the delicate shade of blue transforming it into a huge cavity of

lapis lazuli. _Blesi_ is the traveler’s friend. It provides hot water for

the bath, cooks his food, warms his couch through the medium of the hot

water bag and prepares his coffee. Many a leg of mutton, many a brace of

birds and innumerable are the eggs that have been faithfully prepared

with its friendly heat. It is an easy method of cooking. Fill a pail

with eggs and submerge it till they are soft, medium or hard, the time

required is the same as in the kitchen. Place the meat in a cloth bag

and do the same. Dip up the water and pour it upon the freshly ground

berries, lo! the coffee is prepared and your meal is ready. This spring

never erupts but pours out a steady stream which flows down the slope to

join the runway from _Geysir_.

_Strokr_ is another hot spring with a tube ten feet in diameter and

over forty feet deep. In former days it was most accommodating and

would always give an exhibition of its powers if a couple of bushels of

turf were thrown into the tube. The response came in from five to forty

minutes. It usually threw out the turf and ejected a column of water

upwards of a hundred feet. Again and again would it hurl out the boiling

water until its underground system was exhausted. Some years since a

party of gentlemen, French I believe, desirous of obtaining an extra high

spout threw many stones into the tube on top of the turf. The geyser

siphon was doubtless broken or at least fractured so that superheated

steam can not be stored, for _Strokr_ spouts no more. It boils furiously

all the time with dense clouds of steam and the water rises and falls

in the tube in the most violent manner. In looking into the tube one

is impressed with the idea that there are safer places, as it seems if

_Strokr_ were about to mount into the sky to challenge _Geysir_ which has

so long held the palm.

_Geysir_ is the main attraction. The first mention of this phenomenon

in literature is in the History of Norway written by _Saxo Gramaticus_,

who lived between 1150 and 1206, so that it has been active for over

seven centuries. It has built for itself a mound of geyserite many feet

above the level of the plain and has the appearance of an inverted

oyster shell in its series of terraces. This mound increases with each

eruption by the addition of a film of salts held in solution in the

boiling water. The spring is in the form of a saucer with the inward

sloping side at an angle of thirty degrees. The diameter of this saucer

is nearly seventy feet and the saucer is a true circle. Within a saucer

there is a depression at the bottom, a ring to hold the cup. Within the

center of _Geysir’s_ saucer there is an opening, ten feet in diameter,

which extends straight down to the depth of eighty-four feet. Beyond

this the plumb will not go. Whether there are deeper ramifications of

tubes or not is a matter of conjecture unless the explanation of geyser

action above offered is correct. Again, the shape of _Geysir_ is that of

a funnel, i. e. a tube running downward from a flaring reservoir at the

top. During the irregular periods between the eruptions, the water wells

upwards in the center and overflows the rim of the basin through a foot

square opening in the side. This opening has been shaped by the farmer of

_Haukadalr_ to confine the escaping hot water to one channel. The water

is heavily charged with minerals in solution. An English analysis of a

gallon of the water yielded the following:—

Sodium carbonate, 5.56 grains

Aluminum oxid, 2.80 ”

Silica, 31.38 ”

Sodium chlorid, 14.42 ”

Sodium sulfate, 8.57 ”

-----

Total solids, 62.73 ”

During eruptions large volumes of carbon dioxid and some hydrogen sulfid

and a little free hydrogen are emitted. In 1909 my maximum recording

thermometer was lowered to a depth of eighty feet and the temperature was

110C., or 230 degrees on the Fahrenheit scale.

Words convey but a meager idea of the magnificence of this geyser

during eruption, or the awe with which it inspires the witness of its

extraordinary display of power. It was six-thirty in the evening, eight

hours after we had administered the emetic of soap. Not a cloud dimmed

the blueness of the sky and no air was stirring. The glaciers of _Láng

Jökull_, the long ice-covered mountain, loomed beyond the plain of the

_Hvitá_, White-River, the dome of _Hekla_, Hooded, had momentarily lost

its cloud mantle, all the little geysers and fumaroles were boiling

merrily and steaming furiously. Even quiet _Blesi_ was sending up showers

of carbon dioxid bubbles. The signs were favorable for an exhibition

and the people were gathered close about the Inn in expectation. What

the condition of the air has to do with the eruption, I do not suggest.

Icelanders familiar with _Geysir_ state that “when the wind is from the

north there is never an eruption.” I can only add that during our first

eighteen hours at this place we had a strong wind from the north and no

eruption.

We were at supper. The ground trembled, the building vibrated and a dull

rumbling reached the ears.

“_Geysir! Geysir!_” rose the cry from within and without the building.

The supper was never finished. Johannes, who had been watching for

these first signs ever since we had administered the emetic, met us as

we sprang to the doorway. Everyone rushed to the elevation across from

_Geysir’s_ runway. Again the rumble, heavier than before. The water is

agitated in the basin, it boils up suddenly, subsides, the earth beneath

our feet trembles and a mass of steaming water rises in the center of

the basin to an elevation of fifteen feet and overflows the rim with a

noisy splash. Then all is quiet. Is this what we had travelled forty

miles out of our way to see? Truly a great fuss for nothing. Is this the

wonderful _Geysir_ whose manifestation of power had caused the devout

Henderson to fall upon his knees and to pour out his “soul in solemn

adoration of the Almighty Author of nature, ‘who looketh on the earth,

and it trembled; who toucheth the hills, and they smoke?’” Does _Geysir_

demand more tribute in soap? A few moments of quiet expectation followed.

Then, without further warning, a column of superheated water, ten feet

in diameter, shot like a rocket into the air to the height of one hundred

and twenty-five feet and the abysmal forces maintained that column for

nine minutes. What a flood of water poured down the sloping cone! What

a fountain! Mark Twain said that they “have real fountains in Europe

but in America they only leak.” What would he have said could he have

witnessed this display? The roar of falling water filled the air to the

exclusion of all voices and flowed in hissing cascades down the slope,

into the ravine and across the meadow to the river. The sheep fled before

the advancing column of steam and from a distance gazed with a foolish

stare at a spectacle that they had often witnessed. Volume upon volume

of steam, like the cauliflower-shaped clouds of active Vesuvius, belched

into the air expanding under the reduced pressure and filled the air

to the shutting out of the sun. Fountains of foam well over the brink.

Explosion follows explosion and still that lofty tower of boiling water

stands erect and masses of water fall to earth with a terrific crash. The

column wavers, totters, falls. The eruption is over, the steam clouds

lift and we rush up the dripping slope of geyserite, step over the rim

into the hot basin and peer down into these depths whence came those

rivers of water. The heat penetrates the thick soles of the riding boots

but we walk to the edge of the tube and gaze down into the sizzling

throat of the monster. A mass of foam is over the bottom, eighty feet

below. It rises, we watch its ascent of the tube with the pace of a fly

up a wall. It reaches the junction of the tube with the bottom of the

basin and we photograph it, just a mass of foam with ascending steam.

It wells over into the basin and we retreat. Soon the basin is full and

overflows normally and the only evidence of the change that has taken

place is the dripping cone and the steam rising from the brook as it

rushes to cool itself in the icy river.

[Illustration: _Bridge River, Brúará, near Geysir._

_The Tube of Geysir Filling, Photographed from within the rim of the

Basin._]

During the eruption I caught a glimpse of a dark object in the steam

which fell with a thud upon the grass. After the display and the basin

had filled I sought that spot and found a mass of geyserite twelve inches

square and two inches thick. It was still hot. It is perforated with

steam tubes in every direction. I stowed it in the packing case and it is

now in the Science Museum at Springfield, Mass.

At nine thirty that evening we were again treated to the same phenomenon

by _Geysir_ and again at six the following morning. Three magnificent

ejections at a cost of only ten dollars worth of soap. It was worth

much more. The final display was the finest of the three and lasted ten

minutes. We were dressing when the cry of “_Geysir!_” again reached the

Inn. What did it matter that the toilet was not finished! Travellers from

Denmark, Sweden, Norway, America, Germany and distant parts of Iceland

were there to see _Geysir_ spout and not to be fastidious about coiffure

and raiment. We all assembled hastily at the brink, each unconscious of

the others’ presence until the display was over. Then! What a startled

and confused company! Several were clad only in sleeping costumes, some

had put on one stocking and were holding a shoe and a stocking in the

hand, some dragged a skirt by the band and still others trailed their

pantaloons by the suspenders. One man held his shirt by the sleeve and

had one leg in his trousers while the other was innocent of all clothing.

There were Icelandic matrons and maidens barefooted, some with a skirt

wrapped around them and others with a sheet. Rows of discarded garments

marked the way from the Inn to the mound and during the retreat, which

was a blushing and precipitous one, each caught from the grass the

clothes that had fallen during the advance. Ludicrous describes it well,

but every one was happy and during the breakfast which followed the

confusion was forgotten.

Standing upon the rim of the great basin and gazing at the azure surface

the peacefulness of the scene belies the turbulence of the hour before.

In the distance _Láng Jökull_ glistens in the brilliant sunshine. Yonder,

across the _Hvitá_, cloud-capped and snowy-mantled _Hekla_ rises grand

and lonely above its lava-wasted plain. Around us the numerous springs

and fumaroles emit their endless columns of vapor and _Strokr_ moans and

groans. The little geyser which we packed with turf two nights ago has

been spouting without interruption for two hours. What a contrast! Arctic

ice and Plutonic fire battling for supremacy as they have done for ages

in this land of strange confusion,—and still the conflict wages. Loth

are we to turn from this manifestation of power and imposing grandeur

of _Geysir_, even in his hours of rest, but _Gullfoss_ lies beyond the

_Túngufljót_, the _Thjorsá_ and the _Ölfusá_ must be forded, _Hekla_

challenges from the midst of his desolation, the peaceful pastoral

plains of the south are calling, the weird and frightful solfataras of

_Krisuvik_ entice,—and we must saddle and away.

Iceland: Horseback tours in saga land · 第 8 / 16 章